Geomorphic influences on the distribution and accumulation of pyrogenic carbon (PyC) following a low severity wildfire in northern New Mexico

机译：新墨西哥州北部低严重程度野火后热原碳（PYC）分布及积累的几何影响

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Abstract >The distribution, transport, and accumulation of wildfire‐generated pyrogenic carbon (PyC) has important consequences for contaminant transport and carbon cycling, but a conceptual model for PyC accumulation and loss that includes geomorphic processes is lacking. In this study we quantified PyC concentration in soil samples collected from the Jemez Mountains of New Mexico before and after the 2013 Thompson Ridge (TR) fire, and developed a conceptual model describing PyC redistribution. Pre‐fire samples were fortuitously collected 4?years before the TR burn and post‐fire samples were collected at the same locations 15?months following the TR fire. Samples were collected from the O and A horizon, with sites representing a range of slope angle, aspect, burn severity, and geomorphic setting. PyC was determined by a modified chemo‐thermal oxidation method to compare PyC to total organic carbon (TOC). The mean PyC/TOC ratio was significantly higher post‐fire than pre‐fire (0.14 vs 0.12), indicating increased PyC sequestration. O horizon PyC concentrations were more variable and more responsive to fire than the A horizon. Soil horizon, watershed, and geomorphic setting proved to be the most influential factors in predicting PyC concentration changes. PyC concentrations increased most on hillslopes and in low‐severity burn areas, suggesting higher rates of PyC production or post‐fire accumulation. Burn patchiness appears to facilitate PyC accumulation, with lower severity patches trapping PyC mobilized from high severity patches. While PyC content had greater point scale variance following the fire, the fire also homogenized pre‐fire PyC differences between soil horizons and among watersheds within the burn perimeter, differences that appear to develop over time between fires. The O horizon is a larger sink for PyC in the short ter </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> >分发，野火引发的热原碳（PYC）的运输和积累对污染物运输和碳循环具有重要影响，但缺乏包括地貌过程的PYC积累和损失的概念模型。在这项研究中，我们在2013年汤普森山脊（TR）火灾（TR）火灾之前和之后，从Jemez山脉收集的土壤样本中量化了Pyc浓度，并开发了描述Pyc再分配的概念模型。火前样品偶然收集4？在TR燃烧后的TR燃烧和火灾后样品在TR火灾后15个月收集。从o和地平线收集样品，具有代表一系列倾斜角度，方面，烧伤严重程度和地貌设置的位置。通过改性的化学热氧化方法测定PYC，以将PYC与总有机碳（TOC）进行比较。火后的平均PYC / TOC比率显着高于火火后（0.14 Vs 0.12），表明毕为PYC封存增加。 o Horizo n Pyc浓度比地平线更可变，更响应于火。土壤地平线，流域和地貌设置被证明是预测PYC浓度变化的最有影响力的因素。 Pyc浓度大部分山坡和低严重程度燃烧区域增加，表明Pyc生产或火灾后积累的速度提高。烧坏斑块似乎有助于Pyc累积，捕获从高严重性斑块调动的较低严重性的补丁。虽然PYC含量在火灾后具有更大的点比例方差，但火灾也均质化土壤视野和烧伤周长内的流域之间的火灾预热差异，似乎在火灾之间随着时间的推移而产生的差异。 O Horizo n是短TER中PYC的较大水槽 </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10期</span><b style="margin: 0 2px;">|</b><span>共12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=Galanter Amy&option=202" target="_blank" rel="nofollow">Galanter Amy;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cadol Daniel&option=202" target="_blank" rel="nofollow">Cadol Daniel;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lohse Kathleen&option=202" target="_blank" rel="nofollow">Lohse Kathleen;</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 Earth &</p> <p>Environmental SciencesNew Mexico Institute of Mining &</p> <p>TechnologySocorro New Mexico USA;</p> <p>Department of Earth &</p> <p>Environmental SciencesNew Mexico Institute of Mining &</p> <p>TechnologySocorro New Mexico USA;</p> <p>Department of Biological Sciences;</p> <p>Department of GeosciencesIdaho State UniversityPocatello ID 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=pyrogenic carbon (PyC)&option=203" rel="nofollow">pyrogenic carbon (PyC);</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> <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> </p> <div class="translation"> 机译：热原碳（PYC）;野火;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> 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