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Estimates of nonpoint source pollution to watersheds in Belize using the AGNPS model.

机译:使用AGNPS模型估算伯利兹流域的非点源污染。

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摘要

There are serious pressures on developing countries to convert forest resources to agriculture that could have significant impacts on watershed hydrology. Simulations of rainstorm events using AGNPS (Agricultural Nonpoint Source) for the Double Run subwatershed and the North Stann Creek watershed show significant risk of high nitrogen (N) and sediment loads to Belize's marine environment. Excessive N and sediment loads may adversely affect marine ecosystems and eventually imperil the largest barrier reef in the western hemisphere. Field sampling show annual N loads from the Double Run subwatershed of approximately 4.96 × 107 kg. Empirical relationship between [N] in the river and depth of rainstorm events had an R squared of 0.94. This correlation provides a reliable, cost-effective estimate of [N] in the river based on easily available precipitation data.; AGNPS predictions of [N] in runoff for specific rainstorms are much lower than experimentally determined values. Reasons for this are: AGNPS apportion nitrogen both in the sediment phase and in runoff, assumptions made for calculating [N] in runoff based on [N] in the river, and the large cell size used for the simulation. However, AGNPS provides reliable predictions for storms of depths between 10 mm and 51 mm (R2 is 0.67).; AGNPS users must consider the following limitations of the model; large data requirements, nutrient concentration is apportioned in runoff and adsorbed to sediment, and subsurface flow is not used in stormflow generation. However, AGNPS can be a very effective watershed management tool if used along with extensive field work.
机译:发展中国家面临将森林资源转化为农业的巨大压力,这可能对流域水文学产生重大影响。使用AGNPS(农业非点源)对Double Run子集水区和North Stann Creek集水区进行的暴雨事件模拟显示,高氮(N)和沉积物负载到伯利兹海洋环境的风险很大。过多的氮和沉积物负荷可能会对海洋生态系统产生不利影响,并最终危害西半球最大的堡礁。野外采样显示,Double Run流域每年的N负荷约为4.96×10 7 kg。河中[N]与暴雨事件的深度之间的经验关系的R平方为0.94。这种相关性基于容易获得的降水量数据提供了对河流中[N]的可靠,经济高效的估计。针对特定暴雨的径流[N]的AGNPS预测远低于实验确定的值。原因如下:AGNPS在沉积物阶段和径流中分配氮,基于河流中的[N]计算径流中[N]的假设,以及用于模拟的较大像元大小。但是,AGNPS为10毫米至51毫米之间的深度风暴(R 2 为0.67)提供了可靠的预测。 AGNPS用户必须考虑该模型的以下限制;数据需求大时,养分浓度在径流中分配并吸收到沉积物中,地下流量不用于产生暴雨。但是,如果将AGNPS与广泛的现场工作结合使用,则可以成为非常有效的分水岭管理工具。

著录项

  • 作者

    Morgan, Philip Armando.;

  • 作者单位

    University of Montana.;

  • 授予单位 University of Montana.;
  • 学科 Hydrology.; Environmental Sciences.; Agriculture General.
  • 学位 Ph.D.
  • 年度 2002
  • 页码 p.5613
  • 总页数 195
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 水文科学(水界物理学);
  • 关键词

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