Lea Epple, Oliver Grothum, Anne Bienert, Anette Eltner
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引用次数: 0
摘要
基于相机的土壤表面变化测量是一种经济有效的非侵入性土壤侵蚀评估方法。在这种情况下,一个具有挑战性的方面是,在降雨事件开始时,沉降现象(如土壤固结和压实)掩盖了产沙量(掩蔽效应)。基于相机高程变化和实测的野外观测,我们开发了一种估计这些掩蔽效应和近似校正函数的方法。因此,我们在不同的农业斜坡上进行了10次降雨模拟(3 m x 1 m),测量径流和沉积物浓度。使用延时相机系统,我们每20 秒生成高分辨率数字高程模型。通过非线性回归对每次降雨模拟拟合出s型曲线。我们使用这些函数的变量以及不同现场观测的组合——容重、土壤湿度、粒度分布、总有机碳、坡度、地表覆盖和地表粗糙度——作为调整的输入值。我们能够估计降雨事件开始时的掩蔽效应作为土壤和地块特征的函数,因此有可能增加基于相机的农田土壤侵蚀测量的信息价值。
Decoding rainfall effects on soil surface changes: Empirical separation of sediment yield in time-lapse SfM photogrammetry measurements
Camera-based soil surface change measurement is a cost-efficient and non-invasive approach to assess soil erosion. A challenging aspect in this context is the obscuring of the sediment yield by subsidence phenomenon such as soil consolidation and compaction in the beginning of a rainfall event (masking effect). Based on the camera elevation changes and measured field observations, we develop an approach to estimate these masking effects and to approximate a correction function. We therefore conduct ten rainfall simulations (3 m x 1 m) on different agricultural slopes, measuring runoff and sediment concentration. With a time-lapse camera system, we generate high resolution digital elevation models every 20 s. An s-shaped curve is fitted via non-linear regression for every rainfall simulation. We use the variables of these functions as well as a combination of the different field observations – bulk density, soil moisture, grain size distribution, total organic carbon, slope steepness, surface cover and surface roughness – as input values for an adjustment. We are able to estimate the masking effects at the beginning of rainfall events as functions of soil and plot characteristics and therefore offer a potential to increase the informative value of camera-based soil erosion measurements on agricultural fields.