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A simple model of Cs-137 profile to estimate soil redistribution in cultivated stony soils

机译:用简单的Cs-137剖面模型估算耕作石质土壤中的土壤重新分布

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摘要

A main issue in soil erosion studies is to calibrate 137Cs data to provide satisfactory estimates of erosion and deposition rates. The cultivation on steep slopes in some areas of the South Central Pyrenees results in serious affections to soils due to water erosion that mobilizes soil particles down slope. In the region, the intensive soil use including deforestation, overgrazing and extensive agriculture during the last centuries together with some characteristics of the soils such as poor development, thin soil profiles and high stone contents make them prone to erosion. A model based on 137Cs profile is proposed to calculate erosion or sedimentation rates in these cultivated soils. The model uses parameters such as the volume of the fine fraction of the soils and the depth of cultivation calculated from the values obtained just from the soil sampling. Using a computer program the annual deposit of 137Cs is simulated for an erosion or deposition rate of soil. To test the model, 137Cs profiles of cultivated soils were collected at sampling sites located on temperate slopes in the Sierra de la Carrodilla (South Pyrenees) and experimental results were simulated with the model. The simulation results of the model were consistent with the experimental results of 137Cs concentrations and inventories. The model offers a potential to describe the soil redistribution in stony soils and estimates of erosion and deposition rates can be calculated easily for a range of the most common soils found in Mediterranean environments.
机译:土壤侵蚀研究的主要问题是校准137 Cs数据,以提供令人满意的侵蚀和沉积速率估算。在中比利牛斯山脉中南部某些地区的陡坡上耕种会导致严重的土壤污染,因为水蚀使土壤颗粒向下运动。在该地区,过去几个世纪以来,密集的土壤利用包括森林砍伐,过度放牧和广泛的农业发展,加上土壤的某些特征(例如发育不良,土壤剖面稀薄和石材含量高)容易受到侵蚀。提出了基于137Cs剖面的模型来计算这些耕作土壤中的侵蚀或沉降速率。该模型使用诸如土壤细碎部分的体积和根据仅从土壤采样获得的值计算出的耕种深度等参数。使用计算机程序模拟了137Cs的年沉积量,以评估土壤的侵蚀或沉积速率。为了测试该模型,在位于南比利牛斯山脉(Sierra de la Carrodilla)(南比利牛斯)的温带斜坡上的采样点收集了137 Cs的耕作土壤剖面,并用该模型模拟了实验结果。模型的仿真结果与137Cs浓度和清单的实验结果一致。该模型为描述石质土壤中的土壤重新分布提供了潜力,并且可以很容易地计算出地中海环境中一系列最常见土壤的侵蚀和沉积速率估算值。

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