首页> 外文会议>2nd International Nitrogen Conference , Oct 14-18, 2001, Potomac, Maryland, USA >Impact of a First-Order Riparian Zone on Nitrogen Removal and Export from an Agricultural Ecosystem
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Impact of a First-Order Riparian Zone on Nitrogen Removal and Export from an Agricultural Ecosystem

机译:一阶河岸带对农业生态系统氮素去除和出口的影响

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摘要

Riparian zones are reputed to be effective at preventing export of agricultural groundwater nitrogen (N) from local ecosystems. This is one impetus behind riparian zone regulations and initiatives. However, riparian zone function can vary under different conditions, with varying impacts on the regional (and ultimately global) environment. Rates of groundwater delivery to the surface appear to have significant effects on the N-removing capabilities of a riparian zone. Research conducted at a first-order agricultural watershed with a well-defined riparian zone in the Maryland coastal plain indicates that more than 2.5 kg/day of nitrate-N can be exported under moderate-to-high stream basef low conditions. The total nitrate-N load that exits the system increases with increasing flow not simply because of the greater volume of water export. Stream water nitrate-N concentrations also increase by more than an 0order of magnitude as flow increases, at least during baseflow. This appears to be largely the result of changes in dominant groundwater delivery mechanisms. Higher rates of groundwater exfiltration lessen the contact time between nitrate-carrying groundwater and potentially reducing riparian soils. Subsurface preferential flow paths, in the wetland and adjacent field, also strongly influence N removal. Simple assumptions regarding riparian zone function may be inadequate because of complexities observed in response to changing hydrologic conditions.
机译:据说沿岸带可以有效防止当地生态系统中的农业地下水氮(N)输出。这是沿河带法规和倡议的推动力之一。但是,河岸带功能在不同条件下会有所不同,对区域(乃至全球)环境的影响也不同。地下水向地表的输送速度似乎对河岸带的氮去除能力有重大影响。在马里兰州沿海平原具有明确河岸带的一阶农业流域进行的研究表明,在中低流量的基础上,中高流量的硝态氮可以每天出口超过2.5千克。离开系统的总硝酸盐氮负荷随着流量的增加而增加,这不仅是因为大量的水输出。至少在基流期间,随着流量的增加,溪水中的硝酸盐氮浓度也增加了超过0个数量级。这似乎主要是主要的地下水输送机制发生变化的结果。较高的地下水渗透率可减少携带硝酸盐的地下水与可能减少河岸土壤之间的接触时间。湿地和邻近区域的地下优先流动路径也强烈影响氮的去除。关于河岸带功能的简单假设可能不够充分,因为观察到的响应于不断变化的水文条件的复杂性。

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