Impact of rainfall pattern on interrill erosion process

机译：降雨模式对近代侵蚀过程的影响

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Abstract > The impact of rainfall pattern on the interrill erosion process is not fully understood despite its importance. Systematic rainfall simulation experiments involving various rainfall intensities, stages, intensity sequences, and surface cover conditions were conducted in this study to investigate their effects on the interrill erosion process. Five rainfall patterns designed with the same total kinetic energy/precipitation (increasing, decreasing, rising–falling, falling–rising and constant patterns) were randomly delivered to a pre‐wet clay loam soil surface at a 10° slope gradient. Significant differences in soil losses were observed among the different rainfall patterns and stages, but there was no obvious difference in runoff. Kinetic energy flux (KE <sub>r</sub> ) was a governing factor for interrill erosion, and constant rainfall pattern (CST) produced nine times greater soil loss than runs with no KE <sub>r</sub> . Varied‐intensity patterns had a profound effect on raindrop‐induced sediment transport processes; path analysis results indicated that said effect was complex, interactive and intensity‐dependent. Low hydraulic parameter thresholds further indicated that KE <sub>r</sub> was the dominant factor in detaching soil particles, while overland flow mainly contributed to transporting the pre‐detached particles. This study not only sheds light on the mechanism of interrill sediment transport capacity and detachability, but also may provide a useful database for developing event‐based interrill erosion prediction models. 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> >降雨模式对interi侵蚀的影响尽管重要的是，过程尚未完全明白。在本研究中进行了涉及各种降雨强度，阶段，强度序列和表面覆盖条件的系统降雨模拟实验，以研究它们对易于侵蚀过程的影响。在10°斜率梯度下随机将设计具有相同总动能/沉淀（增加，降低，上升，下降，上升和恒定图案的增加，降低，下降，上升，恒定图案）的降雨量图案。不同的降雨模式和阶段观察到土壤损失的显着差异，但径流没有明显的差异。动能通量（Ke <sub> R </ sub>）是侵蚀侵蚀的控制因素，并且恒定的降雨量（CST）产生的土壤损失九次，而不是NO <SUB> R </ SUB的运行。不同强度模式对雨滴引起的沉积物运输过程产生了深远的影响;路径分析结果表明，所述效果复杂，互动和强度依赖性。低液压参数阈值进一步表明，Ke <sub> R </ sub>是分离土壤颗粒的主要因素，而陆上流动主要有助于运输预拆颗粒。这项研究不仅阐明了缩小的沉积物传输能力和可拆卸能力的机制，而且还可以提供用于开发基于事件的中的侵蚀预测模型的有用数据库。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14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=Wang Bin&option=202" target="_blank" rel="nofollow">Wang Bin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Steiner Jean&option=202" target="_blank" rel="nofollow">Steiner Jean;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zheng Fenli&option=202" target="_blank" rel="nofollow">Zheng Fenli;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gowda Prasanna&option=202" target="_blank" rel="nofollow">Gowda Prasanna;</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 Soil and Water ConservationBeijing Forestry UniversityBeijing P. R. China;</p> <p>USDA‐ARS Grazinglands Research LaboratoryEl Reno OK USA;</p> <p>State Key Laboratory of Soil Erosion and Dryland Farming on the Loess PlateauNorthwest A&</p> <p>F UniversityYangling P. R. China;</p> <p>USDA‐ARS Grazinglands Research LaboratoryEl Reno OK USA;</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=kinetic energy&option=203" rel="nofollow">kinetic energy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=soil erodibility&option=203" rel="nofollow">soil erodibility;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=water erosion mechanism&option=203" rel="nofollow">water erosion mechanism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hydraulic characteristics&option=203" rel="nofollow">hydraulic characteristics;</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> </p> <div class="translation"> 机译：动能;土腐蚀;水蚀机制;液压特性;土壤侵蚀; </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/0704023139078.html">Impact of rainfall pattern on interrill erosion process</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Bin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wang Bin,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Steiner Jean&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Steiner Jean,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zheng Fenli&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zheng Fenli,</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：降雨模式对近代侵蚀过程的影响</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023139269.html">Effects of rainfall, overland flow and their interactions on peatland interrill erosion processes</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Changjia&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Li Changjia,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Holden Joseph&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Holden Joseph,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Grayson Richard&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Grayson Richard </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>2018</span><span>,第7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：降雨，陆地流动及其对泥炭地内腐蚀过程的影响</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023257824.html">Impact of near-surface hydraulic gradient on the interrill erosion process</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> </a> <a href="/journal-foreign-22947/" target="_blank" rel="nofollow" class="tuijian_authcolor">European Journal of Soil Science .</a> <span>2020</span><span>,第4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：近表面液压梯度对近钻侵蚀过程的影响</span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-conference-foreign_meeting-256419_thesis/0705012801598.html">Improving Erosion Modeling on Forest Roads in the Lake Tahoe Basin: Small Plot Rainfall Simulations to Determine Saturated Hydraulic Conductivity and Interrill Erodibility</a> <b>[C]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=N.S. 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