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首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >Topography and land use effects on spatial variability of soil denitrification and related soil properties in riparian wetlands
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Topography and land use effects on spatial variability of soil denitrification and related soil properties in riparian wetlands

机译:地形和土地利用对河岸湿地土壤反硝化空间变异性及相关土壤特性的影响

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Many rivers in the Yangtze River basin have suffered from excess nitrogen due to increased human activities in recent decades. Soil denitrification in riparian wetlands is a key process for removing nitrogen from polluted surface runoff and controlling eutrophication in river ecosystems. Currently, little is known about the influence of topography and land use on the riparian denitrification characteristics in the Yangtze River basin. In this study, we used the acetylene block technique to determine the spatial variability of the soil potential and unamended dentrification rates of 42 riparian wetlands in the Han River basin of China. The results indicated that riparian soils showed great spatial variation in potential denitrification, unamended dentrification and most of the measured physical and chemical properties. Both potential and unamended dentrification rates were positively associated with soil moisture, percentage of fine substrate, organic matter and nitrogen contents, but were negatively related to soil pH and bulk density. Agricultural riparian soils had unamended denitrification rates higher than forested riparian soils. Spearman correlation analysis also indicated that a topographic factor (i.e., elevation) had a negative effect on riparian denitrification rates. Our results suggest that both topography and land use can indirectly influence the soil denitrification rates in riparian wetlands. Low-elevation areas in the agricultural riparian zone are good candidates for wetland restoration or creation for nitrogen removal and water quality improvement in the Yangtze River basin. (C) 2015 Elsevier B.V. All rights reserved.
机译:近几十年来,由于人类活动的增加,长江流域的许多河流都遭受了氮过多的困扰。河岸湿地的土壤反硝化是从受污染的地表径流中除去氮并控制河流生态系统富营养化的关键过程。目前,关于长江流域的地形和土地利用对河岸反硝化特性的影响知之甚少。在这项研究中,我们使用乙炔封堵技术来确定中国汉江流域42个河岸湿地的土壤潜力的空间变异性和未修正的硝化率。结果表明,河岸土壤在潜在的反硝化作用,未改性的硝化作用以及大部分测得的理化性质方面表现出很大的空间变化。潜在的和未修正的硝化速率均与土壤水分,精细基质的百分比,有机质和氮含量呈正相关,而与土壤pH和堆积密度呈负相关。农业河岸土壤的未修正反硝化率高于森林河岸土壤。 Spearman相关分析还表明,地形因素(即海拔)对河岸脱氮率有负面影响。我们的结果表明,地形和土地利用都可以间接影响河岸湿地的土壤反硝化率。农业河岸带的低海拔地区是恢复湿地或创造长江流域脱氮和水质改善的理想选择。 (C)2015 Elsevier B.V.保留所有权利。

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