利用多元分析和多元线性回归模型分析空间地下水盐度

Kristin Ina Binna, R. Yanidar, S. M. P. Marendra, Herika Muhammad Taki, A. D. Astuti
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摘要

地下水开采量的增加将不可避免地带来海水入侵的威胁。本研究的目的是确定雅加达北部、雅加达西部和雅加达中部浅层地下水盐度的分布情况,并建立浅层地下水盐度分布的区域模型。本研究使用的数据来自地下水质量监测数据,这些数据来自大雅加达地区环境办公室于 2022 年发布的《地区环境状况手册》(SLHD),涉及雅加达北部、雅加达西部和雅加达中部共 121 个采样点。主要数据取自 6 个采样点,用于模型验证。研究首先使用层次聚类分析(HCA)方法对数据进行分组。结果发现盐度分布最密集的是第 3 组(3)。在剔除异常值后,使用多重线性分析方法,利用与海岸线的距离(X1)、水井深度(X2)和硬度(X3)变量,建立了一个模型,以确定 EC、TDS 和盐度分布对浅层地下水的影响。得出的结果如下: EC 模型YEC3 = -1.879+ (1.19.X1) + (5.08.X3).TDS 模型:YTDS3 = -2.211.30 + (0.81.x1) + (101.41.x2) + (4.07.x3)。盐度模型:Ysalinity3 = -0.07+ (6.75×10-5.X1) + (2.4×10-4.X3)。模型验证结果为 R2EC3 = 0.70;R2TDS3 = 0.92;R2salinity3 = 0.88。验证结果表明,EC 值为 21.14%,TDS 值为 8.21%,盐度值为 22.87%。这需要通过增加原始样本的数量来进一步研究。
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Analyzing Spatial Groundwater Salinity Using Multivariate Analysis and Multiple Linear Regression Models
The increase in the amount of groundwater withdrawal will inevitably pose a threat of seawater intrusion. The purpose of this research was to identify the distribution of shallow groundwater salinity in North Jakarta, West Jakarta and Central Jakarta and to develop a regional model of shallow groundwater salinity distribution. The data used in this study was that of the groundwater quality monitoring, obtained from the Regional Environment Status Book (SLHD), published by The Environment office of Greater Jakarta released in 2022, involving a total of 121 sample points in North Jakarta, West Jakarta, and Central Jakarta. The primary data was taken at 6 (six) sampling locations for model validation purposes. The study began with data grouping, using the Hierarchical Cluster Analysis (HCA) method. The results of identifying the highest distribution of salinity are in cluster 3 (three). A model was subsequently developed, after removing the outliers, with multiple linear analysis methods using the variable the distance from the coastline (X1), well depth (X2) and hardness (X3), to determine the influence of EC, TDS and salinity distribution in shallow groundwater. The results obtained are as follows; EC Models: YEC3 = -1.879+ (1.19.X1) + (5.08.X3). TDS models: YTDS3 = -2.211.30 + (0.81.X1) + (101.41.X2) + (4.07.X3). Salinity models: Ysalinity3 = -0.07+ (6.75×10-5.X1) + (2.4×10-4.X3). Model verification results for R2EC3 = 0.70; R2TDS3 = 0.92; R2salinity3 = 0.88. Validation results produce 21.14% for EC, 8.21% for TDS, and 22.87% for Salinity. This needs further research by increasing the number of primary samples.
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