Effects of different spatial distributions of physical soil crusts on runoff and erosion on the Loess Plateau in China

机译：物理土壳不同空间分布对中国黄土高原径流和侵蚀的影响

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Abstract > The response of runoff and erosion to soil crusts has been extensively investigated in recent decades. However, there have been few attempts to look at the effects of spatial configuration of different soil crusts on erosion processes. Here we investigated the effects of different spatial distributions of physical soil crusts on runoff and erosion in the semi‐arid Loess Plateau region. Soil boxes (1.5?m long × 0.2?m wide) were set to a slope of 17.6% (10°) and simulated rainfall of 120?mm h ?1 (60?minutes). The runoff generation and erosion rates were determined for three crust area ratios (depositional crust for 20%, 33%, and 50% of the total slope) and five spatial distribution patterns (depositional crust on the lower, lower‐middle, middle, mid‐upper, and upper slope) of soil crusts. The reduction in sediment loss (‘sediment reduction’) was calculated to evaluate the effects of different spatial distributions of soil crusts on erosion. Sediment yield was influenced by the area ratio and spatial position of different soil crusts. The runoff rate reached a steady state after an initial trend of unsteadily increasing with increasing rainfall duration. Sediment yield was controlled by detachment limitation and then transport limitation under rainfall. The shifting time of erosion from a transport to detachment‐limiting regime decreased with increasing area of depositional crust. No significant differences were observed in the total runoff among treatments, while the total sediment yield varied under different spatial distributions. At the same area ratio, total sediment yield was the largest when the depositional crust was on the upper slope, and it was smallest when the crust was deposited on the lower slope. The sediment reduction of structural crust (42.5–66.5%) was greater than that of depositional crust (16.7–34.3%). These results provide a mechanistic understanding of how different spatial distributions of soil crusts affect runoff and sediment production. 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> >径流和侵蚀到土壳的响应近几十年已被广泛调查。然而，很少有尝试查看不同土壳的空间配置对侵蚀过程的影响。在这里，我们研究了物理土壳不同空间分布对半干旱黄土高原地区径流和侵蚀的影响。土壤箱（1.5？M长×0.2？M宽）设定为17.6％（10°）的斜率，并模拟120？mm H （60Ω分钟）的降雨降雨量。确定三个地壳面积比（沉积地壳为20％，33％和总坡度的50％）和五个空间分布图案（下部，中间，中间，中间，中间的沉积地壳）土壤壳体和上坡度）。计算沉积物损失的降低（“沉积物还原”），以评价土壤结壳对侵蚀不同空间分布的影响。沉积物产量受到不同土壳的面积比和空间位置的影响。随着降雨持续时间不安地增加的初步趋势后，径流率达到了稳定状态。沉积物产量由脱离限制控制，然后降雨下的运输限制。随着沉积地壳的增加，从运输到分离限制的运输到分离限制的变速时间降低。在治疗中的总径流中没有观察到显着差异，而在不同的空间分布下的总沉积物产量变化。在相同的面积比下，当沉积地壳在上坡上时，总沉积物产量最大，并且当外壳沉积在下斜率上时，它最小。结构外壳的沉积物（42.5-66.5％）大于沉积地壳（16.7-34.3％）。这些结果提供了对土壤地壳的不同空间分布影响径流和沉积物产生的机械理解。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13期</span><b style="margin: 0 2px;">|</b><span>共8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=Lu Pei&option=202" target="_blank" rel="nofollow">Lu Pei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xie Xinli&option=202" target="_blank" rel="nofollow">Xie Xinli;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Linhua&option=202" target="_blank" rel="nofollow">Wang Linhua;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wu Faqi&option=202" target="_blank" rel="nofollow">Wu Faqi;</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>Institution of Soil and Water ConservationNorthwest A&</p> <p>F UniversityYangling Shaanxi P. R. China;</p> <p>Institution of Soil and Water ConservationNorthwest A&</p> <p>F UniversityYangling Shaanxi P. R. China;</p> <p>Institution of Soil and Water ConservationNorthwest A&</p> <p>F UniversityYangling Shaanxi P. R. China;</p> <p>College of Resources and EnvironmentNorthwest A&</p> <p>F UniversityYangling Shaanxi P. R. 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=depositional crust&option=203" rel="nofollow">depositional crust;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=structural crust&option=203" rel="nofollow">structural crust;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=spatial distribution&option=203" rel="nofollow">spatial distribution;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=runoff rate&option=203" rel="nofollow">runoff rate;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sediment yield&option=203" rel="nofollow">sediment yield;</a> </p> <div class="translation"> 机译：沉积地壳;结构外壳;空间分布;径流率;沉积物产量; </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/0704023139104.html">Effects of different spatial distributions of physical soil crusts on runoff and erosion on the Loess Plateau in China</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lu Pei&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Lu Pei,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xie Xinli&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Xie Xinli,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Linhua&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wang Linhua,</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13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：物理土壳不同空间分布对中国黄土高原径流和侵蚀的影响</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/070402157658.html">Effects of soil crust and crop on runoff and erosion in Loess Plateau</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ma Bo&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ma Bo,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ma Fan&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ma Fan,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Zhanbin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Li Zhanbin,</a> <a href="/journal-foreign-17637/" target="_blank" rel="nofollow" class="tuijian_authcolor">Acta Agriculturae Scandinavica. 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