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Modelling the hydrological processes of a Chinese lowland polder and identifying the key factors using an improved PHPS model

机译:建模中国低地圩区的水文过程,用改进的PHPS模型识别关键因素

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Improved hydrological processes simulation and identification of determinants are urgently needed in risk management to reduce socio-economic losses resulting from polder water problems. This paper improved the lowland Polder Hydrology and Phosphorus modelling System (called PHPS2.0) by coupling the PHPS, Modified Universal Soil Loss Equation (MUSLE), and Integrated Catchments model of Phosphorus dynamics (INCA-P). Then, based on the PHPS2.0 and data collected from the Jianwei polder in southeastern China, a boosted regression tree (BRT) algorithm was used to explore the key factors determining the temporal variations in polder discharge and phosphorus export. The results showed that PHPS2.0 achieved excellent agreements between the simulated and observed discharge, surface water and phosphorus. The model performance was significantly improved because field-scale phosphorus dynamics were considered. The water and phosphorus balances exhibited substantial seasonal changes, especially in terms of fertilization, crop harvest, and discharge. The temporal change in catchment discharge mainly depended on precipitation and evaporation, which accounted for 63.7% of the discharge variations. In contrast, the temporal variation in phosphorus export was determined by the crop cover and fertilizer application, which accounted for 75.4% of the phosphorus variation. To mitigate the phosphorus loss to downstream freshwater, it is recommended to remain crop residues, reduce the overuse of phosphorus chemical fertilizers, and draft emergency plans. This study expands the knowledge of the relationship between polder environmental factors and hydrological processes and provides guidance for pollution controls.
机译:改善水文过程的模拟和鉴定,迫切需要在风险管理中迫切需要,以减少圩区水问题导致的社会经济损失。本文通过耦合PHPS,改进的通用土壤损失方程(MOSE)和磷动力学集成集水模型,改善了低地膨胀器水文和磷造型系统(称为PHPS2.0),磷动力学(INCA-P)。然后,基于从中国东南部的建3S圩区收集的PHPS2.0和数据,用于探讨确定圩区排放和磷输出的时间变化的关键因素。结果表明,PHPS2.0在模拟和观察到的放电,地表水和磷之间实现了良好的协议。模型性能显着提高,因为考虑了场尺度磷动力学。水和磷余额表现出大量的季节变化,特别是在受精,作物收获和放电方面。集水区排放的时间变化主要取决于沉淀和蒸发,占排放变化的63.7%。相比之下,磷原味的时间变化由作物覆盖和肥料应用确定,占磷变异的75.4%。为了减轻下游淡水的磷损失,建议仍然是作物残留物,减少过量使用的磷化肥,以及紧急计划草案。本研究扩大了对圩区环境因素和水文过程之间关系的知识,并为污染管制提供了指导。

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