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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Early Holocene dune field development in Dalarna, central Sweden: A geomorphological and geophysical case study
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Early Holocene dune field development in Dalarna, central Sweden: A geomorphological and geophysical case study

机译:瑞典中部达拉纳的早期全新世沙田开发:地貌和地球物理案例研究

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Abstract > Bon?sheden, Sweden's largest continuous dune field, situated in the county of Dalarna, central Sweden, has been investigated using LiDAR (light detection and ranging) remote sensing, ground penetrating radar as well as by field observations and luminescence dating. The use of LiDAR in conjunction with geographic information system (GIS) software proved to be efficient in mapping the inactive dune field and classifying the dune morphology, especially when slope raster images were used. The dunes have formed mostly by winds from the northwest (NW) and are of a transverse type. Still other dune types, such as parabolic dunes, and transverse dunes with a deviating orientation are present. Also, there seems to be different generations of dunes, suggesting a complex palaeowind environment with a change from predominantly north‐westerly winds to more westerly winds. Luminescence dating finally allows us to have an absolute chronology of the development of the Bon?sheden dune field, revealing formation of the dune field closely following the de‐glaciation of this part of Sweden ( c. 10.5?ka). The well preserved transverse shape of the majority of the dunes suggests rapid stabilization by vegetation, although sand drift still seems to have been active on a noticeable scale for at least 1500?years and also, occasionally and patchy, as coversand deposition during the Late Holocene. A simple model is proposed for the dune field development of Bon?sheden based on our findings. This model is a useful addition since the majority of present day dune field models focus on the formation of parabolic dunes or large unvegetated dune fields. Our results suggest that most models cannot adequately simulate the formation of such small dune fields as that of Bon?sheden, with apparently rapidly fixated transverse dunes in a previously glaciated, now vegetated area. 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> > bon?sheden,瑞典最大的连续沙丘领域位于瑞典中部达拉纳县,已经使用LIDAR(光检测和测距)遥感,地面穿透雷达以及现场观测和发光约会来调查。利用LIDAR与地理信息系统(GIS)软件的使用证明是有效地映射无效的沙丘场并对DUNE形态进行分类,尤其是在使用斜率光栅图像时。沙丘主要由来自西北(NW)的风而形成,并且具有横向型。还存在仍然存在的其他沙丘类型,例如抛物线沙丘和具有偏离取向的横向沙丘。此外,似乎有不同的沙丘,暗示一个复杂的Palaeowind环境,从主要的北风蜿蜒而来,更改为更西风。发光约会终于让我们对Bon的发展的绝对年表?Sheden Dune领域,揭示了瑞典这部分脱冰(</ i> 10.5? K a)。大多数沙丘的良好保存的横向形状表明植被的快速稳定,虽然砂漂面似乎仍然有效,但是至少1500岁,偶尔也是偶尔和沉积的,因为在全新世时期的涵盖和沉积。提出了一个简单的模型,为Bon的沙丘现场发展基于我们的研究结果。此模型是一种有用的添加,因为当今的大多数Dune Field Models专注于抛物面沙丘或大型未推出的沙丘领域的形成。我们的结果表明,大多数模型不能充分模拟这种小沙滩的形成作为Bon?Sheden,在以前冰川的现在,明显地迅速地固定在现成的植物区。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12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=Bernhardson Martin&option=202" target="_blank" rel="nofollow">Bernhardson Martin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Alexanderson Helena&option=202" target="_blank" rel="nofollow">Alexanderson Helena;</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 GeologyLund UniversityLund Sweden;</p> <p>Department of GeologyLund UniversityLund Sweden;</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=aeolian inland dunes&option=203" rel="nofollow">aeolian inland dunes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=LiDAR remote sensing&option=203" rel="nofollow">LiDAR remote sensing;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=GPR&option=203" rel="nofollow">GPR;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Holocene&option=203" rel="nofollow">Holocene;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sweden&option=203" rel="nofollow">Sweden;</a> </p> <div class="translation"> 机译:Aeolian Inland Dunes;Lidar遥感;GPR;全新世;瑞典; </div> </li> </ul> </div> </div> <div class="literature cardcommon" id="literaturereference" style="display:none"> <div class="similarity "> <h3 class="all_title" id="enpatent111">引文网络</h3> <div class="referencetab clearfix"> <ul id="referencedaohang"> <li dataid="referenceul">参考文献</li> <li dataid="citationul">引证文献</li> <li dataid="commonreferenceul">共引文献</li> <li dataid="commoncitationul">同被引文献</li> <li dataid="tworeferenceul">二级参考文献</li> <li dataid="twocitationul">二级引证文献</li> </ul> </div> <div class="reference_details" id="referenceList"> <ul id="referenceul"></ul> <ul id="citationul"></ul> <ul id="commonreferenceul"></ul> <ul id="commoncitationul"></ul> <ul id="tworeferenceul"></ul> <ul id="twocitationul"></ul> </div> </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/0704023139071.html">Early Holocene dune field development in Dalarna, central Sweden: A geomorphological and geophysical case study</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bernhardson Martin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Bernhardson Martin,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Alexanderson Helena&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Alexanderson Helena </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12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:瑞典中部达拉纳的早期全新世沙田开发:地貌和地球物理案例研究</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_environmental-geology_thesis/0204112140648.html">A geomorphological investigation of the formation and evolution of the Kaiafas sand-dune field (Kyparissiakos Gulf, Ionian Sea,eastern Mediterranean) in the Late Holocene</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=S. 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