首页|基于径流事件的农业面源监测采样间隔分析

基于径流事件的农业面源监测采样间隔分析

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选择丹江口库区的五龙池小流域为对象,以典型降雨径流事件的水质水量加密监测数据作为径流过程真实值,通过不同时间间隔和水量间隔模拟采样,分析污染负荷通量估算误差,并确定有效采样间隔。结果显示,五龙池小流域降雨径流事件具有明显的峰值特征(初始流量55m3/h,峰值流量977。3m3/h),TP浓度与径流高度同步(初始浓度为0。05mg/L,峰值浓度为0。25mg/L),TN随径流达到峰值后下降不明显(初始浓度为2mg/L,峰值浓度为8mg/L)。模拟采样表明,时间间隔 5,10,15,20,30,60,120,240,480,720min,采样点数量从 1957 个减少到 14 个;水量间隔 16,32,64,128,256,384,576,800,1600,3200m3,采样点数量从2893个减少到14个;水量间隔采样对径流峰值的捕捉能力明显高于时间间隔采样。负荷估算误差显示,TP误差波动大于TN;以± 5%作为允许的误差范围,降雨径流事件采样监测的有效时间间隔为120min,有效水量间隔为1600m3。
Analysis of sampling interval for monitoring of agricultural non-point sources based on runoff events
The Wulongchi small watershed in Danjiangkou Reservoir area was selected as the object,and the real value of runoff process was taken from the High-frequency monitoring data of typical rainfall runoff events.The error of pollution load flux estimation was analyzed by simulating sampling at different time intervals and water intervals,and the effective sampling interval was determined.The results showed that the rainfall runoff event in Wulongchi Basin had obvious peak characteristics(initial discharge 55m3/h,peak discharge 977.3m3/h),the total phosphorus concentration was highly synchronized with the runoff(initial concentration 0.05mg/L,peak concentration 0.25mg/L),and the total nitrogen did not decrease significantly after reaching the peak with the runoff(initial concentration 2mg/L,peak concentration 8mg/L).In the simulated sampling with interval 5,10,15,20,30,60,120,240,480,720min,the number of sampling points reduced from 1957 t0 14.In the simulated sampling with interval 16,32,64,128,256,384,576,800,1600,3200m3,the number of sampling points reduced from 2893 to 14.The ability of water interval sampling to capture peak runoff is obviously higher than that of time interval sampling.Load estimation error showed that the fluctuation of total phosphorus error is greater than that of total nitrogen error.Taking±5%as the allowable error range,the effective time interval of rainfall runoff event sampling was 120min,and the effective water interval was 1600m3.

rainfall runoff eventsmall watershedagricultural non-point sourceautomatic monitoringsampling interval

王超、王剑、文立群、秦赫、柳根、贾海燕、尹炜

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长江水资源保护科学研究所,湖北武汉 430051

长江水利委员会湖库水源地面源污染生态调控重点实验室,湖北武汉 430051

华中农业大学资源与环境学院,湖北武汉 430070

水环境污染监测先进技术与装备国家工程研究中心,湖南长沙 410205

南水北调中线水源有限责任公司,湖北丹江口 442700

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降雨径流事件 小流域 农业面源 自动监测 采样间隔

国家自然科学基金长江水利委员会科技创新基金

U2040210SWJ-CJX23Z07

2024

中国环境科学
中国环境科学学会

中国环境科学

CSTPCDCHSSCD北大核心
影响因子:2.174
ISSN:1000-6923
年,卷(期):2024.44(2)
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