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首页> 外文期刊>Journal of Hydrology >Estimating groundwater recharge using the SMAR conceptual model calibrated by genetic algorithm
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Estimating groundwater recharge using the SMAR conceptual model calibrated by genetic algorithm

机译:使用遗传算法校准的SMAR概念模型估算地下水补给量

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摘要

Proper groundwater management of a contaminated aquifer requires the accurate estimation of groundwater recharge, which carries the contaminated load. There are many direct and indirect methods and sophisticated models for estimating recharge. However, most of them require many field data or model parameters, which limit their actual field application. To overcome this limitation, the Soil Moisture Accounting and Routing (SMAR), a conceptual rainfall-runoff model, is employed. The SMAR model has the potential for estimating recharge using only rainfall, evaporation and groundwater level data. However, for an aquifer having prominent horizontal groundwater flow, this model cannot be used directly. For this reason a horizontal flow component is added to this model. Model parameters are calibrated by the Genetic Algorithm (GA) optimization technique. Sensitivity of calibrated parameters to model efficiency and estimated recharge, and parameter interdependence are investigated. This model is applied to 11 observation locations in four catchment areas of Miyakojima Island, Japan, where groundwater nitrate contamination is a threat. The effectiveness of the model is evaluated using the model efficiency (R-2), the mean of the sum of square errors (MSE), plots of observed versus estimated groundwater levels, scatter plots of observed versus estimated groundwater levels, measure of timing of the peaks, and the correlation between monthly rainfall and monthly estimated recharge. All show that this technique is very efficient for estimation of recharge. Model efficiency (R-2) up to 92%, minimum MSE 0.32 m(2)/day, average relative error of timing of the peaks 4.13%, and coefficient of determination (r(2)) up to 0.92 are obtained for the study area. The estimated recharge is 45% of the mean annual rainfall and agrees with other finding. It is thus concluded that the SMAR model could be a viable alternative since it can estimate dependable recharge with a minimum of input data. (c) 2004 Elsevier B.V. All rights reserved.
机译:对受污染的含水层进行正确的地下水管理需要准确估算地下水的补给量,而该补给量将承担被污染的负荷。有许多直接和间接的方法以及用于估计充电量的复杂模型。然而,它们中的大多数需要许多现场数据或模型参数,这限制了其实际的现场应用。为了克服这一限制,采用了土壤水分核算和路由(SMAR),一种概念性的降雨径流模型。 SMAR模型具有仅使用降雨,蒸发和地下水位数据估算补给量的潜力。但是,对于水平地下水流较大的含水层,不能直接使用该模型。因此,将水平流分量添加到该模型。模型参数通过遗传算法(GA)优化技术进行校准。研究了校准参数对模型效率和估计补给的敏感性以及参数相互依赖性。该模型适用于日本宫古岛四个集水区的11个观测地点,那里地下水受到硝酸盐污染的威胁。使用模型效率(R-2),平方误差总和(MSE)的平均值,实测水位与估算地下水位的关系图,实测水位与估算地下水位的散点图,测量时间的时序来评估模型的有效性峰值,以及每月降雨量和每月估算补给量之间的相关性。所有人都表明,该技术对于评估充电非常有效。获得了高达92%的模型效率(R-2),最小MSE 0.32 m(2)/天,峰定时的平均相对误差4.13%和高达0.92的测定系数(r(2))。学习区。估计的补给量为年平均降雨量的45%,与其他发现一致。因此可以得出结论,SMAR模型可以作为可行的替代方案,因为它可以用最少的输入数据估算可靠的补给。 (c)2004 Elsevier B.V.保留所有权利。

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