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首页> 外文期刊>Journal of Hydrology >Combined geophysical and analytical methods to estimate offshore freshwater extent
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Combined geophysical and analytical methods to estimate offshore freshwater extent

机译:组合地球物理和分析方法来估算海上淡水程度

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Offshore fresh groundwater is increasingly suggested as a potential water resource for onshore human demands. In many cases, onshore pumping already draws significant fresh groundwater from offshore. However, offshore aquifers and the extent of offshore freshwater are usually poorly characterised due to data scarcity. This study combines geophysical data, hydraulic information and a first-order mathematical analysis to investigate offshore freshwater extent in the Gambier Embayment (Australia). A large seismic data set, combined with onshore and offshore bore-log geological profiles, are used to explore the regional offshore hydro-stratigraphy. Aquifer hydraulic parameters and onshore heads are obtained from onshore investigations. A novel application of Archie's law, geophysical data and onshore hydrochemical data provide useful insights into the salinity profiles within four offshore wells. These are compared to steady-state, sharp-interface estimates of the freshwater extent obtained from a recently developed analytical solution, albeit using simplified conceptual models. Salinities derived from resistivity measurements indicate that in the south of the study area, pore water with total dissolved solids (TDS) of 2.2 g L-1 is found up to 13.2 km offshore. Offshore pore-water salinities are more saline in the northern areas, most likely due to thinning of the offshore confining unit. The analytical solution produced freshwater-saltwater interface locations that were approximately consistent with the freshwater-saltwater stratification in two of the offshore wells, although analytical uncertainty is high. This investigation provides a leading example of offshore freshwater evaluation applying multiple techniques, demonstrating both the benefit and uncertainty of geophysical interpretation and analytical solutions of freshwater extent.
机译:海上新鲜地下水越来越多地建议作为陆上人类需求的潜在水资源。在许多情况下,陆上泵浦已经从海上汲取了重要的新地下水。然而,由于数据稀缺,海上含水层和海上淡水的程度通常很差。本研究结合了地球物理数据,水力信息和一阶数学分析,在冈比尔扶手(澳大利亚)中调查海上淡水程度。大型地震数据集,与陆上和海上钻孔 - 日志地质概况相结合,用于探索区域海上水层面。含水层液压参数和陆上头部是从陆上调查获得的。 ARCHIE法律,地球物理数据和陆上水利化数据的新应用提供了有用的见解盐度在四个海上井中的盐度曲线。这些与稳态,锐利的尖锐接口估计与最近开发的分析解决方案获得的淡水范围相比,尽管使用简化的概念模型。源于电阻率测量的薪水表明,在研究区域的南部,毛孔水总溶解固体(TDS)为2.2g L-1,最高可达13.2公里。海上孔隙水盐水在北部地区的盐水较多,最有可能因离岸限制单位而变薄。分析溶液产生淡水 - 盐水界面位置,虽然分析不确定度高,但淡水 - 盐水界面与淡水盐水分层大致一致。本研究提供了应用多种技术的海上淡水评估的领先例子,展示了地球物理解释和淡水程度分析解决方案的益处和不确定性。

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