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General Solution for Tidal Behavior in Confined and Semiconfined Aquifers Considering Skin and Wellbore Storage Effects

机译:考虑皮肤和井筒储存效果的密闭和半核含水层中的潮汐行为的一般解决方案

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摘要

Tidal analysis provides a cost-effective way of estimating aquifer properties. Tidal response models that link aquifer properties with tidal signal characteristics, such as phase and amplitude, have been established in previous studies, but none of the previous models incorporate the skin effect. It is found in this study that the skin effect and the wellbore storage effect can have significant influence on the results of tidal analysis and should be included in tidal response models. New models are proposed with skin and wellbore storage effects fully incorporated so that aquifer information can be assessed more accurately based on tidal analysis. The models can be applied to confined aquifers with only horizontal flow or semiconfined aquifers with both horizontal flow and vertical flow. For confined aquifers, the new model indicates that positive skin leads to larger phase lag between the tidal response the the theoretical tide, and negative skin can reduce the phase lag or even cause a phase advance. For semiconfined aquifers, both the skin effect and the vertical flow affect the phase difference between the tidal response and the theoretical tide, and with the proposed model, contribution from these two sources can be separated and analyzed independently, making it feasible to evaluate semiconfined aquifer properties considering both factors. Increasing wellbore storage causes larger phase lag or smaller phase advance for both types of aquifers. Real-world examples for confined and semiconfined aquifers are analyzed, respectively, to demonstrate practical applications of the proposed models.
机译:潮汐分析提供了估计含水层特性的成本效益的方法。在先前的研究中建立了与潮汐信号特性的潮汐响应模型,例如相位和幅度,但之前的模型都没有包含皮肤效果。在这项研究中发现,皮肤效应和井筒储存效果可能对潮汐分析结果产生重大影响,并且应包括在潮汐响应模型中。建议使用皮肤和井筒存储效果的新模型完全纳入,以便可以根据潮汐分析更准确地评估含水层信息。该模型可以应用于仅具有水平流和垂直流程的水平流量或半挤出的含水层的受限含水层。对于狭窄的含水层,新模型表明,阳性皮肤在潮汐响应之间导致较大的阶段滞后,理论潮,阴性皮肤可以减少相滞后或甚至导致相位进步。对于半核含水层,皮肤效应和垂直流动都会影响潮汐响应和理论潮之间的相位差,并且随着所提出的模型,可以独立分离和分析这两个来源的贡献,从而可以评估半挤出的含水层考虑两个因素的物业。增加井筒存储会导致两种类型的含水层的相位滞后或较小的相位进步。分别分别分析了狭窄和半核含水层的实际示例,以展示所提出的模型的实际应用。

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  • 来源
    《Water resources research》 |2020年第6期|e2020WR027195.1-e2020WR027195.20|共20页
  • 作者单位

    Stanford Univ Dept Energy Resources Engn Stanford CA 94305 USA;

    Stanford Univ Dept Energy Resources Engn Stanford CA 94305 USA|Univ Tokyo Grad Sch Engn Tokyo Japan;

    Stanford Univ Dept Energy Resources Engn Stanford CA 94305 USA;

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  • 正文语种 eng
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