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Model Assessment of Cattle and Climate Impacts on Stream Fecal Coliform Pollution in the Salmon River Watershed, British Columbia, Canada

机译:加拿大不列颠哥伦比亚省鲑鱼河流域牛和气候对粪便粪大肠菌污染的模型评估

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摘要

A bacterial water quality model (BWQM) was developed and used to evaluate the impacts of cattle farming and climate change on the stream fecal coliform pollution in the Salmon River watershed in south-central British Columbia, Canada. The accuracy of the model simulation was evaluated using the Nash-Sutcliffe coefficient of efficiency (COE). The BWQM simulated the observed field data well, with the values of the COE ranging from 0.76 to 0.78 for the stream flow, from 0.55 to 0.60 for the fecal coliform (FC) concentration, and from 0.85 to 0.89 for the FC loading. The BWQM captured more than 79%, 66%, and 90% variation of the daily stream flow, FC concentration, and FC loading, respectively. The BWQM predicts that between 70% and 80% of the FC were transferred from the cattle farm to the Salmon River through the snowmelt-caused surface runoff during late winter and early spring, with the balance 20% to 30% coming from the soil-lateral flow and the groundwater return flow. The model also indicates that the stream FC concentration is sensitive to the distance of the cattle farm to the Salmon River. The model scenario analysis reveals that the climate change, at an assumed 1℃ increment of daily air temperature, results in an increase in the stream FC concentration in the spring, fall, and winter, but there is also a decrease in the summer. The increased air temperature also changes the seasonal pattern of the stream FC concentration. Rainfall can reduce the stream FC concentration and mitigate the impact of the increased air temperature on the stream FC concentration as long as it does not result in a surface runoff or flooding event.
机译:开发了一种细菌水质模型(BWQM),用于评估养牛业和气候变化对加拿大不列颠哥伦比亚省中南部鲑鱼河流域粪便大肠菌群污染的影响。使用Nash-Sutcliffe效率系数(COE)评估模型仿真的准确性。 BWQM很好地模拟了观测到的现场数据,COE值的范围从0.76-0.78,粪便大肠菌群(FC)浓度从0.55-0.60,FC的0.85-0.89。 BWQM分别捕获了每日流量,FC浓度和FC负荷的超过79%,66%和90%的变化。 BWQM预测,冬季末和初春期间,融雪引起的地表径流会将70%至80%的FC从养牛场转移到鲑鱼河,其余20%至30%来自土壤-横向流和地下水回流。该模型还表明,流FC浓度对养牛场到鲑鱼河的距离敏感。模型情景分析表明,假定每天气温升高1℃,气候变化会导致春季,秋季和冬季的溪流FC浓度增加,而夏季则有所减少。升高的空气温度也改变了流FC浓度的季节性模式。降雨可以降低流FC的浓度,并减轻空气温度升高对流FC的影响,只要它不会导致地表径流或洪水事件。

著录项

  • 来源
    《Water, Air, and Soil Pollution》 |2011年第4期|p.155-176|共22页
  • 作者单位

    Water and Aquatic Sciences Research Program, Department of Biology, University of Victoria, 3800 Finnerty Road, Victoria, BC V8P5C2, Canada;

    Kamloops Range Research Station, Agriculture and Agri-Food Canada, 3015 Ord Road, Kamloops, BC V2B8A9, Canada;

    Water and Aquatic Sciences Research Program, Department of Biology, University of Victoria, 3800 Finnerty Road, Victoria, BC V8P5C2, Canada;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    fecal coliform; water quality; model; cattle farming; climate;

    机译:粪大肠菌群水质;模型;养牛业;气候;

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