A study of a flowslide with significant entrainment in loess areas in China

机译：中国黄土地区具有重要夹带的絮凝物研究

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Abstract >Flowslides are a frequent type of natural disaster in loess areas and may result in the significant loss of properties and/or casualties. The Dagou flowslide is a typical event in a loess area and is accompanied by significant sediment entrainment. To analyze the mechanisms responsible for flowslides and to obtain the parameters for a runout analysis, a field investigation was conducted. Specimens were sampled on site to carry out laboratory tests, including a triaxial test, sieve analysis, and chemical component analysis. The parameters were used in the runout study employing an energy‐based runout model. An analytical entrainment model was adopted to calculate the entrainment after considering physical properties and the mechanism of the entrainment process of the loess. Finally, the entrainment model was incorporated into the runout model to simulate the post‐failure process of this case. Energy dissipation due to the deformation of slices was considered as it was thought to be important for a slide with a significant deformation. The simulation results were compared with the measurements, including runout distance, total volume, erosion depth, deposition height at different sections, and velocities at specific locations. The results indicate that the energy‐based runout model, together with the entrainment model, can capture the kinematic characteristics of the Dagou flowslide. Therefore, it is feasible to use this model to predict the runout characteristics of flowslides in similar areas. Copyright ? 2017 John Wiley & Sons, Ltd. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><abstract xmlns =“http://www.wiley.com/namespaces/wiley”type =“main”xml：lang =“en”> <title type =“main”>抽象</ title> > flowslides是黄土地区经常类型的自然灾害，可能导致性质和/或伤亡的显着损失。 DAGOU FLOWSLIDE是黄土地区的典型活动，并伴随着重要的沉积物夹带。为了分析负责絮凝物的机制，并获得跳动分析的参数，进行了现场调查。在现场采集标本以进行实验室测试，包括三轴试验，筛分分析和化学成分分析。参数用于采用基于能量的跳动模型的跳动研究。采用分析夹带模型在考虑到物理性质和黄土夹带过程的机制后计算夹带。最后，夹带模型被纳入跳动模型，以模拟这种情况的失败后处理。由于切片的变形而导致的能量耗散，因为它被认为对具有显着变形的载玻片是重要的。将模拟结果与测量结果进行比较，包括跳动距离，不同部分的跳动距离，总体积，侵蚀深度，沉积高度，以及特定位置的速度。结果表明，基于能量的跳动模型与夹带模型一起，可以捕获DAGOU Flowslide的运动学特征。因此，使用该模型是可行的，以预测类似领域的流动卷发的跳动特征。版权？ 2017年John Wiley＆amp; SONS，LTD。</ p> </ abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-22319/'>《Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group》</a> <b style="margin: 0 2px;">|</b><span>2017年第14期</span><b style="margin: 0 2px;">|</b><span>共11页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Fanyu&option=202" target="_blank" rel="nofollow">Zhang Fanyu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kang Chao&option=202" target="_blank" rel="nofollow">Kang Chao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chan Dave&option=202" target="_blank" rel="nofollow">Chan Dave;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Xiaochao&option=202" target="_blank" rel="nofollow">Zhang Xiaochao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pei Xiangjun&option=202" target="_blank" rel="nofollow">Pei Xiangjun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Peng Jianbing&option=202" target="_blank" rel="nofollow">Peng Jianbing;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Key Laboratory of Mechanics on Disaster and Environment in Western China The Ministry of Education of China: School of Civil Engineering and MechanicsLanzhou UniversityLanzhou Gansu P. R. China;</p> <p>Department of Civil and Environmental EngineeringUniversity of AlbertaEdmonton Alberta Canada;</p> <p>Department of Civil and Environmental EngineeringUniversity of AlbertaEdmonton Alberta Canada;</p> <p>State Key Laboratory of Geohazard Prevention and Geoenvironment ProtectionChengdu University of TechnologyChengdu P. R. China;</p> <p>State Key Laboratory of Geohazard Prevention and Geoenvironment ProtectionChengdu University of TechnologyChengdu P. R. China;</p> <p>Department of Geological Engineering Chang'an University Xi'anShaanxi P. R. China;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=flowslide&option=203" rel="nofollow">flowslide;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=loess&option=203" rel="nofollow">loess;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=entrainment&option=203" rel="nofollow">entrainment;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=numerical modeling&option=203" rel="nofollow">numerical modeling;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=energy‐based runout model&option=203" rel="nofollow">energy‐based runout model;</a> </p> <div class="translation"> 机译：弗罗德拉莱;黄土;夹带;数值建模;基于能量的跳动模型; </div> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023139135.html">A study of a flowslide with significant entrainment in loess areas in China</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Fanyu&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zhang Fanyu,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kang Chao&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kang Chao,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chan Dave&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Chan Dave,</a> <a href="/journal-foreign-22319/" target="_blank" rel="nofollow" class="tuijian_authcolor">Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group .</a> <span>2017</span><span>,第14期</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：中国黄土地区具有重要夹带的絮凝物研究</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023194535.html">Analysis of retrogressive loess flowslides in Heifangtai, China</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Qi Xing&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Qi Xing,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xu Qiang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Xu Qiang,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Fangzhou&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Liu Fangzhou </a> <a href="/journal-foreign-22625/" target="_blank" rel="nofollow" class="tuijian_authcolor">Engineering Geology .</a> <span>2018</span><span>,第期</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：海夫泰泰，中国的倒退黄土弗洛德莱德分析</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/07040773963.html">Occurrence of landsliding on slopes where flowsliding had previously occurred: an investigation in a loess platform, North-west China.</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xu L.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Xu L.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dai F. 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