Asymmetric hillslope erosion following wildfire in Fourmile Canyon, Colorado

机译：在科罗拉多州四大峡谷的野火后不对称山坡侵蚀

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Abstract > Infrequent, high‐magnitude events cause a disproportionate amount of sediment transport on steep hillslopes, but few quantitative data are available that capture these processes. Here we study the influence of wildfire and hillslope aspect on soil erosion in Fourmile Canyon, Colorado. This region experienced the Fourmile Fire of 2010, strong summer convective storms in 2011 and 2012, and extreme flooding in September 2013. We sampled soils shortly after these events and use fallout radionuclides to trace erosion on polar‐ and equatorial‐facing burned slopes and on a polar‐facing unburned slope. Because these radionuclides are concentrated in the upper decimeter of soil, soil inventories are sensitive to erosion by surface runoff. The polar‐facing burned slope had significantly lower cesium‐137 ( 137 Cs) and lead‐210 ( 210 Pb) inventories ( <fi>p</fi> 0.05) than either the polar‐facing unburned slope or equatorial‐facing burned slope. Local slope magnitude does not appear to control the erosional response to wildfire, as relatively gently sloping (~20%) polar‐facing positions were severely eroded in the most intensively burned area. Field evidence and soil profile analyses indicate up to 4?cm of local soil erosion on the polar‐facing burned slope, but radionuclide mass balance indicates that much of this was trapped nearby. Using a 137 Cs‐based erosion model, we find that the burned polar‐facing slope had a net mean sediment loss of 2?mm (~1?kg?m ?2 ) over a one to three year period, which is one to two orders of magnitude higher than longer‐term erosion rates reported for this region. In this part of the Colorado Front Range, strong hillslope asymmetry controls soil moistu </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> >不常见，高幅度事件导致陡峭的山坡上的沉积物运输量不成比例，但可以获得捕获这些过程的数量数据很少。在这里，我们研究了野火和山坡方面对科罗拉多峡谷峡谷的土壤侵蚀的影响。该地区经历了2010年的四脚火，2011年和2012年的强劲夏季对流风暴，以及2013年9月的极端洪水。我们在这些事件之后不久的是污染，并使用辐射放射性核素来追踪极性和赤道的面向偏离的烧毁倾斜倾向面向偏白的未燃烧的斜坡。因为这些放射性核素浓缩在土壤的上减法中，因此土壤库存对表面径流侵蚀敏感。面向偏光的烧伤斜率显着降低了铯-137（ 137℃）和铅-210（ 210s </ sup> pb）库存（<fi> p </ fi>＆ 0.05）比面向极性的未燃烧的斜面或赤道的烧伤斜面。局部斜率幅度似乎无法控制对野火的侵蚀响应，因为在最强烈地烧毁的区域中，面向偏斜的偏斜（〜20％）的偏振位置被严重侵蚀。现场证据和土壤剖面分析表明，北极地烧伤的斜坡上最多4℃局部土壤侵蚀，但放射性核素质量平衡表明，大部分内容被困在附近。使用基于 137 </ sup> cs的侵蚀模型，我们发现燃烧的偏振斜率净平均沉积物损失为2？mm（〜1？kg？m 2 </ sup >）在一至三年期间，比该地区报告的长期侵蚀率高一到两个数量级。在科罗拉多州的这一部分，强山坡不对称控制土壤潮湿 </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13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=Abrahams Edward R.&option=202" target="_blank" rel="nofollow">Abrahams Edward R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kaste James M.&option=202" target="_blank" rel="nofollow">Kaste James M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ouimet William&option=202" target="_blank" rel="nofollow">Ouimet William;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dethier David P.&option=202" target="_blank" rel="nofollow">Dethier David P.;</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>Department of GeologyThe College of William &</p> <p>MaryWilliamsburg VA USA;</p> <p>Department of GeologyThe College of William &</p> <p>MaryWilliamsburg VA USA;</p> <p>Geography and Center for Integrative GeosciencesUniversity of ConnecticutStorrs CT USA;</p> <p>Department of GeosciencesWilliams CollegeWilliamstown MA 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=soil&option=203" rel="nofollow">soil;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=erosion&option=203" rel="nofollow">erosion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fallout&option=203" rel="nofollow">fallout;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=radionuclides&option=203" rel="nofollow">radionuclides;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=wildfire&option=203" rel="nofollow">wildfire;</a> </p> <div class="translation"> 机译：土壤;侵蚀;辐射;放射性核素;野火; 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