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Estimates of soil movement in a study area in Gonghe Basin, north-east of Qinghai-Tibet Plateau

机译:青藏高原东北部共和盆地研究区的土壤运动估算

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摘要

Accurate data on soil erosion rates by wind and patterns of soil movement are essential for guiding control planning in Gonghe Basin, north-east of Qinghai-Tibet Plateau. This study was conducted to estimate soil erosion rates and assess patterns of soil movement by wind erosion in a 600 ha area during a 37-year period using the ~(137)Cs tracer technique. Two hundred and ' fifty-five soil samples were collected from 125 ~(137)Cs sampling points on a modified grid pattern and analysed for ~(137)Cs activity. Using ordinary point kriging, soil movement rates were interpolated at 7350 points in the sample grid. The kriged mean net soil movement rates were -3·496, -5·026 and 1·77kgm~(-2) year~(-1) on uncultivated grassland, cultivated grassland (farmland) and semi-shifting sand land, respectively. Soil movement by wind erosion in semi-arid steppe area is closely related to land use and soil landscape.
机译:准确的风蚀土壤侵蚀数据和土壤运动模式对于指导青藏高原东北部共和盆地的控制规划至关重要。这项研究是使用〜(137)Cs示踪技术估算37年来600公顷土地上的土壤侵蚀速率并通过风蚀评估土壤运动的方式。在改良的网格模式下,从125〜(137)Cs采样点收集了255个土壤样品,并分析了〜(137)Cs活性。使用普通点克里金法,将土壤运动速率插值到样本网格中的7350个点上。在未耕地,耕地(农田)和半流沙地上,克立顿平均土壤净运动速率分别为-3·496,-5·026和1·77kgm〜(-2)年〜(-1)。半干旱草原地区风蚀引起的土壤运动与土地利用和土壤景观密切相关。

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