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首页> 外文期刊>Journal of the Geological Society of India >Integrated geo-microbial and trace metal anomalies for detection of hydrocarbon microseepage in Ahmedabad block of Cambay basin, India
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Integrated geo-microbial and trace metal anomalies for detection of hydrocarbon microseepage in Ahmedabad block of Cambay basin, India

机译:综合的微生物和痕量金属异常,用于检测印度坎贝盆地艾哈迈达巴德区块的油气微渗漏

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The aim of the present work is to define the geo-microbial signatures along with trace metals, and to investigate whether the geo-microbial anomalies have correlation with trace metal anomalies in Ahmedabad block of Cambay basin. The surface geochemical techniques are based on seepage of light hydrocarbon gases from the oil and gas pools to the shallow surface and can bring up near-surface oxidation reduction zones that favor the development of a diverse array of chemical and mineralogical changes. The paper reports the role of hydrocarbon microseepage in surface alterations of trace metal concentrations and hydrocarbon oxidizing bacteria and its interrelationship. For the purpose a total of 90 soil samples are collected in grid pattern of 2 x 2 km interval. The paper reports the chemical alterations associated with trace metals in soils that are related to hydrocarbon microseepages above some of the major oil and gas fields of this petroliferous region. The concentrations of V (0 to149 ppm), Cr (2 to 192 ppm), Cu (4 to 171 ppm), Se (98 to 440 ppm), Zn (56 to 1215 ppm) are obtained. It is observed that the concentrations of trace elements are tremendously increased when they are compared with their normal concentrations in soils. In this study the hydrocarbon oxidizing bacterial counts ranged between 1.0 x 10(3) and 1.59 x 10(6) cfu/g of soil sample respectively. The attempt has made for the first time, which revealed good correlation as both these anomalies are found as apical in relation. Integrated studies between trace elements and hydrocarbon oxidizing bacterial anomalies showed positive correlation with existing oil and gas wells in the study area.
机译:本工作的目的是定义地质微生物特征以及痕量金属,并调查在坎贝盆地艾哈迈达巴德区块中,地球微生物异常是否与痕量金属异常相关。地表地球化学技术是基于轻质烃类气体从油气藏到浅层表面的渗漏,可以产生近地表氧化还原带,这有利于化学和矿物学变化的发展。本文报道了碳氢化合物微渗漏在痕量金属浓度和碳氢化合物氧化细菌表面变化及其相互关系中的作用。为此目的,以2 x 2 km的间隔网格状收集了总共90个土壤样品。该论文报道了与土壤中微量金属有关的化学变化,这些变化与该含油地区一些主要油气田上方的烃类微渗漏有关。得到V(0至149ppm),Cr(2至192ppm),Cu(4至171ppm),Se(98至440ppm),Zn(56至1215ppm)的浓度。可以看出,与土壤中的正常含量相比,微量元素的含量大大增加。在这项研究中,碳氢化合物氧化细菌的计数范围分别为1.0 x 10(3)和1.59 x 10(6)cfu / g土壤样品。该尝试首次进行,显示出良好的相关性,因为这两个异常均被发现为顶点。痕量元素与碳氢化合物氧化细菌异常之间的综合研究表明,该区域与现有油气井正相关。

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