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Use of CPT and other direct push methods for (hydro-) stratigraphic aquifer characterization - A field study

机译:使用CPT和其他直接推动方法进行(水文)地层含水层表征-现场研究

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摘要

Every environmental site investigation aims at delineating near-surface (hydro-) stratigraphic units and their characterization. To determine the type and hydraulic properties of sedimentary deposits, direct push (DP) sensor probes and tools are promising methods and are therefore frequently applied to measure high-resolution vertical profiles of soil properties. Given the variety of these tools, the objective of this paper is to compare selected DP tools for the (hydro-) stratigraphic subsurface characterization in a heterogeneous unconsolidated sedimentary aquifer. An overview of current DP applications is given and selected DP tools were tested for reproducibility, as well as their ability to reflect soil variability and to estimate hydraulic conductivity, K. Although resolution differences exist, all of the applied methods captured the main aquifer structure. Correlations of the DP-based K estimates or proxies with DP slug tests (DPST) show that it is possible to describe the aquifer hydraulic structure on less than a metre scale by combining DPST data and continuous DP measurements. Although correlations are site-specific and appropriate DP tools must be chosen, DP is a reliable and efficient alternative for characterizing even strongly heterogeneous sites with complex sedimentary architectures.
机译:每个环境现场调查的目的都是勾勒出近地表(水文)地层单位及其特征。为了确定沉积物的类型和水力特性,直接推动(DP)传感器探头和工具是很有前途的方法,因此经常用于测量高分辨率的土壤特性垂直剖面。考虑到这些工具的多样性,本文的目的是比较在非均质非固结沉积含水层中用于(水文)地层地下特征的选定DP工具。概述了当前的DP应用,并测试了所选DP工具的可重复性,以及它们反映土壤变异性和估算水力传导率K的能力。尽管存在分辨率差异,但所有应用方法均捕获了主要含水层结构。基于DP的K估计值或代理与DP段塞测试(DPST)的相关性表明,通过组合DPST数据和连续DP测量,可以在不到一米的规模上描述含水层的水力结构。尽管相关性是针对特定地点的,并且必须选择适当的DP工具,但DP是可靠,有效的替代方法,用于表征具有复杂沉积构造的强异质性地点。

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