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Feasibility of High-Resolution Soil Erosion Measurements by Means of Rainfall Simulations and SfM Photogrammetry

机译:通过降雨模拟和SfM摄影测量法测量高分辨率土壤侵蚀的可行性

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The silty soils of the intensively used agricultural landscape of the Saxon loess province, eastern Germany, are very prone to soil erosion, mainly caused by water erosion. Rainfall simulations, and also increasingly structure-from-motion (SfM) photogrammetry, are used as methods in soil erosion research not only to assess soil erosion by water, but also to quantify soil loss. This study aims to validate SfM photogrammetry determined soil loss estimations with rainfall simulations measurements. Rainfall simulations were performed at three agricultural sites in central Saxony. Besides the measured data runoff and soil loss by sampling (in mm), terrestrial images were taken from the plots with digital cameras before and after the rainfall simulation. Subsequently, SfM photogrammetry was used to reconstruct soil surface changes due to soil erosion in terms of high resolution digital elevation models (DEMs) for the pre- and post-event (resolution 1 × 1 mm). By multi-temporal change detection, the digital elevation model of difference (DoD) and an averaged soil loss (in mm) is received, which was compared to the soil loss by sampling. Soil loss by DoD was higher than soil loss by sampling. The method of SfM photogrammetry-determined soil loss estimations also include a comparison of three different ground control point (GCP) approaches, revealing that the most complex one delivers the most reliable soil loss by DoD. Additionally, soil bulk density changes and splash erosion beyond the plot were measured during the rainfall simulation experiments in order to separate these processes and associated surface changes from the soil loss by DoD. Furthermore, splash was negligibly small, whereas higher soil densities after the rainfall simulations indicated soil compaction. By means of calculated soil surface changes due to soil compaction, the soil loss by DoD achieved approximately the same value as the soil loss by rainfall simulation.
机译:德国东部撒克逊黄土省密集使用的农业景观中的粉质土壤很容易受到水土流失的侵蚀。降雨模拟以及越来越多的运动构造(SfM)摄影测量法已被用作土壤侵蚀研究的方法,不仅可以评估水对土壤的侵蚀,还可以量化土壤流失。本研究旨在通过降雨模拟测量结果来验证SfM摄影测量法确定的土壤流失估计。在萨克森州中部的三个农业地点进行了降雨模拟。除了通过采样(以毫米为单位)测量的数据径流和土壤流失,在降雨模拟之前和之后,还使用数码相机从地块中获取了地面图像。随后,根据事件发生前后的高分辨率数字高程模型(DEM),使用SfM摄影测量法重建由于土壤侵蚀而导致的土壤表面变化(分辨率1×1 mm)。通过多时间变化检测,可以接收到数字差异高程模型(DoD)和平均土壤流失量(以mm为单位),并将其与通过采样的土壤流失进行比较。国防部的土壤流失高于抽样的土壤流失。用SfM摄影测量法确定的土壤流失估计方法还包括对三种不同的地面控制点(GCP)方法的比较,表明最复杂的一种方法是通过DoD传递最可靠的土壤流失方法。另外,在降雨模拟实验期间,测量了该样区以外的土壤容重变化和飞溅侵蚀,以便将这些过程和相关的表面变化与DoD造成的土壤流失分开。此外,飞溅很小,可以忽略不计,而降雨模拟后较高的土壤密度表明土壤压实。通过计算由于土壤压实引起的土壤表面变化,国防部的土壤流失量与降雨模拟的土壤流失量大致相同。

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