Evidence of Coal
Composition and Coalbed Methane (CBM) Source and
Reservoir Potential in
Coal
Cores
Judith Potter1 and David Marchioni2
1 JP Petrographics, Calgary, AB
2 Petro-Logic Services, Calgary, AB
Coal
is both the source rock & reservoir for coalbed methane (CBM).
Source rock potential is typically assessed by desorption testing of
coal
core
or cuttings. Reservoir potential is ultimately assessed by production testing.
The cores cut for gas content testing can also provide valuable information on reservoir potential and/or differences in reservoir potential/performance between wells.
Coal
is a bedded organic sediment and contains laminae that vary markedly
in macroscopic brightness.
Coal
lithotypes are the small sub-sections of the
seam within which the proportions of these bands are relatively uniform, but
significantly different from the proportions in bounding beds. Lithotypes
reflect the composition of
coal
– the proportions of macerals (organic
micro-components) and minerals in different portions of a seam. The lithotype
profile of a seam reflects the variation in depositional conditions in the
precursor mire.
Lithotypes influence gas content as different coal
macerals have
different potential to generate and store gas. In addition, lithotypes influence
cleat development, with cleat density decreasing as the brightness of
coal
decreases.
The fractures in coal
(aka cleat) are the principal permeability
pathways. Description of cleat spacing, length and mineral infilling offers
insight to the permeability potential of the
coal
. Cleat development is
influenced by
coal
rank (aka maturity) and by
coal
composition, which is
reflected in visible lithotypes. However, lateral permeability at lithoptype
boundaries tends to be underestimated. Examples of micropermeameter tests on
slabbed and polished
coal
cores suggest that permeability at lithotypes
boundaries is significant Cores will be presented from coals of different rank
and from the major
coal
zones that are targets of CBM exploration, to illustrate
features of lithotype and cleat variation. Detailed lithotype/cleat profiles
will be displayed alongside the cores.
AAPG Search and Discovery Article #90039©2005 AAPG Calgary, Alberta, June 16-19, 2005