Understanding mass fluvial erosion along a bank profile: using PEEP technology for quantifying retreat lengths and identifying event timing

机译：了解沿银行资料的大规模氟侵蚀：使用PEEP技术来量化撤退长度和识别事件时间

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Abstract >This study provides fundamental examination of mass fluvial erosion along a stream bank by identifying event timing, quantifying retreat lengths, and providing ranges of incipient shear stress for hydraulically driven erosion. Mass fluvial erosion is defined here as the detachment of thin soil layers or conglomerates from the bank face under higher hydraulic shear stresses relative to surface fluvial erosion, or the entrainment of individual grains or aggregates under lower hydraulic shear stresses. > We explore the relationship between the two regimes in a representative, US Midwestern stream with semi‐cohesive bank soils, namely Clear Creek, IA. Photo‐Electronic Erosion Pins (PEEPs) provide, for the first time, in situ measurements of mass fluvial erosion retreat lengths during a season. The PEEPs were installed at identical locations where surface fluvial erosion measurements exist for identifying the transition point between the two regimes. This transition is postulated to occur when the applied shear stress surpasses a second threshold, namely the critical shear stress for mass fluvial erosion. >We hypothesize that the regimes are intricately related and surface fluvial erosion can facilitate mass fluvial erosion. Selective entrainment of unbound/exposed, mostly silt‐sized particles at low shear stresses over sand‐sized sediment can armor the bank surface, limiting the removal of the underlying soil. The armoring here is enhanced by cementation from the presence of optimal levels of sand and clay. Select studies show that fluvial erosion strength can increase several‐fold when appropriate amounts of sand and clay are mixed and cement together. Hence, soil layers or conglomerates are entrained with higher flows. >The critical shear stress for mass fluvial erosion was found to be an order of magnitude higher than that of surface fluvial erosion, and proceeded with higher (approximately 2–4 times) erodibility. The results were well represented by a mechanistic detachment model that captures the two regimes. 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”> <title type =“main”>抽象</ title> >本研究提供了对大规模河流侵蚀的基本检查通过识别事件定时，量化撤退长度以及为液压驱动侵蚀提供初剪的范围来沿着流银行。这里定义了大规模氟侵蚀，因为在较高液压剪切应力下，在相对于表面潮流的较高液压剪切应力下的薄土层或砾岩的分离，或在较低液压剪切应力下夹带单粒或聚集体。> >我们探讨了两个代表的制度之间的关系，美国中西部溪流与半凝聚力池土壤，即清晰的小溪，IA。照片 - 电子侵蚀引脚（窥视）首次提供原位</ i>在季节期间的大规模河流侵蚀撤退长度的测量。窥视安装在相同的位置，存在用于识别两种制度之间的过渡点的表面氟侵蚀测量。当施加的剪切应力超过第二阈值时，将出现这种转变，即批量氟侵蚀的临界剪切应力。我们假设制度是错综复杂的相关，表面氟腐蚀可以促进质量氟侵蚀。选择性夹带未结合的/暴露，大多数淤泥颗粒在砂浆沉积物上的低剪切应力，可以装甲堤表面，限制底层土壤。这里的铠装是通过最佳水平的沙子和粘土的存在而增强。选择研究表明，当适量的沙子和粘土混合并水解时，氟尿侵蚀强度可以增加几倍。因此，土壤层或聚合物夹带较高的流量。</ p> >对大规模氟腐蚀的临界剪切应力被发现是高于表面氟侵蚀的级，并且进行更高（约2 -4次）蚀刻性。结果由机械分离模型表示符合捕获两种制度的机械脱离模型。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11期</span><b style="margin: 0 2px;">|</b><span>共16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=Papanicolaou A. N. Thanos&option=202" target="_blank" rel="nofollow">Papanicolaou A. N. Thanos;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wilson Christopher G.&option=202" target="_blank" rel="nofollow">Wilson Christopher G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tsakiris Achilles G.&option=202" target="_blank" rel="nofollow">Tsakiris Achilles G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sutarto Tommy E.&option=202" target="_blank" rel="nofollow">Sutarto Tommy E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bertrand Fabienne&option=202" target="_blank" rel="nofollow">Bertrand Fabienne;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rinaldi Massimo&option=202" target="_blank" rel="nofollow">Rinaldi Massimo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dey Subhasish&option=202" target="_blank" rel="nofollow">Dey Subhasish;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Langendoen Eddy&option=202" target="_blank" rel="nofollow">Langendoen Eddy;</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>Department of Civil and Environmental EngineeringUniversity of TennesseeKnoxville TN USA;</p> <p>Department of Civil and Environmental EngineeringUniversity of TennesseeKnoxville TN USA;</p> <p>Department of Civil and Environmental EngineeringUniversity of TennesseeKnoxville TN USA;</p> <p>Civil Engineering Samarinda State PolytechnicSamarinda East Kalimantan Indonesia;</p> <p>Civil Engineering IIHRThe University of IowaIowa City IA USA;</p> <p>Dipartimento di Scienze della TerraUniversità di FirenzeFirenze Italy;</p> <p>Department of Civil EngineeringIndian Institute of TechnologyKharagpur West Bengal India;</p> <p>USDA Agricultural Research ServiceNational Sedimentation LaboratoryOxford MS USA;</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=mass fluvial erosion&option=203" rel="nofollow">mass fluvial erosion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=PEEPs&option=203" rel="nofollow">PEEPs;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=erodibility&option=203" rel="nofollow">erodibility;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=armoring&option=203" rel="nofollow">armoring;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=cementation&option=203" rel="nofollow">cementation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Clear Creek&option=203" rel="nofollow">Clear Creek;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Iowa&option=203" rel="nofollow">Iowa;</a> </p> <div class="translation"> 机译：大规模氟侵蚀;偷看;蚀刻;铠装;胶泥;清溪;爱荷华州; </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/0704023139082.html">Understanding mass fluvial erosion along a bank profile: using PEEP technology for quantifying retreat lengths and identifying event timing</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Papanicolaou A. 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