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首页> 外文期刊>Hydrology and Earth System Sciences >Using an inverse modelling approach to evaluate the water retention in a simple water harvesting technique
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Using an inverse modelling approach to evaluate the water retention in a simple water harvesting technique

机译:使用逆建模方法以简单的集水技术评估保水率

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In arid and semi-arid zones, runoff harvesting techniques are oftenapplied to increase the water retention and infiltration on steepslopes. Additionally, they act as an erosion control measure toreduce land degradation hazards. Nevertheless, few efforts wereobserved to quantify the water harvesting processes of thesetechniques and to evaluate their efficiency. In this study, acombination of detailed field measurements and modelling with theHYDRUS-2D software package was used to visualize the effect of aninfiltration trench on the soil water content of a bare slope innorthern Chile. Rainfall simulations were combined with high spatialand temporal resolution water content monitoring in order toconstruct a useful dataset for inverse modelling purposes. Initialestimates of model parameters were provided by detailed infiltrationand soil water retention measurements. Four different measurementtechniques were used to determine the saturated hydraulicconductivity (Ksat) independently. The tensioninfiltrometer measurements proved a good estimator of the Ksat value and a proxy for those measured under simulated rainfall,whereas the pressure and constant head well infiltrometermeasurements showed larger variability. Six different parameteroptimization functions were tested as a combination of soil-watercontent, water retention and cumulative infiltration data.Infiltration data alone proved insufficient to obtain high modelaccuracy, due to large scatter on the data set, and water contentdata were needed to obtain optimized effective parameter sets withsmall confidence intervals. Correlation between the observed soilwater content and the simulated values was as high as R2=0.93for ten selected observation points used in the model calibrationphase, with overall correlation for the 22 observation points equalto 0.85. The model results indicate that the infiltration trench hasa significant effect on soil-water storage, especially at the baseof the trench.
机译:在干旱和半干旱地区,经常采用径流收集技术来增加陡坡上的保水量和入渗量。此外,它们还作为减少土地退化危害的侵蚀控制措施。然而,很少有人努力量化这些技术的集水过程并评估其效率。在这项研究中,结合详细的现场测量和建模与HYDRUS-2D软件包一起使用,以可视化渗滤沟对智利北部裸露坡地土壤水分的影响。降雨模拟与高时空分辨率的水含量监测相结合,以构建一个有用的数据集以进行逆建模。通过详细的入渗和土壤保水测量,可以提供模型参数的初始估计。分别采用四种不同的测量技术来确定饱和水力传导率( K sat )。张力渗滤仪的测量结果证明了 K sat 值的良好估计值,并且可以替代模拟降雨条件下的测量值,而压力和恒定压头井浸渗仪的测量结果则显示出较大的变异性。结合土壤水分,保水量和累积入渗数据对六个不同的参数优化函数进行了测试,仅由于入渗数据在数据集上分散较大,仅靠入渗数据不足以获得较高的模型精度,并且需要含水量数据来获得优化的有效参数置信区间小的集合。在模型校准阶段使用的十个选定观测点,观测到的土壤含水量与模拟值之间的相关性高达 R 2 = 0.93,与22个观测值的总体相关性点等于0.85。模型结果表明,入渗沟对土壤水的储藏有显着影响,尤其是在沟底。

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