土壤热释碳酸盐(ΔC)测定法及其在油气普查中的应用

    THE DETERMINATION OF THERMAL RELEASEDCARBONATES IN SOILS (AC) AND ITS APPLICATIONIN GEOCHEMICAL PROSPECTING FOR OIL AND GAS

    • 摘要: △C是地球化学直接找寻油气藏的一个重要指标。本文报导△C测定最佳条件,各种碳酸盐干扰影响,方法精度及测定装置选配等方面的详细研究结果。建立了适用于石油、天然气及煤藏普查的△C测定方法和便于推广应用的测定装置系统。方法的相对标准偏差为±15—25%。指出土壤中存在的非油气成因碳酸盐的量一般超过数毫克即有干扰。根据本文测定的各种碳酸盐热分解温度,指出现在沿用的500—600℃温区测定△C有漏掉部份△C异常的可能性。因此△C测定的最佳温区应根据实际情况研究选择。用该方法在一个已知小油田上发现了一个似环状弱△C异常与构造及油储相符,在某未知地区的剖面测量中,发现了几处强度高,范围大的异常带。

       

      Abstract: △C is au important geochemical indicator for prospecting and locating oiland gas amumulations. In view of the fact that no detailed analytical methodwas previously worked out in China,we have carried out a series of experiment.This paper introduces the detailed experimental results of △C analysis,including the optimization of analytical conditions, the interference of carbona-tes other than △C, the precision of the method as well as a description of themeasuring system. The relative standard deviation of thc analytical method lieswithin ±15-25%.

       

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