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The origin of high hydrocarbon groundwater in shallow aquifer: experimental evidences from water-rock interaction

机译:浅层含水层高碳氢化合物地下水的起源:水岩互动的实验证据

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摘要

The current studies had already revealed the hydrocarbons could migrate from relatively high hydrocarbon potential stratum to shallow groundwater by corrosion emission and extraction emission in karst area and further impact on human health. Then, the comprehensive experiments were used to understand the mechanism and process of hydrocarbon emission as a continuation of a long-term study on original high hydrocarbon groundwater in shallow Triassic aquifer, taking northwest Guizhou, China, as a reference. The results determined water-rock interaction that lead to the hydrocarbon emission into groundwater with salinity acting as the main driving force. Relatively high salinity promotes the rock corrosion and hydrocarbon emission in the study area. The hydrocarbon emission process varied with different strata, as the results show that the hydrocarbon uniformly distributed in T(2)g(3) than that in T(1)yn(4). Furthermore, the stratum with uniformly distributed hydrocarbon would likely contain high hydrocarbon groundwater, as determined by the process of sedimentation. In addition, "corrosion rate estimation method" and "mineral constituent estimation method" were firstly employed to estimate the hydrocarbon concentration in groundwater to date. Compared with the hydrocarbon concentration of local groundwater samples (0 to 0.14 mg L-1), the result of "mineral constituent estimation method" was analogous to measured value of groundwater samples in the area (0.05 to 0.50 mg L-1), indicating the concentration of hydrocarbon could be estimated by mineral constitutions of groundwater, which was related to the concentration of Ca2+ and Mg2+. Based on the methods and theories in this study, the concentration of original hydrocarbon in shallow groundwater could be estimated and help to understand the mechanism of water-rock interaction in shallow aquifer and original high hydrocarbon groundwater strategic assessment.
机译:目前的研究已经揭示了碳氢化合物可以通过喀斯特地区的腐蚀排放和提取排放,从喀斯特地区的腐蚀排放和对人体健康的进一步影响,碳氢化合物从相对高的烃潜在地层迁移到浅层地下水。然后,综合实验用于了解碳氢化合物排放的机制和过程,作为浅三叠腹含水层原始高碳氢化合物地下水的长期研究,以中国西北部为基础为参考。结果确定了水岩相互作用,其导致碳氢化合物排放到地下水中,用作主要驱动力。相对较高的盐度促进了研究区域中的岩腐蚀和烃排放。烃排放过程随不同的地层而变化,结果表明,烃均匀地分布于T(2)G(3)中,而不是T(1)yN(4)。此外,具有均匀分布的烃的层可能含有高烃地下水,如通过沉降过程所确定的。另外,首先使用“腐蚀速率估计方法”和“矿物成分估计方法”以估计地下水中的烃浓度至今。与局部地下水样品的烃浓度(0至0.14mg L-1)相比,“矿物成分估计方法”的结果类似于该区域中地下水样品的测量值(0.05至0.50mg L-1),表明烃的浓度可以通过地下水的矿物构成估计,其与Ca2 +和Mg2 +的浓度有关。基于本研究的方法和理论,估计浅地下水中原始烃的浓度有助于了解浅层含水层和原始高碳氢化合物地下水战略评估中的水岩相互作用的机制。

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