Abstract
The morphology of the failure scar has been a long-debated issue concerning the Loess Plateau of China, and the lack of normative data has hampered vital research in this area. In this chapter, a series of laboratory experiments were conducted to observe the failure geometries and volumes under rainfall simulations. The following six failure-scar types occurred: Tf, Cd, Cu, Ia, Ps, and Co. Tf, Cd, and Cu were the three major types of failure scars during the process of gravity erosion on a steep loess slope, and the scar Tf was the most significant. A relatively dangerous failure scar (Tf) might appear if the slope became steeper, or if the rainfall became more intensive. In addition, a long-duration storm could easily induce a large-volume failure with a Cu scar. The experimental results obtained here provide a morphogenic insight into the gravity-erosion control on a loess gully sidewall.
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Xu, X., Zhu, T., Zhang, H., Gao, L. (2020). Detecting Fingerprints of Gravity Erosion Drivers: A Laboratory Experiment. In: Experimental Erosion. Springer, Singapore. https://doi.org/10.1007/978-981-15-3801-8_11
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