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Estimation of irrigation return flow from paddy fields considering the soil moisture

机译:考虑土壤水分的稻田灌溉回流估算

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The objective of this study was to estimate irrigation return flow in irrigated paddy fields considering the soil moisture. The proposed model was applied to examine its feasibility with regard to the growing period of rice. Simulation results showed a good agreement between the observed and simulated values: root mean square error (RMSE) of 6.05-7.27mmdayp#, coefficient of determination (R po) of 0.72-0.73, and coefficient of efficiency (E) of 0.54-0.55. The estimated average annual irrigation return flow during the period from 1998 to 2001 was 306.2mm, which was approximately 25.7% of the annual irrigation amounts. Of this annual irrigation return flow, 14.1% was attributable to quick and 11.6% to delayed return flow. These results indicate that considerable amounts of irrigation water in the paddy fields were returned to streams and canals by surface runoff and groundwater discharge. The modeling assessment method proposed in this study can be used to manage agriculture water and estimate irrigation return flow under different hydrological and water management conditions.
机译:这项研究的目的是考虑土壤湿度来估计灌溉稻田的灌溉回流。所提出的模型用于检验其在水稻生长期方面的可行性。仿真结果表明,观测值与仿真值之间具有很好的一致性:均方根误差(RMSE)为6.05-7.27mmdayp#,测定系数(R po)为0.72-0.73,效率系数(E)为0.54-0.55 。 1998年至2001年期间,估计的年平均灌溉回流量为306.2mm,约占年灌溉量的25.7%。在每年的灌溉回流中,有14.1%归因于快速回流,而11.6%归因于延迟回流。这些结果表明,稻田中的大量灌溉水通过地表径流和地下水排放而返回溪流和运河。本研究提出的建模评估方法可用于管理农业用水并估算不同水文和水管理条件下的灌溉回流。

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