首页> 外文会议>International Conference on Computer Simulation in Risk Analysis and Hazard Mitigation(RISK 2004); 2004; Rhodes(GR) >Small-scale experiments on soil roughness evolution and first applications to soil erosion risk assessment
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Small-scale experiments on soil roughness evolution and first applications to soil erosion risk assessment

机译:土壤粗糙度演变的小规模试验及其在土壤侵蚀风险评估中的首次应用

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This paper presents experimental data on the geometric and morphometric evolution of small scale soil parcels after simulated cycles of rainfall with the aim to contribute to the understanding of soil roughness dynamics. Furthermore we will show some results on erosion modelling and radar remote sensing application related to soil roughness. Starting from chosen parcels on crops or bare soils, rainfall simulations have been undertaken over repeated cycles of storms in the Chianti region (central Italy). At the beginning of experiments and after each event, a high resolution DEM of the parcel was automatically generated by means of a recently developed digital stereo-photogrammetric ground-based technique. At the same time, sediment yield and runoff were measured. Initial topographies could basically be considered as random space functions with quasi-isotropic distribution of the micro-relief. In a second phase, the DEMs have been reciprocally compared and elaborated to produce an evolutionary sequence of small scale relief which has been studied and analysed in order to show how the experimental data can be explained in terms of roughness and landscape evolution. The results of the study were subsequently used to calibrate remote sensed radar data derived from SAR Shuttle missions in order to include the roughness parameter in the backscattering models. At the same time the computed roughness was used to derive the friction coefficient f in interrill areas for the application of hydrological-erosive models to assess the soil erosion risk in the area.
机译:本文提供了模拟降雨后小规模土壤包裹几何和形态演化的实验数据,目的是有助于了解土壤粗糙度动态。此外,我们将显示与土壤粗糙度有关的侵蚀模型和雷达遥感应用的一些结果。从农作物或裸露的土地上选定的包裹开始,在基安蒂地区(意大利中部)的暴风雨反复循环中进行了降雨模拟。在实验开始时和每次事件发生后,借助于最近开发的基于地面的数字立体摄影测量技术,将自动生成高分辨率的DEM。同时,测量了沉积物的产量和径流。最初的地形基本上可以被认为是具有微浮雕的准各向同性分布的随机空间函数。在第二阶段,对DEM进行了相互比较和细化,以产生小规模浮雕的演化序列,对此序列进行了研究和分析,以显示如何用粗糙度和景观演化来解释实验数据。随后将研究结果用于校准从SAR航天飞机任务获得的遥感雷达数据,以便将粗糙度参数包括在反向散射模型中。同时,计算出的粗糙度被用于得出钻探间区域的摩擦系数f,以应用水文侵蚀模型来评估该区域的土壤侵蚀风险。

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