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Groundwater quality assessment of Birjand plain aquifer using kriging estimation and sequential Gaussian simulation methods

机译:使用Kriging估计和顺序高斯模拟方法的Birjand普通含水层的地下水质量评估

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The performance of geostatistical estimation methods of ordinary kriging and sequential Gaussian simulation have been investigated in this study to evaluate the qualitative characteristics of groundwater in Birjand plain. For that purpose, 81 water samples were collected from groundwater wells and thirteen hydro-chemical parameters of calcium (Ca), chlorine (Cl), electrical conductivity (EC), bicarbonate (HCO3-), magnesium (Mg), sodium percent (Na%), sodium (Na), sodium absorption ratio (SAR), sulfate (SO42-), total dissolved solids (TDS) and total hardness (TH) were analyzed and interpreted. Variography of the variables was performed after the normalization and experimental variograms were plotted in GS(+). The best theoretical models were then fitted to the experimental variograms. Validation of variograms was performed by two methods of cross-validation and residual analysis. Geostatistical estimation maps were then prepared for each groundwater variable. Since the smoothing effect is one of the major drawbacks of ordinary kriging estimations, the sequential Gaussian simulation method was also used to prepare the simulation maps of variables. The simulation results were more reliable than those obtained by ordinary kriging.
机译:本研究已经研究了普通克里格汀和顺序高斯模拟地质稳态估计方法的性能,以评估BIRJAND平原地下水的定性特征。为此目的,从地下水井和13个水化学参数中收集81个水样,钙(CA),氯(Cl),电导率(EC),碳酸氢盐(HCO3-),镁(Mg),钠百分比(NA)分析并解释了%),硫酸钠(Na),钠吸收比(SAR),硫酸钠(SO 42-),总溶解固体(TDS)和总硬度(TH)。在归一化之后进行变量的变形例,并且在GS(+)中绘制了实验变异函数。然后适用于实验变异函数的最佳理论模型。通过两种交叉验证和残余分析进行变速仪的验证。然后为每个地下水变量准备地质统计估计图。由于平滑效果是普通Kriging估计的主要缺点之一,因此还用于制备变量的模拟映射的顺序高斯仿真方法。仿真结果比普通克里格获得的仿真结果更可靠。

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