Estimation of large wood budgets in a watershed and river corridor at interdecadal to interannual scales in a cold‐temperate fluvial system

机译：在冷水温带河流系统中跨越流域和河流走廊大型木材预算的估算

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Abstract >Large wood (LW) is a ubiquitous feature in rivers of forested watersheds worldwide, and its importance for river diversity has been recognized for several decades. Although the role of LW in fluvial dynamics has been extensively documented, there is a need to better quantify the most significant components of LW budgets at the river scale. The purpose of our study was to quantify each component (input, accumulation, and output) of a LW budget at the reach and watershed scales for different time periods (i.e. a 50‐year period, decadal cycle, and interannual cycle). The LW budget was quantified by measuring the volumes of LW inputs, accumulations, and outputs within river sections that were finally evacuated from the watershed. The study site included three unusually large but natural wood rafts in the delta of the Saint‐Jean River (SJR; Québec, Canada) that have accumulated all LW exported from the watershed for the last 50?years. We observed an increase in fluvial dynamics since 2004, which led to larger LW recruitment and a greater LW volume trapped in the river corridor, suggesting that the system is not in equilibrium in terms of the wood budget but is rather recovering from previous human pressures as well as adjusting to hydroclimatic changes. The results reveal the large variability in the LW budget dynamics during the 50‐year period and allow us to examine the eco‐hydromorphological trajectory that highlights key variables (discharge, erosion rates, bar surface area, sinuosity, wood mobility, and wood retention). Knowledge on the dynamics of these variables improves our understanding of the historical and future trajectories of LW dynamics and fluvial dynamics in gravel‐bed rivers. Extreme events (flood and ice‐melt) significantly contribute to LW dynamics in the SJR river system. 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> >大木（lw）是一个无处不在的功能在全球森林流域的河流中，几十年来，河流多样性的重要性得到了认可。虽然LW在河流的动态中的作用被广泛记录，但需要更好地量化河流规模的LW预算中最重要的组成部分。我们的研究目的是在不同时间段（即50年期间，截止周期和际周期中，量化LW预算的每个组件（输入，累积和输出）和流域等级。通过测量最终从流域疏散的河段内的LW输入，累积和输出量来量化LW预算。该研究现场包括三个异常大但天然的木筏，在圣徒河河（SJR;Québec，加拿大）积累了过去50岁的流域出口的所有LW。我们观察到自2004年以来的河流动力学增加，导致了较大的LW招聘和陷入河流走廊中的更大的LW体积，表明该系统在木材预算方面并不均衡，而是从以前的人类压力恢复以及调整循环变化。结果揭示了50年期间LW预算动态的巨大可变性，并允许我们检查突出关键变量的生态水形式轨迹（放电，侵蚀率，酒吧表面积，污染，木材流动性和木材保留）。关于这些变量动态的知识可以改善我们对砾石床河流LW动态和河流动力学的历史和未来轨迹的理解。极端事件（洪水和冰冻）在SJR河流系统中显着促进LW动态。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13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=Boivin Maxime&option=202" target="_blank" rel="nofollow">Boivin Maxime;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Buffin‐Bélanger Thomas&option=202" target="_blank" rel="nofollow">Buffin‐Bélanger Thomas;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Piégay Hervé&option=202" target="_blank" rel="nofollow">Piégay Hervé;</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>Département de Biologie Chimie et Géographie and Centre d'études Nordiques (CEN)Université du Québec à RimouskiRimouski Québec Canada;</p> <p>Département de Biologie Chimie et Géographie and Centre d'études Nordiques (CEN)Université du Québec à RimouskiRimouski Québec Canada;</p> <p>Université de LyonENS de Lyon CNRS UMR 5600 EVSLyon 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=large wood in river&option=203" rel="nofollow">large wood in river;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=large wood budget&option=203" rel="nofollow">large wood budget;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=eco‐hydromorphology trajectory&option=203" rel="nofollow">eco‐hydromorphology trajectory;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=watershed scale&option=203" rel="nofollow">watershed scale;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=wood transport&option=203" rel="nofollow">wood transport;</a> </p> <div class="translation"> 机译：河里大木材;大型木材预算;生态水形式轨迹;流域秤;木运输; 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