首页> 外文期刊>地理学报(英文版) >黄土丘陵小流域土地利用格局对径流与土壤养分流失的影响--土壤侵蚀控制的意义
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黄土丘陵小流域土地利用格局对径流与土壤养分流失的影响--土壤侵蚀控制的意义

机译:黄土丘陵小流域土地利用格局对径流与土壤养分流失的影响--土壤侵蚀控制的意义

摘要

Serious soil erosion is one of the major issues threatening sustainable land use in semiarid areas, especially in the Loess Plateau of China. Understanding the effects of land use on soil and water loss is important for sustainable land use strategy. Two sub-catchments: catchment A (CA) and catchment B (CB) with distinct land uses were selected to measure soil moisture, runoff and soil nutrient loss in Da Nangou catchment of the Loess Plateau of China. The effects of land use patterns on runoff and nutrient losses were analyzed based on soil moisture pattern by kriging and soil nutrients using multiple regression model. The results indicated that there were significant differences in runoff yield and soil nutrient losses between the two sub-catchments. With similar land uses, the CA produced an average sediment yield of 49 kg ha-1 and 22.27 kg ha-1 during two storm events.Meanwhile, there was almost no runoff in the CB with dissimilar land uses during the same events.Buffer zones should be established to re-absorb runoff and to trap sediments in catchment with similar land use structure such as the CA. Moreover, land use management strategy aiming to increase the infiltration threshold of hydrological response units could decrease the frequency of runoff occurrence on a slope and catchment scale.
机译:严重的土壤侵蚀是威胁半干旱地区可持续土地的主要问题之一,特别是在中国黄土高原。了解土地利用对土壤和水损的影响对于可持续土地利用策略至关重要。选择了两种子集水区:集水区A(CA)和集水区B(CB)具有不同的土地用途,以测量中国黄土高原大南沟集水区的土壤水分,径流和土壤养分损失。基于使用多元回归模型的克里格和土壤营养素分析土地利用模式对径流和养分损失的影响。结果表明,两个子集液之间的径流产量和土壤养分损失存在显着差异。具有类似的土地用途,CA在两个风暴事件中产生了49公斤HA-1和22.27公斤HA-1的平均沉积物。偶尔,CB几乎没有径流,不同的土地在同一事件中使用。缓冲区应该建立重新吸收径流,并在集水区内陷阱,与加利福等类似的土地使用结构。此外,旨在提高水文响应单元渗透阈值的土地利用管理策略可以降低斜坡和集距量表的径流发生频率。

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