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Numerical simulations of nutrient transport changes in Honghu Lake Basin, Jianghan Plain

机译:江汉平原洪湖流域养分运移变化的数值模拟。

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Nutrients transported from catchments are one of the most important sources for lake eutrophication. In this study, the Honghu Lake Basin, located at the middle reaches of the Yangtze River, was chosen as the study area, and the watershed hydrological distribution model SWAT ( Soil Water Assessment Tool) was applied to evaluate the trajectory of watershed nutrient transportation over time. Based on the analysis of driving factors, three experiments corresponding to natural, traditional and modern agriculture processes respectively were designed to evaluate the changes of nutrient inputs from catchments under the three environments. The simulation results showed that there were variations in nutrient production and changes in the range and rate. For three periods of the experiments, TN concentrations have changed as 0.12 -> 0.31 -> 1.15 mg/L, and production as 420 -> 1650 -> 6522 T/a; while TP concentrations changed as 0.018 -> 0.057 -> 0.117 mg/L, and production as 78 -> 303 -> 665 T/a. The nutrient transportation experienced slowly long-term increases during 1840-1950, then showed a relatively rapid increase during the period of 1950-1980s and the period from 1980 to early 1990s, with increasing rate of 1.4% and 2.4% respectively. And from the later 1990s to now, an obviously increasing trend with 15% increasing rate occurred. The effect from human activities on the watershed nutrient transportation increased rapidly, and had become a dominant factor in changes of the nutrient transportation.
机译:从集水区运来的营养素是湖泊富营养化的最重要来源之一。本研究以长江中游洪湖流域为研究区域,采用流域水文分布模型SWAT(土壤水分评估工具)评估流域养分流失的轨迹。时间。在驱动因素分析的基础上,设计了分别与自然,传统和现代农业过程相对应的三个实验,以评估三种环境下流域营养输入的变化。模拟结果表明,养分产量存在差异,范围和速率也存在变化。在三个实验阶段中,TN浓度变化为0.12-> 0.31-> 1.15 mg / L,产量为420-> 1650-> 6522 T / a。 TP浓度变为0.018-> 0.057-> 0.117 mg / L,产量为78-> 303-> 665 T / a。在1840-1950年间,养分运移经历了长期缓慢的增长,然后在1950-1980年代和1980到1990年代初呈现出相对较快的增长,增长率分别为1.4%和2.4%。从1990年代后期到现在,出现了明显的增长趋势,增长率为15%。人类活动对流域养分输送的影响迅速增加,并已成为影响养分输送变化的主要因素。

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