ESurfD Earth Surface Dynamics Discussions ESurfD Earth Surf. Dynam. Discuss. 2196-6338 Göttingen, Germany 10.5194/esurf-2022-38 Influences of Slope Angle on Propagation and Deposition of Laboratory Landslides Wu Yan-Bin https://orcid.org/0000-0002-3395-1027 1 2 Duan Zhao 2 3 Peng Jian-Bing 4 5 Zhang Qing 1 2 Graduate Student, College of Geology and Environment, Xi’an University of Science and Technology, Xi’an 710054, China Institute of Ecological Environment Restoration in Mine Areas of West China, Xi’an University of Science and Technology, Xi’an, 710054, China Associate Professor, College of Geology and Environment, Xi’an University of Science and Technology, Xi’an 710054, China School of geology engineering and Geomatics, Chang’an University, Xi’an 710054, China Key Laboratory of western Mineral Resources and Geological Engineering of Ministry of Education, Chang’an University, Xi’an 710054, China National Natural Science Foundation of China 42177155 National Natural Science Foundation of China 41790442 National Natural Science Foundation of China 41702298 26 07 2022 2022 1 34 Copyright: © 2022 Yan-Bin Wu et al. 2022 This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit https://creativecommons.org/licenses/by/4.0/ This article is available from https://esurf.copernicus.org/preprints/esurf-2022-38/ The full text article is available as a PDF file from https://esurf.copernicus.org/preprints/esurf-2022-38/esurf-2022-38.pdf

<p>Slope angle is an important influence on the motion characteristics and deposit morphologies of landslides. In this study, an advanced 3D scanner was used to study laboratory landslides at various slope angles. The laboratory landslides had different motion characteristics. An increase of the runout of the laboratory landslides with the slope angles meant that the amount of energy loss was great due to the collision of sliding mass at the slope break. The length and area of these laboratory landslides increased first and then decreased during their whole motion. The surface morphologies of the deposits differed according to the slope angles. At low slope angles, they exhibited a series of transverse ridges formed by overthrusting. At moderate slope angles, they exhibited conjugate troughs (X-shape wash) formed by shearing on the accumulation zone. At high slope angles, they exhibited a double-upheaval morphology formed by the rear portion of the sliding mass impacting the forward portion. A theoretical relationship between the apparent friction coefficient and slope angle is proposed, based on a hypothesis the ratio of energy dissipation occurring when an object collides with a plane is exponentially related to the acute angle between the object&rsquo;s direction and the plane&rsquo;s normal direction. The study will support studies on the morphological variation during the whole motion and mobility of landslides.</p>