Results 1 to 10 of about 72 (65)
Slope Rill Erosion and Morphological Evolution Based on UAV Nap-of-the-object Photogrammetry [PDF]
, 2023 [Objective] This study was conducted to determine a rill erosion technology having high efficiency, high accuracy and strong adaptability, and overcome deficiencies associated with traditional measurement methods (low efficiency, high cost, poor ...
Gao Zhaoliang +7 more
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Evaluation of Collapse Susceptibility Based on a Contribution Rate Model [PDF]
, 2022 [Objective] The spatial database of geological disaster field survey was conducted to analyze the formation mechanism and failure mode of collapse in the area where granite weathered residual soil was developed, to explore the contribution rate of ...
Cai Junjian +4 more
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Major Achievements and Future Key Fields of Soil Erosion Research in China [PDF]
, 2022 [Objective] The developing history of soil erosion research in China was reviewed, the major research achievements were summarized, and the current problems and key research fields in the future were analyzed to provide a reference for China's soil and ...
Cai Qiangguo, Ke Qihua, Zhang Keli
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Assessment of landslide susceptibility in the Huangshui River Basin based on catastrophe theory [PDF]
, 2023 The Huangshui River Basin, an important upstream tributary of the upper reaches of the Yellow River, serves as the political, economic, and cultural center of Qinghai Province, and is also a region with a high incidence of geological disasters.
Bin LI +4 more
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Shuitu Baochi Xuebao, 2023 南方花岗岩崩岗侵蚀区崩壁常见形似内凹洞的特殊地貌(龛穴),该地貌的发育可引起崩壁失稳并扩大崩岗侵蚀范围。通过刻画龛穴形态演变过程,研究龛穴发生的物质条件与驱动因素,并结合力矩分析方法构建力学模型评价崩壁及龛穴稳定性。研究表明:龛穴形态演变经历"雏形—发育—形成"3个过程,剖面土层异质性是龛穴发育的基础条件,水力与重力作为外部因素共同作用驱动龛穴发育。龛穴稳定性随其高度增加、角度减小而降低。龛穴的发育可能是崩岗溯源侵蚀启动的标志,遏制龛穴形成有利于提高崩壁稳定性,研究结果为崩岗侵蚀治理提供理论依据。
何玲, 邓羽松
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Shuitu Baochi Xuebao, 2022 为探究我国南方花岗岩红壤地区崩岗的起始标志和发育阶段。在湖北省通城县和广西岑溪市2个典型崩岗区调查崩岗的发育过程。结果表明，2个调查区都存在一种细沟发育而来的龛状浅沟，将其命名为龛沟。龛沟具有3个特征：上游有明显细沟，沟壁陡峭且具有上窄下宽的宽深梯形形态。龛沟主要发生在砂土层裸露、具有一定汇水面积和局地坡度>30°的裸露坡面。龛沟是一种特殊形态的浅沟，其定义、形态和侵蚀营力都不同于常规浅沟、切沟和Amphitheatershaped canyons等沟蚀地貌 ...
高钰淏 +5 more
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Shuitu Baochi Xuebao, 2022 为提高崩岗土体稳定性,抑制崩壁崩塌。试验共设计6次干湿循环,利用工业相机对脱湿过程中崩岗4层土进行定时定点拍照并结合数字图像处理技术,研究干湿效应下崩岗土体的裂隙演化及收缩变形规律。结果表明:(1)脱湿过程中土体形态变化顺序为轴向收缩、径向收缩和裂隙发育;(2)表面裂隙率与 液限、塑性指数、黏粒含量呈显著正相关关系,4层土中表面裂隙率最大值为过渡层18.78%,最小值为砂土层5.41%,崩岗土体剖面上两者为相邻土层,较大差异性会严重破坏崩岗的稳定性;(3)随干湿循环的进行,径向收缩不再发生,轴向收缩 ...
王佳妮 +5 more
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The festival of fast-breaking Eid al-Fitr in the Great Mosque of Lhasa. Some observations [PDF]
, 2016 Cet article décrit la fête de la rupture de jeûne célébrée à la fin du Ramadan par les musulmans de Lhasa au Tibet. Il s’appuie sur une enquête de terrain qui s’est déroulée du 6 août au 6 septembre 2011.This article describes the fast-breaking festival ...
Yang, Xiaochun
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Shuitu Baochi Xuebao, 2021 裂隙发育降低土体承载力、抗剪强度、凝聚力等力学特性，促使崩壁崩塌。在控制土体厚度（0.8，1.6，2.2 cm）条件下，对崩岗4层土体进行室内脱湿试验，通过相机定时定点拍照，并结合数字图像处理技术分析崩岗土体的裂隙演化特征。结果表明：（1）脱湿过程中土体变形均先产生核心收缩，后产生裂隙，且4层土中过渡层最早产生核心收缩与裂隙发育现象；（2）4层土之间，裂隙发育程度呈现为过渡层>红土层>表土层>砂土层，过渡层与砂土层的较大差异会破坏土体的稳定性，加速崩壁崩塌；（3）随着土体厚度的增加，裂隙发育现象减弱 ...
王娜, 王佳妮, 张晓明, 段晓阳
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