Predicting the geomorphological responses of gravel‐bed rivers to flow and sediment source perturbations at the watershed scale: an application in an Alpine watershed

机译：预测流域水垢流动和沉积物源扰动的砾石床河流的地貌响应：高山流域的应用

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Abstract > Predicting morphological channel changes using physically‐based models requires extended data for the description of the river channel and for hydrological and sedimentological inputs. At the watershed scale, these data are usually scarce, and such a refined modeling is typically difficult to build. A simpler modeling of the morphological impacts due to the changes in the principal drivers that control channel shape and dynamics is more adaptable. In this study we focused on the morphological responses of gravel‐bed rivers to flow and sediment source perturbation at watershed scale. The aim is to develop and test a tool capable of semi‐quantitatively predicting the morphological river response at the watershed scale due to a set of spatially distributed perturbations. The model considers flow regime (Q) and sediment supply (S) as the two main factors controlling the fluvial morphology in alluvial rivers. Two indicators have been proposed to evaluate the alteration on Q and S, and they are illustrated as vectors on each reach of the river network. The magnitude of the vectors corresponds to the intensity of the perturbation and its direction represents the changing trend that nine selected morphological variables (bed elevation, slope, width, depth, wetted area, width to depth ratio, d50, terrace formation, and colonization of vegetation) are likely to follow from an initial state. The trends or trajectories of changes were assessed based on empirical relations, case studies, and conceptual models. This method was applied to the Isère watershed (5700 km 2 ) at Grenoble (France), a river that hosts large and complex hydropower plant systems constructed during 50s ‐70s. The predictions over 23 river reaches and eight variables were evaluated in the range where the model was capable of predict </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> >预测形态使用基于物理模型的频道变化需要扩展数据，用于河道的描述和水文和沉积物输入。在流域的规模处，这些数据通常是稀缺的，并且这种精致的建模通常难以构建。由于控制信道形状和动态的主要驱动因素的变化而更简单的形态学影响更适合。在这项研究中，我们专注于砾石床河流的形态学响应流域水垢的流动和沉积源扰动。目的是开发和测试一种能够半定量预测流域规模的形态学河响应的工具，由于一组空间分布的扰动。该模型认为流量（Q）和沉积物供应作为控制冲积河流中河流形态的两个主要因素。已经提出了两种指标来评估Q和S的改变，它们被称为河网络每次到达的载体。 vectors的幅度对应于扰动的强度，其方向代表了九个所选形态变量（床海拔，斜坡，宽度，深度，湿润的区域，深度比，D50，露天地层和定植的变化趋势植被）可能从初始状态下遵循。根据经验关系，案例研究和概念模型评估变更的趋势或轨迹。该方法应用于Grenoble（法国）的Isère流域（5700 km 2 </ sup>），该河流在50年代-70s构建的大型和复杂的水电厂系统中占有大型和复杂的水电厂。在模型能够预测的范围内评估超过23次河流达到的预测和八个变量 </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4期</span><b style="margin: 0 2px;">|</b><span>共15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=Alcayaga Hernán A.&option=202" target="_blank" rel="nofollow">Alcayaga Hernán A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mao Luca&option=202" target="_blank" rel="nofollow">Mao Luca;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Belleudy Philippe&option=202" target="_blank" rel="nofollow">Belleudy Philippe;</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 EngineeringUniversidad Diego Portales UDPSantiago Chile;</p> <p>Department of Ecosystems and EnvironmentPontificia Universidad Catolica de ChileSantiago Chile;</p> <p>Univ. Grenoble Alpes CNRS IRD Grenoble INP IGE38000 Grenoble France;</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=predictor model&option=203" rel="nofollow">predictor model;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=morphological response&option=203" rel="nofollow">morphological response;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Alpine GBR&option=203" rel="nofollow">Alpine GBR;</a> </p> <div class="translation"> 机译：预测模型;形态反应;高山GBR; </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/0704023139204.html">Predicting the geomorphological responses of gravel‐bed rivers to flow and sediment source perturbations at the watershed scale: an application in an Alpine watershed</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Alcayaga Hernán A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Alcayaga Hernán A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mao Luca&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Mao Luca,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Belleudy Philippe&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Belleudy Philippe </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>2018</span><span>,第4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：预测流域水垢流动和沉积物源扰动的砾石床河流的地貌响应：高山流域的应用</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_gsa-bulletin_thesis/020416177152.html">Predicting grain size in gravel-bedded rivers using digital elevation models: Application to three Maine watersheds</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Noah P. 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V. </a> <span>1979</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：IJC menomonee河流域研究：menomonee河流域的土壤，沉积物，尘埃和土壤的土壤和元素组成的分散性。第6卷</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201295532222.html">喀斯特流域空间结构与地貌瞬时单位线应用──以贵州后寨地下河流域为例</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王腊春&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 王腊春</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=杨晓轩&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,杨晓轩</a> <span> <a href="/journal-cn-56805/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 南京大学学报：自然科学版 </a> </span> <span> . 1995</span><span>,第4期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-lake-sciences_thesis/0201270246408.html">云南小江流域典型泥石流沟中底栖动物群落特征及其对河流地貌的响应</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=朱朋辉&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 朱朋辉</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=潘保柱&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,潘保柱</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李志威&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李志威</a> <span> <a href="/journal-cn-4955/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 湖泊科学 </a> </span> <span> . 2019</span><span>,第003期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_seismology-geology_thesis/0201253220840.html">涪江流域河流地貌特征对虎牙断裂带活动性的响应</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=梁欧博&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 梁欧博</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=任俊杰&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,任俊杰</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=吕延武&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,吕延武</a> <span> <a href="/journal-cn-4916/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地震地质 </a> </span> <span> . 2018</span><span>,第001期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_technology-wind_thesis/0201289122642.html">基于等价地貌参数的地貌单位线在羊昌河流域的构建与应用</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张程玥&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 张程玥</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=朱少成&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,朱少成</a> <span> <a href="/journal-cn-5179/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 科技风 </a> </span> <span> . 2021</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_hubei-forestry-science-technology_thesis/0201260329427.html">喀斯特地貌小流域生态恢复对策研究——以贵州沿河县白泥河流域为例</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵志国&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 赵志国</a> <span> <a href="/journal-cn-6988/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 湖北林业科技 </a> </span> <span> . 2013</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-40610_thesis/020222455965.html">干旱区内陆河流域植被覆盖度对土地利用变化的响应——以石羊河流域为例</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=WEI Wei&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . WEI Wei</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=魏伟&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,魏伟</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=JIE Bin-bin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,JIE Bin-bin</a> <span> <a href="/conference-cn-40610/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 2016’中国新时期土地资源科学与新常态创新发展战略研讨会暨中国自然资源学会土地资源研究专业委员会30周年纪念会 </a> <span> <span> . 2016</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020315927210.html">云南小江流域典型泥石流沟中底栖动物对河流地貌的响应研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=朱朋辉&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 朱朋辉</a> <span> . 2020</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" 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href="/patent-detail/06130448176351.html">Non-contacting flow monitoring system suitable for e.g. medical or analytic applications, comprises a heat source inducing thermal perturbations detectable downstream</a> <b>[P]</b> . <span> 外国专利：  DE10063998A1 </span> <span> . 2001-07-05</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：非接触式流量监控系统适用于例如医学或分析应用，包括引起热扰动的热源，可在下游进行检测 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704023139204','4',7,2,1,'',this,24)" 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