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Geochemical attributes of shale such as the TOC content, thermal maturity and kerogen properties provide useful insights on its gas generation potential.
Published reports on geochemical attributes, burial histories and hydrocarbon generation phases of potential source units in the Northern Delta depobelt have been suggested.
The input data required are: meteorological data, landuse/cover map with event mean concentration attributes, geological maps with hydraulic and geochemical attributes, and topographic and water table elevation data in grid form.
The focus of the present research work encompasses the lignite deposits of the Cambay basin of Gujarat in a view to understand the petrological and geochemical attributes of the lignite deposits of Gujarat, because very little petrological data exists about these lignites as compared to the wealth of literature available on Indian Gondwana coals.
A brief comparison of the geochemical attributes across these five sites is necessary for evaluating potential functional differences among the numerically dominant phyla identified in each microbial community.
The phylogeny of specific functional genes provides direct insight towards the possible role of individual population(s) within each community, and provided candidate genes whose distribution may be a function of major geochemical attributes such as pH, dissolved oxygen, Fe and or S species.
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It is hypothesized that geochemical and hydrodynamic attributes of each site control the phylogenetic composition and corresponding functional capabilities of these microbial communities.
The fact that this microbial community is dominated by a single bacterial population(s) within the Aquificales suggests that this population is highly adapted to the geochemical and hydrological attributes of this environment.
The concentration-area fractal method takes into account such attributes of geochemical landscapes.
The large variation in EC is mainly attributed to geochemical processes prevailing in this region.
The factors responsible for large variation in EC are attributed to geochemical processes such as ionic exchange, reverse exchange, evaporation, silicate weathering, rock water interaction, sulphate reduction and oxidation processes and anthropogenic activities (Ramesh and Elango 2012).
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