首页> 外文期刊>Journal of caves and karst studies: the National Speleological Society bulletin >ON THE TEMPORAL BEHAVIOR OF KARST AQUIFERS, ZAGROS REGION, IRAN: A GEOSTATISTICAL APPROACH
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ON THE TEMPORAL BEHAVIOR OF KARST AQUIFERS, ZAGROS REGION, IRAN: A GEOSTATISTICAL APPROACH

机译:扎格罗斯地区岩溶含水层的时间行为:地统计学方法

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A geostatistical approach was used to study temporal structures in a time series of discharge and electrical conductivity (EC) in 15 karst springs from the Zagros mountain range, Iran. Two types of temporal behaviors, a periodic structure and nugget effect, plus one or two temporal structures, were identified and interpreted. These correspond to characteristics of karst systems, such as the catchment area, percent of conduit flow, and general degree of karst development. Springs were grouped into three categories based on their ranges (e.g., residence time) obtained by variogram analysis. The first group of springs include those that present the same temporal behaviour in variograms of discharge and EC. These springs are characterized by generally constant EC with increasing discharge suggesting the existence of a large underground reservoir. The second group of springs are those with varying temporal periodic behavior in variograms of discharge and EC. Positive correlation between discharge and EC values is the main characteristic of these springs and is interpreted to result from a piston-flow system in poorly developed karst aquifers. The third group of springs includes those that exhibit different temporal behaviors when compared with the periodic and non-periodic variograms. This group exhibits a negative correlation in scatterplots of discharge versus EC values suggesting a well-developed solution-conduit system that facilitates rapid response of the karst system to precipitation events. This study's results document the role of variogram analysis in delineating temporal structures of spring behaviors by means of time series of discharge and EC. Variogram analysis can be considered as a valuable tool for hydrogeological investigations in karstic terranes.
机译:地统计学方法用于研究伊朗Zagros山脉的15个喀斯特温泉在放电和电导率(EC)时序中的时间结构。识别并解释了两种类型的时间行为,即周期性结构和块效应,以及一个或两个时间结构。这些与岩溶系统的特征相对应,例如集水区,导管流量的百分比以及岩溶发育的总体程度。根据通过变异函数分析获得的范围(例如,停留时间)将弹簧分为三类。第一组弹簧包括在放电和EC的变化图中表现出相同时间行为的弹簧。这些温泉的特征是EC大致恒定,流量增加,表明存在大型地下水库。第二组弹簧是在放电和EC的变化图中具有变化的时间周期性行为的弹簧。排放量与EC值之间的正相关关系是这些弹簧的主要特征,并被解释为由发育不良的岩溶含水层中的活塞流系统产生。第三组弹簧包括那些与周期性和非周期性变化图相比表现出不同的时间行为的弹簧。该组在排放散点图与EC值之间显示负相关,表明完善的溶液管道系统有助于岩溶系统对降水事件的快速响应。这项研究的结果证明了变异函数分析在通过放电和EC的时间序列描述弹簧行为的时间结构中的作用。变异函数分析可以认为是岩溶地层水文地质调查的宝贵工具。

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