Oblique aggradation: a novel explanation for sinuosity of low‐energy streams in peat‐filled valley systems

机译：倾斜委托：泥炭谷系统中低能量流陷性的新颖解释

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Abstract > Low‐energy streams in peatlands often have a high sinuosity. However, it is unknown how this sinuous planform formed, since lateral migration of the channel is hindered by relatively erosion‐resistant banks. We present a conceptual model of Holocene morphodynamic evolution of a stream in a peat‐filled valley, based on a palaeohydrological reconstruction. Coring, ground‐penetrating radar (GPR) data, and 14 C and OSL dating were used for the reconstruction. We found that the stream planform is partly inherited from the Late‐Glacial topography, reflecting stream morphology prior to peat growth in the valley. Most importantly, we show that aggrading streams in a peat‐filled valley combine vertical aggradation with lateral displacement caused by attraction to the sandy valley sides, which are more erodible than the co‐evally aggrading valley‐fill. Owing to this oblique aggradation in combination with floodplain widening, the stream becomes stretched out as channel reaches may alternately aggrade along opposed valley sides, resulting in increased sinuosity over time. Hence, highly sinuous planforms can form in peat‐filled valleys without the traditional morphodynamics of alluvial bed lateral migration. Improved understanding of the evolution of streams provides inspiration for stream restoration. Copyright ? 2016 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> >低泥炭地的能量流往往具有高度的秩序。然而，由于通道的横向迁移是由相对腐蚀的堤坝阻碍的，因此是如何形成这种蜿蜒的平面形状的。我们基于古物学重建，在泥炭堆中的泥炭谷中流入的全新世形态动力学演变的概念模型。取芯，地面穿透雷达（GPR）数据和<SUP> 14 </ sup> C和OSL约会用于重建。我们发现流塑料部分是从晚期冰川地形继承的，反映在谷地泥浆中的生长之前的流形态。最重要的是，我们表明，泥炭填充谷中的加重流与由吸引引起的横向位移相结合，该横向位移与沙谷侧面上的横向位移相比，这比共同避免的加速谷填充更易于侵蚀。由于这种倾斜的加重与泛洪叶扩大，由于通道达到沿着相对的山谷侧，该沟伸出的流延伸，导致随着时间的推移增加了秩序的增加。因此，高度蜿蜒的平面形式可以在泥炭填充的山谷中形成，而没有激发床横向迁移的传统形态学。改善了对流的演变的理解提供了流恢复的灵感。版权？ 2016 John Wiley＆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15期</span><b style="margin: 0 2px;">|</b><span>共18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=Candel Jasper H.J.&option=202" target="_blank" rel="nofollow">Candel Jasper H.J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Makaske Bart&option=202" target="_blank" rel="nofollow">Makaske Bart;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Storms Joep E.A.&option=202" target="_blank" rel="nofollow">Storms Joep E.A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wallinga Jakob&option=202" target="_blank" rel="nofollow">Wallinga Jakob;</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>Soil Geography and Landscape groupWageningen UniversityP.O. Box 47 6700AA Wageningen The Netherlands;</p> <p>Soil Geography and Landscape groupWageningen UniversityP.O. Box 47 6700AA Wageningen The Netherlands;</p> <p>Faculty of Civil Engineering and GeosciencesDelft University of TechnologyP.O. Box 5048 2628CN Delft The Netherlands;</p> <p>Soil Geography and Landscape groupWageningen UniversityP.O. Box 47 6700AA Wageningen The Netherlands;</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;"> </p> </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/0704023139147.html">Oblique aggradation: a novel explanation for sinuosity of low‐energy streams in peat‐filled valley systems</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Candel Jasper H.J.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Candel Jasper H.J.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Makaske Bart&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Makaske Bart,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Storms Joep E.A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Storms Joep E.A.,</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15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：倾斜委托：泥炭谷系统中低能量流陷性的新颖解释</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_science-total-environment_thesis/020412019668.html">The effects of mountaintop mines and valley fills on the physicochemical quality of stream ecosystems in the central Appalachians: A review</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Michael B. 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