Scrivener Publishing
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Salem, MA 01970

Scrivener Publishing Collections Editors

James E. R. Couper      Richard Erdlac
Rafiq Islam Pradip Khaladkar
Vitthal Kulkarni Norman Lieberman
Peter Martin W. Kent Muhlbauer
Andrew Y. C. Nee S. A. Sherif
  James G. Speight

Publishers at Scrivener
Martin Scrivener (martin@scrivenerpub1ishing.com)
Phillip Carmical (pcarmical@scrivenerpublishing.com)

This book is dedicated to Wu Ying, my loving wife.
She is the love of my life and a constant source of inspiration.

Contents

Preface

Acknowledgement

Chapter 1 Introduction

1.1 Acid Gas

1.1.1 Hydrogen Sulfide

1.1.2 Carbon Dioxide

1.2 Anthropogenic CO2

1.3 Flue Gas

1.3.1 Sulfur Oxides

1.3.2 Nitrogen Oxides

1.4 Standard Volumes

1.4.1 Gas Volumes

1.4.2 Liquid Volumes

1.5 Sulfur Equivalent

1.6 Sweetening Natural Gas

1.6.1 Combustion Process Gas

1.6.1.1 Post-Combustion

1.6.1.2 Pre-Combustion

1.7 Acid Gas Injection

1.8 Who Uses Acid Gas Injection?

1.8.1 Western Canada

1.8.2 United States

1.8.3 Other Locations

1.8.4 CO2 Flooding

1.9 In Summary

References

Appendix 1A Oxides of Nitrogen

Appendix 1B Oxides of Sulfur

Chapter 2 Hydrogen Sulfide and Carbon Dioxide

2.1 Properties of Carbon Dioxide

2.2 Properties of Hydrogen Sulfide

2.3 Estimation Techniques for Physical Properties

2.3.1 Thermodynamic Properties

2.3.1.1 Ideal Gas

2.3.1.2 Real Gas

2.3.2 Saturated Liquid and Vapor Densities

2.3.2.1 Liquids

2.3.2.2 Corresponding States

2.3.3 Thermodynamic Properties

2.3.4 Transport Properties

2.3.4.1 Low Pressure Gas

2.3.4.2 Gases Under Pressure

2.3.4.3 Liquids

2.3.5 Viscosity Charts

2.4 Properties of Acid Gas Mixtures

2.4.1 Thermodynamic Properties

2.4.1.1 Corresponding States

2.4.2 Transport Properties

2.4.3 Word of Caution

2.5 Effect of Hydrocarbons

2.5.1 Density

2.5.2 Viscosity

2.6 In Summary

References

Appendix 2A Transport Properties of Pure Hydrogen Sulfide

2A.1 Viscosity

2A.1.1 Liquid

2.A.1.2 Vapor

2A.2 Thermal Conductivity

References

Appendix 2B Viscosity of Acid Gas Mixtures

2B.1.1 Correcting for High Pressure

2B.1.2 Carbon Dioxide

2B.1.3 Generalization

2B.1.4 Mixtures

2B.1.5 Final Comments

References

Appendix 2C Equations of State

2C.1.1 Soave-Redlich-Kwong Equation of State

2C.1.2 Peng-Robinson Equation of State

2C.1.3 The Patel-Teja Equation of State

Chapter 3 Non-Aqueous Phase Equilibrium

3.1 Overview

3.2 Pressure-Temperature Diagrams

3.2.1 Pure Components

3.2.2 Mixtures

3.2.3 Binary Critical Points

3.2.4 Effect of Hydrocarbons

3.2.4.1 Methane

3.2.4.2 Ethane and Propane

3.2.4.3 Butane and Heavier

3.2.4.4 In Summary

3.3 Calculation of Phase Equilibrium

3.3.1 Equations of State

3.3.2 K-Factor Charts

3.4 In Summary

References

Appendix 3A Some Additional Phase Equilibrium Calculations

3A.1.1 Hydrogen Sulfide + Hydrocarbons 86

3A.1.2 Carbon Dioxide + Hydrocarbons

3A.1.3 Multicomponent Mixtures

References

Appendix 3B Accuracy of Equations of State for VLE in Acid Gas Mixtures

References

Chapter 4 Fluid Phase Equilibria Involving Water

4.1 Water Content of Hydrocarbon Gas

4.2 Water Content of Acid Gas

4.2.1 Carbon Dioxide

4.2.2 Hydrogen Sulfide

4.2.3 Practical Representation

4.2.3.1 In Summary

4.3 Estimation Techniques

4.3.1 Simple Methods

4.3.1.1 Ideal Model

4.3.1.2 McKetta-Wehe Chart

4.3.1.3 Maddox Correction

4.3.1.4 Wichert Correction

4.3.1.5 Alami et al.

4.3.2 Advanced Methods

4.3.2.1 AQUAlibrium

4.3.2.2 Other Software

4.4 Acid Gas Solubility

4.4.1 Henry’s Law

4.4.2 Solubility in Brine

4.4.2.1 Carbon Dioxide in NaCl

4.4.2.2 Hydrogen Sulfide in NaCl

4.4.2.3 Mixtures of Gases

4.4.2.4 Effect of pH

4.5 In Summary

References

Appendix 4A Compilation of the Experimental Data for the Water Content of Acid Gas

References

Appendix 4B Comments on the Work of Selleck et al.

Appendix 4C Density of Brine (NaCl) Solutions

Chapter 5 Hydrates

5.1 Introduction to Hydrates

5.2 Hydrates of Acid Gases

5.3 Estimation of Hydrate Forming Conditions

5.3.1 Shortcut Methods

5.3.2 Rigorous Methods

5.4 Mitigation of Hydrate Formation

5.4.1 Inhibition with Methanol

5.4.2 Water-Reduced Cases

5.4.2.1 Carbon Dioxide

5.4.2.2 Dehydration

5.4.2.3 To Dehydrate or Not to Dehydrate? – That is the Question!

5.4.3 Application of Heat

5.4.3.1 Line Heaters

5.4.3.2 Heat Tracing

5.4.3.3 Final Comment

5.5 Excess Water

5.6 Hydrates and AGI

5.7 In Summary

References

Chapter 6 Compression

6.1 Overview

6.2 Theoretical Considerations

6.3 Compressor Design and Operation

6.4 Design Calculations

6.4.1 Compression Ratio

6.4.2 Ideal Gas

6.4.3 Efficiency

6.4.4 Ratio of the Heat Capacities

6.5 Interstage Coolers

6.5.1 Design

6.5.2 Pressure Drop

6.5.3 Phase Equilibrium

6.6 Compression and Water Knockout

6.6.1 Additional Cooling

6.7 Materials of construction

6.8 Advanced design

6.8.1 Cascade

6.8.2 CO2Slip

6.9 Case studies

6.9.1 Wayne-Rosedale

6.9.2 Acheson

6.9.3 West Pembina

6.10 In Summary

References

Appendix 6A Additional Calculations

Chapter 7 Dehydration of Acid Gas

7.1 Glycol Dehydration

7.1.1 Acid Gas Solubility

7.1.2 Desiccant

7.2 Molecular Sieves

7.2.1 Acid Gas Adsorption

7.3 Refrigeration

7.3.1 Selection of Inhibitor

7.4 Case Studies

7.4.1 CO2 Dehydration

7.4.2 Acid Gas Dehydration

7.4.2.1 Wayne-Rosedale

7.4.2.2 Acheson

7.5 In Summary

References

Chapter 8 Pipeline

8.1 Pressure Drop

8.1.1 Single Phase Flow

8.1.1.1 Friction Factor

8.1.1.2 Additional Comments

8.1.2 Two-Phase Flow

8.1.3 Transitional Flow

8.2 Temperature Loss

8.2.1 Carroll’s Method

8.3 Guidelines

8.4 Metering

8.5 Other Considerations

8.6 In Summary

References

Appendix 8A Sample Pipeline Temperature Loss Calculation

8A.1 AQUAlibrium 3.0

8A.1.1 Acid Gas Properties

8A.1.1.1 Conditions

8A.1.1.2 Component Fractions 212

8A.1.1.3 Phase properties

8A.1.1.4 Warnings

Chapter 9 Injection Profiles

9.1 Calculation of Injection Profiles

9.1.1 Gases

9.1.1.1 Ideal Gas

9.1.1.2 Real Gas

9.1.2 Liquids

9.1.3 Supercritical Fluids

9.1.4 Friction

9.1.5 AGIProfile

9.2 Effect of Hydrocarbons

9.3 Case Studies

9.3.1 Chevron Injection Wells

9.3.1.1 West Pembina

9.3.1.2 Acheson

9.3.2 Anderson Puskwaskau

9.4 Other Software

9.5 In Summary

References

Appendix 9A Additional Examples

Chapter 10 Selection of Disposal Zone

10.1 Containment

10.1.1 Reservoir Capacity

10.1.2 Caprock

10.1.3 Other Wells

10.2 Injectivity

10.2.1 Liquid Phase

10.2.2 Gas Injection

10.2.3 Fracturing

10.2.4 Horizontal Wells

10.3 Interactions With Acid Gas

10.4 In Summary

References

Chapter 11 Health, Safety and The Environment

11.1 Hydrogen Sulfide

11.1.1 Physiological Properties

11.1.2 Regulations

11.1.3 Other Considerations

11.2 Carbon Dioxide

11.2.1 Physiological Properties

11.2.2 Climate Change

11.2.3 Other Considerations

11.3 Emergency Planning

11.3.1 Accidental Releases

11.3.2 Planning Zones

11.3.3 Other Considerations

11.3.3.1 Sour vs. Acid Gas

11.3.3.2 Wind

11.3.3.3 Carbon Dioxide

11.3.3.4 Sensitive Areas

References

Chapter 12 Capital Costs

12.1 Compression

12.1.1 Reciprocating Compressor

12.1.2 Centrifugal

12.2 Pipeline

12.3 Wells

12.4 In Summary

References

Chapter 13 Additional Topics

13.1 Rules of Thumb

13.1.1 Physical Properties

13.1.2 Water Content

13.1.3 Hydrates

13.1.4 Compression

13.1.5 Pipelines

13.1.6 Reservoir

13.2 Graphical Summary

13.2.1 Pressure-Temperature

13.2.2 Water Content

13.2.3 Operation

13.2.4 Summary

13.3 The Three Types of Gas

13.3.1 Example Gases

Index

Preface

Acid gas injection (AGI) has become a mature technology for disposing of acid gas, a mixture of CO2 and H2S. AGI is particularly useful for small producers who have few options for dealing with the H2S. Larger producers, however, have seen the value in AGI as well and the industry has discovered that AGI is an environmentally friendly solution to a difficult problem.

This book presents the art, the science, and the engineering aspects of AGI, and to present it in a manner that is accessible to the average engineer. It begins with a discussion of the basic data and models for designing an injection scheme. In particular it is important that those working in the field have a good understanding of the phase equilibria involved. Most of the operational problems are related to the formation of an unwanted phase. Admittedly, some of these concepts are a little complicated, and it is a challenge to present them in a form that is comprehensible to a wide audience.

Next the engineering aspects are presented. These include the design of the compressor and pipeline and in particular what makes them different from standard designs. Finally, some of the subsurface aspects are reviewed. Admittedly, the focus of this book is the surface aspects of AGI, but the subsurface aspects cannot be overlooked, even by the process engineer.

Hopefully, those involved in the emerging field of CO2 sequestration will note the similarities and take the information presented here and apply it to their projects. Lessons learned in AGI can be exported to the technology of carbon sequestration.

Acknowledgements

There are many people to thank when one writes a book. The first, and certainly the most important, is my employer Gas Liquids Engineering, and in particular the company principals Doug MacKenzie and Jim Maddocks but also my colleague Peter Griffin. They provided me the opportunity to present the course and much of the time to write the manuscript.

In addition, through my job at Gas Liquids Engineering, I have had the chance to work on many acid gas injection projects throughout the world. Some of these were just studies that have not yet come to fruition, but others have been operating for many years. Much of what is presented in this book has come from lessons learned from working on those projects.

Alan Mather has been my long time friend and mentor. He is an important source of information, often from obscure sources. Plus his lab is the source of much of the useful information in this field. The research studies of his group are vital to the advancement of many fields in the gas processing.

This book is based on a course on acid gas injection that I have presented throughout the world. Feedback from the attendees over the years has greatly improved the quality and content of both the course and this book. The acid gas injection course has also been presented in Chinese and Polish. I have received excellent feedback from Eugene Grynia, my Polish translator, and Ying Wu, my Chinese translator.

1

Introduction

Although many gases are natural (air, for example), the term “natural gas” refers to the hydrocarbon-rich gas that is found in underground formations. These gases are organic in origin, and thus along with oil, coal, and peat are called “fossil fuels.” Time and the effects of pressure and temperature have converted the originally living matter into hydrocarbon gases that we call natural gas.

Natural gas is largely made up of methane but also contains other light hydrocarbons, typically ethane through hexane. In addition, natural gas contains inorganic contaminants – notably hydrogen sulfide and carbon dioxide, but also nitrogen and trace amounts of helium and hydrogen.

The formations and the gas contained therein are almost always associated with water, and thus the gas is usually water-saturated. The water concentration depends on the temperature and pressure of the reservoir and to some extent on the composition of the gas.

Natural gas that contains hydrogen sulfide is referred to as “sour.” Gas that does not contain hydrogen sulfide, or at least contains hydrogen sulfide but in very small amounts, is called “sweet.”

Contaminants in natural gas, like hydrogen sulfide and carbon dioxide, are usually removed from the gas in order to produce a sales gas. Hydrogen sulfide and carbon dioxide are called “acid gases” because when dissolved in water they form weak acids.

Hydrogen sulfide must be removed because of its high toxicity and strong, offensive odor. Carbon dioxide is removed because it has no heating value. Another reason these gases must be removed is because they are corrosive. In Alberta, sales gas must typically contain less than 16 ppm1 hydrogen sulfide and less than 2% carbon dioxide. However, different jurisdictions have different standards.

Once removed from the raw gas, the question arises as to what should be done with the acid gas. If there is a large amount of acid gas, it may be economical to build a Claus-type sulfur plant to convert the hydrogen sulfide into the more benign elemental sulfur. Once the H2S has been converted to sulfur, the leftover carbon dioxide is emitted to the atmosphere. Claus plants can be quite efficient, but even so, they also emit significant amounts of sulfur compounds. For example, a Claus plant processing 10 MMSCFD of H2S and converting 99.9% of the H2S into elemental sulfur (which is only possible with the addition of a tail gas clean up unit) emits the equivalent of 0.01 MMSCFD or approximately 0.4 ton/day of sulfur into the atmosphere. Note that there is more discussion of standard volumes and sulfur equivalents later in this chapter.

For small acid gas streams, Claus-type sulfur plants are not feasible. In the past, it was permissible to flare small amounts of acid gas. However, with growing environmental concerns, such practices are being legislated out of existence.

In the natural gas business, acid gas injection has quickly become the method of choice for the disposal of such gases. Larger producers are also considering injection because of the volatility of the sulfur markets.

1.1 Acid Gas

As noted earlier, hydrogen sulfide and carbon dioxide are called acid gases. When dissolved in water they react to form weak acids.

The formation of acid in water is another reason that acid gases are often removed from natural gas. The acidic solutions are very corrosive and require special materials to handle them.

On the other hand, the acidity of the acid gases is used to our advantage in processes for their removal.

1.1.1 Hydrogen Sulfide

Hydrogen sulfide is a weak, diprotic acid (i.e., it undergoes two acid reactions). The ionization reactions are as follows:

The subscript (aq) indicates that the reaction takes place in the aqueous (water-rich) phase.

It is the H+ ion that makes the solution acidic. Hydrogen sulfide is diprotic because it has two reactions that both form the hydrogen ion. Furthermore, when hydrogen sulfide is dissolved in water it exists as three species – the molecular form (H2S) and the two ionic forms: the bisulfide ion (HS) and the sulfide ion (S2−).

The measure of how far these reactions proceed is the equilibrium ratios. For our purposes, these ratios are as follows:

where the square brackets indicate the concentration of each species. These relations are valid only if the concentration is small. The fact that these ratios are so small indicates that these reactions do not proceed very far, and thus, in an otherwise neutral solution, most of the hydrogen sulfide is found in the solution in the molecular form. The concentration of the ionic species is greatly affected by the presence of an alkaline and to some extend the presence of an acid. And since hydrogen sulfide is an acid, the effect of an alkaline is very significant.

At 25°C and 101.325 kPa (1 atm) the distribution of the various species in the aqueous solution can be calculated from the solubility and the equilibrium ratios. The distribution is:

The units of concentration used here are molality or moles of species per kg of solvent (water).

1.1.2 Carbon Dioxide

Carbon dioxide is also a weak diprotic acid, but the reactions for CO2 are slightly different. The first reaction is a hydrolysis (a reaction with water):

The second is a simple acid formation reaction:

Again, these reactions take place in the aqueous phase. The carbon dioxide exists in three species in the aqueous phase – the molecular form CO2, and two ionic forms: the bicarbonate ion, also call the hydrogen carbonate ion (HCO3), and the carbonate ion (CO32−).

The equilibrium ratios for these reactions are:

Again, the square brackets are used to indicate the concentration of the various species. As with hydrogen sulfide, these ratios are very small, and thus in an otherwise neutral solution most of the carbon dioxide exist in the molecular form. At 25°C and 101.325 kPa (1 atm) the distribution of the various species in the aqueous solution is:

The pH of the CO2 solution is slightly less than that for H2S even though the solubility of CO2 is significantly less. This is because more of the carbon dioxide ionizes, which in turn produces more of the H+ ion – the acid ion.

1.2 Anthropogenic CO2

The disposal of man-made carbon dioxide into the atmosphere is becoming an undesirable practice. Whether or not one believes that CO2 is harmful to the environment has almost become a moot point. The general consensus is that CO2 is contributing to global climate change. Furthermore, it is clear that legislators all around the world believe that it is a problem. In some countries there is a carbon tax applied to such disposal. Engineers will increasingly be faced with the problem of disposing of CO2.

Some of the technologies for dealing with this CO2 are the same as acid gas injection, and thus they will be discussed here as well.

1.3 Flue Gas

Flue gas, as used here, is the byproduct of the combustion of fuels. Typically the fuels of concern here are natural gas, oil (and distillates from oil such as gasoline), coal, wood, etc.

Combustion is a process involving oxygen. However, air is composed of only 21% oxygen, which is required for combustion, and 79% inerts, mostly nitrogen. Thus for every mole of oxygen consumed in the combustion of a paraffin hydrocarbon, more than 9.5 moles of air must be supplied.

The combustion of a carbon-based fuel (coal, natural gas, or oil) produces a gaseous byproduct called flue gas. First consider the combustion of a paraffin hydrocarbon.

For example, the reaction for the combustion of methane is:

So the combustion of a hydrocarbon releases carbon dioxide and water. In addition, the combustion of one mole of methane consumes 2 moles of oxygen.

Table 1.1 summarizes the amount of oxygen and air required for the combustion of several light paraffin hydrocarbons. It is interesting to note that as the hydrocarbon becomes larger, the amount of carbon dioxide produced by the combustion process also increases.

Table 1.1 Air requirements for the combustion of one mole of various paraffin fuels.

Table 1.2 Approximate flue gas composition from the combustion of various paraffin hydrocarbon fuels (water-free basis).

From table 1.2 we can see that the flues gas is more than three quarters nitrogen and only about 20% carbon dioxide. In addition, when 15% excess air is used in the combustion process, then the flue gas also includes slightly more than 2.5% oxygen. As noted below, the flue gas will also include small amounts of oxides of nitrogen and oxides of sulfur.

It is probably undesirable to attempt to inject the entire flue gas stream. As we shall see, the cost of a disposal stream is directly related to the volume of gas injected.

In some cases, there is insufficient oxygen and one gets incomplete combustion to form carbon monoxide:

Carbon monoxide is a very dangerous chemical. It is gaseous at room conditions, and it is colorless, odorless, and highly toxic. It is often referred to as the “silent killer.”

1.3.1 Sulfur Oxides

Most of the fuels we use contain some sulfur compounds. Even “sweet” natural gas has some sulfur in it. These sulfur compounds burn to form the so-called sulfur oxides – SOx: sulfur dioxide (SO2) and sulfur trioxide (SO3). At room conditions, pure SO2 is a gas but pure SO3 is a liquid (boiling pt 45°C). Like carbon dioxide and hydrogen sulfide, these compounds form acids when dissolved in water.

More properties of the sulfur oxides are provided in the appendix.

1.3.2 Nitrogen Oxides

There are two sources of nitrogen in the combustion process. Some fuels, notably coal and heavier oil, contain nitrogen compounds. When these fuels are burned they release oxides of nitrogen. The other source of nitrogen is the high temperature reaction of atmospheric oxygen and nitrogen.

More properties of the oxides of nitrogen are given in the appendix.

1.4 Standard Volumes

In the petroleum business it is common to report flow rates in standard volumes per unit time.

1.4.1 Gas Volumes

The common units for the flow rate of a gas stream are MMSCFD, Sm3/d or Nm3/d. These are equivalent to the following number of moles of gas:

The use of the prefix symbol M is a cause of much confusion in the natural gas business. In standard SI Units, M means mega and has the multiplier 106. Therefore, in SI Units, 1 MJ is one mega-joule or one million Joules. In American Engineering Units, the M is taken from Roman numerals, where M means one thousand. Thus 1 MSCF is one thousand standard cubic feet and not one million standard cubic feet. To indicate one million, two M’s are used (1,000 × 1,000 = 1,000,000), so one million standard cubic feet is denoted 1 MMSCF. In spite of the confusion, this notation will be used in this work.

1.4.2 Liquid Volumes

In the oil business, a barrel is a volume exactly 42 USgal, which is equivalent to 5.61458 ft3 or 158.99 L. The density of a liquid is affected by the temperature, not as significantly as a gas, but it changes nonetheless. Therefore, a standard barrel is the volume occupied at 60°F (15.56°C).

By definition (GFA, 1996) we have:

So one standard barrel (usually referred to as a barrel) of liquefied acid gas has a mass of about 2801b or 127 kg. It will weigh slightly less due to the presence of light hydrocarbon in the mixture. The conversion from standard barrels to standard meters is 1 bbl = 0.158 987 Sm3 or 6.2898 bbl = 1 Sm3.

Furthermore, as was given earlier, 1 MMSCF is 1.195 × 106 mol, so 1 MMSCFD of compressed H2S is equal to 40 728 kg/d, which equals 320 bpd. Similarly for CO2 1 MMSFD is 405 bpd. Although 1 barrel of H2S has approximately the same mass as 1 bbl of CO2, there is a significant difference when converting from standard cubic feet. This is because the molecular mass of CO2 is significantly larger than that of H2S. So as an approximation, 1 MMSCFD of acid gas is equal to approximately 350 bbl of liquefied acid gas.

1.5 Sulfur Equivalent

It is common to express the sulfur content of a stream in terms of sulfur equivalent. This assumes that all of the hydrogen sulfide in a gas stream is converted to elemental sulfur via the reaction:

According to this reaction, 1 mole of hydrogen sulfide is converted to one mole of S.

First you must determine the number of moles of hydrogen sulfide in the gas stream, as discussed earlier. Therefore to obtain the molar flow rate of H2S in the gas stream, multiply the flow rate by the molar equivalent given above and then multiply by the mole fraction H2S in the stream.

From the chemical reaction, one mole of H2S produces one mole of S. Therefore:

Finally, use the molar mass of sulfur, 32.066 g/mol, to convert to a molar flow rate in g/day. This is converted to tonne/day using the conversion factor 106 g = 1t.

The more common form of sulfur is actually S8. Therefore the chemically more correct version of the reaction is:

However, when we express the flow rate on a mass basis it is independent of the form of the elemental sulfur. Other species of elemental sulfur also exist, but if the sulfur rate is expressed on a mass basis, it does not matter which species you assume for the elemental sulfur.

Examples

1.1 An acid gas stream of 1 MMCSFD is 75% H2S. What is the sulfur equivalent for this stream?

Answer: Using equation (1.11) yields:

This is equivalent to 31.6 ton/day4.

1.2 An acid gas stream of 20 × 103 Sm3/day is 5% H2S. What is the sulfur equivalent for this stream?

Answer: Again using equation (1.11) yields:

1.6 Sweetening Natural Gas

Although many processes are available to sweeten natural gas – that is to remove the acid gases – those based on alkanolamines are the most common.

Alkanolamines are ammonia-like organic compounds. When dissolved in water they form weak bases. The bases react with the acids formed when H2S and CO2 dissolve in water. This acid-base reaction greatly enhances the solubility of the acid gases. Because the alkanolamines are weak bases, the process can be reversed. When the solutions are heated, the acid gases are liberated and the solvent regenerated.

The process for absorbing acid gas takes place in two stages: (1) absorption and (2) regeneration. The absorption takes place in a column where the sour gas is contacted with the lean solvent. The rich solvent is sent to a second column where the solvent is regenerated. Heat is applied to the system via a reboiler and the overheads are condensed, typically in an aerial cooler. The solvent regeneration is done not only at higher temperature, but also at lower pressure. Figure 1.1 is a schematic of the process.

Other processes are available for sweetening natural gas, but the alkanolamine systems are by far the most common. More discussion about processes for sweetening natural gas can be found in Kohl and Nielsen (1997).

1.6.1 Combustion Process Gas

In the carbon capture world there are two approaches to capturing the carbon dioxide: 1. post-combustion and 2. pre-combustion. The post-combustion approach is to take the CO2 from the combustion process, purify it, and then inject it. In the pre-combustion approach, the carbon is removed from the fuel before combustion. These two approaches are discussed in the following sections.

Figure 1.1 A simplified schematic diagram of the process for removing acid gas from natural gas.

1.6.1.1 Post-Combustion

As was mentioned earlier, it is probably wise to separate the carbon dioxide from the flue gas and inject only a CO2-rich stream. This is the so-call “capture” part of the carbon capture and storage.

At first look, we should be able to achieve this using a process similar to those used for sweetening natural gas. However, there are several factors that complicate this.

  1. High Temperature – Since the source of the stream is a combustion process, this stream will be at high temperature. It may be necessary to cool the flue gas stream before sending it to the treating process.

  2. Low Pressure – The flue gas stream is produced at near atmospheric pressure. At a minimum, blower will probably have to be used to raise the pressure of the gas to a sufficient level such that it can flow through the process equipment.

    In addition, and perhaps more importantly, the absorption process is favored by higher pressure.

    The low pressure also means that there is a very high actual flow rate. This means that larger diameter towers are required for the absorption process.

  3. Solvent Losses – The combination of the high temperature and low pressure noted above result in significant solvent losses. Some extra process, such as a residue gas scrubber, is needed to reduce these losses.

  4. Impurities – There are two key impurities in the flue gas: oxygen and oxides of sulfur.

    1. Sulfur Oxides – Sulfur oxides are also acid gases in as much as they form acidic solution in water. However they are much stronger acids than H2S or CO2 and for this reason they react irreversibly with most bases, including the alkano-lamines commonly used to sweeten natural gas streams.

    2. Oxygen – Oxygen is also known to cause problems in the alkanolamine process.

Chemical vendors and engineering companiesare working diligently to overcome these and other problems associated with the decar-bonation of flue gas.

1.6.1.2 Pre-Combustion

The hydrocarbon can be converted to hydrogen and carbon monoxide using the steam reforming reaction.

Although the reaction given is for methane, other hydrocarbons can be substituted instead and the products remain hydrogen and carbon monoxide. The carbon monoxide can be further reacted with water via the water-shift reaction:

which produces additional hydrogen. The net result of these two reactions is a stream that contains hydrogen and carbon dioxide. The hydrogen and carbon dioxide are separated, and one obtains a high-pressure carbon dioxide stream and a hydrogen stream that can be used as a fuel. The combustion of hydrogen is a relatively clean process producing only water as a by-product.

The reactions given above are not new technology. This is the most commonly used process for producing hydrogen and is used in most petroleum refineries that require hydrogen.

The carbon dioxide from this process can then be injected. Since this is a high pressure stream, it requires only a fraction of the power to compress the low pressure stream that results from the post-combustion separation.

A project like this was proposed by a company lead by BP in Peterhead, Scotland. The CO2 was to be injected into the offshore Miller field, which had reached the end of its productive life. However, it was canceled largely due to delays by the government regarding incentives.

Another project of this type lead by Shell and Statoil in Tjeldbergodden, Norway, was also abandoned because it was deemed uneconomic.

1.7 Acid Gas Injection

With growing environmental concerns, the disposal of small quantities of acid gas is a problem. In the past, producers could flare these acid gases; however, in many jurisdictions this is no longer the case. New and stricter regulations are curbing the disposal of sulfur compounds into the atmosphere. Usually a sulfur plant is not an option for these small producers. Thus, other methods must be developed to deal with the unwanted acid gas.

Acid gas injection is quickly becoming the method of choice for disposing of these gases. The acid gas is compressed and injected, usually into a non-producing formation. Recently though, some have investigated the value of using the compressed acid gas as a part of a miscible flood scheme. Such a scheme is usually not recommended because it will lead to a build-up of acid gas and ultimately an increased the load on the amine unit. The goal is to dispose of the acid gas, not necessarily to recycle it.

In addition, with the current depressed market for sulfur, some larger producers are considering acid gas injection as an alternative for dealing with unwanted sulfur.

Injection of the acid gas also eliminates the release of carbon dioxide and sulfur oxides to the atmosphere. Sulfur plants emit all of the CO2 to the atmosphere and even the most efficient emit small amounts of SOx.