水文地质、测井和机器学习对干旱地区含水层水力特性预测的贡献:以埃及Farafra绿洲努比亚砂岩含水层为例

IF 5.7 3区 环境科学与生态学 Q1 WATER RESOURCES
Ahmed Nosair, Muhammad Nabih, Ahmed Bakry
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引用次数: 0

摘要

在水文地质学中,评估含水层的关键水力参数,如透射率(T)、导电性(K)和孔隙度(PHIE),对于有效的地下水管理至关重要。传统上,这些参数是通过泵送试验和测井数据获得的。然而,大多数地下水井往往缺乏孔隙度测井。虽然中子密度测井通常用于孔隙度估算,但由于地下水勘探中记录的测井资料很少,因此我们的研究独特地使用电阻率测井来计算孔隙度。因此,本研究旨在利用常规测井和水文地质数据,利用机器学习(ML)算法,包括随机森林(RF)、梯度增强(GB)、线性回归(LR)和支持向量机(SVM),预测T、K和PHIE。该方法应用于埃及法拉法拉绿洲的努比亚砂岩含水层(NSA)的案例研究。首先,通过分析10口井的长时间泵送试验记录,确定了T和k值。通过测试井,对ML算法在预测渗透率和导流率方面的性能进行了严格评估。RF模型具有较高的精度,W-6井的T和K预测值分别为113.11 m2/h和0.2271 m/h, W-8井的T和K预测值分别为104.15 m2/h和0.1867 m/h。实际值和预测值之间的密切一致强调了RF模型在估计这些参数方面的可靠性,有效地识别了数据集中的基本趋势。对于孔隙度预测,RF和GB模型与log-derived PHIE具有良好的相关性,相关系数分别为0.95和0.96。相比之下,LR模型的表现尚可,而SVM模型的相关性相对较低。这些发现突出了ML模型,特别是RF和GB模型在准确预测关键含水层水力参数方面的潜力,从而增强了对地下水含水层的理解和管理。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Contribution of hydrogeological, well logs and machine learning in predicting the aquifer hydraulic properties in arid regions: a case study of Nubian Sandstone aquifer, Farafra Oasis, Egypt

In hydrogeology, assessing key aquifer hydraulic parameters such as transmissivity (T), hydraulic conductivity (K), and porosity (PHIE) is crucial for effective groundwater management. Traditionally, these parameters are obtained through pumping tests and well log data. However, porosity logs are often lacking in most groundwater wells. While neutron density logs are commonly used for porosity estimation, our study uniquely employs resistivity logs to calculate porosity due to the scarcity of recorded logs in groundwater exploration. Consequently, this research aims to use conventional well log and hydrogeological data to predict T, K, and PHIE using machine learning (ML) algorithms, including random forest (RF), gradient boosting (GB), linear regression (LR), and support vector machines (SVM). This methodology is applied as a case study in the Nubian Sandstone Aquifer (NSA) in Farafra Oasis, Egypt. Firstly, T and k values were determined by analysis of the long duration pumping test records for ten wells penetrated the NSA. The performance of the ML algorithms in predicting transmissivity and hydraulic conductivity was rigorously evaluated using test wells. The RF model demonstrated superior accuracy, with predicted values of T and K being 113.11 m2/h and 0.2271 m/h in well W-6, and 104.15 m2/h and 0.1867 m/h in well W-8, respectively. The close agreement among actual and predicted values underscores the RF model’s reliability in estimating these parameters, effectively identifying the fundamental trends within the dataset. For porosity prediction, the RF and GB models exhibited excellent correlation with log-derived PHIE, achieving correlation coefficients of 0.95 and 0.96, respectively. In contrast, the LR model showed acceptable performance, while the SVM model had comparatively lower correlation. These findings highlight the potential of ML models, particularly RF and GB, in accurately predicting key aquifer hydraulic parameters, thereby enhancing the understanding and management of the groundwater aquifers.

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来源期刊
Applied Water Science
Applied Water Science WATER RESOURCES-
CiteScore
9.90
自引率
3.60%
发文量
268
审稿时长
13 weeks
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