Identification of Hydrocarbon Microseepage Using Trace
Metal Indicators in Petroliferous Region of South Cambay Basin, Gujarat, India
M. A. Rasheed1, P. L. Srinivasa Rao.1, Anand Patil.1, Harshit Patel1, Shubhangi Kala1, Annapurna Boruah.1, Syed Zaheer Hasan.1, P.H. Rao1, T.Harinarayana1
Citation : M. A. Rasheed,et.al, Identification of Hydrocarbon Microseepage Using Trace Metal Indicators in Petroliferous Region of South Cambay Basin, Gujarat, India International Journal of Petroleum and Petrochemical Engineering 2015, 1(1) : 12-19
The concentrations of trace elements have been used as indirect proxy for detection of hydrocarbon
microseepage. The long-term seepage of hydrocarbons, either as macro or micro-seepage, can set up nearsurface
oxidation reduction zone that favors the development of a diverse array of chemical and mineralogical
changes. Under the reducing environment the hydrocarbon seepage, the solubility of trace elements increases
that transports, due to hydrodynamic flow in the soil leading to the movement of soluble elements towards the
reducing area. This study compares the trace element concentrations with adsorbed soil gaseous hydrocarbons
and explains the trace elements concentrations pertaining to the hydrocarbon micro seepages. Total 81 numbers
of soil samples were collected from the depth range of 1-2.5 meters below the ground level from Southern part
of the Cambay Basin.
The trace metals such as Chromium (Cr), Copper (Cu), Arsenic (As), Selenium (Se) and Antimony (Sb) in the
soil samples were analyzed using Atomic Absorption Spectrometer. The analytical results show the varying
range of concentrations as Cr (0 to 76ppm), Cu (59 to 168ppm), as (63 to 155ppm), Se (72 to 182ppm) and Sb
(6 to 19ppm). It has been observed that the concentrations of these elements are more when they are compared
with their normal concentrations in the soils. The analyses of adsorbed soil gases show the presence of high
concentrations of methane (CH4) ranged between 2 to 290 ppb, and sum of concentrations of SC2+ (C2H6, C3H8
and n-C4H10) ranged between 7 to 118 ppb. The integrated approach of trace elements over adsorbed light
gaseous hydrocarbon (SC2+) anomalies showed better understanding. The increased concentrations of trace
metals, suggest a soil chemical change to a reducing environment, presumably due to the influence of
hydrocarbon microseepage. This methodology could further integrated with other geo-scientific studies such as
3D Seismic studies which may evolve with the holistic picture of identification of hydrocarbon bearing
formations within the exploration blocks and the frontier areas.