Assessment of long‐term Holocene soil erosion rates in Polish loess areas using sedimentary archives from closed depressions

Ko?odyńska‐Gawrysiak Renata; Poesen Jean; Gawrysiak Leszek

摘要

Abstract >Soil erosion is a particularly important problem in the loess areas of Central Europe. Numerous studies of past and present soil erosion based on colluvial sediments have so far been conducted. The main problem is the fact that colluvia usually do not represent the complete sedimentation record. Closed depressions (CDs) collect all colluvial sediments from their catchment, therefore, constitute sediment stores enabling the calculation of soil erosion rates. > Colluvial sediments and fossil soils, infilling four CDs in the Polish loess belt, were OSL and C‐14 dated. Human settlements near the studied CDs were analyzed. Phases of soil erosion and colluviation from the Neolithic (5400–2900? <sc>bc</sc> ), from the Middle Bronze Age to the Early Iron Age (1600–0? <sc>bc</sc> ), and from the Early Middle Ages to Modern Times (500?AD until today) were documented within the CDs studied. Phases of low soil erosion rate and pedogenesis occurred from the Late Vistulian to the Early Neolithic and from the Iron Age to Early Middle Ages. This study reveals that these phases are not synchronous with the soil erosion phases in Central Europe, as the latter mainly occurred in the Bronze Age, Roman Period and Middle Ages. The obtained soil erosion rates were compared with erosion rates in different areas of Central Europe. This study indicates that in loess regions with long‐term agricultural land use, mean erosion rates (i.e. 3.7–5.9?t ha ‐1 ?yr ‐1 ) from the Middle Ages to Modern Times were ten times higher than during the entire prehistoric period (0.39–0.67?t ha ‐1 ?yr ‐1 ). The mean soil erosion rates for forested CDs was 0.24–0.74?t ha ‐1 </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> >土壤侵蚀是中欧黄土地区是一个特别重要的问题。迄今为止，迄今为止，迄今为止基于血管沉积物的过去和目前土壤侵蚀的众多研究。主要问题是Colluvia通常不代表完整的沉降记录。闭合凹陷（CDS）从其集水区收集所有抗癌沉积物，因此构成沉积物储存，从而能够计算土壤侵蚀率。</ p> >在波兰黄土腰带中in in in in in in 4 cds indill沉积物和化石土壤是osl和C-14约会。分析了研究附近的人类沉淀。来自新石器时代（5400-2900？<sc> Bc </ sc>）的土壤腐蚀和脱离的阶段，从中间青铜年龄到早期铁的年龄（1600-0？<sc> bc </ sc>），从中世纪早期到现代（500岁？截至今天）在学习的CD中记录。降低土壤侵蚀率和基础的阶段发生从晚期到新石器时代的早期，从铁时期到中世纪早期。本研究表明，这些阶段与中欧的土壤侵蚀阶段不同步，因为后者主要发生在青铜时代，罗马时期和中世纪。将获得的土壤侵蚀率与中欧不同地区的侵蚀率进行了比较。本研究表明，在长期农业用地使用的黄土地区，平均侵蚀速率（即3.7-5.9？t ha -1 </ sup>Δyr -1 </ sup>）近代的年龄比整个史前时期高十倍（0.39-0.67？t ha -1 </ sup>Δyr -1 </ sup>）。用于森林CD的平均土壤侵蚀率为0.24-0.74？t ha -1 </ sup> </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5期</span><b style="margin: 0 2px;">|</b><span>共23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=Ko?odyńska‐Gawrysiak Renata&option=202" target="_blank" rel="nofollow">Ko?odyńska‐Gawrysiak Renata;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Poesen Jean&option=202" target="_blank" rel="nofollow">Poesen Jean;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gawrysiak Leszek&option=202" target="_blank" rel="nofollow">Gawrysiak Leszek;</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>Faculty of Earth Science and Spatial ManagementMaria Curie‐Sk?odowska UniversityAl. Kra?nicka 2 CD 20‐718 Lublin Poland;</p> <p>Department of Earth and Environmental SciencesKU Leuven Celestijnenlaan 200EB‐3001 Leuven Heverlee Belgium;</p> <p>Faculty of Earth Science and Spatial ManagementMaria Curie‐Sk?odowska UniversityAl. Kra?nicka 2 CD 20‐718 Lublin Poland;</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=Poland&option=203" rel="nofollow">Poland;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=water erosion&option=203" rel="nofollow">water erosion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=colluvium&option=203" rel="nofollow">colluvium;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=land use&option=203" rel="nofollow">land use;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=OSL and C14 dating&option=203" rel="nofollow">OSL and C14 dating;</a> </p> <div class="translation"> 机译：波兰;水侵蚀;凝血;土地使用;OSL和C14约会; </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/0704023139254.html">Assessment of long‐term Holocene soil erosion rates in Polish loess areas using sedimentary archives from closed depressions</a> <b>[J]</b> . 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href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张岩&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,张岩</a> <span> <a href="/conference-cn-13309/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国水利水电科学研究院第十届青年学术交流会 </a> <span> <span> . 2010</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020314034481.html">近1万年以来特征时期黄土高原土壤侵蚀及其对黄河下游沉积的影响</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵宏飞&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 赵宏飞</a> <span> . 2018</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120110851679.html">一种模拟黄土地区土壤侵蚀特性的实验装置与方法</a> <b>[P]</b> . <span> 中国专利： CN108362858A </span> <span> . 2018-08-03</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" 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