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Modification and evaluation of WEPP water table management model.

机译:WEPP地下水位管理模型的修改和评估。

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Three constructed Wetland-Reservoir-SubIrrigation Systems (WRSIS) have been built in Northwest Ohio. The overall goal of this study was to model the hydrology of a WRSIS using the Water Erosion Prediction Project (WEPP) model. Modifications were made in the water balance algorithms of the WEPP hillslope model to improve the model's capability for subsurface drained cropland.; Drain flow and water table depth predictions from WEPP were evaluated against measured drain flows from North Central Ohio and water table depths predicted using DRAINMOD. Results showed that (i) WEPP drain flow simulations produced large average deviations; (ii) daily drain flows were overpredicted for all storm events; and (iii) predicted cumulative drain flows at the end of the evaluation season for each year were almost four times larger than the measured drain flows. WEPP midspace water table depth predictions were very poor. WEPP does not predict continuous water table depths and it may not be truly simulating water table depth.; The WEPP hillslope model was modified to help improve the water balance, runoff, drain flow, and water table depth prediction capabilities for cropland where subsurface drainage, controlled drainage, and/or subirrigation systems exist or are planned. The modified model is WEPP-Water Table Management (WEPP-WTM). Most of the water balance algorithms related to subsurface drainage, controlled drainage, and subirrigation were taken from DRAINMOD. Upward flux rate from the water table was calculated using the concept of matrix flux potential.; The performance of the WEPP-WTM model in simulating runoff, drain flow, and water table depth for subsurface drained cropland conditions was tested against field measured data from two sites. Field data obtained from a North Central Ohio site were used to evaluate drain flow and runoff predictions. Water table depth predictions were evaluated against a field data set from Aurora, North Carolina. Overall, WEPP-WTM produced drain flow and runoff results similar to those from DRAINMOD and better than all of those obtained with WEPP. To evaluate the water table depth prediction accuracy of WEPP-WTM, standard errors were compared with those obtained from published results using DRAINMOD, ADAPT, and SWATREN. Overall, the predictions of water table depth from WEPP-WTM were very comparable to those from the other models.
机译:在俄亥俄州西北部已建立了三个湿地-水库-地下灌溉系统(WRSIS)。这项研究的总体目标是使用水蚀预测项目(WEPP)模型对WRSIS的水文学进行建模。 WEPP山坡模型的水平衡算法进行了修改,以提高该模型对地下排水农田的能力。针对来自俄亥俄州中北部的实测排水流量和使用DRAINMOD预测的地下水位深度,评估了WEPP的排水量和地下水位深度预测。结果表明:(i)WEPP排水流模拟产生较大的平均偏差; (ii)所有风暴事件的每日排水流量都被高估了; (iii)每年评估季节结束时的预计累积排水量几乎是实测排水量的四倍。 WEPP中空地下水位深度预测非常差。 WEPP不能预测连续的地下水位深度,也可能无法真正模拟地下水位的深度。修改了WEPP山坡模型,以帮助改善存在或计划进行地下排水,控制排水和/或地下灌溉系统的农田的水平衡,径流,排水流量和地下水位深度预测能力。修改后的模型是WEPP-水表管理(WEPP-WTM)。与地下排水,控制排水和地下灌溉有关的大多数水平衡算法均来自DRAINMOD。使用矩阵通量势的概念计算出地下水位的向上通量率。针对来自两个地点的现场测量数据,测试了WEPP-WTM模型在模拟地下排水农田条件下的径流量,排水流量和地下水位深度方面的性能。从俄亥俄州中北部的站点获得的现场数据用于评估排水流量和径流预测。根据北卡罗莱纳州奥罗拉的野外数据集评估了地下水位深度。总体而言,WEPP-WTM产生的排水流量和径流结果与DRAINMOD相似,并且优于所有使用WEPP获得的结果。为了评估WEPP-WTM的地下水位预测精度,将标准误差与使用DRAINMOD,ADAPT和SWATREN从已发布结果中获得的标准误差进行了比较。总体而言,WEPP-WTM对地下水位深度的预测与其他模型的预测非常可比。

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