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Transport of colloidal and solute tracers in three different types of alpine karst aquifers - Examples from southern Germany and Slovenia

机译:三种不同类型高山喀斯特含水层的胶体和溶质示踪剂运输 - 来自德国南部和斯洛文尼亚的例子

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In many alpine karst regions, bacteriological pollution resulting from agriculture is the most important problem in groundwater protection. Colloidal tracers like fluorescent polystyrene microspheres are used to evaluate the hygienic risk for groundwater resources. Different sizes of colloids may be used to simulate the fate and transport of different types of micro-organisms. For the field tracer tests, three different types of karst systems within the alpine fold belt have been selected: karst aquifers in carbonate conglomerates and limestones in southern Germany, and unsaturated fissured carbonates in Slovenia. Large parts of Tertiary gravel fans in the foreland of European alpine orogens are made of coarsegrained conglomerates, which mainly consist of carbonate components in a carbonatic matrix. These rocks are predisposed to karstification and show a large variety of karst phenomena like dolines, karren, karst springs and estavelles. Tracer tests with fluorescent dyes and particles show high flow velocities and travel distances of up to 8 km. The flow orientation reflects the geological structure. This demonstrates the need for special groundwater protection schemes that take into consideration the heterogeneity and anisotropy of this aquifer type. The Helvetic nappes form parts of he Northern Alps and mainly consist of Jurassic and Cretaceous carbonate rocks. During low-flow conditions, a comparative tracer test with fluorescent-dyes and microspheres was carried out in the Hoelloch, Germany's longest cave (9,343 m). The Association of Tracer Hydrologists (ATH) conducted a comparative tracer test in the Slovenian Dinarids in order to evaluate the behaviour of different tracers in the unsaturated zone of the fissured karst aquifer in Sinji Vrh. The behaviour of the tracers shows important differences, especially for solute and particle tracers. Therefore, the authors strongly recommend using particle tracers for the evaluation of hygienic risks to groundwater.
机译:在许多高山喀斯特地区,农业产生的细菌污染是地下水保护中最重要的问题。荧光聚苯乙烯微球等胶体示踪剂用于评估地下水资源的卫生风险。不同尺寸的胶体可用于模拟不同类型的微生物的命运和运输。对于现场示踪剂测试,已经选择了高山折叠带内的三种不同类型的岩溶系统:在德国南部的碳酸盐群和石灰石中的喀斯特含水层,以及斯洛文尼亚的不饱和裂缝碳酸盐。欧洲高山OROGEN的前沿的大三级砾石风扇的大型部分由甘露出的基质中的碳酸盐组分组成。这些岩石倾向于岩溶,显示出大量的喀斯特人类现象,如Dolines,Karren,Karst Springs和Estavelles。具有荧光染料和颗粒的跟踪器测试显示高达8公里的高流速和行程距离。流量取向反映了地质结构。这证明了需要特殊地下水保护计划,即考虑这种含水层类型的异质性和各向异性。 Helvetic Nappes形成北阿尔卑斯山北部的部分,主要由侏罗纪和白垩纪碳酸盐岩组成。在低流动条件下,在Hoelloch,德国最长的洞穴(9,343米)中进行了荧光染料和微球的比较示踪试验。示踪剂水文学家(ATH)在斯洛文尼亚二列中进行了对比较示踪试验,以评估SINJI VRH在裂隙岩溶含水层的不饱和区中不同示踪剂的行为。示踪剂的行为显示了重要的差异,特别是对于溶质和粒子示踪剂。因此,作者强烈建议使用粒子示踪剂来评估地下水的卫生风险。

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