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Application of system dynamics approach for time varying water balance in aerobic paddy fields

机译:系统动力学方法在需氧稻田水平衡时变中的应用

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Increasing water scarcity has necessitated the development of irrigated rice systems that require less water than the traditional flooded rice. The cultivation of aerobic rice is an effort to save water in response to growing worldwide water scarcity with the pressure to reduce water use and increase water productivity. An accurate estimation of different water balance components at the aerobic rice fields is essential to achieve effective use of limited water supplies. Some field water balance components, such as percolation, capillary rise and evapotranspiration, can not be easily measured; therefore a soil water balance model is required to develop and to test water management strategies. This paper presents results of a study to quantify time varying water balance under a critical soil water tension based irrigation criteria for the cultivation of non-ponded “aerobic rice” fields along the lower parts of the Yellow River. Based on the analysis and integration of existing field information on the hydrologic processes in an aerobic rice field, this paper outlines the general components of the water balance using a conceptual model approach. The time varying water balance is then analyzed using the feedback relations among the hydrologic processes in a commercial dynamic modeling environment, Vensim. The model simulates various water balance components such as actual evapotranspiration, deep percolation, surface runoff, and capillary rise in the aerobic rice field on a daily basis. The model parameters are validated with the observed experimental field data from the Huibei Irrigation Experiment Station, Kaifeng, China. The validated model is used to analyze irrigation application soil water tension trigger under wet, dry and average climate conditions using daily time steps. The scenario analysis show that to conserve scarce water resources during the average climate years the irrigation scheduling criteria can be set as ?30 kPa average root zone soil water tension; whereas it can be set at ?70 kPa during the dry years, however, the associated yields may reduce. Compared with the flooded lowland rice and other upland crops, with these two alternatives irrigation event triggers, aerobic rice cultivation can lead to significant water savings.
机译:日益严重的缺水状况导致必须发展灌溉水稻系统,该系统所需的水量要少于传统的淹没水稻。有氧水稻的种植是为了应对全球日益缺水的问题,以减少用水和提高水生产率的压力来节水。对有氧稻田中不同水分平衡成分的准确估算对于有效利用有限的供水至关重要。某些田间水平衡要素,例如渗滤,毛细血管上升和蒸散量,不易测量。因此,需要土壤水平衡模型来开发和测试水管理策略。本文提出了一项研究结果,以量化基于临界土壤水分张力的灌溉标准下的时变水平衡,用于沿黄河下游种植无池塘的“好氧稻田”。在对已有的稻田水文过程中水文过程的现场信息进行分析和整合的基础上,本文使用概念模型方法概述了水平衡的一般组成部分。然后使用商业动态建模环境Vensim中水文过程之间的反馈关系来分析随时间变化的水平衡。该模型每天模拟需氧稻田中的各种水分平衡成分,例如实际蒸散量,深层渗滤,地表径流和毛细血管上升。通过从中国开封市惠北灌溉实验站观察到的实验现场数据验证了模型参数。经过验证的模型用于分析灌溉应用中土壤水分张力的触发条件,包括每天的湿,干和平均气候条件。情景分析表明,为保护平均气候年稀缺的水资源,灌溉调度标准可设置为?30 kPa平均根区土壤水分张力。尽管在干旱年份可以将其设置为?70 kPa,但是相关的产量可能会降低。与淹没的低地水稻和其他陆地作物相比,通过这两种替代灌溉事件触发因素,有氧水稻种植可以节省大量水。

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