首页> 外文期刊>Environment and Natural Resources Research >Integrated Use of Geological, Geophysical, Radiocarbon and Stable Isotopes Data for Tracing the Conduit Flow Paths in a Small Karstic Aquifer: Poocher Swamp Freshwater Lens, South Australia
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Integrated Use of Geological, Geophysical, Radiocarbon and Stable Isotopes Data for Tracing the Conduit Flow Paths in a Small Karstic Aquifer: Poocher Swamp Freshwater Lens, South Australia

机译:地质,地球物理,放射性碳和稳定同位素数据的综合利用,用于追踪小型岩溶含水层中的导管流径:南澳大利亚Poocher沼泽淡水透镜

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An integrated approach combining lithological logs, downhole geophysics, electromagnetic survey and the distribution of radiocarbon (14C) and the stable isotopes of water molecules (18O) were used to identify the conduit flow paths of a small freshwater lens. Lost circulation zones, where drilling fluid flows into geological formation instead returning up the annulus recorded during water well drilling, were considered as the major fracture zones. The presence of high porosity zones within boreholes were identified using caliper, gamma and neutron logs. These methods were used to identify the depth intervals at which cavities and the existence of conduit porosity within the boreholes. Transient electromagnetic (TEM) method was used to investigate resistivity anomalies in the profiles along nine pre-determined lines across the freshwater lens. Resistivity anomalies were related to borehole information and other surface features such as sinkholes. Low resistivity zones of the TEM tomography sections had excellent correlation to fracture zones identified during well drilling, and downhole geophysical logs. Similarly, high resistivity zones in the profiles correlate well with the zones of cemented or recrystallized limestone identified from the lithological logs. The interpreted resistivity anomaly accurately depicts depth to watertable at 15-18 m, presence of main fracture zone at 20-25 m, presence of possible conduits flow paths and the cemented or recrystallized limestone below 35 m depth. The 14C, 13C and 18O signatures of the groundwater confirm the presence of conduits and potential pathways of preferential flows. This investigation illustrates the effectiveness using an integrated approach to trace the conduit flow paths in karst aquifers. The information gained from the study is currently being used for the management of the freshwater lens.
机译:结合岩性测井,井下地球物理,电磁勘测和放射性碳(14C)的分布以及水分子的稳定同位素(18O)的集成方法来识别小型淡水透镜的导管流动路径。失水带,即钻井液流入地质构造而不是返回水井钻井时记录的环空区域,被认为是主要的裂缝区域。使用卡尺,伽马和中子测井仪确定了井眼中高孔隙率区域的存在。这些方法用于确定井眼中的孔洞和导管孔隙存在的深度间隔。瞬变电磁(TEM)方法用于研究沿淡水晶状体的9条预定线的剖面电阻率异常。电阻率异常与井眼信息和其他表面特征(例如井眼)有关。 TEM层析成像断层的低电阻率区域与钻井过程中发现的裂缝区域以及井下地球物理测井曲线具有极好的相关性。同样,剖面中的高电阻率区域与从岩性测井中识别出的胶结或重结晶石灰岩区域具有很好的相关性。解释的电阻率异常准确地描述了在15-18 m处的地下水位深度,在20-25 m处存在主裂缝区,在35 m深度以下存在可能的导管流动路径以及胶结或重结晶的石灰石。地下水的14C,13C和18O特征确认了存在导管和优先流动的潜在途径。这项研究说明了使用综合方法来追踪岩溶含水层中的导管流动路径的有效性。从研究中获得的信息目前正用于淡水镜的管理。

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