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SEMINAR
                             ON

   COAL BED METHANE:
 A STRATEGIC OVERVIEW
                          Presented by

                    Rupam Sarmah
                      6TH SEMESTER
               PETROLEUM ENGINEERING
                      D.U.I.E.T




          In fulfillment for the Completion
                               Of
                 WINTER INTERNSHIP
             DECEMBER 26TH, 2011 – JANUARY 15TH, 2012
                               In



RANCO ENERGY PROJECTS PRIVATE LIMITED, MUMBAI
ABSTRACT
Currently, gas demand exceeds supply by 30
per cent. While the demand for natural gas in
India is 118 million metric standard cubic
meter per day (MMSCMD), the current supply
from various sources is 80 MMSCMD, leaving
a shortfall of 28 MMSCMD. That deficiency
can be covered by CBM production.



                                                2
OVERVIEW OF COAL
      AND
  CBM RESERVES
BENEATH THE SURFACE…




Global coal distribution   Identified CBM basins
COAL : World’s number two source of primary
                energy with 27% of demand
        According to the baseline scenario used by the IEA in its World
       Energy Outlook 2009, the consumption of coal is expected to rise
       by 1.9% per year between now and 2030, by which time it should
            account for 29% of global primary energy requirements




Distribution of recoverable coal reserves     CBM Reserves (Gas in Place) by country
A GENESIS MODEL OF COAL




PEATIFICATION      Geochemical Transformation   COALIFICATION
CBM RESERVOIR
 PROPERTIES
A Comparative Analysis:
 GAS STORAGE: Instead of occupying void spaces as a free gas
between sand grains, the methane is held to the solid surface of the coal by
adsorption in numerous micro pores. The adsorption mechanism creates
the paradox of high gas storage in a reservoir rock of porosity less than
2.5%.

 GAS FLOW:
                                              • Mass transport through solid
                                              coal (micro pore structure) is
                                              governed by Ficks law of
                                              diffusion,



                                               • Mass transport through the
                                               fracture system is governed by
                                               Darcy’s law,
 GAS PRODUCTION: Dictated by the pressure-lowering process of dewatering, Coal
beds feature production rates of methane that initially increase and then slowly decline as
gas production continues over a long period.
 GAS CONTENT: Gas adsorbed on the coal cannot be detected on geophysical logs as
in a conventional reservoir, and the gas amount must be determined by volumetric
calculations based on coring data. Gas content of coals may increase with depth, however,
due to the positive influence of pressure on adsorptive capacity rather than the
compressibility of the gas.
 WATER PRODUCTION: The formation waters generated from natural fractures in
coal must be removed before methane can be desorbed in the early production life of a
well.
ROCK PROPERTY: Conventional oil and gas formations are inorganic. Organic
formations contain CBM; these formations may contain about 10–30% inorganic ash.
HYDROFRACTURING: The coal usually has low permeability and depends on natural
fractures to act as gas and liquid conduits. Without hydraulic fracturing, these low-
permeability coals are usually commercially non-productive.
STRESS DEPENDENT PERMEABILITY: The permeability is stress-dependent, so,
whether the coals exhibit a low permeability or exhibit an extensive, unstressed network of
fractures with high permeability is a critical parameter in any decision to invest in a CBM
process.
KEY PARAMETERS IN CBM RESERVOIRS
GAS CONTENT : Standard volume of gas per unit weight of coal or
rock. (scf/ton)

Estimation of gas content:

• Desorbed gas : Estimated by the
“Direct Method” or Canister desorption test.
• Lost gas : Volume of the gas that desorbs from
 the sample during the recovery process before
the core sample can be sealed in a desorption
 canister and is estimated by analyzing the data
obtained during the canister desorption tests.
•Residual gas : Gas that remains sorbed on the sample at the conclusion
of the canister desorption test and is estimated by crushing the entire
desorption sample to smaller than a 60 mesh grain size and measuring the
gas volume released at the reservoir temperature.

TOTAL GAS VOLUME ═ DESORBED GAS + LOST GAS + RESIDUAL GAS
RESERVOIR THICKNESS:

• Gross coal thickness usually can be determined accurately with wire line
logs (Generally, Open-hole density logs).
• The gross reservoir thickness is commonly computed by summing the
thicknesses of the intervals having densities less than a cut off value
generally equal to the coal ash density.
• Determining net thickness is complicated but it can be estimated by using
Resistivity logs, Well tests, Production logs, or Zonal isolation tests.

 LANGMUIR VOLUME (VL) : Maximum amount of gas that can be
 adsorbed on a piece of coal at infinite pressure. This value is
 asymptotically approached by the isotherm as the pressure increases.
 Typically, the units for the Langmuir volume parameter (VL) are scf/ton.

 LANGMUIR PRESSURE (PL) : This parameter affects the shape of
 the isotherm. The Langmuir pressure is the pressure at which half of the
 Langmuir volume can be adsorbed.
• Relationship used to represent the sorption mechanism in coal bed methane
reservoir is given as:

Where,

Gs = Gas storage capacity, SCF/ton; P = Pressure, psia; V L = Langmuir volume constant,
SCF/ton; PL = Langmuir pressure constant, psia
• The impact of VL and PL on the shape of the isotherm curve:
SORPTION TIME : Sorption time (τ ) is the time required to desorb 63.2 percent
of the initial gas volume.
Where,
σ = matrix shape factor, dimensionless
D = matrix diffusivity constant, sec-1

As the coal rank increases, τ also increases. Greater the value of τ, greater will be
the time taken by gas for desorption

PERMEABILITY : It is the volume of interconnected pores in a rock.

                                          Primary Permeability (Cleat)
Permeability of CBM Reservoir

                                                 Secondary Permeability (Pore)
POROSITY : In CBM reservoirs, porosity is saturated with water.
So, greater porosity will lead to greater water production and vice- versa.
Thus, unlike conventional reservoirs, high porosity is unfavourable
for CBM reservoirs.
                                          Micro-porosity of coal
FLOWING BOTTOM HOLE PRESSURE : Pressure at the bottom of the
hole

Calculation : Let x be the mean depth of perforation from the surface in meter.
             Let y be the water level in annulus from the surface in meter.

Then,
         BHP=(x-y)*3.28*0.433        in psi.

Where,
0.433 is the water pressure gradient in psi/ft.

The aim of production operations is to bring
 the level of water below the perforation so
that BHP decreases. When flowing BHP is
decreased, drawdown will increase and
correspondingly production will also increase.
DEPTH :

As depth increases, coal rank increases, increasing gas content of coal, but
at the same time decreasing permeability. Thus, the depth at which
optimum value of gas content and permeability can be expected ranges
between 700 to 1000 m.

DENSITY OF COAL :

If coal density is low, desorption will take place easily and vice-versa.
COALBED METHANE –
A RESERVOIR APPROACH
Coalbed methane is stored in four ways:

As free gas within the micro pores (pores with a diameter of less
than .0025 inches) and cleats (sets of natural fractures in the coal);

 As dissolved gas in water within the coal;

 As adsorbed gas held by molecular attraction on surfaces of
macerals (organic constituents that comprise the coal mass), micro
pores, and cleats in the coal; and

 As absorbed gas within the molecular structure of the coal
molecules.
Physical and chemical characteristics of plant debris and coals with maturation
The most important characteristics of coal reservoir are:

Coal is a source rock and a reservoir rock. The depositional environment and burial
history of the coal affect the composition of the gas as well as the gas content,
diffusivity, permeability, and gas storage capacity of the coal.
The gas storage mechanism of coal. Most of the gas in coal reservoirs is adsorbed
onto the internal structure of the coal. Because large amounts of gas can be stored at
low pressures in coal reservoirs, the reservoir pressure must be drawn down to a very
low level to achieve high gas recovery.
 The fracture system of coal reservoirs. Coals contain small (typically, several per
inch), regularly-spaced, naturally occurring fractures called face cleats and butt cleats.
Coal reservoirs also contain larger-scale natural fractures.
Coal reservoirs often require pumping water before gas is produced. Typically, water
must be produced continuously from coal seams to reduce reservoir pressure and
release the gas. The cost to treat and dispose of produced water can be a critical factor
in the economics of a coalbed methane project.
The unique mechanical properties of coal. Coal is relatively compressible compared
to the rock in many conventional reservoirs. Thus, the permeability of coal is more
stress- dependent than most reservoir rocks. The friable, cleated nature of coal affects
the success of hydraulic fracturing treatments, and in certain locations allows for
cavitation techniques to dramatically increase production.
STAGES OF PRODUCTION




                        Isotherm showing reservoir initial condition
STAGE   1:   WATER   PRODUCTION:   DEWATERING
                                                           STAGE 2: GAS PRODUCTION: DEWATERED STAGE
STAGE




Isotherm showing dewatering    Water flow rate with time   Isotherm showing amount of gas released Gas flow rate with time
SIMULATING
   CBM
RESERVOIR
Reservoir simulation is the process of integrating geology, petro physics,
reservoir engineering, and production operations to more effectively develop and
produce petroleum resources

DESCRIPTION OF CBM SIMULATORS

Dual porosity nature of coalbed;
Darcy flow of gas and water (i.e., multiphase flow) in the natural fracture system
in coal;
Diffusion of a single gas component (i.e., pure gas) from the coal matrix to the
natural fracture system;
Adsorption/Desorption of a single gas component (i.e., pure gas) at the coal
surface;
Coal matrix shrinkage due to gas desorption.

TYPES OF SIMULATORS

Gas Sorption and Diffusion Simulators
Compositional Simulators
Black-Oil Simulators
DATA NEEDED FOR SIMULATION
GRID SYSTEMS




Three-dimensional Cartesian grid        r-θ-z geometry using Polar Cylindrical coordinates

                    RESULTS FROM COMET-3 (By Advanced Resources International)
GENERAL
TERMINOLOGIES
      &
   GENERAL
  OVERVIEW
                26
Coal bed Methane Terminologies




                                 27
Methane gas from Coal beds:
•Coal bed Methane (CBM) : Methane contained in
coal seams. Often referred to as virgin coal bed
methane, or coal seam gas.

•Coalmine Methane (CMM) : CBM that is released
from the coal seams during coal mining.

•Abandoned Mine Methane (AMM) : Methane that
continues to be released from closed and sealed mines.
May also be referred to as coal mine methane because
the liberated methane is associated with past coal
mining activity.                                     28
GENERAL OVERVIEW
Air Drilling Rig For CBM     PC Pumps running at test wells




Plantation at test                                 Separators installed
    well site                                         at test wells




                           Gas flare                                29
DRILLING OF A
 CBM WELL

                30
31
INTRODUCTION
• Methane can be extracted from the coal
  seams by the process of desorption
  according to which the initial reservoir
  pressure is reduced, by dewatering, to the
                reduced
  critical desorption pressure. Thereafter, the
  coal seams release methane gas as the
  pressure is reduced. The abandonment
  pressure is the lowest pressure at which no
  more methane can be produced. Before an
  exercise of drilling for the purpose of
  methane extraction can be undertaken, an
  estimate of the reserves of coal bed methane
  gas is made.
                                              32
INTRODUCTION (contd.)
• The primary concerns for drilling are
  overpressure of gas/water kicks, high
  permeability which leads to loss of
  circulation fluid, formation damage due to
  the nature of coal and hole sloughing.
• Due to presence of large amount of water
  in the reservoir, often water influx is
  encountered during drilling.


                                               33
INTRODUCTION (contd.)
• However as the gas is found in
  shallower depths, the drilling is cost
  effective in case of CBM than those of
  conventional oil and gas reservoir drilling.
• Normally directional wells are favored for
  CBM reservoir as it can lead to
  production of large amount of gas
  economically and as the depth is not a
  major problem so it is cost effective.
                                                 34
Figure:
Drilling for
methane
gas in coal
       35
DIRECTIONAL DRILLING TECHNOLOGY




                             36
DIRECTIONAL DRILLING TECHNOLOGY (contd.)
•To give an idea of the effectiveness of horizontal
drilling, the U.S. Department of Energy indicates
that using horizontal drilling can lead to an increase
in reserves in place by 2% of the original oil in place.
The production ratio for horizontal wells versus
vertical wells is 3.2 to 1, while the cost ratio of
horizontal versus vertical wells is only 2 to 1.




                                     Figure: Schematic Diagram
                                     of a Directionally Drilled Pre-
                                     Mine Degasification
                                                                 37
TECHNICAL LIMITATIONS AND
  BARRIERS TO IMPLEMENTATION
1. Poor vertical permeability or impermeable
   streaks : Compositionally, coal is often heterogeneous
   with the different coal types generally segregated into
   bands; this can range in thickness from several millimeters
   up to several to tens of centimeters. The degree of cleat
   development varies greatly between these coal types; for
   example vitrain bands tend to be well cleated, while durain
   bands tend to be poorly cleated. The alternation of well
   cleated/poorly cleated bands can substantially reduce
   vertical permeability. Additionally, coal bed often contain
   thin shale beds or stringers which would further limit
   vertical permeability.
                                                           38
TECHNICAL LIMITATIONS AND
 BARRIERS TO IMPLEMENTATION
           (contd.)

2. Variable formation depth and
   thickness : Some coal bed were formed in
  depositional systems which resulted in erratic
  or uneven coal seam deposition. In such cases,
  it would be difficult to keep a horizontal or near-
  horizontal hole in the seam while drilling.



                                                    39
TECHNICAL LIMITATIONS AND BARRIERS
      TO IMPLEMENTATION (contd.)
While it is technically feasible to drill multiple horizontal legs at
different depths, there are some unique characteristics of how coal
bed methane wells are produced which must be considered:
1.First, only one leg of a horizontal well with multiple legs can be
cased. Because coal is often friable, uncased horizontal wellbores will
be prone to sloughing and collapse. The loss of wellbore integrity will
inhibit both the dewatering process and gas production.
2.Second, dewatering operations in horizontal wells are more
complicated than vertical well operations. The majority of coal bed
methane wells in the U.S. are dewatered using conventional "beam" or
"sucker rod" pumps. Formation water is produced by a down-hole
pump, which is operated via an up and down motion imparted to the
rods by the pump jack on the surface. Because the pumping system is
designed to operate in a vertical plane, the connecting rods tend to
break when flexed, as would be the case in a horizontal wellbore.



                                                                      40
PRODUCTION
FROM A CBM
 GAS WELL
             41
42
Figure :
Coal Bed Matrix
illustrating gas
surrounding the
coal bound by
water and rock
          43
INTRODUCTION
Since CBM travels with ground water in coal seams,
extraction of CBM involves pumping available water from
the seam in order to reduce the water pressure that holds
gas in the seam. CBM has very low solubility in water and
readily separates as pressure decreases, allowing it to be
piped out of the well separately from the water. Water
moving from the coal seam to the well bore encourages
gas migration toward the well.

CBM producers try not to dewater the coal seam, but
rather seek to decrease the water pressure (or head of
water) in the coal seam to just above the top of the seam.
However, sometimes the water level drops into the coal
seam.                                                      44
Figure:
CBM Well
Construction
      45
INTRODUCTION (Contd.)
• The production profiles of CBM wells are typically
  characterized by a "negative decline" in the gas rate as
  water is pumped away and gas begins to desorb and
  flow. A dry CBM well does not look very different from a
  standard well, except that the gas rates are lower and
  decline at a much slower rate.




                                Figure: A typical ten-year CBM gas
                                rate forecast, showing a negative
                                decline for the first couple years of
                                production.                       46
INTRODUCTION (Contd.)
•   The methane desorption process follows a curve (of gas content vs. reservoir
    pressure) called a Langmuir isotherm. The isotherm can be analytically
    described by a maximum gas content (at infinite pressure), and the pressure at
    which half that gas exists within the coal. These parameters (called the Langmuir
    volume and Langmuir pressure, respectively) are properties of the coal, and vary
    widely. A coal in Alabama and a coal in Colorado may have radically different
    Langmuir parameters, despite similar other coal properties.




                                                Figure: A typical CBM isotherm      47
INTRODUCTION (Contd.)
• The increasing gas rates seen in a negative decline
  are caused by increasing relative permeability as the
  water saturation around the wellbore decreases. As
  there is less water in the coal cleats, the gas is able
  to flow more and more into the wellbore to be
  produced.




                                   Figure : A set of relative permeability
                                   curves ( As water saturation
                                   decreases, more gas and less water is
                                   produced from the coal.)
                                                                   48
ENHANCED RECOVERY OF CBM
• There are three main methods which can
  induce methane release from coal:
1.Reduce the overall pressure, usually by
  dewatering the formation either through
  pumping or mining
2.Reduce the partial pressure of the methane
  by injecting another inert gas into the
  formation
3.Replace the methane on the surface with
  another compound, such as CO2.
                                               49
ENHANCED RECOVERY OF CBM (contd.)
• The process is implemented by injecting inert gas at one
  location and recovering methane gas at another.




                                                        Figure:
                                                        Gas is injected
                                                        in one well and
                                                        methane is
                                                        recovered in
                                                        another
                                                        well       50
ENHANCED RECOVERY OF CBM (contd.)
    Concerned hazards and methods to
                reduce:
•   Deep unmineable coal formations provide an opportunity to both sequester
    CO2 into coal seams (from anthropogenic sources) and increase the
    production of methane where the adsorption of CO2 causes the desorption
    of methane. This process has the potential to sequester large volumes of
    CO2 (reducing its impacts on possible global warming), while improving the
    efficiency and potential profitability of natural gas recovery. Lab studies
    indicate that coal adsorbs nearly twice as much volume of CO2 as methane.
    There are some concerns, however, that injection of CO2 into mineable
    coals presents a safety hazard, as the mines are required to have a
    limit of 3% CO2 by volume in the mine air.

•   One potential method for reducing CO2 levels in the mine air is to use a
    mixture of CO2 and other gases, such as nitrogen. Studies indicate that for
    each volume of nitrogen that is injected, two volumes of methane are
    produced. There is growing interest in mixed Nitrogen/CO2 injection for
    two reasons:

•   There may be a synergy of production mechanisms, and
•   Its use would result in the lowering of CO2 levels in the mine air.
                                                                              51
ENHANCED RECOVERY OF CBM (contd.)
           LIMITATIONS/ BARRIERS TO
               IMPLEMENTATION :
•   The potential barriers or limitations to ECBM fall into the three broad
    categories:
1. Geologic.
2. Economic.
3. Policy.

The geologic limitations are fixed in the absence of advances in
  technology; if the gas is not present in commercial quantities or if
  the gas cannot be produced, the project would not support an
  ECBM project, especially given the additional costs. Assuming
  favorable geologic characteristics, the operator must then examine
  the economics of the project. A wide variety of factors can influence
  project economics, and thus, the likely application of ECBM
  processes in mineable coal seams. Finally, regulatory requirements
  and/or potential financial incentives can tip the balance for or
  against marginal projects.
                                                                              52
ENHANCED RECOVERY OF CBM (contd.)
     LIMITATIONS/ BARRIERS TO IMPLEMENTATION
                     (contd.) :
Important factors to consider within each of these
               categories include:

 •Geological :                  • Economic :
 •Homogeneity                   •   Cost of CO2
 •Permeability >1 md
                                •   Cost of N2
 •Depth 300-1,500 meters
                                •   Availability of injecting gas
 •Concentrated coal geometry
                                •   Value of methane
 •Production rates
                                •   Cost of processing
 •Development timing
                                •   Cost of implementation
 •Water disposal
                                •   Transportation
 •Amount of available gas


                                                                    53
OTHER FACTORS CONSIDERED
  FOR CBM PRODUCTION :

1.   CBM CEMENTING.
2.   ORIENTED PERFORATING.
3.   COILFRAC STIMULATION.
4.   FRACTURING CBM.
5.   DEWATERING AND FINES CONTROL.
6.   STIMULATION SOLUTIONS.

                                     54
LOGGING SOLUTIONS FOR
OPTIMIZING FIELD DEVELOPMENT :

 1.   Full range of well evaluation services.
 2.   Cased hole geochemical logging.
 3.   High-resolution density measurement.
 4.   Open hole geochemical logging.
 5.   Integrated open hole logging suite.
 6.   Sonic imaging measurements.

                                                55
FRACTURING OF
CBM RESERVOIR AS
  A STIMULATION
    TECHNIQUE

               56
FRACTURING
           TECHNOLOGIES :
• Fracture stimulation technologies for enhancing
  well deliverability can generally be categorized in
  three types, according to the rate at which
  energy is applied to the target horizon to induce
  fracturing:
1.Hydraulic fracturing .
2.Pulse fracturing .
3.Explosive fracturing .
                                                    57
Figure: Comparison of
                                Pressure Histories for Rock
                                Fracturing Techniques.




Figure: Comparison of Created
Fracture Geometries for Rock
                                                         58
Fracturing Techniques
FRACTURING TECHNOLOGIES(contd.)

HYDRAULIC FRACTURING

1. Fracturing with Liquid Carbon Dioxide
   (CO2) with Prop-pant.
2. Fracturing with Nitrogen.
3. Coiled Tubing Fracturing.


                                           59
FRACTURING TECHNOLOGIES(contd.)

 PULSE FRACTURING

                              Figure:
                              Conceptual
                              Model of Pulse
                              Fracturing results



1. Propellant Fracturing.
2. Pulse Fracturing with Nitrogen .

                                          60
CBM PRODUCT WATER
        AND
ENVIRONMENTAL ASPECTS
Effect of CBM product water in stream channels and landscape
Ground water flow systems




Ground water flow
systems impacted
 by CBM wells
PRINCIPAL CONCERNS :
Air quality, caused by the dust from the extensive network of
unpaved access roads,
Wildlife, from noise disturbances; the direct loss of critical
winter range habitat; habitat alteration such as water
temperature, quality and quantity changes in stream conditions;
increases in hunting pressure;
Livestock grazing, this will be almost totally excluded from the
land
Cultural resources and
Agricultural land which may be lost or damaged by low quality
water coming from CBM production.

                                       RECOMMENDATIONS :
                               Adopt the precautionary principle
                               Provide public input on decisions
                               Improve public information on CBM development
                               Improve the regulatory process on CBM development
                               Adopt best practices for operations
                               Evaluate enhanced recovery of CBM using CO2
INDIAN COAL WITH
 SPECIAL REFERENCE TO
TERTIARY COAL FOUND IN
   NORTH-EAST INDIA
Major Coalfields of India
INDIA’S CBM EXPERIENCE
           AND
         RESERVE
(Source: Oil & Gas Journal, Dec’2007)   Distribution of India’s CBM Resource
       India’s Energy Scenario
CURRENT STATUS OF CBM EXPLORATION IN INDIA
CBM BIDDING ROUNDS
CBM-I, 2002           CBM-II, 2003




CBM-III, 2005         CBM-IV, 2008
POSSIBLE UTILIZATION
        OF
       CBM
         IN
       INDIA
POWER GENERATION
AUTO FUEL IN FORM OF COMPRESSED
NATURAL GAS (CNG)
FEED STOCK FOR FERTILIZER
FUEL FOR INDUSTRIAL USE
USE OF CBM AT STEEL PLANTS
CMM USE IN METHANOL PRODUCTION
CASE STUDIES

• CASE STUDY – 1: JHARIA COALFIELD.
• CASE STUDY – 2: MARGHERITA COAL
                  FIELD.
• CASE STUDY – 3: RANIGANJ FIELD, DURGAPUR.
• CASE STUDY – 4: EAST OGAN KOMERING
                  BLOCK 2, SOUTH
                  SUMATERA BASIN,INDONESIA.
• CASE STUDY – 5: WEST OGAN, SOUTH
                  SUMATERA BASIN, INDONESIA.


                                               75
FACTS
• Coal is the world′s most abundant energy source
• Coal is a major source of hydrocarbons such as
  methane gas
• When plant material is converted into coal it
  generates large quantities of methane-rich gas
• Methane gas is then stored within the coal beds
  making coal a reservoir as well as a gas source
• It is estimated that coal and methane gas can be
  found in 13% of all the land in the lower 48 states
  of the US.
• Coal bed methane gas accounted for almost 8%
  of the U.S. natural gas demand.
                                                        76
FACTS (contd.)
• Coal bed methane is currently a huge undeveloped
  energy resource
• Coal bed methane can be used as an clean energy
  source
• It is a safe, efficient and an environmentally more
  acceptable energy source
• Over the last two decades, the development of
  domestic natural gas supplies declined while
  consumption increased. There is now greater world
  market demand for cleaner fuels like Coal Bed
  Methane Gas and Natural Gas.
                                                        77
REFERENCES
•   Website of Director General of              •   Data and Consulting Service,
    Hydrocarbons                                    Schlumberger Website
•   BU-Screen-Chapter 2-Introduction to CBM     •   Simulation of CBM reservoirs, Under the
    By David Epperly.                               guidance of Dr S.K.Singh Gm-CBM,
•   Methane Gas an Unconventional Energy            EEPIL, Mumbai
    Resource, Paper by Alpana Singh &           •   Advanced Resources International, US,
    Bhagwan D. Singh                                1994
•   Diamond, W. P. and Oyler, D. C., 1986,      •   Kristin Keith, Jim Bauder, Bozeman John
    “Direction Drilling for Degasification of       Wheaton, Montana Bureau of Mines &
    Coalbeds in Advance of Mining                   Geology, 2003- “Coalbed Methane-
•   Govt. of British Columbia – “CBM                Frequently Asked Questions”
    Brochure”                                   •   Ministry of Coal, India, Annual Report
•   HELP MANUAL, FAST CBM, SOFTWARE             •   GEOLOGICA BELGICA (2004) By-Saikat
•   After O.H.Barzandji, J. Bruining,               MAZUMDER & Karl-Heinz A. A. WOLF ,
    Combination Of Laboratory Experiments           Delft University of Technology
    And Field Simulations On The Improvement    •   Dissertation of Mr. Prasenjit Talukder,
    Of Coalbed Methane Production By Carbon         M.Tech, Petroleum Technology; Asstt.
    Dioxide Injection, Delft University of          Professor, D.U.I.E.T.
    Technology Second International Methane
    Mitigation Conference, Novosibirsk,         •   WORLD WIDE WEB
    Russia, June 18-23, 2000

                                                                                         78
ACKNOWLEDGEMENT
We reserve our profound gratitude for Mrs. Leena Sonpal, Director, Ranco Energy
& Projects Pvt. Ltd-Mumbai for providing us this great opportunity. Words are
inadequate and indescribable to acknowledge the great care and guidance by our
mentor Mr.Prasenjit Talukder, Assistant Professor, Department of Petroleum
Engineering, Dibrugarh University Institute of Engineering Technology,
Dibrugarh University. Our association with him throughout the project was a great
process of learning. We would like to express our gratitude to the esteemed faculty
members of Dibrugarh University Institute of Engineering Technology for their
encouragement and valuable support. We express our gratitude towards our
esteemed faculty members, Mr. Gautom Neog ,Mr. Nayan Medhi and Mr. Santanu
Sarmah for their care & support, for their constant motivation to work positively and
for extending a helping hand whenever in need. We are greatly indebted and thankful
to for their altruistic teaching and continuous guidance throughout two and half years
of our study at Dibrugarh University Institute of Engineering Technology.
We would also like to thank all those who are knowingly or unknowingly involved in
completion of our project. Finally, our head bows with veneration before our
respected parents who have given us strength, patience and will to complete this
project.
                                                                                 79
THANK YOU

   PROJECT UNDERTAKEN AND COMPLETED AT
DIBRUGARH UNIVERSITY INSTITUTE OF ENGINEERING
              AND TECHNOLOGY.

                                           80

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Coal Bed Methane

  • 1. SEMINAR ON COAL BED METHANE: A STRATEGIC OVERVIEW Presented by Rupam Sarmah 6TH SEMESTER PETROLEUM ENGINEERING D.U.I.E.T In fulfillment for the Completion Of WINTER INTERNSHIP DECEMBER 26TH, 2011 – JANUARY 15TH, 2012 In RANCO ENERGY PROJECTS PRIVATE LIMITED, MUMBAI
  • 2. ABSTRACT Currently, gas demand exceeds supply by 30 per cent. While the demand for natural gas in India is 118 million metric standard cubic meter per day (MMSCMD), the current supply from various sources is 80 MMSCMD, leaving a shortfall of 28 MMSCMD. That deficiency can be covered by CBM production. 2
  • 3. OVERVIEW OF COAL AND CBM RESERVES
  • 4. BENEATH THE SURFACE… Global coal distribution Identified CBM basins
  • 5. COAL : World’s number two source of primary energy with 27% of demand According to the baseline scenario used by the IEA in its World Energy Outlook 2009, the consumption of coal is expected to rise by 1.9% per year between now and 2030, by which time it should account for 29% of global primary energy requirements Distribution of recoverable coal reserves CBM Reserves (Gas in Place) by country
  • 6. A GENESIS MODEL OF COAL PEATIFICATION Geochemical Transformation COALIFICATION
  • 9.  GAS STORAGE: Instead of occupying void spaces as a free gas between sand grains, the methane is held to the solid surface of the coal by adsorption in numerous micro pores. The adsorption mechanism creates the paradox of high gas storage in a reservoir rock of porosity less than 2.5%.  GAS FLOW: • Mass transport through solid coal (micro pore structure) is governed by Ficks law of diffusion, • Mass transport through the fracture system is governed by Darcy’s law,
  • 10.  GAS PRODUCTION: Dictated by the pressure-lowering process of dewatering, Coal beds feature production rates of methane that initially increase and then slowly decline as gas production continues over a long period.  GAS CONTENT: Gas adsorbed on the coal cannot be detected on geophysical logs as in a conventional reservoir, and the gas amount must be determined by volumetric calculations based on coring data. Gas content of coals may increase with depth, however, due to the positive influence of pressure on adsorptive capacity rather than the compressibility of the gas.  WATER PRODUCTION: The formation waters generated from natural fractures in coal must be removed before methane can be desorbed in the early production life of a well. ROCK PROPERTY: Conventional oil and gas formations are inorganic. Organic formations contain CBM; these formations may contain about 10–30% inorganic ash. HYDROFRACTURING: The coal usually has low permeability and depends on natural fractures to act as gas and liquid conduits. Without hydraulic fracturing, these low- permeability coals are usually commercially non-productive. STRESS DEPENDENT PERMEABILITY: The permeability is stress-dependent, so, whether the coals exhibit a low permeability or exhibit an extensive, unstressed network of fractures with high permeability is a critical parameter in any decision to invest in a CBM process.
  • 11. KEY PARAMETERS IN CBM RESERVOIRS GAS CONTENT : Standard volume of gas per unit weight of coal or rock. (scf/ton) Estimation of gas content: • Desorbed gas : Estimated by the “Direct Method” or Canister desorption test. • Lost gas : Volume of the gas that desorbs from the sample during the recovery process before the core sample can be sealed in a desorption canister and is estimated by analyzing the data obtained during the canister desorption tests. •Residual gas : Gas that remains sorbed on the sample at the conclusion of the canister desorption test and is estimated by crushing the entire desorption sample to smaller than a 60 mesh grain size and measuring the gas volume released at the reservoir temperature. TOTAL GAS VOLUME ═ DESORBED GAS + LOST GAS + RESIDUAL GAS
  • 12. RESERVOIR THICKNESS: • Gross coal thickness usually can be determined accurately with wire line logs (Generally, Open-hole density logs). • The gross reservoir thickness is commonly computed by summing the thicknesses of the intervals having densities less than a cut off value generally equal to the coal ash density. • Determining net thickness is complicated but it can be estimated by using Resistivity logs, Well tests, Production logs, or Zonal isolation tests. LANGMUIR VOLUME (VL) : Maximum amount of gas that can be adsorbed on a piece of coal at infinite pressure. This value is asymptotically approached by the isotherm as the pressure increases. Typically, the units for the Langmuir volume parameter (VL) are scf/ton. LANGMUIR PRESSURE (PL) : This parameter affects the shape of the isotherm. The Langmuir pressure is the pressure at which half of the Langmuir volume can be adsorbed.
  • 13. • Relationship used to represent the sorption mechanism in coal bed methane reservoir is given as: Where, Gs = Gas storage capacity, SCF/ton; P = Pressure, psia; V L = Langmuir volume constant, SCF/ton; PL = Langmuir pressure constant, psia • The impact of VL and PL on the shape of the isotherm curve:
  • 14. SORPTION TIME : Sorption time (τ ) is the time required to desorb 63.2 percent of the initial gas volume. Where, σ = matrix shape factor, dimensionless D = matrix diffusivity constant, sec-1 As the coal rank increases, τ also increases. Greater the value of τ, greater will be the time taken by gas for desorption PERMEABILITY : It is the volume of interconnected pores in a rock. Primary Permeability (Cleat) Permeability of CBM Reservoir Secondary Permeability (Pore) POROSITY : In CBM reservoirs, porosity is saturated with water. So, greater porosity will lead to greater water production and vice- versa. Thus, unlike conventional reservoirs, high porosity is unfavourable for CBM reservoirs. Micro-porosity of coal
  • 15. FLOWING BOTTOM HOLE PRESSURE : Pressure at the bottom of the hole Calculation : Let x be the mean depth of perforation from the surface in meter. Let y be the water level in annulus from the surface in meter. Then, BHP=(x-y)*3.28*0.433 in psi. Where, 0.433 is the water pressure gradient in psi/ft. The aim of production operations is to bring the level of water below the perforation so that BHP decreases. When flowing BHP is decreased, drawdown will increase and correspondingly production will also increase.
  • 16. DEPTH : As depth increases, coal rank increases, increasing gas content of coal, but at the same time decreasing permeability. Thus, the depth at which optimum value of gas content and permeability can be expected ranges between 700 to 1000 m. DENSITY OF COAL : If coal density is low, desorption will take place easily and vice-versa.
  • 17. COALBED METHANE – A RESERVOIR APPROACH
  • 18. Coalbed methane is stored in four ways: As free gas within the micro pores (pores with a diameter of less than .0025 inches) and cleats (sets of natural fractures in the coal);  As dissolved gas in water within the coal;  As adsorbed gas held by molecular attraction on surfaces of macerals (organic constituents that comprise the coal mass), micro pores, and cleats in the coal; and  As absorbed gas within the molecular structure of the coal molecules.
  • 19. Physical and chemical characteristics of plant debris and coals with maturation
  • 20. The most important characteristics of coal reservoir are: Coal is a source rock and a reservoir rock. The depositional environment and burial history of the coal affect the composition of the gas as well as the gas content, diffusivity, permeability, and gas storage capacity of the coal. The gas storage mechanism of coal. Most of the gas in coal reservoirs is adsorbed onto the internal structure of the coal. Because large amounts of gas can be stored at low pressures in coal reservoirs, the reservoir pressure must be drawn down to a very low level to achieve high gas recovery.  The fracture system of coal reservoirs. Coals contain small (typically, several per inch), regularly-spaced, naturally occurring fractures called face cleats and butt cleats. Coal reservoirs also contain larger-scale natural fractures. Coal reservoirs often require pumping water before gas is produced. Typically, water must be produced continuously from coal seams to reduce reservoir pressure and release the gas. The cost to treat and dispose of produced water can be a critical factor in the economics of a coalbed methane project. The unique mechanical properties of coal. Coal is relatively compressible compared to the rock in many conventional reservoirs. Thus, the permeability of coal is more stress- dependent than most reservoir rocks. The friable, cleated nature of coal affects the success of hydraulic fracturing treatments, and in certain locations allows for cavitation techniques to dramatically increase production.
  • 21. STAGES OF PRODUCTION Isotherm showing reservoir initial condition STAGE 1: WATER PRODUCTION: DEWATERING STAGE 2: GAS PRODUCTION: DEWATERED STAGE STAGE Isotherm showing dewatering Water flow rate with time Isotherm showing amount of gas released Gas flow rate with time
  • 22. SIMULATING CBM RESERVOIR
  • 23. Reservoir simulation is the process of integrating geology, petro physics, reservoir engineering, and production operations to more effectively develop and produce petroleum resources DESCRIPTION OF CBM SIMULATORS Dual porosity nature of coalbed; Darcy flow of gas and water (i.e., multiphase flow) in the natural fracture system in coal; Diffusion of a single gas component (i.e., pure gas) from the coal matrix to the natural fracture system; Adsorption/Desorption of a single gas component (i.e., pure gas) at the coal surface; Coal matrix shrinkage due to gas desorption. TYPES OF SIMULATORS Gas Sorption and Diffusion Simulators Compositional Simulators Black-Oil Simulators
  • 24. DATA NEEDED FOR SIMULATION
  • 25. GRID SYSTEMS Three-dimensional Cartesian grid r-θ-z geometry using Polar Cylindrical coordinates RESULTS FROM COMET-3 (By Advanced Resources International)
  • 26. GENERAL TERMINOLOGIES & GENERAL OVERVIEW 26
  • 27. Coal bed Methane Terminologies 27
  • 28. Methane gas from Coal beds: •Coal bed Methane (CBM) : Methane contained in coal seams. Often referred to as virgin coal bed methane, or coal seam gas. •Coalmine Methane (CMM) : CBM that is released from the coal seams during coal mining. •Abandoned Mine Methane (AMM) : Methane that continues to be released from closed and sealed mines. May also be referred to as coal mine methane because the liberated methane is associated with past coal mining activity. 28
  • 29. GENERAL OVERVIEW Air Drilling Rig For CBM PC Pumps running at test wells Plantation at test Separators installed well site at test wells Gas flare 29
  • 30. DRILLING OF A CBM WELL 30
  • 31. 31
  • 32. INTRODUCTION • Methane can be extracted from the coal seams by the process of desorption according to which the initial reservoir pressure is reduced, by dewatering, to the reduced critical desorption pressure. Thereafter, the coal seams release methane gas as the pressure is reduced. The abandonment pressure is the lowest pressure at which no more methane can be produced. Before an exercise of drilling for the purpose of methane extraction can be undertaken, an estimate of the reserves of coal bed methane gas is made. 32
  • 33. INTRODUCTION (contd.) • The primary concerns for drilling are overpressure of gas/water kicks, high permeability which leads to loss of circulation fluid, formation damage due to the nature of coal and hole sloughing. • Due to presence of large amount of water in the reservoir, often water influx is encountered during drilling. 33
  • 34. INTRODUCTION (contd.) • However as the gas is found in shallower depths, the drilling is cost effective in case of CBM than those of conventional oil and gas reservoir drilling. • Normally directional wells are favored for CBM reservoir as it can lead to production of large amount of gas economically and as the depth is not a major problem so it is cost effective. 34
  • 37. DIRECTIONAL DRILLING TECHNOLOGY (contd.) •To give an idea of the effectiveness of horizontal drilling, the U.S. Department of Energy indicates that using horizontal drilling can lead to an increase in reserves in place by 2% of the original oil in place. The production ratio for horizontal wells versus vertical wells is 3.2 to 1, while the cost ratio of horizontal versus vertical wells is only 2 to 1. Figure: Schematic Diagram of a Directionally Drilled Pre- Mine Degasification 37
  • 38. TECHNICAL LIMITATIONS AND BARRIERS TO IMPLEMENTATION 1. Poor vertical permeability or impermeable streaks : Compositionally, coal is often heterogeneous with the different coal types generally segregated into bands; this can range in thickness from several millimeters up to several to tens of centimeters. The degree of cleat development varies greatly between these coal types; for example vitrain bands tend to be well cleated, while durain bands tend to be poorly cleated. The alternation of well cleated/poorly cleated bands can substantially reduce vertical permeability. Additionally, coal bed often contain thin shale beds or stringers which would further limit vertical permeability. 38
  • 39. TECHNICAL LIMITATIONS AND BARRIERS TO IMPLEMENTATION (contd.) 2. Variable formation depth and thickness : Some coal bed were formed in depositional systems which resulted in erratic or uneven coal seam deposition. In such cases, it would be difficult to keep a horizontal or near- horizontal hole in the seam while drilling. 39
  • 40. TECHNICAL LIMITATIONS AND BARRIERS TO IMPLEMENTATION (contd.) While it is technically feasible to drill multiple horizontal legs at different depths, there are some unique characteristics of how coal bed methane wells are produced which must be considered: 1.First, only one leg of a horizontal well with multiple legs can be cased. Because coal is often friable, uncased horizontal wellbores will be prone to sloughing and collapse. The loss of wellbore integrity will inhibit both the dewatering process and gas production. 2.Second, dewatering operations in horizontal wells are more complicated than vertical well operations. The majority of coal bed methane wells in the U.S. are dewatered using conventional "beam" or "sucker rod" pumps. Formation water is produced by a down-hole pump, which is operated via an up and down motion imparted to the rods by the pump jack on the surface. Because the pumping system is designed to operate in a vertical plane, the connecting rods tend to break when flexed, as would be the case in a horizontal wellbore. 40
  • 41. PRODUCTION FROM A CBM GAS WELL 41
  • 42. 42
  • 43. Figure : Coal Bed Matrix illustrating gas surrounding the coal bound by water and rock 43
  • 44. INTRODUCTION Since CBM travels with ground water in coal seams, extraction of CBM involves pumping available water from the seam in order to reduce the water pressure that holds gas in the seam. CBM has very low solubility in water and readily separates as pressure decreases, allowing it to be piped out of the well separately from the water. Water moving from the coal seam to the well bore encourages gas migration toward the well. CBM producers try not to dewater the coal seam, but rather seek to decrease the water pressure (or head of water) in the coal seam to just above the top of the seam. However, sometimes the water level drops into the coal seam. 44
  • 46. INTRODUCTION (Contd.) • The production profiles of CBM wells are typically characterized by a "negative decline" in the gas rate as water is pumped away and gas begins to desorb and flow. A dry CBM well does not look very different from a standard well, except that the gas rates are lower and decline at a much slower rate. Figure: A typical ten-year CBM gas rate forecast, showing a negative decline for the first couple years of production. 46
  • 47. INTRODUCTION (Contd.) • The methane desorption process follows a curve (of gas content vs. reservoir pressure) called a Langmuir isotherm. The isotherm can be analytically described by a maximum gas content (at infinite pressure), and the pressure at which half that gas exists within the coal. These parameters (called the Langmuir volume and Langmuir pressure, respectively) are properties of the coal, and vary widely. A coal in Alabama and a coal in Colorado may have radically different Langmuir parameters, despite similar other coal properties. Figure: A typical CBM isotherm 47
  • 48. INTRODUCTION (Contd.) • The increasing gas rates seen in a negative decline are caused by increasing relative permeability as the water saturation around the wellbore decreases. As there is less water in the coal cleats, the gas is able to flow more and more into the wellbore to be produced. Figure : A set of relative permeability curves ( As water saturation decreases, more gas and less water is produced from the coal.) 48
  • 49. ENHANCED RECOVERY OF CBM • There are three main methods which can induce methane release from coal: 1.Reduce the overall pressure, usually by dewatering the formation either through pumping or mining 2.Reduce the partial pressure of the methane by injecting another inert gas into the formation 3.Replace the methane on the surface with another compound, such as CO2. 49
  • 50. ENHANCED RECOVERY OF CBM (contd.) • The process is implemented by injecting inert gas at one location and recovering methane gas at another. Figure: Gas is injected in one well and methane is recovered in another well 50
  • 51. ENHANCED RECOVERY OF CBM (contd.) Concerned hazards and methods to reduce: • Deep unmineable coal formations provide an opportunity to both sequester CO2 into coal seams (from anthropogenic sources) and increase the production of methane where the adsorption of CO2 causes the desorption of methane. This process has the potential to sequester large volumes of CO2 (reducing its impacts on possible global warming), while improving the efficiency and potential profitability of natural gas recovery. Lab studies indicate that coal adsorbs nearly twice as much volume of CO2 as methane. There are some concerns, however, that injection of CO2 into mineable coals presents a safety hazard, as the mines are required to have a limit of 3% CO2 by volume in the mine air. • One potential method for reducing CO2 levels in the mine air is to use a mixture of CO2 and other gases, such as nitrogen. Studies indicate that for each volume of nitrogen that is injected, two volumes of methane are produced. There is growing interest in mixed Nitrogen/CO2 injection for two reasons: • There may be a synergy of production mechanisms, and • Its use would result in the lowering of CO2 levels in the mine air. 51
  • 52. ENHANCED RECOVERY OF CBM (contd.) LIMITATIONS/ BARRIERS TO IMPLEMENTATION : • The potential barriers or limitations to ECBM fall into the three broad categories: 1. Geologic. 2. Economic. 3. Policy. The geologic limitations are fixed in the absence of advances in technology; if the gas is not present in commercial quantities or if the gas cannot be produced, the project would not support an ECBM project, especially given the additional costs. Assuming favorable geologic characteristics, the operator must then examine the economics of the project. A wide variety of factors can influence project economics, and thus, the likely application of ECBM processes in mineable coal seams. Finally, regulatory requirements and/or potential financial incentives can tip the balance for or against marginal projects. 52
  • 53. ENHANCED RECOVERY OF CBM (contd.) LIMITATIONS/ BARRIERS TO IMPLEMENTATION (contd.) : Important factors to consider within each of these categories include: •Geological : • Economic : •Homogeneity • Cost of CO2 •Permeability >1 md • Cost of N2 •Depth 300-1,500 meters • Availability of injecting gas •Concentrated coal geometry • Value of methane •Production rates • Cost of processing •Development timing • Cost of implementation •Water disposal • Transportation •Amount of available gas 53
  • 54. OTHER FACTORS CONSIDERED FOR CBM PRODUCTION : 1. CBM CEMENTING. 2. ORIENTED PERFORATING. 3. COILFRAC STIMULATION. 4. FRACTURING CBM. 5. DEWATERING AND FINES CONTROL. 6. STIMULATION SOLUTIONS. 54
  • 55. LOGGING SOLUTIONS FOR OPTIMIZING FIELD DEVELOPMENT : 1. Full range of well evaluation services. 2. Cased hole geochemical logging. 3. High-resolution density measurement. 4. Open hole geochemical logging. 5. Integrated open hole logging suite. 6. Sonic imaging measurements. 55
  • 56. FRACTURING OF CBM RESERVOIR AS A STIMULATION TECHNIQUE 56
  • 57. FRACTURING TECHNOLOGIES : • Fracture stimulation technologies for enhancing well deliverability can generally be categorized in three types, according to the rate at which energy is applied to the target horizon to induce fracturing: 1.Hydraulic fracturing . 2.Pulse fracturing . 3.Explosive fracturing . 57
  • 58. Figure: Comparison of Pressure Histories for Rock Fracturing Techniques. Figure: Comparison of Created Fracture Geometries for Rock 58 Fracturing Techniques
  • 59. FRACTURING TECHNOLOGIES(contd.) HYDRAULIC FRACTURING 1. Fracturing with Liquid Carbon Dioxide (CO2) with Prop-pant. 2. Fracturing with Nitrogen. 3. Coiled Tubing Fracturing. 59
  • 60. FRACTURING TECHNOLOGIES(contd.) PULSE FRACTURING Figure: Conceptual Model of Pulse Fracturing results 1. Propellant Fracturing. 2. Pulse Fracturing with Nitrogen . 60
  • 61. CBM PRODUCT WATER AND ENVIRONMENTAL ASPECTS
  • 62. Effect of CBM product water in stream channels and landscape
  • 63. Ground water flow systems Ground water flow systems impacted by CBM wells
  • 64. PRINCIPAL CONCERNS : Air quality, caused by the dust from the extensive network of unpaved access roads, Wildlife, from noise disturbances; the direct loss of critical winter range habitat; habitat alteration such as water temperature, quality and quantity changes in stream conditions; increases in hunting pressure; Livestock grazing, this will be almost totally excluded from the land Cultural resources and Agricultural land which may be lost or damaged by low quality water coming from CBM production. RECOMMENDATIONS : Adopt the precautionary principle Provide public input on decisions Improve public information on CBM development Improve the regulatory process on CBM development Adopt best practices for operations Evaluate enhanced recovery of CBM using CO2
  • 65. INDIAN COAL WITH SPECIAL REFERENCE TO TERTIARY COAL FOUND IN NORTH-EAST INDIA
  • 67.
  • 68.
  • 70. (Source: Oil & Gas Journal, Dec’2007) Distribution of India’s CBM Resource India’s Energy Scenario
  • 71. CURRENT STATUS OF CBM EXPLORATION IN INDIA
  • 72. CBM BIDDING ROUNDS CBM-I, 2002 CBM-II, 2003 CBM-III, 2005 CBM-IV, 2008
  • 73. POSSIBLE UTILIZATION OF CBM IN INDIA
  • 74. POWER GENERATION AUTO FUEL IN FORM OF COMPRESSED NATURAL GAS (CNG) FEED STOCK FOR FERTILIZER FUEL FOR INDUSTRIAL USE USE OF CBM AT STEEL PLANTS CMM USE IN METHANOL PRODUCTION
  • 75. CASE STUDIES • CASE STUDY – 1: JHARIA COALFIELD. • CASE STUDY – 2: MARGHERITA COAL FIELD. • CASE STUDY – 3: RANIGANJ FIELD, DURGAPUR. • CASE STUDY – 4: EAST OGAN KOMERING BLOCK 2, SOUTH SUMATERA BASIN,INDONESIA. • CASE STUDY – 5: WEST OGAN, SOUTH SUMATERA BASIN, INDONESIA. 75
  • 76. FACTS • Coal is the world′s most abundant energy source • Coal is a major source of hydrocarbons such as methane gas • When plant material is converted into coal it generates large quantities of methane-rich gas • Methane gas is then stored within the coal beds making coal a reservoir as well as a gas source • It is estimated that coal and methane gas can be found in 13% of all the land in the lower 48 states of the US. • Coal bed methane gas accounted for almost 8% of the U.S. natural gas demand. 76
  • 77. FACTS (contd.) • Coal bed methane is currently a huge undeveloped energy resource • Coal bed methane can be used as an clean energy source • It is a safe, efficient and an environmentally more acceptable energy source • Over the last two decades, the development of domestic natural gas supplies declined while consumption increased. There is now greater world market demand for cleaner fuels like Coal Bed Methane Gas and Natural Gas. 77
  • 78. REFERENCES • Website of Director General of • Data and Consulting Service, Hydrocarbons Schlumberger Website • BU-Screen-Chapter 2-Introduction to CBM • Simulation of CBM reservoirs, Under the By David Epperly. guidance of Dr S.K.Singh Gm-CBM, • Methane Gas an Unconventional Energy EEPIL, Mumbai Resource, Paper by Alpana Singh & • Advanced Resources International, US, Bhagwan D. Singh 1994 • Diamond, W. P. and Oyler, D. C., 1986, • Kristin Keith, Jim Bauder, Bozeman John “Direction Drilling for Degasification of Wheaton, Montana Bureau of Mines & Coalbeds in Advance of Mining Geology, 2003- “Coalbed Methane- • Govt. of British Columbia – “CBM Frequently Asked Questions” Brochure” • Ministry of Coal, India, Annual Report • HELP MANUAL, FAST CBM, SOFTWARE • GEOLOGICA BELGICA (2004) By-Saikat • After O.H.Barzandji, J. Bruining, MAZUMDER & Karl-Heinz A. A. WOLF , Combination Of Laboratory Experiments Delft University of Technology And Field Simulations On The Improvement • Dissertation of Mr. Prasenjit Talukder, Of Coalbed Methane Production By Carbon M.Tech, Petroleum Technology; Asstt. Dioxide Injection, Delft University of Professor, D.U.I.E.T. Technology Second International Methane Mitigation Conference, Novosibirsk, • WORLD WIDE WEB Russia, June 18-23, 2000 78
  • 79. ACKNOWLEDGEMENT We reserve our profound gratitude for Mrs. Leena Sonpal, Director, Ranco Energy & Projects Pvt. Ltd-Mumbai for providing us this great opportunity. Words are inadequate and indescribable to acknowledge the great care and guidance by our mentor Mr.Prasenjit Talukder, Assistant Professor, Department of Petroleum Engineering, Dibrugarh University Institute of Engineering Technology, Dibrugarh University. Our association with him throughout the project was a great process of learning. We would like to express our gratitude to the esteemed faculty members of Dibrugarh University Institute of Engineering Technology for their encouragement and valuable support. We express our gratitude towards our esteemed faculty members, Mr. Gautom Neog ,Mr. Nayan Medhi and Mr. Santanu Sarmah for their care & support, for their constant motivation to work positively and for extending a helping hand whenever in need. We are greatly indebted and thankful to for their altruistic teaching and continuous guidance throughout two and half years of our study at Dibrugarh University Institute of Engineering Technology. We would also like to thank all those who are knowingly or unknowingly involved in completion of our project. Finally, our head bows with veneration before our respected parents who have given us strength, patience and will to complete this project. 79
  • 80. THANK YOU PROJECT UNDERTAKEN AND COMPLETED AT DIBRUGARH UNIVERSITY INSTITUTE OF ENGINEERING AND TECHNOLOGY. 80