首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >Soil nitrogen distributions for different land uses and landscape positions in a small watershed on Loess Plateau, China
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Soil nitrogen distributions for different land uses and landscape positions in a small watershed on Loess Plateau, China

机译:黄土高原小流域不同土地利用方式和景观位置的土壤氮素分布

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The comprehensively managed Shanghuang watershed has been subjected to vegetation restoration since 1982 and is continuing through the Grain for Green project. Because land use and landscape position are the most important factors that influence soil nitrogen, understanding the effects of landforms and slope position on the distribution of soil nitrogen is an important prerequisite for estimating soil quality on the Loess Plateau. The results of our study showed that soil total nitrogen, nitrate nitrogen and ammonium nitrogen were highly variable in the small watershed. The soil nitrogen concentrations declined in the following order: natural grassland > shrub land > abandoned farmland > orchard > farmland > man-made grassland. Among the different landscape positions, soil nitrogen showed the highest values in valleys. There was a significant positive correlation between soil nitrogen and soil organic carbon, which were negatively correlated with soil pH and soil bulk density. The total soil nitrogen concentration decreased with increasing soil depth, and the highest nitrate nitrogen content and lowest ammonium nitrogen concentration were detected in the 10-30-cm layer. Regarding land use conversion, farmland to shrub land and abandoned farmland was more effective than orchard and man-made grassland for increasing total soil nitrogen and promoting soil nitrogen mineralization, which plays an essential role in ecological restoration. The potential contribution of land use change on soil organic carbon (SOC) and total N concentration could be estimated by assessing the land use conversion in the Shanghuang watershed. It was found that the implemented projects on the Chinese Loess Plateau were successful with regard to benefiting soil nitrogen.
机译:全面管理的上黄流域自1982年以来就进行了植被恢复,并一直通过“退耕还林”工程进行。由于土地利用和景观位置是影响土壤氮素的最重要因素,因此了解地形和坡位对土壤氮素分布的影响是估算黄土高原土壤质量的重要前提。我们的研究结果表明,在小流域,土壤总氮,硝态氮和铵态氮变化很大。土壤氮含量按以下顺序下降:天然草地>灌木地>废弃农田>果园>农田>人工草地。在不同的景观位置中,山谷中的土壤氮含量最高。土壤氮与有机碳之间存在显着的正相关,与土壤pH和土壤容重呈负相关。土壤总氮浓度随土壤深度的增加而降低,在10-30cm的土壤层中最高的硝酸盐氮含量和最低的铵态氮浓度被发现。在土地利用转换方面,耕地改为灌木地和废弃农田比果园和人工草地在增加土壤总氮和促进土壤氮矿化方面更为有效,这在生态恢复中起着至关重要的作用。土地利用变化对土壤有机碳(SOC)和总氮浓度的潜在贡献可以通过评估上黄流域的土地利用转化来估算。研究发现,在黄土高原地区实施的项目在提高土壤氮素方面是成功的。

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