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Excavation of subglacial bedrock channels by seasonal meltwater flow

机译:季节性熔融流动挖掘子夹层基岩通道

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摘要

Abstract > Subglacial water flow drives the excavation of a variety of bedrock channels including tunnel valleys and inner gorges. Subglacial floods of various magnitudes – events occurring once per year or less frequently with discharges larger than a few hundred cubic metres per second – are often invoked to explain the erosive power of subglacial water flow. In this study we examine whether subglacial floods are necessary to carve bedrock channels, or if more frequent melt season events (e.g. daily production of meltwater) can explain the formation of substantial bedrock channels over a glacial cycle. We use a one‐dimensional numerical model of bedrock erosion by subglacial meltwater, where water flows through interacting distributed and channelized drainage systems. The shear stresses produced drive bedrock erosion by bed‐ and suspended‐load abrasion. We show that seasonal meltwater discharge can incise an incipient bedrock channel a few tens of centimetres deep and several metres wide, assuming abrasion is the only mechanism of erosion, a particle size of <fi>D</fi> =256 mm and a prescribed sediment supply per unit width. Using the same sediment characteristics, flood flows yield wider but significantly shallower bedrock channels than seasonal meltwater flows. Furthermore, the smaller the shear stresses produced by a flood, the deeper the bedrock channel. Shear stresses produced by seasonal meltwater are sufficient to readily transport boulders as bedload. Larger flows produce greater shear stresses and the sediment is carried in suspension, which produces fewer contacts with the bed and less erosion. We demonstrate that seasonal meltwater discharge can excavate bedrock volumes commensurate with channels several tens of metres to a few hundred metres wide and several tens of metre </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”xml:id =“esp4367-abs-abs-0001”> <标题类型=“main” >摘要</ title> >底透射水流驱动各种基岩通道的挖掘,包括隧道谷和内部峡谷。各种大小的底污水 - 每年发生一次或者每秒大于每秒大于几百立方米的排放发生的事件 - 经常调用以解释底透射水流的腐蚀力。在这项研究中,我们研究了雕刻基岩频道是否需要底裂洪水,或者如果更频繁的熔体季事件(例如,每日生产的熔融水)可以解释在冰川周期上的基本上基岩通道的形成。我们使用沉淀熔融水的基岩侵蚀的一维数值模型,其中水流通过交互分布和通道的排水系统。剪切应力通过床和悬浮载荷磨损产生了驱动基岩侵蚀。我们表明,季节性熔融水排放可以切割出初始的基岩通道几十厘米深,几米宽,假设磨损是侵蚀的唯一机制,粒度为<fi> d </ fi> = 256毫米和一个规定的每单位宽度的沉积物供应。使用相同的沉积物特性,洪水流量越来越宽,但显着较浅的基岩通道比季节熔融流动。此外,洪水产生的剪切应力越小,基岩通道越深。由季节熔融水产生的剪切应力足以容易地将巨石运输为床单。较大的流量产生更大的剪切应力,并且沉积物悬浮在悬浮液中,其与床和较少的侵蚀产生较少的接触。我们证明季节性熔融水排放可以挖掘基岩体积与通道相称,几十米到几百米宽,几十米 </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>2018年第9期</span><b style="margin: 0 2px;">|</b><span>共13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=Beaud Flavien&option=202" target="_blank" rel="nofollow">Beaud Flavien;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Venditti Jeremy G.&option=202" target="_blank" rel="nofollow">Venditti Jeremy G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Flowers Gwenn E.&option=202" target="_blank" rel="nofollow">Flowers Gwenn E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Koppes Michele&option=202" target="_blank" rel="nofollow">Koppes Michele;</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 Earth SciencesSimon Fraser UniversityBurnaby V5A1S6 British Columbia Canada;</p> <p>Department of GeographySimon Fraser UniversityBurnaby V5A1S6 British Columbia Canada;</p> <p>Department of Earth SciencesSimon Fraser UniversityBurnaby V5A1S6 British Columbia Canada;</p> <p>Department of GeographyUniversity of British ColumbiaVancouver V6T1Z2 British Columbia Canada;</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=glacial erosion&option=203" rel="nofollow">glacial erosion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subglacial hydrology&option=203" rel="nofollow">subglacial hydrology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subglacial meltwater erosion&option=203" rel="nofollow">subglacial meltwater erosion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tunnel valley&option=203" rel="nofollow">tunnel valley;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=inner gorge&option=203" rel="nofollow">inner gorge;</a> </p> <div class="translation"> 机译:冰川侵蚀;底透明水文;底裂解熔融侵蚀;隧道山谷;内峡谷; 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