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首页> 外文期刊>Water resources research >Predicting hydrofacies and hydraulic conductivity from direct-push data using a data-driven relevance vector machine approach: Motivations, algorithms, and application
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Predicting hydrofacies and hydraulic conductivity from direct-push data using a data-driven relevance vector machine approach: Motivations, algorithms, and application

机译:使用数据驱动的相关向量机方法从直接推算数据预测水相和水力传导率:动机,算法和应用

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摘要

The spatial heterogeneity of hydraulic conductivity (K) exerts a major control on groundwater flow and solute transport. The heterogeneous spatial distribution of K can be imaged using indirect geophysical data as long as reliable relations exist to link geophysical data to K. This paper presents a nonparametric learning machine approach to predict aquifer K from cone penetrometer tests (CPT) coupled with a soil moisture and resistivity probe (SMR) using relevance vector machines (RVMs). The learning machine approach is demonstrated with an application to a heterogeneous unconsolidated littoral aquifer in a 12 km(2) subwatershed, where relations between K and multiparameters CPT/SMR soundings appear complex. Our approach involved fuzzy clustering to define hydrofacies (HF) on the basis of CPT/SMR and K data prior to the training of RVMs for HFs recognition and K prediction on the basis of CPT/SMR data alone. The learning machine was built from a colocated training data set representative of the study area that includes K data from slug tests and CPT/SMR data up-scaled at a common vertical resolution of 15 cm with K data. After training, the predictive capabilities of the learning machine were assessed through cross validation with data withheld from the training data set and with K data from flowmeter tests not used during the training process. Results show that HF and K predictions from the learning machine are consistent with hydraulic tests. The combined use of CPT/SMR data and RVM-based learning machine proved to be powerful and efficient for the characterization of high-resolution K heterogeneity for unconsolidated aquifers.
机译:水力传导率(K)的空间异质性对地下水流量和溶质运移具有重要控制作用。只要存在可靠的关系将地球物理数据链接到K,就可以使用间接地球物理数据对K的异质空间分布进行成像。本文提出了一种非参数学习机方法,可通过锥形渗透仪测试(CPT)结合土壤湿度来预测含水层K和使用相关矢量机(RVM)的电阻率探头(SMR)。学习机方法通过在12 km(2)小流域中的非均质非固结滨海含水层中的应用得到了证明,其中K和多参数CPT / SMR测深之间的关系显得复杂。我们的方法包括在训练RVM进行HF识别和仅基于CPT / SMR数据进行K预测之前,基于CPT / SMR和K数据进行模糊聚类以定义水相(HF)。该学习机由代表研究区域的同一地点的训练数据集构建而成,该数据集包括来自子弹测试的K数据和以15 cm的常见垂直分辨率与K数据按比例放大的CPT / SMR数据。训练后,通过交叉验证对学习机的预测能力进行评估,交叉验证使用的是训练数据集中保留的数据,以及来自训练过程中未使用的流量计测试的K数据。结果表明,学习机的HF和K预测与液压测试一致。 CPT / SMR数据和基于RVM的学习机的结合使用被证明对非固结含水层的高分辨率K异质性进行表征是强大而有效的。

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