Simulative Study of Influences of Agricultural Non-point Source Pollution on Water Resources in Yitong River Watershed
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Simulative Study of Influences of Agricultural Non-point Source Pollution on Water Resources in Yitong River Watershed
Bulletin of Soiland Water ConservationVol. 32, Issue 3, Pages: 139-143(2013)
作者机构:
1. 吉林大学环境与资源学院,吉林,长春,130021
2. 中核第四研究设计工程有限公司,河北,石家庄,050021
3. 吉林省地质环境监测总站,吉林,长春,130021
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Published:2013
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SUN Xiao-qing, BIAN Jian-min, ZHA En-shuang, et al. Simulative Study of Influences of Agricultural Non-point Source Pollution on Water Resources in Yitong River Watershed[J]. Bulletin of Soiland Water Conservation, 2013, 32(3): 139-143.
DOI:
SUN Xiao-qing, BIAN Jian-min, ZHA En-shuang, et al. Simulative Study of Influences of Agricultural Non-point Source Pollution on Water Resources in Yitong River Watershed[J]. Bulletin of Soiland Water Conservation, 2013, 32(3): 139-143.DOI:
Simulative Study of Influences of Agricultural Non-point Source Pollution on Water Resources in Yitong River Watershed
According to the agricultural non-point pollution problems in Yitong River
a model of agricultural non-point pollution in this area was constructed using SWAT model with the support of GIS technology and watershed foundation database.The model was used to simulate the temporal and spatial distributions of N
P and sediment
as well as the total nitrogen delivered into groundwater in the study area.Results from the calibration and verification for the model showed that the precision of the model can meet the requirements.Through the calculation of model simulation
sediment yields in 1985and 2008were 7.031 6and 3.458 7million ton
respectively.In 1985
total nitrogen and phosphorus outputs were 20 400and 2 300ton
respectively
and in 2008
was about half of that in 1985.For one year
pollution output from June to August took up90% of the total amount.The simulation result showed that the amount of nitrogen delivered into ground water by infiltration was considerable in 1985and 2008
the amounts of nitrogen delivered into groundwater were 2.4and 5.5times of those in other forms of output.