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Assessment of the impact of different vegetation patterns on soil erosion processes on semiarid loess slopes

机译:评估不同植被模式对半干旱黄土斜坡土壤侵蚀过程的影响

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Abstract > Soil erosion hinders the recovery and development of ecosystems in semiarid regions. Rainstorms, coupled with the absence of vegetation and improper land management, are important causes of soil erosion in such areas. Greater effort should be made to quantify the initial erosion processes and try to find better solutions for soil and water conservation. In this research, 54 rainfall simulations were performed to assess the impacts of vegetation patterns on soil erosion in a semiarid area of the Loess Plateau, China. Three rainfall intensities (15?mm?h ‐1 , 30?mm?h ‐1 and 60?mm?h ‐1 ) and six vegetation patterns (arbors‐shrubs‐grass ‐A‐S‐G‐, arbors‐grass‐shrubs ‐A‐G‐S‐, shrubs‐arbors‐grass ‐S‐A‐G‐, shrubs‐grass‐arbors ‐S‐G‐A‐, grass‐shrubs‐arbors ‐G‐S‐A‐ and grass‐arbors‐shrubs ‐G‐A‐S‐) were examined at different slope positions (summits, backslopes and footslopes) in the plots (33.3%, 33.3%, 33.3%), respectively. Results showed that the response of soil erosion to rainfall intensity differed under different vegetation patterns. On average, increasing rainfall intensity by 2 to 4 times induced increases of 3.1 to 12.5 times in total runoff and 6.9 to 46.4 times in total sediment yield, respectively. Moreover, if total biomass was held constant across the slope, the patterns of A‐G‐S and A‐S‐G (planting arbor at the summit position) had the highest runoff (18.34?L?m ‐2 ?h ‐1 ) and soil losses (197.98?g?m ‐2 ?h ‐1 ), while S‐A‐G had the lowest runoff (5.51?L?m ‐2 ?h ‐1 ) and soil loss (21.77?g?m ‐2 </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> >土壤侵蚀阻碍了半干旱地区生态系统的恢复和发展。与缺乏植被和土地管理不当的暴雨,都是土壤侵蚀在此类地区的重要原因。应更加努力量化初始侵蚀过程,并试图找到更好的土壤和水资源解决方案。在本研究中,进行了54种降雨模拟,以评估植被模式对中国黄土高原半干旱区土壤侵蚀的影响。三个降雨强度(15?mm?h -1 </ sup>,30?mm≤h -1 </ sup>和60?mm?h -1 </ sup>)六种植被图案(轴灌木 - 草-a-s-g-,arbors-grass-灌木-a-g-s-,灌木 - arbors-grass-a-g-,灌木 - 草齿轮 - -G-A-,草灌木 - 仲裁 - 仲裁齿轮灌木 - 灌木 - 灌木 - S-arbors-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-s-arb-s-s-s-arb-a-s-s-s-s-s-s-s-arch-s-s-s-s-s-s-s-s-s-s-s-s-r)中(33.3分别为%,33.3%,33.3%)。结果表明,在不同植被模式下,土壤侵蚀对降雨强度的反应不同。平均而言,将降雨强度提高2至4次诱导总径流的增加3.1至12.5倍,分别为6.9至46.4倍,总沉积物产量分别为6.9至46.4倍。此外,如果总生物质在斜坡上保持恒定,则A-G-S和A-S-G(在峰会位置的种植轴)的图案具有最高径流(18.34Ω·L≥M -2 < / sup>?h -1 </ sup>)和土壤损失(197.98?g?m -2 </ sup>Δh -1 </ sup>),而s-a -g径流最低(5.51?l?m -2 -2ηh -1 </ sup>)和土壤损失(21.77?g?m -2 </ 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9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=Feng Tianjiao&option=202" target="_blank" rel="nofollow">Feng Tianjiao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wei Wei&option=202" target="_blank" rel="nofollow">Wei Wei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Liding&option=202" target="_blank" rel="nofollow">Chen Liding;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rodrigo‐Comino Jesús&option=202" target="_blank" rel="nofollow">Rodrigo‐Comino Jesús;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Die Chen&option=202" target="_blank" rel="nofollow">Die Chen;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Feng Xinran&option=202" target="_blank" rel="nofollow">Feng Xinran;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ren Kemeng&option=202" target="_blank" rel="nofollow">Ren Kemeng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Brevik Eric C.&option=202" target="_blank" rel="nofollow">Brevik Eric C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yu Yang&option=202" target="_blank" rel="nofollow">Yu Yang;</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>State Key Laboratory of Urban and Regional EcologyResearch Center for Eco‐environmental Sciences Chinese Academy of SciencesBeijing 100085 China;</p> <p>State Key Laboratory of Urban and Regional EcologyResearch Center for Eco‐environmental Sciences Chinese Academy of SciencesBeijing 100085 China;</p> <p>State Key Laboratory of Urban and Regional EcologyResearch Center for Eco‐environmental Sciences Chinese Academy of SciencesBeijing 100085 China;</p> <p>Instituto de Geomorfología y Suelos Department of GeographyUniversity of Málaga Edificio Ada Byron Ampliación del Campus de Teatinos29071 Málaga Spain;</p> <p>State Key Laboratory of Urban and Regional EcologyResearch Center for Eco‐environmental Sciences Chinese Academy of SciencesBeijing 100085 China;</p> <p>State Key Laboratory of Urban and Regional EcologyResearch Center for Eco‐environmental Sciences Chinese Academy of SciencesBeijing 100085 China;</p> <p>State Key Laboratory of Urban and Regional EcologyResearch Center for Eco‐environmental Sciences Chinese Academy of SciencesBeijing 100085 China;</p> <p>Department of Natural Sciences 291 Campus DriveDickinson State UniversityDickinson ND 58601 USA;</p> <p>State Key Laboratory of Urban and Regional EcologyResearch Center for Eco‐environmental Sciences Chinese Academy of SciencesBeijing 100085 China;</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=vegetation pattern&option=203" rel="nofollow">vegetation pattern;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rainfall simulation&option=203" rel="nofollow">rainfall simulation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=runoff&option=203" rel="nofollow">runoff;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=soil erosion&option=203" rel="nofollow">soil erosion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=semi‐arid areas&option=203" rel="nofollow">semi‐arid areas;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Loess Plateau&option=203" rel="nofollow">Loess Plateau;</a> </p> <div class="translation"> 机译:植被模式;降雨模拟;径流;土壤侵蚀;半干旱地区;黄土高原; </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/0704023138901.html">Assessment of the impact of different vegetation patterns on soil erosion processes on semiarid loess slopes</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Feng Tianjiao&option=202" target="_blank" rel="nofollow" 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A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Branson, F. A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shown, L. M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Shown, L. M. </a> <span>1989</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:科罗拉多州丹佛市附近绿山北坡和南坡之间的植被,土壤,微气候和地貌过程的对比</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_agricultural-research-arid-areas_thesis/020121761785.html">不同前茬与施氮量对半干旱黄土高原夏玉米产量和土壤有机碳库的影响</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=孙小花&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 孙小花</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=牛俊义&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,牛俊义</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵刚&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,赵刚</a> <span> <a href="/journal-cn-7286/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 干旱地区农业研究 </a> </span> <span> . 2018</span><span>,第001期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201294178296.html">黄土高原不同植被类型与降水因子对土壤侵蚀的影响研究</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=沈玉芳&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 沈玉芳</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=高明霞&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,高明霞</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=吴永红&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,吴永红</a> <span> <a href="/journal-cn-56915/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 水土保持研究 </a> </span> <span> . 2003</span><span>,第2期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_climatic-environmental-research_thesis/0201254050532.html">不同陆面过程模式对半干旱区通榆站模拟性能的检验与对比</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=孟祥新&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 孟祥新</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=符淙斌&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,符淙斌</a> <span> <a href="/journal-cn-4998/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 气候与环境研究 </a> </span> <span> . 2009</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-sichuan-agricultural-university_thesis/0201270697788.html">半干旱黄土区不同植被类型对土壤水分的影响</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=罗梦娇&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 罗梦娇</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=艾宁&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,艾宁</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘长海&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘长海</a> <span> <a href="/journal-cn-7251/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 四川农业大学学报 </a> </span> <span> . 2019</span><span>,第002期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_science-soil-water-conservation_thesis/0201257379940.html">煤矸石山不同植被恢复模式对土壤侵蚀和养分流失的影响</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王丽艳&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 王丽艳</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张成梁&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,张成梁</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=韩有志&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,韩有志</a> <span> <a href="/journal-cn-6799/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国水土保持科学 </a> </span> <span> . 2011</span><span>,第002期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-15009_thesis/020221297841.html">不同植被恢复模式对黄土丘陵区土壤抗蚀性的影响</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=薛萐&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 薛萐</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李占斌&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李占斌</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李鹏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李鹏</a> <span> <a href="/conference-cn-15009/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 第三届亚洲精细农业会议暨第五届智能化农业信息技术国际学术会议 </a> <span> <span> . 2009</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020316329361.html">半干旱黄土区煤矿复垦区不同植被修复模式对土壤细菌、酶活性影响的研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郭鹏杰&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 郭鹏杰</a> <span> . 2021</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120111950743.html">一种减轻黄土区沟壁土壤侵蚀的植被建设方法</a> <b>[P]</b> . <span> 中国专利: CN111919630A </span> <span> . 2020-11-13</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120112359357.html">一种研究连续径流冲刷作用对不同季节土壤侵蚀特征影响的方法</a> <b>[P]</b> . <span> 中国专利: CN112378802A </span> <span> . 2021-02-19</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130422069551.html">AFFORESTATION SOIL COMPOSITION FOR STABILIZING STEEP SLOPES CAPABLE OF MINIMIZING THE EROSION OF SOILTHROUGH THE COHERENCE OF SOIL IN SLOPES</a> <b>[P]</b> . <span> 外国专利: <!-- 韩国专利: --> KR20120030205A </span> <span> . 2012-03-28</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:通过使坡面土壤的凝聚力最小化能够使土壤侵蚀最小化的稳定陡坡的造林土壤成分 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130462006895.html">VEGETATION METHOD OF FACE OF SLOPE AND SOIL AND SAND INJECTING MAT FOR VEGETATION METHOD OF FACE OF SLOPE</a> <b>[P]</b> . <span> 外国专利: <!-- 日本专利: --> JPH0477088B2 </span> <span> . 1992-12-07</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:边坡土面植被方法及喷沙垫边坡面植被方法 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130467981336.html">VEGETATION METHOD OF FACE OF SLOPE AND SOIL AND SAND INJECTING MAT FOR VEGETATION METHOD OF FACE OF SLOPE</a> <b>[P]</b> . <span> 外国专利: <!-- 日本专利: --> JPH01169018A </span> <span> . 1989-07-04</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:边坡土壤植被的植被方法及喷沙垫 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" 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