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Estimating groundwater recharge and its associated uncertainty: Use of regression kriging and the chloride mass balance method

机译:估算地下水补给及其相关不确定性:使用回归克里格和氯化物质量平衡法

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The chloride mass balance method of estimating groundwater recharge is generally applied at a point scale but water resources management generally requires information at a regional scale. To estimate groundwater recharge regionally previously used upscaling methods have ranged from simple averaging to empirical relationships and geostatistical interpolation. This study combined the best components of these methods by using regression kriging: in data-sparse areas the recharge is upscaled using global regression equations with gridded rainfall and surface geology as covariates, while in data-dense areas the kriging of the regression equation residuals ensures that the upscaled recharge estimates respect the point estimates of recharge. The uncertainty in the recharge estimates was quantified using 1000 stochastic replicates of the chloride deposition of rainfall, the chloride exported in runoff, the chloride concentration of the groundwater and the regression equations used to perform the upscaling. This study focused on the coal bearing Sydney, Gunnedah, Gloucester and Surat Basins of Eastern New South Wales (Australia). Historically, groundwater recharge to the Permian units of these basins has received little attention due to their low yields of poor quality water. The increased potential extraction of regional groundwater due to coal development has demanded a greater understanding of the water balance. We found that recharge is highest in the younger productive aquifers (up to 20% of long-term mean annual rainfall) and lowest in the Permian units (-1% of long-term mean annual rainfall). The magnitude of the uncertainty is often close to the magnitude of the median recharge estimate. The method developed here for upscaling the point estimates of recharge using the chloride mass balance provides robust estimates of recharge and its associated uncertainty. The method is applicable to any regional study with variable density input data. Crown Copyright (C) 2017 Pub
机译:估计地下水补给的氯化物质量平衡方法通常以点规模应用,但水资源管理通常需要在区域规模上提供信息。为了估计地下水再充电,以前使用的升高方法从简单的平均到经验关系和地统计插值。本研究将这些方法的最佳组成部分结合使用回归克里格:在数据稀疏区域中,使用全球回归方程的充值是使用与Cridded降雨的全局回归方程,作为协变量,而在数据密度区域中,回归方程残留的克里明确保了回归方程残留的克里明上升的充值估计尊重充值点估计。使用1000个随机重复的降雨量的氯化物沉积的随机复制量化,在径流中出口的氯化物,地下水的氯化物浓度和用于执行升级的回归方程的氯化物浓缩的不确定性。本研究专注于煤炭轴承悉尼,Gunnedah,Gloucester和东部新南威尔士州(澳大利亚)的苏拉特盆地。从历史上看,由于它们低质量水的产量低,地下水对这些盆地的二叠单位进行了很少的关注。由于煤炭发展导致的区域地下水的增加的潜在提取要求更大了解水平。我们发现,在年轻的生产含水层(长期平均年度降雨量的高达20%的高达20%)中的充电最高,在二叠单位中最低(占长期平均年降雨量的1%)。不确定性的幅度通常接近中值充电估计的大小。这里开发的方法用于使用氯质量平衡来提高充电点估计,提供了对充电的稳定估计及其相关的不确定性。该方法适用于具有可变密度输入数据的任何区域研究。皇冠版权(c)2017酒吧

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