The process of capturing Carbon Dioxide (CO2) from a source that is Stationary ( Power Station may be) , to transport the processed product ( Using a Pipeline may be) and finally to inject it a suitable place ( a Geological formation) is known as Geo Sequestration of CO2. The project under taken mainly focuses on the various process and each stage expanantion of understanding how the CO2 can be captured from any source. All kinds of issues and problems that may incur and hinder the process at any stage in developing this product. CO2 once obtained needs to be stored and transported to the subject site where it can be injected for long time. While undertaking all this process there are many risks and issues that may occur in completing this process. All the risks regarding this are identified and are managed in all possible ways using Risk Management procedures. All the project management techniques are identified and discussed in details using all various tools and mechanisms. One of the most suitable ways and technique of project management is to use and follow PMBOK technique. Using the project management technique to the complete sequestration process and consolidating it as a complete project is discussed in detail and managed as a complete project. All the cost and risks involved in this complete procedure are discussed and taken into account in order to evolve it as a whole some project. All the various project management techniques and ways are considered and applied to the project. The Green House impact is discussed in detail with all its possible processes. All the various types of gases emitted are discussed with all possible ways to control and reduce it. The Green House gases are extremely injurious to health and may have various dangerous effects oh lungs, skins and physically as well. CO2 as a complete project is a laborious task and involves tedious mechanisms which needs to be undertaken with great care and consideration. and applied and CO2 sequestration geologically and projects related to it most of the times have several multiple criteria’s and issues to finish it successfully for all the stake holders.
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Geo Sequestration involves the capture of Carbon Di oxide ( CO2) using any source that is stationary such as any power station source and further transportation using any means such as a pipeline so that it can be injected into a suitable site such as a geological formation. There are several other terms that may be used for sequestration such as Carbon Capture Storage (CSS) or Carbon or Carbon Di oxide Capture and Geological Storage (CCGS) and Carbon Capture and its Geological Sequestration ad Geological Disposal. However, we can conclude that there is no universal word or nomenclature that we can used for Sequestration. The term “Storage” is usually preferred in European Nomenclature. Whereas the storage has the connotation with CO2 that can retrived at some stage , how ever as a matter of fact there is unlikely or technically oreconomically not possible and technically not feasible in almost all the circumstances to retrieve it . The term Storage hwoever doest not encompass the storage from ocean in which the CO2 is stored in deep inside water column of any ocean ) as the geological storage. The term Geological Sequestration is getting increasingly popular in USA . However , the used term of Geo Sequestration has been taken to incorpaorate the CO2 Capture , Transport and Geologically storing it .
Figure below shows the complete process
There are several reasons because of which the Ocean Storage can not be considered for the Ocean storage. At times it becomes out of scope for many reasons . Furthermore the used technology is immateur and porbably it is not at a positon where it is ready for application. In addition to it there are serious and obvious reasons in which the oceans storage remains an enviornmnetly feasible mitigation option , which may lead to ultimate acidification of the subject oceab with clear negative imact on Marine Fauna . Howere the deep geological CO2 storage may be under taken deep under the ocean sea floor , that doesn’t mean that it is ocean storage , since the injected CO2 is not expected to enter even the ocean , it always locks away under the floor of ocean.
However it is imporatnat to note that since there are various geological storage sites which are known to occur offshore , which occur under the shelf of continential shelf which may include the Austrlian Continential Shelf.
Moving on further , the chemical reaction of CO2 with purely finely grounded mineral of rocks such as alumina silicates indicates an advanced storage known as mineral storage. Hving many similarities with Geo Sequestration, it may be under taken as a full surface chemical process. While being examined on various occasions , it is not seen and considered as a viable economic option . Mineral Storage how ever is not considered here at all.
Over a last decade there has been a constant concern regarding the increased atmospheric amound and content of Carbon Di oxide (CO2) and other gases emitted because of Green House effect. All these gases have a very serious impact on climate of earth and is growing siginicanlty over the period of time .
There many coutries of the world including United states that are fightin to bring in a balance between economic development and meeting a near ending term goals where as to minimize the long term risks realted to environment. In process of finding a solution to these grave problems specially the build up of Green House Gases in the Atmosphere, a study conducted and pursued by the United States Department of Energy (DOE) the National Energy Technology Labortarty with its partners realted to academics , the sequestration of Carbon Dioxide has been a prime solution to almost all problems related to Green House impact. In this process a permanenet storage of CO2 emissions in geological underground formation has been eveloved which ultimately avoids CO2 to relase in atmosphere and reacting with different gases to produce various harmful by products.
In order to cater for the emssions of Green House Gases particularly fossil fuels fired power plants , the Carbon dioxide sequestration always proves to be one of the most feasible and suitable option. In this process the mechanism is evolved in order to captute the subjected Carbon Dioxide , transport it to the sequestrated site and to inject it ulatilamtely to the geological formation. Whereas , the process of CO2 sequestrations in geoloigical formations can never be achived siignificanlty in reducing the Green House Gases emssions till the time it not acceptable to the concerned regulators , the stake holders and the general public that involves that the risks involved are judged to the acceptable limit .
In order to achieve this , there is one tool that can be used to get the acceptance to geological sequestration of CO2 , that is known as Risk Assessment of complete process. Risk assessment has proved itself to managze the hazards objectively the hazardious effects of facilities such as the oil nad natural gas fields , the refinineres, the used pipelines and different chemical plants in use. In order to cater for the CO2 Sequestration the Probabilistic Risk Assessment (PRA) which has been applied in many other areas has proved itself infancy for this sequestration . .
The Geo Sequestraion of Carbon Dioxide always remains a tedious and complex task. The whole procedure involves a complete chain of events. Starting from the capture of carbon dioxide , its storage , transporting it to the subject poses various problems at different stages. The final stage of injecting it to the suitable formation is the most critical step and always involves a thorough site considerations, suitbale temperature conditions and a complex mechanism overall. The burning of Coal , gas and Oil under standard and suitbale circumstances produces the Carbon Dioxide Gas. Acording to most of the scientists the most largest contributor to Green House effect is Carbon Dioxide which always traps heat that is coming from the Sun in the atmosphere of earth. This causes change in climate. Other gases such as methane , nitro, choloforcarbons (CFCs),Hexaflorocarbons and and the Sulphur Hexa fluroise also adds in to the problem .
The report regarding Geo Sequestartion of Carbon Dioxide will be oraginzed in way that will involve a complete descrtioiopn of this Sequestration Process. The Green House Effect and its impact in atmosphere will be discussed. The greenhouse gases emitted with its various hazards will be considered in detail. The relation between Geo Sequestration and its use to cater for and to reduce the Green House Gases will be discussed in detail. The whole process is taken as a complete project and after disuccing in depth all techniques of project management , the PMBOK procdure will be used to manage the complete project. There are various risks involved in managing this project , the complete Risk Management procedure will be used to manage the things in a suitable manner.
In the terrestrial sequestration using the perennial vegetation is the most vital element. It role in the ecosystem dynamics is very known to all. Due to the industrial and technological advancement that has been achieved by the human society with time, the paradoxical related to vegetation has undergone the degradation and destruction in the modern times. Due to this advancement there has been observed a signincant emission in Carbon Dioxide as a whole. Therefore, it is an hour of need to deal with this environmental menace that is a constant source of hazard and danger of environment. Carbon Dioxide are produced mostly by the trees since 50 % of their overall standing mass is carbon itself. The importance of carbon sequestration in forested area is well accepted and documented. Similar to forsted tress, the needle leaf vegetation and green fruit trees also have same sequestration of CO2. The most alarming part is that there is no attempt that is made to study and to classify the area that is based to see the quantity of CO2 that is sequested. Study has been carried out to predict Carbon Sequestration using the cashew and casurina planaation of Tamil Nadu that is used to remote sense and use ecosystem modeling.
According to one of the estimate , the standing biomass in India was equal to 8376meter in the year 1985, and the storage is expected tobe 4280meter. The carbon that is stored in the forests that includes soil as well , estiamtes to about 9570 meters. Whereas, the emissons of carbon from the fossil fuels based on energy production and its realted consumption ativaties in india amounts to about 150- 230 meter annualy. The estimates given by different scientists and ecologists vary quite differently from each and other. Agricultural activites aht includes burininf of fuel ranges from 40 to 120meters . The presenet rate of reforestration is being balanced by the current emission of carbon by the agricultural industry and forestry sectors . As a result of it , the entire fossil fuel industry remains unabated. Accroding to one of the estimates , in various areas in area , the experiments regarding sequestration of carbon prved to be successful and were proved to be successful in the tears to come . These experiments paved a new way towards development and much greater progress.
The Earths climate is powered by Sun in which the radiaitons from sun are emitted at very short wavelengths. The spectrum that is produced remains visible or nearly visible that is Ultravoilet rays being the part of Spectrum . According to one of the studies being carried out , nearly one third of the solar energy in the form of rays that reaches the earths atmosphere top, is reflected back to space. Where as the remaining teo third portion remains absorbed by the surface and uppto a lesser extent is absorbed by the atmosphere. In order to balance out this phenomonemon as a whole, as a general principle, the Earth in turn must also radaiate the same amount of energy back into the space. Since the Earth in comparison is much more colder than the sun , it radiates much more longer wavelengths , that are in particular in infra red spectrum . The radiations emitte by the Land and ocean are the thermal radiations that may also include clouds and they are therefore reradiated backwards towards the Earth. The process involved as a whole is known as Green House Effect. In the Green House , the glass wall helps to reduce the airflow and ultimaltey increases the temperature of the whole air inside. The average temperature at the surface of earth remains below the freezing point of water , without the natural greenhouse effect .
The possibility iif life on the planet earth is possible because of Earths Natural Green house effect . However, the activites of human beings on earth because an ever gowing increase in industrial revolution and the burning of the fossil fuels that involves almost every step , have immensely increased and intensfifed the naturally occurring green house effets and is contricuting signicantly towards the most commonly known phenonmen of Global Warming. As far as atmosphere is concerned , the most abudndunt gases that are present in atmosphere are Nitrogen (making 78 % of dry atmosphere ) and oxygen that ( makes almost 21 %) of gases exerts nearly no green house effect. The molecules that are a bit more complex and are less common , instead, comes from the Green house effect. The vapours of Water remains the most siginifccant content and carbon dioide remains on the second most important greesn house gas. Nitrous oxide , the Methan gas and many other gases that are present in atmosphere in very small amount also contributes towads the Green house effect.
Using Flask measurments located at Mauna Lua Laboratary in Hauwaii , in 1958 , a very high quality concentrations of CO2 began and started with a new discovery. In the experiements carried out it was clearly visible that annual content concentration of CO2 present in atmosphere rasied to an amount from 320 ppmv (parts per million of volume ) in 1959 to round about 345 ppmv in 1998. In the Northern Hemisphere , It has been observed to have a clear annual cycle in Mauna Loa Dara which correspondes to an annual cycle plant of respiration in the Hemsiphere of Northern Region. The content of CO2 concentration always increased in the Fall and Winter and after wards declined during the season of summer and Spring. In the Southern Hemisphere , however, the complete cycle followed the growth and its through die back of vegetation, and it then disappeared completey in data measuremenet near the Equator.
Over the last complete decade, the rate of increase in abundance of methane has been at the declining end , and became more siginifcant dramatically from 1990 to 1993 , however it showed an apparent increase in the growth rate particualy in late 1995. As a whole , the average trend from 1981 to 1991 was about 14 ppbv/year ( parts per billion by volume /year)
In industrial applications , the family of man made gases are commonly known as Flourninated Gases. Their major use is as an Ozone Depleting Substances since they ever danage the ozone layer present in atmosphere. Hence , the F- gases have proved to be very powerful green shouse gases , with global warming upto 24000 times greater than Carbon Dioxide. However, their emissions are increasing rapidly .
The Green house gases emitted are already discussed in the above section . All these gases have adverse effect on atmosphere and its effect is increasing at a dramatic rate which is ultimately contributing towards a complete catastrophic situation . The gases emitted parituclarly because of burning of various types of fossil fuels remains a very dangerous concern. Furthermore , due to a continuous advancement in technology the use of Choloflorcarbons have been siginifcantly increased which is now creating a complete menace for not only humanity but in particular the major portion of population living in urban areas.
The greenhouse gases such as methane are produced by carrying out agricultural practices such as manure management of livestock that remains a prime concern because of an ever growing increase in population and to cater for day to ay human needs. Other gases such as Carbon Dioxde , CO2, comes for the natural process of respiration and furthermore from the fossile fuel like oil, gas and coal burning whixh remains a neccssity of an ever growing industrial growth as a whole . 70 percent of the electricity produced in United states of america comes from Suphur Oxide emissions which shows imminanelty the harzardious effect it has on enviornement. In addition to it the electricity production also includes about 13 % of nitrogen oxide emissions and 45 percent of Carbon Dioxde emssions that comes from natural atmosphere.
One of the other major cause is the cutting of trees and bigger plants that are use to produce heat or various wood related products, they relase the carbon dioxide that is stored in all such products during the process of photosynthesis. Ccording to the Global Forest Resource recent Assessment, there has been a nearly billion ton production of cabon because of various reasons and causes.
According to the research undertaken by EPA ,it has been observed that the gases emitted by green house effect , can offset the effect when a forestration practice is carried out at a large scale. The Replnation of tress at a large scale helps to increase and build up the Carbon Dioxide content in atmosphere , as it is growing and the tress seuester the carbon dioxide through the process of photosynthesis. The Atmospheric carbon dioxde is first of all converted , and then stored in vegetation and other soil formatios of any forest. Futhermore it has been observed that , the forests being created cannot alobe sequester the Carbon Dioxide that is emiiteed to the atmosphere by the burining of the foissil fuels and ultimately a reduction in emssioon of the gasses is still very vital and neccssaery to avoid its major build up in the complete atmosphere.
The output of Green house effect gases is a prime and grave concern now a days throughout the whole world. With a very rapid increase in industrialization from the year in particular from 2009 , the level of Carbon Dioxide have been increased to almost 40 percent and the production of methande have been increased dramaitically to the amount of about 139 % . Accroding to the research department, NASA, the major portion of increase has been dueinf the past 50 years of world history . After 1998, because of the menace of Global Warming , the year of 2014, was recorded as the most warmest year of the world and furthermore thae 10 most hottest years have come after 1997.
“The warming we observe affects atmospheric circulation, which impacts rainfall patterns globally. This will lead to big environmental changes, and challenges, for people all across the globe,” Josef Werne, an associate professor in the department of geology and planetary science at the University of Pittsburgh, told Live Science.
According to the scinetists and various researchers , it has been found that, the worst effects of global warming may have the worst effects ever that may include
The Burning of fossil fuels remains a prime concern in the rapid increase in gases that emiited in the atmosphere because of green house effect. There are various gases that are emitted because of this poricess out of which the CO2 is the most significant of all . The hazardious effects and impact of Carbon Dioxde remains a prime concern and need serious efforts to resolve it like using the techcinque of Geo sequestration of CO2.
A research published by the Duke University it has been observed and proved through various experminemnets under taken that the second cause of CO2 relase is the deforestation that is increasing sigincicanlty through out the world due to an ever increase in not only population but a rapidly increasing industry growth as well .
One of the other major cause is the cutting of trees and bigger plants that are use to produce heat or various wood related products, they relase the carbon dioxide that is stored in all such products during the process of photosynthesis. Ccording to the Global Forest Resource recent Assessment, there has been a nearly billion ton production of cabon because of various reasons and causes.
With the sudden increase in population , there has been a gradual increase in agricultural development and production . The world is facing problems because of shortage of the agricultural products. The various proceses involved in agriiculural growth and landfills of farming lands are the major contributor towards this grave hazard.
The relation ship between the change in climate the impact of Green house gases is well known . All the gase emitted because of various reasons contribute siginifcantly towards a major change in climate and may impact the human life in a very harmful manner. Efforts done in order to reduce the imoact of greenhouse effect seems useless. The various dangerious hazards caused by this phenonmnon remains a grave concern of all scintentis and efforts are bing made to control the temperature as much as possible .
The effect of green houses gases is very imminent to biodiversity . The vaiorus gasses emitted due to this process are extremely dangerous for bio diversity . The impact is not only dangerous but diverse as well . It encompeses all biological products that are dealt under this dimension.
The abrupt change in climate remains a concern for the human beings living on the globe. Because of green house effect there has been a visible spike in temperature in all dimensions. The various gases emitted from burning of fossil fuels and cutting of trees remains a prime source and conern which as a whole plays a very vital part in casuing temeprautre variation making human life uncomfortable on planet earth .
Morover , this meannce of Green houses gases have also effected the trends in rainfall . There has been a visible change in amount of rainfall through the world and the researchers and scientists have proved trhough studies and experiments that the major rolse has been played by the greenhouses gases emitted because if an ever increasing industrial growth and development.
It has been observed throughout the in addition to various other problems posed in , the rise of sea level remains a great concer. It is not increasing the land covered by the sea water but also adds in to death tolls every year because of its hazardeous impact on whole man kind.
The worst effects of global warming are numerous in nature and huge in danger. Its impact on globe, human life , plant life and on animals is quite obvious and visible . Moreove, the predicted impact of global warming on human life and environment remains varied and very grave in nature. It is considered that It is difficlut to attribute speciaifcally any natural phenonmena for a ling term in order to solve issues related to health being caused by global warming . It is an hour of need to analyze this problem seriously to solve this menace to humanity .
As the climate warms, it changes the nature of global rainfall, evaporation, snow, stream flow and other factors that affect water supply and quality. Freshwater resources are highly sensitive to variations in weather and climate. Climate change is projected to affect water availability. In areas where the amount of water in rivers and streams depends on snow melting, warmer temperatures increase the fraction of precipitation falling as rain rather than as snow, causing the annual spring peak in water runoff to occur earlier in the year. This can lead to an increased likelihood of winter flooding and reduced late summer river flows. Rising sea levels cause saltwater to enter into fresh underground water and freshwater streams. This reduces the amount of freshwater available for drinking and farming. Warmer water temperatures also affect water quality and accelerate water pollution
Food scarcity is a major key for many populations and is one of the prominent concerns with the changing climate. Currently, 1/6 of the global population are without adequate food supply. By 2050, the global population is projected to reach 9 billion requiring global food productions to increase by 50% to meet population demand.
Current short-, medium- and long-term projections for global energy demand still point to fossil fuels being combusted in quantities incompatible with levels required to stabilise greenhouse gas (GHG) concentrations at safe levels in the atmosphere.
All technologies along the CCS chain are known. They have been in operation in various industries for decades, although at relatively small scale. However, for the sole purpose of limiting climate change, these technologies have been put together in industrial scale (>1Mt CO2 captured and stored per year) in only a small number of installations.
The starting point for geosequestration is storage of relatively pure CO2. In a few instances, industrial processes emit fairly pure CO2 and that CO2 can be captured and separated relatively cheaply. Such processes include the manufacture of some fertilizers and natural gas processing. The latter is especially signiﬁ cant because it provides a relatively pure stream of CO2 at little additional incremental cost. The reason for this is that CO2 must be separated from methane to meet sales gas speciﬁ cations. It is also for this reason that some of the earliest geosequestration projects are based on natural gas activities (Sleipner in Norway; In Salah in Algeria). In Australia the Gorgon LNG project is currently planned to be the ﬁ rst large scale commercial geosequestration project in Australia.
The issue of separation of CO2 from natural gas is likely to be signiﬁ cant to Australia in the future, as approximately half of our identiﬁ ed natural gas resources have high concentrations of CO2. This means virtually all natural gas used for liqueﬁ ed natural gas (LNG) will need to have the CO2 removed. Domestic gas sales have higher sales gas speciﬁ cations for CO2, but in many cases in the future will still have unacceptable CO2 concentrations. Therefore, as natural gas production increases so will the amount of pure CO2 separated at the production facility. For these reasons, natural gas processing is a potential “early mover” in the application of geosequestration in Australia.
Prior to storage, the emitted gas stream is concentrated to 95% or more of CO2 and compressed to a dense supercritical ﬂ uid – a liquid which has a density (depending on the pressure) of around 0.5 -0.7 grams/cc (water has a density of 1gm/cc). Provided the CO2 is injected to a depth of 800 m or more, it will remain in this dense form, which means that far more CO2 can be stored than if it were to be injected in a gaseous state.
The storage of CO2 involves keeping the CO2 secured deep underground in an appropriate geological formation. The main geological conditions for this include a porous and permeable reservoir rock, a trap, and an impermeable caprock. Expertise in locating such geological formations is well established within the oil and gas industry, and geoscientists and engineers utilise mature technology to identify and evaluate speciﬁ c sites for their geosequestration potential. Each site is evaluated for its potential storage volume as well as to ensure that conditions for safe and effective long-term storage are present.
Since the injected CO2 is less dense than the formation water, it will slowly rise to the top of the geological reservoir, and a geological trap is needed to ensure that it does not escape and reach the surface or potable groundwater. The most common traps found in Australia are structural (e.g. an anticline), stratigraphic (“pinchout” of a reservoir rock) or hydrodynamic (CO2 entrained in the formation water). An overlying impermeable top seal is required to keep the CO2 within the storage formation. Such seals are generally very ﬁ ne grained rocks with low porosity and low permeability. The seal must be of sufﬁ cient thickness to prevent microfractures and through-going faults from developing as possible CO2 leakage pathways.
Depleted oil and natural gas ﬁ elds, which generally have proven geologic traps, reservoirs and seals are potentially excellent sites for storage of injected CO2. In some circumstances it may be possible to combine geological storage of CO2 with enhanced oil recovery or enhanced gas recovery. This has not been carried out to date in Australia but is an area of research for CO2CRC because of the potential to beneﬁ cially combine geosequestration with increased production of hydrocarbons. CSIRO, the University of Queensland and CO2CRC are also undertaking reseacrh into the use of CO2 storage to enhance the production of coal bed methane. When injecting into a depleted ﬁ eld care must be taken that all existing wellbores are adequately cemented before sequestration operations begin, to ensure that there is no leakage of CO2 from old wells.
Nearly every activity within an organization could be labeled as a project possessing unique characteristics and varying levels of importance to the organization. A project is defined as a planned undertaking of related activities to reach an objective that has a beginning and an end. All projects solve some type of problem, but projects may also be established simply to determine and define feasible alternative solutions to problems. Seven primary characteristics of a project include:
In the past, a company typically decided to undertake a project effort, assigned the project and the “necessary” resources to a carefully selected individual and assumed they were using some form of project management. Organizational implications were of little importance. Although the basic concepts of project management are simple, applying these concepts to an existing organization is not. Richard P. Olsen, in his article “Can Project Management Be Defined?” defined project management as “…the application of a collection of tools and techniques…to direct the use of diverse resources toward the accomplishment of a unique, complex, one-time task within time, cost, and quality constraints. Each task requires a particular mix of these tools and techniques structured to fit the task environment and life cycle (from conception to completion) of the task.” 
Employing project management technologies minimizes the disruption of routine business activities in many cases by placing under a single command all of the skills, technologies, and resources needed to realize the project. The skills required depend on each specific project and the resources available at that time. The greater the amount of adjustments a parent organization must make to fulfill project objectives, the greater chance exists for project failure. The form of project management will be unique for every project endeavor and will change throughout the project.
The project management process typically includes four key phases: initiating the project, planning the project, executing the project, and closing the project.
Initiating the Project
The project management techniques related to the project initiation phase include: 
1. Establishing the project initiation team. This involves organizing team members to assist in carrying out the project initiation activities.
2. Establishing a relationship with the customer. The understanding of your customer’s organization will foster a stronger relationship between the two of you.
3. Establishing the project initiation plan. Defines the activities required to organize the team while working to define the goals and scope of the project.
4. Establishing management procedures. Concerned with developing team communication and reporting procedures, job assignments and roles, project change procedure, and how project funding and billing will be handled.
5. Establishing the project management environment and workbook. Focuses on the collection and organization of the tools that you will use while managing the project.
Planning the Project
The project management techniques related to the project planning phase include:
1. Describing project scope, alternatives, and feasibility. The understanding of the content and complexity of the project. Some relevant questions that should be answered include:
o What problem/opportunity does the project address?
o What results are to be achieved?
o What needs to be done?
o How will success be measured?
o How will we know when we are finished?
2. Divide the project into tasks. This technique is also known as the work breakdown structure. This step is done to ensure an easy progression between tasks.
3. Estimating resources and creating a resource plan. This helps to gather and arrange resources in the most effective manner.
4. Developing a preliminary schedule. In this step, you are to assign time estimates to each activity in the work breakdown structure. From here, you will be able to create the target start and end dates for the project.
5. Developing a communication plan. The idea here is to outline the communication procedures between management, team members, and the customer.
6. Determining project standards and procedures. The specification of how various deliverables are produced and tested by the project team.
7. Identifying and assessing risk. The goal here is to identify potential sources of risk and the consequences of those risks.
8. Creating a preliminary budget. The budget should summarize the planned expenses and revenues related to the project.
9. Developing a statement of work. This document will list the work to be done and the expected outcome of the project.
10. Setting a baseline project plan. This should provide an estimate of the project’s tasks and resource requirements.
Executing the Project
The project management techniques related to the project execution phase include:
1. Executing the baseline project plan. The job of the project manager is to initiate the execution of project activities, acquire and assign resources, orient and train new team members, keep the project on schedule, and assure the quality of project deliverables.
2. Monitoring project progress against the baseline project plan. Using Gantt and PERT charts, which will be discussed in detail further on in this paper, can assist the project manager in doing this.
3. Managing changes to the baseline project plan.
4. Maintaining the project workbook. Maintaining complete records of all project events is necessary. The project workbook is the primary source of information for producing all project reports.
5. Communicating the project status. This means that the entire project plan should be shard with the entire project team and any revisions to the plan should be communicated to all interested parties so that everyone understands how the plan is evolving.
Closing Down the Project
The project management techniques related to the project closedown phase include:
1. Closing down the project. In this stage, it is important to notify all interested parties of the completion of the project. Also, all project documentation and records should be finalized so that the final review of the project can be conducted.
2. Conducting post project reviews. This is done to determine the strengths and weaknesses of project deliverables, the processes used to create them, and the project management process.
3. Closing the customer contract. The final activity is to ensure that all contractual terms of the project have been met.
Project management is the discipline of initiating, planning, executing, controlling, and closing the work of a team to achieve specific goals and meet specific success criteria. A project is a temporary endeavor designed to produce a unique product, service or result with a defined beginning and end (usually time-constrained, and often constrained by funding or deliverables) undertaken to meet unique goals and objectives, typically to bring about beneficial change or added value. The temporary nature of projects stands in contrast with business as usual (or operations), which are repetitive, permanent, or semi-permanent functional activities to produce products or services. In practice, the management of these two systems is often quite different, and as such requires the development of distinct technical skills and management strategies.
The primary challenge of project management is to achieve all of the project goals within the given constraints. This information is usually described in a user or project manual, which is created at the beginning of the development process. The primary constraints are scope, time, quality and budget. The secondary — and more ambitious — challenge is to optimize the allocation of necessary inputs and integrate them to meet pre-defined objectives.
In this methodology, the project scope is a variable. Additionally, the time and the cost are constants for the project. Therefore, during the project execution, the project scope is adjusted in order to get the maximum business value from the project.
Agile software development methodology is for a project that needs extreme agility in requirements. The key features of agile are its short-termed delivery cycles (sprints), agile requirements, dynamic team culture, less restrictive project control and emphasis on real-time communication.
In crystal method, the project processes are given a low priority. Instead of the processes, this method focuses more on team communication, team member skills, people and interaction. Crystal methods come under agile category.
This is the successor of Rapid Application Development (RAD) methodology. This is also a subset of agile software development methodology and boasts about the training and documents support this methodology has. This method emphasizes more on the active user involvement during the project life cycle.
Lowering the cost of requirement changes is the main objective of extreme programming. XP emphasizes on fine scale feedback, continuous process, shared understanding and programmer welfare. In XP, there is no detailed requirements specification or software architecture built.
This methodology is more focused on simple and well-defined processes, short iterative and feature driven delivery cycles. All the planning and execution in this project type take place based on the features.
This methodology is a collection of best practices in project management. ITIL covers a broad aspect of project management which starts from the organizational management level.
Involving the client from the early stages with the project tasks is emphasized by this methodology. The project team and the client hold JAD sessions collaboratively in order to get the contribution from the client. These JAD sessions take place during the entire project life cycle.
Lean development focuses on developing change-tolerance software. In this method, satisfying the customer comes as the highest priority. The team is motivated to provide the highest value for the money paid by the customer.
PRINCE2 takes a process-based approach to project management. This methodology is based on eight high-level processes.
This methodology focuses on developing products faster with higher quality. When it comes to gathering requirements, it uses the workshop method. Prototyping is used for getting clear requirements and re-use the software components to accelerate the development timelines.
In this method, all types of internal communications are considered informal.
RUP tries to capture all the positive aspects of modern software development methodologies and offer them in one package. This is one of the first project management methodologies that suggested an iterative approach to software development.
This is an agile methodology. The main goal of this methodology is to improve team productivity dramatically by removing every possible burden. Scrum projects are managed by a Scrum master.
Spiral methodology is the extended waterfall model with prototyping. This method is used instead of using the waterfall model for large projects.
This is a conceptual model used in software development projects. In this method, there is a possibility of combining two or more project management methodologies for the best outcome. SDLC also heavily emphasizes on the use of documentation and has strict guidelines on it.
This is the legacy model for software development projects. This methodology has been in practice for decades before the new methodologies were introduced. In this model, development lifecycle has fixed phases and linear timelines. This model is not capable of addressing the challenges in the modern software development domain.
In a sequential methodology, informally known as the waterfall, the analysis phase comes first, then the design phase, followed by the implementation phase, and finally by the testing phase. The team that does each phase may be different, and there may be a management decision point at each phase transition.
While it may be debatable whether this is a true project management methodology, you will find organizations that say they use the PMI or PMBOK method for managing projects. What this simply means is they break down their projects into the five process groups agreed upon by the Project Management Institute (PMI) and documented in the Guide to the Project Management Body of Knowledge (PMBOK), namely: initiating, planning, executing, controlling, and closing.
Project management purists however insist that PMBOK is not so much a methodology as it is an agreed upon set of standards and conventions for managing projects. A similar analogy is that the dictionary is not a method for creating books, but it collects the agreed-upon vocabulary used to write books.
There are the methodologies that deal with managing projects but with an extra focus on change management especially planning for risks and taking control of change when it happens. Notable methods include:
The underlying idea behind event chain methodology is that there are potential risks that often lie outside the project’s scope. It’s important to prepare for these risks and plan what to do if they occur. Why? Unexpected events will impact your project’s schedule, deliverables, and potentially its success.
Extreme project management (XPM) is the opposite of Waterfall in that it offers you a way to manage massive change and still move forward to project completion. In XPM, you can alter the project plan, budget, and even the final deliverable to fit changing needs, no matter where the project is. It’s the perfect way to manage projects that have a short timeline of anywhere from a few weeks to mere days.
PDCA (plan–do–check–act or plan–do–check–adjust) is an iterative four-step management method used in business for the control and continual improvement of processes and products. It is also known as the Deming circle/cycle/wheel, Shewhart cycle,control circle/cycle, or plan–do–study–act (PDSA). Another version of this PDCA cycle is OPDCA. The added “O” stands for observation or as some versions say “Grasp the current condition.” This emphasis on observation and current condition has currency withLean manufacturing/Toyota Production System literature.
Establish the objectives and processes necessary to deliver results in accordance with the expected output (the target or goals). By establishing output expectations, the completeness and accuracy of the specification is also a part of the targeted improvement. When possible start on a small scale to test possible effects.
Implement the plan, execute the process, make the product. Collect data for charting and analysis in the following “CHECK” and “ACT” steps.
Study the actual results (measured and collected in “DO” above) and compare against the expected results (targets or goals from the “PLAN”) to ascertain any differences. Look for deviation in implementation from the plan and also look for the appropriateness and completeness of the plan to enable the execution, i.e., “Do”. Charting data can make this much easier to see trends over several PDCA cycles and in order to convert the collected data into information. Information is what you need for the next step “ACT”.
If the CHECK shows that the PLAN that was implemented in DO is an improvement to the prior standard (baseline), then that becomes the new standard (baseline) for how the organization should ACT going forward (new standards are enACTed).
Carbon dioxide is part of the atmosphere we breathe and is essential to all life forms. It is odourless and non-toxic. However, as it is denser than air, if it accumulates in low-lying areas in high concentrations then it can prove harmful to humans and animals.
The most substantial risk associated with CCS is the leakage of CO2 from storage sites. While there is some experience with geological storage of CO2 and natural gas for periods of approximately 10-20 years, long term storage over many hundreds or thousands of years
has not been proven.
However, as argued by CSIRO, the ongoing study of naturally occurring underground accumulations of CO2 has increased knowledge and confidence in the viability of CO2 storage.
The IPCC Special Report on CCS suggests that the environmental risks associated with CO2 capture and storage are low. As the IPCC stated: …well-selected geological formations are likely to retain over 99% of their storage over a period of 1,000 years. Overall, the risks of CO2 storage are comparable to the risks in similar existing industrial operations such as underground naturalgas storage and [EOR].
Furthermore, according to many submissions, the safety, health and environmental risks associated with CCS are similar to, or less than, those already experienced in the oil and gas industry.21 5.25 Nevertheless, concerns have been expressed regarding the long term storage of CO2. Two types of CO2 leakage that may occur are: „ abrupt leakage through injection well failure or leakage up an abandoned well; and „ gradual leakage, through undetected faults, fractures or wells.
Abrupt or catastrophic leaks of CO2 could have serious consequences to the environment, potentially causing the death of humans and animals.23 Leakages have been known to occur naturally, such as at Lake Nyos in Cameroon in 1986.
There is the potential for CO2 that is sequestered as part of the CCS processes to leak from storage points. Such leakage could occur if the well seal at the point of storage failed thereby resulting in the release of sequestered CO2. 5.28 Evidence to the Committee from Greenpeace and the Australian Government also suggested that pressure built up by injected CO2 could trigger small seismic events.25 5.29 In his submission Dr Maddison also raised potential risks associated with CCS, stating that: carbon dioxide sequestration is poorly conceived, cannot guarantee sequestration of gas forever as is necessary and has potential for great harm due to accidental or deliberate release.26 5.30 It has been suggested that CO2 storage sites may become potential terrorist targets or that failure of the seal could result in catastrophic release. Greenpeace points out that concentration of CO2 greater than 7-10 per cent by volume in the air puts the lives and health of people in the vicinity in immediate danger.27 5.31 However, evidence suggests that if storage sites are carefully selected, the chances of a catastrophic leak would be minimal. Current demonstration projects, such as the Otway Demonstration Project, extend understanding of the scientific processes and risk minimisation associated with the selection, sequestration and monitoring of CO2 in an Australian context.
Gradual leakage 5.32 Gradual leakage could occur as a result of incorrect site selection and inadequate preparation.28 This leakage would compromise the initial objective of removing the CO2 from the atmosphere. 5.33 Other dangers associated with gradual leakage have also been highlighted. According to the International Association of Hydrogeologists, CCS is a potential environmental risk to overlying fresh groundwater resources and therefore CCS should only be considered in geological formations which are not potential groundwater resources i.e. aquifers which are not connected with active groundwater flow systems.29 5.34 In terms of assessing the probability of leakage and escape of CO2, Greenpeace points out that little is known about the behaviour of large quantities of CO2. Greenpeace suggests that, because of the complex geology of each individual storage site, evaluation can only be conducted on a case by case basis. 5.35 Greenpeace states that storing CO2 underground can dissolve the minerals that help stop the gas from escaping. The results from tests that injected CO2 into saline aquifers in Texas showed that sequestration made aquifer water more acidic. This acidity attacked the surrounding rock formations, causing them to dissolve and thereby potentially allowing the gas to leak into the water table.30 5.36 In his evidence, Dr Maddison expresses similar concerns regarding potential leakage. He contends that there may be problems associated with the use of depleted gas fields, including rocks cracking as gas is removed causing structural changes which may result in the rock structure no longer being able to hold their contents for long periods of time. Furthermore, problems also exist in association with the repressurising of rocks when injecting CO2 and the integrity of the well plug. Dr Maddison states that ‘there is no proof that once a field is filled with carbon dioxide, the plug can or will remain intact over the rest of time.’31
Rigorous risk mitigation strategies should be developed and implemented in order to reduce the risk of CO2 leakage. For example, in evidence to the Committee it was noted that the risks of leakage during pipeline transportation can be reduced if care is taken that the water content of the CO2 stream is kept low. This will avoid corrosion of the carbon manganese steel used in most pipe construction Greenpeace raised concerns about the relative lack of experience with CCS risk mitigation strategies and the need for long term monitoring techniques.33 5.39 The CSIRO states that proper regulation is necessary to ‘ensure that operators are competent, sites are appropriately chosen, and that wells are properly cemented.’34 5.40 CSIRO contends that catastrophic leakage is unlikely if sites are well selected, operators are competent and wells are properly sealed.35 Rigorous site selection, diligent monitoring and management of the injection site are all critical factors and it is important that these activities are appropriately regulated.36 Likewise, Chevron stated that ‘the most effective way to mitigate the risk of containment failure is through rigorous site selection and management of injection operations’
Consider a scenario in which the organization you are working for has been handed a number of project contracts. But due to resource constraints, the organization cannot take up all the projects at once. Therefore, a decision has to be made as to which project needs to be taken up to maximize profitability.
This is where Project Selection Methods come into play. There are various methods to help you choose a project. These can be divided into two categories, namely:
These nine areas are outlined with strategies on how to implement them.
Project integration management is a collection of processes that outline the project so that the venture is successful. Project integration management consists of seven steps:
Scope management deals with five processes meant to ensure that the project is self-contained and does not meander. The scope element section includes:
A third element of project management PMBOK covers is time management. This element includes processes for:
Cost management deals with resources and budgeting. Processes included under cost management consist of:
Quality management has to do with the deliverables of the project. The goal of project managment is to produce quality deliverables. Proceses of quality management include planning quality, assuring quality, and controlling quality.
This element deals with all aspects of managing human resources, from resource planning to acquiring, developing, and managing the project team. Many articles on human resource management can be found on Bright Hub’s Project Management Channel including Gary’s “Employing Effective Resource Management at Your Company.”
Effective communication is very important during the project management process. This element of PMBOK deals with who needs to know what, when. Processes covered by communication management include:
Risk Management is a crucial element of managing a successful project. Risk management processes in PMBOK literature include:
Bright Hub has a wealth of information on risk management in project management including Joe Taylor’s Risk Management Series.
Managing Procurables is the final element of PMBOK project managing. This element includes six processes. These six processes are:
The Program Evaluation and Review Technique (PERT) is a widely used method for planning and coordinating large-scale projects. As Harold Kerzner explained in his book Project Management, “PERT is basically a management planning and control tool. It can be considered as a road map for a particular program or project in which all of the major elements (events) have been completely identified, together with their corresponding interrelations’¦. PERT charts are often constructed from back to front because, for many projects, the end date is fixed and the contractor has front-end flexibility.” A basic element of PERT-style planning is to identify critical activities on which others depend. The technique is often referred to as PERT/CPM, the CPM standing for “critical path method.”
PERT was developed during the 1950s through the efforts of the U.S. Navy and some of its contractors working on the Polaris missile project. Concerned about the growing nuclear arsenal of the Soviet Union, the U.S. government wanted to complete the Polaris project as quickly as possible. The Navy used PERT to coordinate the efforts of some 3,000 contractors involved with the project. Experts credited PERT with shortening the project duration by two years. Since then, all government contractors have been required to use PERT or a similar project analysis technique for all major government contracts.
A Gantt chart is a type of bar chart, devised by Henry Gantt in the 1910s, that illustrates a project schedule. Gantt charts illustrate the start and finish dates of the terminal elements and summary elements of aproject. Terminal elements and summary elements comprise the work breakdown structure of the project. Modern Gantt charts also show the dependency (i.e., precedence network) relationships between activities. Gantt charts can be used to show current schedule status using percent-complete shadings and a vertical “TODAY” line as shown here.
Although now regarded as a common charting technique, Gantt charts were considered revolutionary when first introduced. This chart is also used in information technology to represent data that has been collected.
A Network Diagram is a visual representation of a project’s schedule. Well known complements to network diagrams include the PERT and Gantt charts. A network diagram in project management is useful for planning and tracking the project from beginning to finish. It represents a project’s critical path as well as the scope for the project.
A good network diagram will be a clear and concise graphic representation of a project.
“A display of cumulative costs, labor hours or other quantities plotted against time. The name derives from the S-like shape of the curve, flatter at the beginning and end and steeper in the middle, which is typical of most projects. The beginning represents a slow, deliberate but accelerating start, while the end represents a deceleration as the work runs out.”
There are a variety of S-curves that are applicable to project management applications, including:
One tool that can be used to achieve acceptance of geologic sequestration of CO2 is risk assessment, which is a proven method to objectively manage hazards in facilities such as oil and natural gas fields, pipelines, refineries, and chemical plants. Although probabilistic risk assessment (PRA) has been applied in many areas, its application to geologic CO2 sequestration is still in its infancy.
The most significant risk from geologic carbon sequestration is leakage of CO2. Two types of CO2 releases are possible— atmospheric and subsurface. High concentrations of CO2 caused by a release to the atmosphere would pose health risks to
humans and animals, and any leakage of CO2 back into the atmosphere negates the effort expended to sequester the CO2. Subsurface risks, attributable to subsurface releases, arise from the displacement of fluids by the injected CO2 that could damage nearby hydrocarbon resources or trigger small seismic events. There is also the potential for sequestered CO2 to leak into non-saline formations, which could cause problems with potable uses of this water. However, overall, risks from CO2 sequestration are believed to be small.
Implementation of CO2 sequestration is being approached in phases. The DOE is currently sponsoring a series of pilot tests to generate important data that will elucidate the risks involved in geologic sequestration and lead to the development of risk management protocols. This phased approach should ensure that potential sources of leakage are identified, consequences are quantified, events with the potential to cause harm are analyzed to estimate their frequency and associated risk, and safeguards are put in place to further reduce risks for an operation for which risks already appear to be low.
Concern about increasing atmospheric concentrations of carbon dioxide (CO2) and other greenhouse gases (GHG) and the potential impact of these increases on the earth’s climate has grown significantly over the last decade. Many countries, including the United States, wrestle with balancing economic development and meeting critical near-term environmental goals while minimizing long-term environmental risks. One promising solution being pursued by the U.S. Department of Energy’s (DOE) National Energy Technology Laboratory (NETL) and its industry and academic partners is carbon sequestration—a process of permanent storage of CO2 emissions in underground geologic formations, thus avoiding CO2 release into the atmosphere. This option looks particularly attractive for point source emissions of GHGs, such as fossil fuel fired power plants. In this case, CO2 would be captured, either pre- or post-combustion, compressed to a dense fluid, transported, most likely by pipeline, to a storage site, and sequestered in an appropriate geologic formation, such as a depleted oil or natural gas field, a saline formation, or an unmineable coal seam .
The most significant risk from geologic carbon sequestration is leakage of CO2. Two types of CO2 releases are possible— atmospheric and subsurface. These may be caused by slow leaks through slightly permeable cap rock or catastrophic releases due to rupture of a pipeline, failure of a field well, or opening of a fault. In general, CO2 is not classified as a toxic material; however, high concentrations of atmospheric releases pose health risks to humans and animals. Additional risks are attributable to subsurface release of injected CO2. Although methodologies exist to estimate and report leakage from storage sites, further development is needed.
One tool that can be used to achieve acceptance of CO2 sequestration is risk assessment, an essential step in risk management. Risk management involves selecting appropriate prevention and control options, policies, and processes to manage risks. Evaluating risk is a proven method to manage hazards objectively in facilities such as oil and natural gas fields, refineries, and chemical and pharmaceutical plants. Although probabilistic risk assessment (PRA) has been applied in these areas, its application to geologic CO2 sequestration is still in its infancy. A PRA evaluates both the likelihood and the impact of an unplanned event. Use of PRAs allows decisions to be made on the most cost effective risk reduction and management options.
Prudent handling and management of CO2 are required to offset potential health hazards. Implementation of CO2 sequestration is being approached in a series of phases. This should ensure that potential sources of leakage are identified, consequences are quantified, events with the potential to cause harm are analyzed to estimate their frequency and associated risk, and safeguards are put in place to reduce risk to an acceptable level.
As national policy makers, project developers, and investors begin to evaluate potential investment opportunities and technology options for undertaking emissions reduction activities, evaluation of the cost and overall environmental effectiveness of each technology option is necessary. Moreover, any analysis of applicable technologies must take into account the siting, energy, resource, and policy constraints of the region, state, or city in question. A critical component of this type of evaluation is assessing the risks associated with a particular technology and/or practice. With geologic sequestration, risk assessment will primarily focus on the probability and consequences of CO2 leakage from a geologic storage site over time and the potentially adverse effects of this leakage on health, safety, the environment, and public policy. This paper addresses these questions.
Risk = Frequency x Consequences
Thus, one can have the same level of risk for a frequent event with a low level of damage as for a rare event with a very high level of damage. Therefore, in developing a risk assessment, one must evaluate both frequency and potential damage from an event. Risk assessment can address public safety, employee safety, property damage, revenue loss, and environmental damage. This methodology, called probabilistic risk assessment (PRA), is the industry standard.
PRAs use probability distributions to characterize variability or uncertainty in risk estimates. In a PRA, one or more variables in the risk equation are defined as probability distributions rather than as single values. Similarly, the output of a PRA is a range or probability distribution of risks. Geologic storage of CO2 is well suited to analysis using PRAs because sequestration is a process-driven problem occurring over a long period of time.
In general, the major risks associated with the operation of an underground CO2 storage project are related to leakage from the formation. CO2 leakage from the formation may migrate into potable aquifers or even to the surface, which could result in a significant safety risk. To evaluate this risk requires an improved understanding of formation properties and how the injected CO2 spreads and interacts with the rock matrix and reservoir fluids. Geologic formations typically consist of layers of rock with different porosities, thicknesses, and chemical compositions. All of these factors affect the suitability of the formation as a site for CO2 sequestration. Porosity and thickness determine the storage capacity of the formation, and chemical composition determines the interaction of CO2 with the minerals in place. Also, an impervious cap rock is necessary to prevent the sequestered CO2 from migrating to the surface. Finally, if the formation consists of a series of aquifers, it is necessary to ensure that CO2 stored in a saline formation does not migrate to a potable aquifer.
For geologic sequestration to be a viable technical option for climate change mitigation, the risks associated with this activity must be evaluated, including environmental, health and safety, and economic risks. By identifying which aspects of geologic sequestration present potential risks, appropriate actions can be taken prior to the commencement of injection activities to obviate the occurrence of problems.
From an environmental point of view, leakage is the most serious potential problem. First, leakage to the atmosphere negates the effort expended in sequestering the CO2. Leakage serves as a CO2 source and increases atmospheric CO2, as well as representing an economic loss. Another potential problem is accumulation of CO2 in pockets on the surface of the earth. Furthermore, CO2 could migrate into other strata, with the potential for contaminating fresh water or causing other problems. If the formation into which CO2 is being injected is below the ocean, leakage of CO2 into the marine environment could affect ocean chemistry and have potentially serious consequences for marine life. Additional risks arise from potential damage to nearby hydrocarbon resources caused by the displacement of fluids by the injected CO2, such as saline water production at wells that had been producing oil or gas. Finally, if a project does not operate within prescribed injection rates and pressures, there is some potential for initiating seismic activity.
Injected CO2 may interact with formation minerals, which may have beneficial or detrimental effects. At this time, mineral interactions are not as well understood as transport processes. The interactions may be beneficial by permanently sequestering the CO2 or may be harmful by plugging the formation and reducing permeability. There is some evidence that CO2 injected into coal seams causes the coal to swell, which could affect overlying strata.
Health and Safety Risks Information on the responses of animals and vegetation to elevated and potentially hazardous levels of CO2 and low levels of oxygen (O2) can be found in the literature related to physiology, respiratory physiology, comparative physiology, plant physiology, botany, food preservation, and aerospace. Ecosytem impacts resulting from high CO2 concentrations are less well known than impacts on humans.
Human exposure to elevated levels of CO2 can be hazardous in two ways—by a reduction in the oxygen content of the ambient air causing hypoxia or through direct CO2 toxicity. The National Institute of Occupational Safety and Health (NIOSH) confined-space-hazard classification system defines CO2 as a nontoxic, inert gas that displaces oxygen . In most cases of hazardous CO2 exposure, the gas is presumed to act as a simple asphyxiant. However, extensive research indicates that exposure to elevated CO2 concentrations (>3 percent) has significant effects before oxygen dilution becomes physiologically significant. As O2 concentration drops below 17 percent, increasingly severe physiological effects occur until below six percent O2, loss of consciousness is rapid, and death takes place within minutes.
Another safety problem results from the potential for accidents from working around the facilities required to capture, condense, transport, and inject the CO2. If hydrogen sulfide (H2S) is sequestered along with CO2, health risks are significantly increased, as H2S is highly toxic.
Economic Risks Regardless of the formation chosen for carbon storage, it is essential that its use be economically feasible. Large-scale application of CO2 injection for enhanced oil recovery (EOR) is considered a commercially proven process; however, there are still issues that need to be addressed, a key area of concern being the economic risk of implementing geologic sequestration. It is quite expensive to capture and transport anthropogenic CO2. Retrofitting existing pulverized coal (PC) fired units with currently available CO2 post-combustion capture and storage technologies could increase the cost of electricity by as much as 65 percent. In the case of integrated gasification combined cycle (IGCC) plants with pre-combustion capture, cost increases are expected to be in the 20-30 percent range (with an ultimate target of only a 10 percent increase).
Aside from the issue of the effect on power costs, there are other economic risks that need to be considered. Economic liability could result if, for example, a pipeline were to rupture and cause injury or death. Such risks are routinely faced by industry and are typically covered by purchasing insurance. Also, a sequestration project might fail to operate as planned. For example, it might be discovered that the site is unsuitable because of the presence of an undetected fault, thus requiring abandoning the project and forfeiting the investment.
There are also risks associated with potential leakage from a storage site. If such leakage were to result in a high enough CO2 concentration to cause harm, liability could result. CO2 leakage could result in other types of economic liability. If, for example, a carbon tax were instituted, then CO2 leakage might be treated as a CO2 source and the sequestration project operator might have to pay a tax on the CO2 leakage to the atmosphere. Economic liability could also arise if CO2 leaked into a potable aquifer and caused problems, or if injected CO2 caused water to be produced at a hydrocarbon well that had been producing oil or natural gas.
As indicated above, one of the major risks associated with CO2 sequestration is the potential for leakage. In order to reduce this risk, technologies are needed for the measurement, mitigation, and verification (MMV) of stored CO2. MMV is concerned with the capability to measure the amount of CO2 stored at a specific sequestration site, map its spatial disposition, develop techniques to mitigate potential leakage, and verify that the CO2 is stored or isolated as intended and will not adversely impact the host ecosystem. MMV for geologic sequestration consists of three areas: modeling and analysis of the geologic structure before injection occurs, subsurface monitoring of the movement of the CO2 plume, and above-surface measurements that verify that the CO2 remains sequestered .
Modeling and Simulation Prior to Injection Prior to initiating a CO2 injection project, the target geologic structure must be thoroughly understood, and the movement of the injected CO2 must be reasonably well predicted in order to properly site above-ground measurement equipment. A number of models and simulation software packages currently exist to track the movement of underground fluids; however, none are designed for geologically sequestered CO2 plumes. Modifications to any existing models and simulators to accommodate CO2 were done for EOR analysis. To effectively model underground CO2 behavior, three basic types of models are available:
• Standard reservoir simulator • Geomechanical simulator • Geochemical simulator
Which one or combination of these are used will depend on the geological attributes of the storage site and the major risks. These simulators can be tailored to meet the unique needs of CO2 injection and geologic sequestration. Significant understanding of candidate geologic sequestration sites already exists; however, gaps still remain in understanding how CO2 will behave at these sites. Application of MMV simulators to CO2 injection will improve the knowledge base and provide greater accuracy of detecting CO2 movement in underground structures.
Subsurface Measurement of CO2 Plume Movement Geophysical tools, such as fluid movement monitoring and seismic studies, will be used to monitor injected CO2 behavior in targeted structures. These tools will validate and/or calibrate the pre-injection models and simulations and also provide locations of potential above-ground leakage.
Surface Verification That CO2 Remains Sequestered Surface verification that the injected CO2 remains sequestered will take place near or above the surface of the underground formation. These surface MMV methods involve the direct detection and measurement of the CO2 or, in some cases, of tracer substances moving with the injected CO2. However, large-scale surface verification detection systems have not been tested to determine if they have sufficient accuracy.
The Mountaineer Project consists of drilling a 9,200 foot well in the Ohio River Valley to determine if the geology of this region is suitable for the injection of CO2 into saline formations. The site for the project is American Electric Power’s (AEP) Mountaineer plant near New Haven, WV. Prior to drilling the well, seismic studies were conducted to characterize the area. The Ohio River Valley is believed to be an ideal candidate for carbon capture and sequestration because of the nature of the geology of the area and because the region is home to many fossil fuel-fired electric generation plants. The data generated by this project are being used for CO2 sequestration simulations, risk assessments, permit applications, and the design of monitoring facilities for future CO2 injection projects. Based on the site characterization results, several potential CO2 injection zones have been identified.
Risk assessment is an important part of this project. This includes site characterization, storage and migration modeling, identification of potential hazards and their risk, and final risk assessment. This information will be evaluated to develop risk management procedures. The conceptual site framework is being used with the reservoir models to simulate injection scenarios for various injection well designs and injection rates. Atmospheric and aqueous dispersion models may be used to evaluate the impact of any CO2 buildup in shallow water or air and to design monitoring systems. The site information and simulation results are put into a risk assessment framework which includes hazard identification/analysis, dose-response assessment, exposure assessment, and consequence assessment.
Performance assessments and projects that have been conducted have shown that geologic settings are highly suitable for longterm subsurface storage of CO2. These studies have highlighted the significant capacity of the geosphere to effectively store CO2 and prevent its migration to the biosphere. Suitable formations include depleted oil and natural gas formations, unmineable coal seams, and saline formations.
Health effects should be minimal from slow leakage of CO2, since low levels of CO2 are nontoxic. The major risk to life would appear to be from a massive leak of CO2, such as might occur from a pipeline rupture, a well blowout, or the opening of a fault. Years of pipeline operations with natural gas and, to a lesser extent, CO2 should provide the experience needed for the safe design, operation, and management of CO2 pipelines. However, there is always the chance that seismic or construction activity could lead to pipeline rupture. The Weyburn risk analysis indicated that the most probable path for transmission of CO2 from one stratum to another or to the biosphere is along a well bore. Therefore, wells must be carefully drilled and monitored. If CO2 sequestration is practiced in depleted oil and natural gas fields, then the presence of abandoned wells could cause problems. These wells will need to be effectively plugged and monitored. If H2S, sulfur oxides (SOx), or nitrogen oxides (NOx) are sequestered along with CO2, then potential health risks from slow leakage are considerably greater.
The largest uncertainty about leakage may come from sequestration in saline formations, since the presence of an impermeable cap rock is not as certain as in the case of depleted oil and natural gas reservoirs. CO2 in coal seams should be
relatively stable as long as the seam is otherwise undisturbed. The methane in coal seams has been kept in place for perhaps millions of years, and there is no reason that CO2 cannot be sequestered for at least thousands of years.
In addition to health and environmental risks, there are technical risks. The major technical risk is that the injected CO2 will affect the strata into which it is being injected in such a way that permeability and/or porosity is decreased, thus limiting the rate or quantity of CO2 that can be injected. Decreased permeability can be overcome to some extent by increasing injection pressure, but this increases cost, and there is a limit to injection pressure to avoid fracturing the cap rock. These risks will be decreased by employing the data generated by pilot projects, but the risks will need to be included in project risk assessments. Ultimately, the risks associated with geologic sequestration identified in this paper, which are believed to by already low will be further mitigated by effective and comprehensive risk management strategies.
 S.M. Klara, R.D. Srivastava, and H.G. McIlvried, “Integrated Collaborative Technology Development Program for CO2 Sequestration in Geologic Formations—United States Department of Energy R&D,” Energy Conversion and Management 44:2699-2712, 2003.  NIOSH, “NIOSH, Occupation Health Guidelines for Chemical Hazards,” Publication No. 81-123, United States Government Printing Office, Washington, DC. 1981  K.K. Cohen, S.M. Klara, and R.D. Srivastava, “A Survey of Measurement, Mitigation, and Verification Field Technologies for Caron Sequestration Geologic Storage,” American Geophysical Union Fall Meeting, San Francisco, CA, 2004.  R. Pitblado and M. Mossemiller, “Risk Assessment Methods for Geosequestration of CO2,” Technical Report 700112 for PTRC, Det Norske Verikas (U.S.A.), 58p, cited in IEA GHG Weyburn CO2 Monitoring and Storage Project Summary Report 2000-2004, Petroleum Technology Research Center (PTRC), Regina, 2004.  C.M. Oldenburg, and A.A. Unger, “Transport and Dispersion Processes for CO2 in the Unsaturated Zone and Surface Layer,” Paper presented at 2nd Annual Conference on Carbon Sequestration, Alexandria, VA, 2003  J.T. Litynski, S.M. Klara, H.G. McIlvried, and R.D. Srivastava, “The United States Department of Energy’s Regional Carbon Sequestration Partnerships program: A collaborative approach to carbon management,” Environment International, 32:128-146, 2006.  S. Whittaker, D.White, D. Law, and R. Chalaturnyk, “IEA GHG Weyburn CO2 Monitoring & Storage Project Summary Report 2000-2004,” published in the proceeding of the 7th International Conference on Greenhouse Gas Control Technologies, September 5-9, Vancouver, Canada, Vol. III. Petroleum Technology Research Center (PTRC), Regina, 2004.  Geological Survey of Alabama http://portal.gsa.state.al.us/CO2/DFNModler/dfnm.htm, 2005.  S.H. Stevens, J.M. Pearce, and A.A.J. Riggs, “Natural Analogs for Geological Storage of CO2,” First National Conference on Carbon Sequestration, Washington, DC, 2001.
Like most large-scale infrastructure projects, carbon dioxide (CO2) geological sequestration (GS) projects have multiple success criteria and multiple stakeholders. In this context “risk evaluation” encompasses multiple scales. Yet a risk management program aims to maximize the chance of project success by assessing, monitoring, minimizing all risks in a consistent framework.
The 150,000 – km2 Illinois Basin underlies much of the state of Illinois, USA, and parts of adjacent Kentucky and Indiana. Its potential for CO2 storage is first-rate among basins in North America, an impression that has been strengthened by early testing of the injection well of the Midwest Geological Sequestration Consortium’s (MGSC’s) Phase III large scale demonstration project, the Illinois Basin – Decatur Project (IBDP). The IBDP, funded by the U.S. Department of Energy’s National Energy Technology Laboratory (NETL), represents a key trial of GS technologies and project-management techniques. Though risks are specific to each site and project, IBDP risk management methodologies provide valuable experience for future GS projects.
IBDP views risk as the potential for negative impact to any of these five values: Health and safety, environment, financial, advancing the viability and public acceptability of a GS industry, and research. Research goals include monitoring one million metric tonnes of injected CO2 in the subsurface. Risk management responds to the ways in which any values are at risk: For example, monitoring is designed to reduce uncertainties in parameter values that are important for research and system control, and is also designed to provide public assurance. Identified risks are the primary basis for risk-reduction measures: Risks linked to uncertainty in geologic parameters guide further characterization work and guide simulations applied to performance evaluation.
Formally, industry defines risk (more precisely risk criticality) as the product L*S, the Likelihood multiplied by the Severity of negative impact. L and S are each evaluated on five-point scales, yielding a theoretical spread in risk values of 1 through 25. So defined, these judgment-based values are categorical and ordinal–they do not represent physically measurable quantities, but are nonetheless useful for comparison and therefore decision support. The “risk entities” first evaluated are FEPs–conceptual Features, Events, and Processes based on the list published by Quintessa Ltd. After concrete scenarios are generated based on selected FEPs, scenarios become the critical entities whose associated risks are evaluated and tracked.
In IBDP workshops, L and S values for 123 FEPs were generated through expert elicitation. About 30 experts in the project or in GS in general were assigned among six facilitated working groups, and each group was charged to envision risks within a sphere of project operations. Working groups covered FEPs with strong spatial characteristics–such as those related to the injection wellbore and simulated plume footprint–and “nonspatial” FEPs related to finance, regulations, legal, and stakeholder issues.
Within these working groups, experts shared information, examined assumptions, refined and extended the FEP list, calibrated responses, and provided initial L and S values by consensus. Individual rankings were collected in a follow-up process via emailed spreadsheets. For each of L and S, three values were collected: Lower Bound, Best Guess, and Upper Bound. The Lower-Upper Bound ranges and the spreads among experts can be interpreted to yield rough confidence measures.
Based on experts’ responses, FEPs were ranked in terms of their L*S risk levels. FEP rankings were determined from individual (not consensus or averaged) results, thus no high-risk responses were damped out. The higher-risk FEPs were used to generate one or more concrete, well defined risk-bearing scenarios for each FEP. Any FEP scored by any expert as having associated risk of at least moderate level–roughly the top half of the evaluated list–was used to generate risk scenarios.
Textual risk-response information collected during the FEP evaluation process was augmented after scenarios were defined. Risk responses were then disaggregated into approximately 200 risk-response actions, which were regrouped into 30 areas of function or expertise. Each “risk response action group” has been assigned to a specific individual to organize and confirm its execution.
Responses to the higher identified risks have influenced plans for reservoir characterization, monitoring, communications, and coordination among project member organizations. Uncertainties in geologic parameters are being addressed through sensitivity analysis in reservoir simulations and through further data acquisition. Because the risk-bearing scenarios are linked to formal, assigned risk-response actions, they provide a basis for tracking and managing risk throughout the project.
Important benefits of face-to-face, ”live” expert elicitation include team formation and the subsequent establishment of project understandings, roles, and working relationships. Interchanges that occur during a FEPs-based elicitation process can stimulate conceiving and considering risk-bearing chains of events, and can help avoid blind spots that could occur if all scenarios were pre-defined. Through using both group-consensus and individual values, the IBDP risk management process benefited from group discussion and calibration, while avoiding the impairment of independent judgment that can arise through group dynamics. Further developments in collecting, analyzing, and managing the risk-evaluation data are expected to streamline risk management tasks, and to provide suitable risk management frameworks that are more broadly applicable to geological sequestration.