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Identifying influencing wells for gradient estimation in the confined portion of the Gulf Coast aquifer near Kingsville, TX

机译:在德克萨斯州金斯维尔附近的墨西哥湾沿岸含水层受限区域中确定影响井,进行梯度估算

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Hydraulic gradient is a fundamental aquifer characteristic required to estimate groundwater flow and quantify advective fluxes of pollutants. Graphical and local estimation schemes using potentiometric head information from three or four wells are used to compute hydraulic gradients but suffer from imprecision and subjectivity. The use of linear regression is recommended when hydraulic head data from a groundwater monitoring network consisting of several wells are available. In such cases, statistical influence analysis can be carried out to evaluate how each well within the network impacts the gradient estimate. A suite of five metrics, namely-(1) the hat-values, (2) studentized residuals, (3) Cook's distance, (4) DFBETAs and (5) Covariance ratio (COVRATIO) are used in this study to identify influential wells within a regional groundwater monitoring network in Kleberg County, TX. The hat-values indicated that the groundwater network was reasonably well balanced and no well exerted an undue influence on the regression. The studentized residuals and Cook's distance indicated the wells with the highest influence on the regression predictions were those that were close to high groundwater production centers or affected by coastal-aquifer interactions. However, the wells in the proximity of the production centers had the highest impact on the estimated gradient values as ascertained using DFBETAs. The covariance ratio which indicates the sensitivity of a monitoring well on the estimated standard error of regression was noted to be significant at most wells within the network. Therefore, networks seeking to address changes in groundwater gradients due to climate and anthropogenic influences need to be denser than those used to ascertain synoptic gradient estimates alone. The magnitude of the groundwater velocity was greatly underestimated when the influential wells were excluded from the network. The direction of flow was affected to a lesser extent, but a complete gradient reversal was noted when the network consisted of only four peripheral wells. The influence analysis therefore provides a valuable tool to assess the importance of individual wells within a monitoring network and can therefore be useful when existing networks are to be pruned due to fiscal constraints.
机译:水力梯度是估算地下水流量和量化污染物平流所需的基本含水层特征。使用来自三个或四个井的电位头信息的图形和局部估计方案用于计算水力梯度,但存在不精确和主观性的问题。当可获得由几口井组成的地下水监测网络的水头数据时,建议使用线性回归。在这种情况下,可以进行统计影响分析以评估网络中的每个井如何影响梯度估计。本研究中使用了一组五个指标,即-(1)帽值,(2)学生化残差,(3)Cook距离,(4)DFBETAs和(5)协方差比(COVRATIO)来确定有影响力的井在德克萨斯州克莱伯格县的区域地下水监测网络中。帽值表明,地下水网络平衡良好,没有对回归产生过大的影响。学生化的残差和库克距离表明,对回归预测影响最大的井是那些靠近地下水高产中心或受沿海-含水层相互作用影响的井。但是,使用DFBETA确定的,生产中心附近的油井对估计的梯度值影响最大。协方差比表明监测井对估计的回归标准误差的敏感性,在网络中的大多数井中都非常重要。因此,寻求解决由于气候和人为影响而引起的地下水梯度变化的网络比用于确定天气梯度估计值的网络更密集。当将有影响的井排除在网络之外时,地下水流速的幅度被大大低估了。流动的方向受到的影响较小,但是当网络仅由四个外围井组成时,可以观察到完全的梯度反转。因此,影响分析提供了一种有价值的工具,可用于评估监控网络中各个井的重要性,因此在由于财政限制而要修剪现有网络时可能很有用。

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