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首页> 外文期刊>Journal of Applied Geophysics >A concept for calculating accumulated clay thickness from borehole lithological logs and resistivity models for nitrate vulnerability assessment
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A concept for calculating accumulated clay thickness from borehole lithological logs and resistivity models for nitrate vulnerability assessment

机译:从钻孔岩性测井和电阻率模型计算累积黏土厚度的概念,以评估硝酸盐的脆弱性

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摘要

We present a concept that combines lithological information from boreholes with resistivity information from geophysical data to produce an accumulated clay thickness (ACT) estimate as a proxy for assessing the vulnerability of the groundwater to contamination from nitrate. The groundwater's vulnerability to nitrate is strongly dependent on the hydraulic conductivity and the thickness of the protective layers. Low permeable clays in the overburden offer good protection to underlying aquifers by increasing the transit time. This means that the accumulated clay thickness is a good indicator for aquifer vulnerability to nitrate. In geophysically derived resistivity models clays are characterized by low electrical resistivity, but non-unique clay-sand resistivity transition prevents direct mapping of resistivity models to clay thickness. Within the ACT concept, a translator model linking the resistivity to the accumulated clay thickness is calibrated by borehole information, ensuring consistency between the resistivity and the borehole data. An accumulated clay thickness map of the aquifer overburden (e.g., top 30 m) is then calculated, based on the calibrated translatormodel and geophysically derived resistivity models. We demonstrate the concept on a large-scale nitrate vulnerability assessment survey in Denmark. The concept successfully delineates the clay-dominated areas that play a key role in the assessment of the aquifer's vulnerability to nitrate pollution.
机译:我们提出了一个概念,将井眼的岩性信息与地球物理数据的电阻率信息相结合,以产生累积的粘土厚度(ACT)估计值,作为评估地下水对硝酸盐污染的脆弱性的代理。地下水对硝酸盐的脆弱性在很大程度上取决于水力传导率和保护层的厚度。覆盖层中的低渗透性粘土通过增加渡越时间为下层含水层提供了良好的保护。这意味着累积的粘土厚度是含水层易受硝酸盐侵蚀的良好指标。在从地球物理推导的电阻率模型中,粘土的特征在于电阻率低,但非唯一的粘土-砂土电阻率跃迁阻止了电阻率模型与粘土厚度的直接映射。在ACT概念中,通过井眼信息校准将电阻率与累积的粘土厚度相关联的转换模型,以确保电阻率与井眼数据之间的一致性。然后根据校准的平移器模型和地球物理推导的电阻率模型,计算出含水层上覆层(例如顶部30 m)的累积粘土厚度图。我们在丹麦进行的大规模硝酸盐脆弱性评估调查中演示了该概念。该概念成功地勾勒出了以粘土为主的地区,这些地区在评估含水层对硝酸盐污染的脆弱性方面起着关键作用。

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