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Distribution characteristics of ~(137)Cs in wind-eroded soil profile and its use in estimating wind erosion modulus

机译:〜(137)Cs在风蚀土壤剖面中的分布特征及其在风蚀模量估算中的应用

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摘要

Due to its inert reaction in soil system and distinctive vertical distribution in soil profile, caesium-137 (~(137)Cs) has been used as a tracer to assess wind erosion. In this study, 62 soil samples were collected from 4 sampling sites in Taipusi County, Inner Mongolia; Caesium-137 activities for those soil samples were measured using a gamma-ray spectrometry in Sichuan University, Chengdu. Distribution pattern of Cs in vertical soil profile was different for different land use and land cover types. Caesium-137 was distributed homogeneously in plow layer of cropland, and negatively exponential in low to medium cover grassland. Distribution pattern in high covered grassland was represented by a peak at 2 — 4 cm soil depth followed by a negative exponential curve. Based on those findings, simplified mass balance model was chosen to estimate the rate of wind erosion for cropland, while profile distribution model was used for grassland. Estimated wind erosion rates were 7990,4270 and 1808 Mg·km~(-2)·a~(-1) for cropland, low cover grassland and medium cover grassland, respectively. Wind erosion intensity correlated negatively with plant cover.
机译:由于其在土壤系统中的惰性反应和在土壤剖面中独特的垂直分布,铯137(〜(137)Cs)已被用作示踪剂以评估风蚀。在这项研究中,从内蒙古泰普斯县的4个采样点采集了62个土壤样品。在成都的四川大学使用伽马射线能谱法测量了这些土壤样品中的铯137活性。不同土地利用和土地覆被类型下,垂直土壤剖面中Cs的分布规律不同。铯137在耕地耕层均匀分布,在中低覆盖度草地呈负指数分布。高覆盖草原上的分布模式以土壤深度2-4 cm处的峰值和负指数曲线表示。基于这些发现,选择简化的质量平衡模型来估计农田的风蚀率,而剖面分布模型用于草地。农田,低覆盖草地和中覆盖草地的估计风蚀率分别为7990、4270和1808 Mg·km〜(-2)·a〜(-1)。风蚀强度与植物覆盖度呈负相关。

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