位置:首页 >地球科学 >地球化学与地球物理学 >Acta Geophysica >A comparative study of artificial neural networks and multivariate regression for predicting groundwater depths in the Arak aquifer

人工神经网络和多元回归预测阿拉克含水层地下水深度的比较研究

A comparative study of artificial neural networks and multivariate regression for predicting groundwater depths in the Arak aquifer

作者:Javad Varvani,

发表时间:2024年

  • 文献详情
  • 相似文献

摘要

近年来,阿拉克平原地下水资源严重紧张,部分地区因水井干涸,增加了井的深度以获取水。一些地区地下水埋深较高,未来将导致这些土地盐碱化。使用区域模型来组织和衡量阿拉克平原地下水资源对不同管理和实施方案的响应。本研究旨在调查地下水埋深的影响因素,为阿拉克平原含水层的多元线性回归(MLR)方法提供区域模型。为此,阿拉克平原的平均地下水潜力图(GPM)作为因变量,以及含水层的透射率、地下水开采值、海拔、该地区的平均降水量、蒸发量和距离水资源被视为自变量,并在 SPSS 软件介质中进行回归分析。这样做是为了呈现一个线性模型。在下一阶段,通过将所提出的模型应用到不使用其统计数据和信息来呈现模型的地方来评估所提出的模型,最后,通过在GIS环境中应用该模型,创建该地区的GPM。研究已准备就绪。此外,还使用人工神经网络(ANN)来模拟地下水的深度。人工神经网络的性能是通过均方根误差 (RMSE) 以及实际输出和期望输出之间的相关系数 (R) 等参数来衡量的。两种方法的结果表明,含水层的渗透率、GPM 下降、地形(流域水平上井场的高度)、井最大作业半径处的地下水开采值以及距水资源的距离是毛利率下降的主要因素。但 ANN 在估计 GPM 回撤方面的有效性高于 MLR 方法。所实施的方法可以推广到其他存在地下水管理缺水问题的流域。


Abstract

In recent years, the groundwater resources of Arak plain have been under severe stress, so in some areas, due to the drying up of wells, the depth of wells has increased to access water. In some areas, the groundwater depth is high, which will lead to the salinization of those lands in the future. Regional modeling was used to organize and measure the response of the groundwater resources of Arak plain against the implementation of different management and implementation scenarios. This study aims to investigate the effective factors in the groundwater depth to provide a regional model with multiple linear regression (MLR) methods for Arak plain aquifer. For this purpose, the average groundwater potential maps (GPMs) in the Arak plain, as a dependent variable, and the transmissivity of the aquifer formations, groundwater exploitation values, altitude, average precipitation of the region, the amount of evaporation, and the distance from water resources are considered independent variables and regression analysis is done in SPSS software media. It was done to present a linear model. In the next stage, the presented model was evaluated by applying it to places where its statistics and information were not used to present the model, and finally, by applying this model in the GIS environment, the GPMs for the region were created. The study was prepared. Also, an artificial neural network (ANN) was used to simulate the depth of underground water. The performance of the ANN was measured through parameters such as root-mean-square error (RMSE) and correlation coefficient between real and desired outputs (R). The results of both methods indicate that factors such as the transmissivity of aquifer formations, GPMs drawdown, topography (the height of the well site on the level of the watershed), the groundwater exploitation values at the maximum operating radius of the well, and the distance from water resources are the main factors of GPMs drawdown. But the effectiveness of ANN in estimating GPMs drawdown is higher than the MLR method. The implemented methodology could be generalized to other watersheds with water scarcity problems for groundwater management.