首页> 外文会议>Annual International Meeting of the American Society of Agricultural and Biological Engineers >DESIGNING EROSION AND NUTRIENT CONTROL PRACTICES IN WATERSHEDS IN HUMID REGIONS: LESSONS LEARNED
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DESIGNING EROSION AND NUTRIENT CONTROL PRACTICES IN WATERSHEDS IN HUMID REGIONS: LESSONS LEARNED

机译:在潮湿地区的流域设计侵蚀和养分控制实践:学习经验教训

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For close to a century, governments have encouraged soil and water conservation measures on farmers' fields using universal technologies independent of environmental and social context. Most of these conservation technologies-based infiltration-excessrunoff mechanisms were beneficial over an extended time in the drier climates for water conservation and erosion control, but only for short times in humid areas and in neither climate for nutrient control. The objective of this presentation is to document the hydrological and management factors that should be considered in the optimum performance of soil and water conservation practices in humid regions and then use them to find more effective practices. We are using the humid and sub humid Ethiopianhighlands landscape and the New York City source watersheds in the Catskill Mountains as case studies. We show that since infiltration-excess hardly occurs in these humid regions, direct runoff is generated from areas that become saturated on valley bottoms, near rivers, and on hillsides with the most severely degraded soils and perched water. Only practices that consider the saturation runoff mechanisms are effective in reducing non-point source pollution and erosion. This includes protecting areas andlimiting nutrient additions in areas near streams that generate surface runoff.
机译:对于近年来,各国政府采用了独立于环境和社会环境的普遍技术鼓励对农民领域的土壤和水资源保护措施。基于保护技术的大多数渗透 - 过度润滑机制在干燥气候中的延长时间有利于水养护和侵蚀控制,但仅在潮湿地区的短时间内,既不是营养控制的气候。本介绍的目的是记录水文和管理因素,应在潮湿地区的土壤和水资源保护实践的最佳性能下考虑,然后使用它们来查找更有效的实践。我们正在使用Catskill Mountains的潮湿和潜伏的埃塞俄比亚高风景观和纽约市来源流域作为案例研究。我们表明,由于在这些潮湿的区域中渗透过多,因此在这些潮湿的区域内几乎发生了直接的径流,这些区域产生在谷底部,近河附近的区域,以及最严重降解的土壤和栖息的水域。仅考虑饱和径流机制的实践是有效地减少非点源污染和侵蚀。这包括保护区域,并在产生表面径流的溪流附近的区域中保护营养添加。

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