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Effects of riparian forest buffers on in-stream nutrient retention in agricultural catchments.

机译:河岸带森林缓冲带对农业流域内流中养分保留的影响。

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In northeastern Austria, marshlands have been turned into the most productive arable land of the country. As a result, most headwater streams show structurally degraded channels, lacking riparian buffer zones, which are heavily loaded with nutrients from the surrounding crop fields. The present study examines whether longitudinally restricted riparian forest buffers can enhance the in-stream nutrient retention in nutrient-enriched headwater streams. We estimated nutrient uptake from pairwise, short-term addition experiments with NH, NH, PO, and NaCl within reaches with riparian forest buffers (RFB) and degraded reaches (DEG) of the same streams. Riparian forest buffers originated from the conservation of the pristine vegetation or from restoration measures. Hydrologic retention was calculated with the model OTIS-P on the basis of conductivity break-through curves from the salt injections. A significant increase in surface transient storage was revealed in pristine and restored RFB reaches compared with DEG reaches due to the longitudinal step-pool pattern and the frequent occurrence of woody debris on the channel bed. Ammonium uptake lengths were significantly shorter in RFB reaches than in DEG reaches, resulting from the higher hydrologic retention. Uptake velocities did not differ significantly between RFB and DEG reaches, indicating that riparian forest buffers did not affect the biochemical nutrient demand. Uptake of NH was mainly driven by autotrophs. Net PO uptake was not affected by riparian forest buffers. The study shows that the physical and biogeochemical effects of riparian forest buffers on the in-stream nutrient retention are limited in the case of highly eutrophic streams. Copyright Copyright by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America, Inc.
机译:在奥地利东北部,沼泽地已变成该国生产力最高的耕地。结果,大多数源头水流显示出结构退化的河道,缺乏河岸缓冲带,这些河岸缓冲带重载了周围农田的养分。本研究研究了纵向限制的河岸森林缓冲区是否可以增强营养丰富的源头溪流中的河内养分保留。我们通过在河岸森林缓冲带(RFB)和同一河段的退化河段(DEG)范围内使用NH,NH,PO和NaCl的成对,短期添加实验估算养分吸收。河岸森林缓冲源于原始植被的保护或恢复措施。根据盐注入的电导率突破曲线,使用OTIS-P模型计算水文保留率。与原始DEG相比,原始的表面瞬态存储显着增加,与之相比,RFB到达的恢复率更高,这是由于纵向阶梯池模式和通道床上的木屑频繁发生所致。由于较高的水文截留率,RFB到达铵的长度明显短于DEG到达铵的长度。 RFB和DEG到达之间的吸收速度没有显着差异,表明河岸森林缓冲带不会影响生化养分需求。 NH的吸收主要由自养生物引起。净PO吸收量不受河岸森林缓冲区的影响。研究表明,在高度富营养化的河流中,河岸森林缓冲带对河流中养分保留的物理和生物地球化学作用受到限制。版权美国农艺学会,美国作物科学学会和美国土壤科学学会版权所有。

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