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首页> 外文期刊>Journal of plant nutrition and soil science >Root development of winter wheat in erosion‐affected soils depending on the position in a hummocky ground moraine soil landscape
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Root development of winter wheat in erosion‐affected soils depending on the position in a hummocky ground moraine soil landscape

机译：侵蚀受影响土壤中冬小麦的根系发展取决于雨水泥土园林景观中的位置

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Abstract > Agricultural soil landscapes of hummocky ground moraines are characterized by 3D spatial patterns of soil types that result from profile modifications due to the combined effect of water and tillage erosion. We hypothesize that crops reflect such soil landscape patterns by increased or reduced plant and root growth. Root development may depend on the thickness and vertical sequence of soil horizons as well as on the structural development state of these horizons at different landscape positions. The hypotheses were tested using field data of the root density ( RD ) and the root lengths ( RL ) of winter wheat using the minirhizotron technique. We compared data from plots at the CarboZALF‐D site (NE Germany) that are representing a non‐eroded reference soil profile (Albic Luvisol) at a plateau position, a strongly eroded profile at steep slope (Calcaric Regosol), and a depositional profile at the footslope (Anocolluvic Regosol). At each of these plots, three Plexiglas access tubes were installed down to approx. 1.5 m soil depth. Root measurements were carried out during the growing season of winter wheat (September 2014–August 2015) on six dates. The root length density ( RLD ) and the root biomass density were derived from RD values assuming a mean specific root length of 100 m g ?1 . Values of RD and RLD were highest for the Anocolluvic Regosol and lowest for the Calcaric Regosol. The maximum root penetration depth was lower in the Anocolluvic Regosol because of a relatively high and fluctuating water table at this landscape position. Results revealed positive relations between below‐ground (root) and above‐ground crop parameters ( < </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> >农业土壤Hummocky Link Moraines的景观是由于水和耕作侵蚀的综合修改，由型材改性引起的土壤类型的3D空间模式。我们假设作物通过增加或降低的植物和根生长来反映这种土壤景观模式。根部发展可能取决于土壤视野的厚度和垂直序列以及不同景观位置的这些地平线的结构发展状态。使用MiniRhizotron技术使用根密度（ Rd </ i>）的现场数据和冬小麦的根长度（ rl </ i>）来测试假设。我们将数据与碳氮卓-D站点（NE德国）的绘图进行比较，该数据在高原位置表示非侵蚀的参考土壤曲线（albic luvisol），在陡坡（钙雷科雷科尔）和沉积轮廓下是强烈侵蚀的曲线在鞋子（Anocolluvic regosol）。在这些图中的每一个，三个有机玻璃接入管安装到约。 1.5米的土壤深度。在冬小麦的生长季节（2015年9月至2015年8月）期间进行了根测量。根长密度（ rld </ i>）和根生物量密度衍生自3℃的均比根长度为100mg 1 </ sup>的值。 Rd </ i>和 rld </ i>的值最高用于Anocolluvic regosol，最低用于滑稽素升降液。由于这种景观位置的水位相对高，波动的水位，最大根渗透深度较低。结果揭示了地下（根）和地上作物参数之间的正关系（< </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-35667/'>《Journal of plant nutrition and soil science》</a> <b style="margin: 0 2px;">|</b><span>2018年第2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=Herbrich Marcus&option=202" target="_blank" rel="nofollow">Herbrich Marcus;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gerke Horst H.&option=202" target="_blank" rel="nofollow">Gerke Horst H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sommer Michael&option=202" target="_blank" rel="nofollow">Sommer Michael;</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>Leibniz Centre for Agricultural Landscape Research (ZALF)Institute of Soil Landscape ResearchEberswalder Strasse 84 D–15374 Müncheberg Germany;</p> <p>Leibniz Centre for Agricultural Landscape Research (ZALF)Institute of Soil Landscape ResearchEberswalder Strasse 84 D–15374 Müncheberg Germany;</p> <p>Leibniz Centre for Agricultural Landscape Research (ZALF)Institute of Soil Landscape ResearchEberswalder Strasse 84 D–15374 Müncheberg Germany;</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/212.html" title="农业基础科学">农业基础科学;</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=minirhizotron&option=203" rel="nofollow">minirhizotron;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=root density&option=203" rel="nofollow">root density;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=root lengths density&option=203" rel="nofollow">root lengths density;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=root biomass&option=203" rel="nofollow">root biomass;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=root penetration&option=203" rel="nofollow">root penetration;</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=soil horizonation&option=203" rel="nofollow">soil horizonation;</a> </p> <div class="translation"> 机译：MIRHIZOTRON;根密度;根长度密度;根生物量;根渗透;土壤侵蚀;土壤侵蚀;土壤范围; 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Galina Zvaigzne</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=加林娜·兹瓦伊格涅&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,加林娜·兹瓦伊格涅</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Janin Wendisch&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,Janin Wendisch</a> <span> <a href="/conference-cn-65008/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . ISA-2018第八届国际沙棘协会大会 </a> <span> <span> . -1</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020311888793.html">雨水在城市园林景观中的利用研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=马梦思&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 马梦思</a> <span> . 2017</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/061204487984.html">兼顾提升土壤肥力的肥料在冬小麦免追肥种植中的应用</a> <b>[P]</b> . <span> 中国专利： CN111264115B </span> <span> . 2021.06.25</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120110884826.html">一种冬小麦-夏玉米轮作修复石灰性土壤中铅污染的方法</a> <b>[P]</b> . <span> 中国专利： CN108372193A </span> <span> . 2018-08-07</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130408473721.html">METHOD FOR ARRANGING ANTI-EROSION WATER-SAVING PIPELESS CLOSED DRAINAGE ON CATENA IN MORAINE SOILS</a> <b>[P]</b> . <span> 外国专利： <!-- 俄罗斯专利： --> RU2628354C1 </span> <span> . 2017-08-16</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：在冰TEN土壤中安排抗侵蚀的节水无孔密闭排水方法 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130421781071.html">Soil bulk density improving method for e.g. subsoil sink redevelopment areas, involves directly utilizing ground water near ground sinks or water logging surfaces as working level of carrier unit for soil improvement</a> <b>[P]</b> . <span> 外国专利： <!-- 德国专利： --> DE102010022802A1 </span> <span> . 2011-12-08</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：改良土壤堆积密度的方法地下储水池的重建区域，涉及直接利用地下储水池或注水面附近的地下水作为承载单元的工作水平，以改良土壤 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130429270384.html">Soil conditioner, where a sieved out lignite, wood fibers, rock flour, limestone flour, wheat straw, chaffed maize straw, crushed leaves and feed slices are used, useful e.g. for the recultivation of biologically- and erosion-damaged soil</a> <b>[P]</b> . <span> 外国专利： <!-- 德国专利： --> DE102007047533A1 </span> <span> . 2009-04-09</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：土壤改良剂可用于例如筛分的褐煤，木纤维，岩粉，石灰石粉，小麦秸秆，玉米秸秆碎屑，碎叶和饲料切片等。用于修复受生物和侵蚀破坏的土壤 </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 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