Statistical Modeling for Spatial Groundwater Potential Map Based on GIS Technique

被引:16
作者
Azma, Aliasghar [1 ]
Narreie, Esmaeil [2 ]
Shojaaddini, Abouzar [3 ]
Kianfar, Nima [4 ]
Kiyanfar, Ramin [5 ]
Alizadeh, Seyed Mehdi Seyed [6 ]
Davarpanah, Afshin [7 ]
机构
[1] Beijing Univ Technol, Coll Architecture & Civil Engn, Beijing 100124, Peoples R China
[2] Grad Univ Adv Technol, Fac Civil & Surveying Engn, Dept Surveying Engn, Kerman 7631133131, Iran
[3] Tarbiat Modares Univ, Coll Agr, Soil Sci Dept, Tehran 14115336, Iran
[4] KN Toosi Univ Technol, Fac Geodesy & Geomat Engn, Tehran 158754416, Iran
[5] Payame Noor Univ, Dept Art & Architecture, Shiraz 193954697, Iran
[6] Australian Coll Kuwait, Petr Engn Dept, West Mishref 13015, Kuwait
[7] Aberystwyth Univ, Dept Math, Aberystwyth SY23 3FL, Dyfed, Wales
关键词
carbonate aquifer; digital elevation model; modeling; multivariate linear regression; principal component regression; groundwater quality assessment;
D O I
10.3390/su13073788
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In arid and semi-arid lands like Iran water is scarce, and not all the wastewater can be treated. Hence, groundwater remains the primary and the principal source of water supply for human consumption. Therefore, this study attempted to spatially assess the groundwater potential in an aquifer in a semi-arid region of Iran using geographic information systems (GIS)-based statistical modeling. To this end, 75 agricultural wells across the Marvdasht Plain were sampled, and the water samples' electrical conductivity (EC) was measured. To model the groundwater quality, multiple linear regression (MLR) and principal component regression (PCR) coupled with elven environmental parameters (soil-topographical parameters) were employed. The results showed that that soil EC (SEC) with Beta = 0.78 was selected as the most influential factor affecting groundwater EC (GEC). CaCO3 of soil samples and length-steepness (LS factor) were the second and third effective parameters. SEC with r = 0.89 and CaCO3 with r = 0.79 and LS factor with r = 0.69 were also characterized for PC1. According to performance criteria, the MLR model with R-2 = 0.94, root mean square error (RMSE) = 450 mu Scm(-1) and mean error (ME) = 125 mu Scm(-1) provided better results in predicting the GEC. The GEC map indicated that 16% of the Marvdasht groundwater was not suitable for agriculture. It was concluded that GIS, combined with statistical methods, could predict groundwater quality in the semi-arid regions.
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页数:18
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