利用铯-137 测量数据和 RUSLE 模型探讨土地利用变化对意大利南部一个中型集水区土壤侵蚀和沉积率的影响

IF 4.3 3区 材料科学 Q1 ENGINEERING, ELECTRICAL & ELECTRONIC ACS Applied Electronic Materials Pub Date : 2024-04-01 DOI:10.1016/j.ijsrc.2023.11.004
Paolo Porto , Giovanni Callegari , Abid Ouadja , Ernesto Infusino
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引用次数: 0

摘要

在意大利南部的一些地区,过去四五十年间土地用途的改变增加了对土地和水资源的压力,并造成了不同形式的土壤退化。为了减轻土壤侵蚀的程度,一些地区采取了不同的策略,包括修建防洪设施和植树造林计划。然而,由于缺乏对土壤侵蚀的直接测量,很难量化这些策略的效果。为了弥补这一信息空白,分布式数值模型的使用与放射性核素铯 137(137Cs)的测量相结合,为传统的实验场地(小区、集水区)提供了一个很好的替代方案。本文首先以卡拉布里亚的一个代表性集水区为例,描述了洪泛区 137Cs 的测量结果,以重建过去六十年间土壤沉积率的变化趋势。这些测量值与利用修订的通用土壤流失方程 (RUSLE) 模型获得的土壤流失估算值进行了整合,并提供了不同时期的土地利用图。最后,通过比较 RUSLE 模型提供的集水区土壤侵蚀估算值和沉积区 137Cs 测量值得出的沉积速率,可以获得有关这些地区土壤侵蚀和沉积速率趋势的有趣信息。
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Using Cs-137 measurements and RUSLE model to explore the effect of land use changes on soil erosion and deposition rates in a mid-sized catchment in southern Italy

In some areas of southern Italy, the change in land use over the last 4–5 decades has increased pressure on land and water resources and caused different forms of soil degradation. In order to mitigate the magnitude of soil erosion, different strategies that include construction of flood control structures and reforestation programs have been done in several areas. However, quantifying the effectiveness of these strategies is difficult in absence of direct measurements of soil erosion. To cover this information gap, the use of distributed numerical models coupled with measurements of the radionuclide cesium-137 (137Cs) offers a good alternative to the classic experimental sites (plot, catchments) that, on the contrary, require long term datasets to produce reliable estimates of soil loss. In this paper, measurements of 137Cs in a floodplain area are firstly described for a representative Calabrian catchment as an example to reconstruct the trend of soil deposition rates during the last six decades. These measurements have been integrated with estimates of soil loss obtained with the Revised Universal Soil Loss Equation (RUSLE) model for which land use maps of different periods are available. The final comparison between estimates of soil erosion provided by the RUSLE at catchment scale and sedimentation rates derived from 137Cs measurements on depositional areas allowed interesting information on the trend of soil erosion and deposition rates in these areas to be obtained.

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4.30%
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