Holocene fluvial valley fill sources of atmospheric mineral dust in the Skeleton Coast, Namibia

机译：全新世河流谷填补骨骼海岸大气矿物尘埃的来源，纳米比亚

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Abstract >Western Namibia is a significant global source of atmospheric mineral dust. We investigate the relationship between dust and source sediments, assessing the sustainability of dust flux. Remote sensing studies have highlighted specific ephemeral fluvial systems as important contributors to dust flux, including highlighting sections of valleys that are the origins of dust plumes in the period 2005–2008. Little is known however about the specific within‐valley dust sediment sources, particularly whether dust is derived from modern ephemeral channel floors or older valley fill sediments, many of which have been reported in the region. As part of a region‐wide analysis of aeolian dust flux, we investigate the sediment properties of atmospheric dust samples and valley sediments from the Huab valley, one of the principal regional dust sources. Trapped dust samples contain up to 88% very fine sand and silt when collected samples are disaggregated prior to analysis. Valley fill surface samples comprise 80% very fine sand and silt, and the surface of the modern ephemeral channel 30%. Valley fill sediments were sampled at depths up to 3.6?m below the present surface and reveal Holocene depositional ages from 0.6?±?0.03?ka back to 9.79?±?0.73?ka. These sediments contain 30% to 6% very fine sand and silt, with levels decreasing with depth and age. Aeolian bedforms in the valley system (nebkhas on the fill surface and climbing dunes on valley margins) indicate that aeolian processes under the influence of strong seasonal easterly winds likely result in dust being winnowed out of the valley fill surfaces, with sandy bedforms being constructed from the coarser component of the fill sediments. The volume of valley fill sediment suggests dust sourced from Holocene sediments is likely to continue into the future regardless of flow conditions in the modern channel 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> >西纳米比亚是一个重要的全球大气来源矿物粉尘。我们调查粉尘和源沉积物之间的关系，评估灰尘通量的可持续性。遥感研究突出了特定的短暂血液系统作为灰尘助焊剂的重要贡献者，包括突出谷的部分，这些部分是2005 - 2008年期间的灰尘羽毛的起源。然而，对于谷谷内尘沉积物来源，特别是灰尘是少量的，特别是灰尘是从现代短暂的渠道地板或较旧的谷填充沉积物中衍生出来，其中许多已经在该地区报道。作为海湾尘埃通量的区域广泛分析的一部分，我们研究了Huab Valley的大气粉尘样品和谷沉积物的沉积物，其中一个主要区域尘埃源。被困的粉尘样品含有高达88％的非常细小的砂和淤泥，在分析之前分解在分析之前。谷填充表面样品包括80％非常细小的沙子和淤泥，以及现代短暂通道的表面30％。谷填充沉积物在当前表面下方的深度上进行采样，并揭示从0.6？±0.03的全茂沉积年龄0.03？ka回到9.79？±0.73？ka。这些沉积物含有30％至6％的非常细小的沙子和淤泥，水平随深度和年龄而降低。在谷系统中的Aeolian玻璃形式（填充表面上的Nebkhas和山谷边缘上升的沙丘）表明，在强大的季节性东风的影响下的风速过程可能导致谷填充表面的灰尘，砂质叶形是由填充沉积物的较粗糙分量。无论现代渠道系统中的流动条件如何，谷填充沉积物的体积都表明来自全新世沉积物的灰尘可能会继续下将未来。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11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=Thomas David S.G.&option=202" target="_blank" rel="nofollow">Thomas David S.G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Durcan Julie A.&option=202" target="_blank" rel="nofollow">Durcan Julie A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dansie Andrew&option=202" target="_blank" rel="nofollow">Dansie Andrew;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wiggs Giles F.S.&option=202" target="_blank" rel="nofollow">Wiggs Giles F.S.;</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>School of Geography and the EnvironmentUniversity of OxfordOxford OX1 3QY UK;</p> <p>School of Geography and the EnvironmentUniversity of OxfordOxford OX1 3QY UK;</p> <p>School of Geography and the EnvironmentUniversity of OxfordOxford OX1 3QY UK;</p> <p>School of Geography and the EnvironmentUniversity of OxfordOxford OX1 3QY UK;</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=mineral dust&option=203" rel="nofollow">mineral dust;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=valley fill&option=203" rel="nofollow">valley fill;</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=Aeolian&option=203" rel="nofollow">Aeolian;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Namibia&option=203" rel="nofollow">Namibia;</a> </p> <div class="translation"> 机译：矿物粉尘;山谷填充;全新世;纳米利亚语;纳米比亚; </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/0704023139074.html">Holocene fluvial valley fill sources of atmospheric mineral dust in the Skeleton Coast, Namibia</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Thomas David S.G.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Thomas David S.G.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Durcan Julie A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Durcan Julie A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dansie Andrew&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Dansie Andrew,</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：全新世河流谷填补骨骼海岸大气矿物尘埃的来源，纳米比亚</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704015586754.html">A ground-penetrating radar survey of late Holocene fluvial sediments in NW Namibian river valleys: characterization and comparison</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Leopold M&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Leopold M,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Volkel J&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Volkel J,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Heine K&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Heine K </a> <a href="/journal-foreign-36018/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of the Geological Society .</a> <span>2006</span><span>,第6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：纳米比亚西北河谷晚全新世河流沉积物的探地雷达调查：特征与比较</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_palaios_thesis/020413072425.html">Changing Fluvial Environments and Vertebrate Taphonomy in Response to Climatic Drying in a Mid-Triassic Rift Valley Fill: The Omingonde Formation (Karoo Supergroup) of Central Namibia</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ROGER M.H. 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