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Microaggregates in soils

机译:土壤中的微烧结

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摘要

Abstract > All soils harbor microaggregates, i.e ., compound soil structures smaller than 250 μm. These microaggregates are composed of diverse mineral, organic and biotic materials that are bound together during pedogenesis by various physical, chemical and biological processes. Consequently, microaggregates can withstand strong mechanical and physicochemical stresses and survive slaking in water, allowing them to persist in soils for several decades. Together with the physiochemical heterogeneity of their surfaces, the three‐dimensional structure of microaggregates provides a large variety of ecological niches that contribute to the vast biological diversity found in soils. As reported for larger aggregate units, microaggregates are composed of smaller building units that become more complex with increasing size. In this context, organo‐mineral associations can be considered structural units of soil aggregates and as nanoparticulate fractions of the microaggregates themselves. The mineral phases considered to be the most important as microaggregate forming materials are the clay minerals and Fe‐ and Al‐(hydr)oxides. Within microaggregates, minerals are bound together primarily by physicochemical and chemical interactions involving cementing and gluing agents. The former comprise, among others, carbonates and the short‐range ordered phases of Fe, Mn, and Al. The latter comprise organic materials of diverse origin and probably involve macromolecules and macromolecular mixtures. Work on microaggregate structure and development has largely focused on organic matter stability and turnover. However, little is known concerning the role microaggregates play in the fate of elements like Si, Fe, Al, P, and S. More recently, the role of microaggregates in the formation of microhabitats and the biogeography and d </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> >所有土壤港口微烧结, IE </ i>。,化合物土结构小于250μm。这些微烧结由各种物理,化学和生物过程组成的多种矿物质,有机和生物材料。因此,微烧结可以承受强大的机械和物理化学应力并在水中存活,允许它们在土壤中持续数十年。与它们的表面的生理化学异质性一起,微烧结的三维结构提供了各种各样的生态利基,有助于土壤中发现的广大生物多样性。如据报道,对于较大的聚合单位,微烧结由较小的建筑单元组成,随着较大的尺寸变得更加复杂。在这种情况下,有机矿物关联可以被认为是土壤聚集体的结构单元和作为微烧结本身的纳米颗粒部分。被认为是Microggregate的形成材料是最重要的矿物相是粘土矿物和Fe-(氢)氧化物。在微烧结中,矿物质主要通过涉及粘合和胶合剂的物理化学和化学相互作用。前者包括碳酸盐和Fe,Mn和Al的短距离有序相。后者包括不同起源的有机材料,可能涉及大分子和大分子混合物。微磁结构和发展的工作主要集中在有机物稳定性和周转方面。然而,关于在Si,Fe,Al,P和S的元素的命运中,众所周知,最近众所周知的是众所周知的榜样,微烧结在微藻和生物地表和D的形成中的作用 </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1期</span><b style="margin: 0 2px;">|</b><span>共33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=Totsche Kai Uwe&option=202" target="_blank" rel="nofollow">Totsche Kai Uwe;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Amelung Wulf&option=202" target="_blank" rel="nofollow">Amelung Wulf;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gerzabek Martin H.&option=202" target="_blank" rel="nofollow">Gerzabek Martin H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guggenberger Georg&option=202" target="_blank" rel="nofollow">Guggenberger Georg;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Klumpp Erwin&option=202" target="_blank" rel="nofollow">Klumpp Erwin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Knief Claudia&option=202" target="_blank" rel="nofollow">Knief Claudia;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lehndorff Eva&option=202" target="_blank" rel="nofollow">Lehndorff Eva;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mikutta Robert&option=202" target="_blank" rel="nofollow">Mikutta Robert;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Peth Stephan&option=202" target="_blank" rel="nofollow">Peth Stephan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Prechtel Alexander&option=202" target="_blank" rel="nofollow">Prechtel Alexander;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ray Nadja&option=202" target="_blank" rel="nofollow">Ray Nadja;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=K?gel-Knabner Ingrid&option=202" target="_blank" rel="nofollow">K?gel-Knabner Ingrid;</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>Institut für GeowissenschaftenFriedrich-Schiller-Universit?t Jena07749 Jena Germany;</p> <p>Soil Science and Soil EcologyUniversit?t BonnNussallee 13 53115 Bonn Germany;</p> <p>Institute of Soil ResearchUniversity of Natural Resources and Life Sciences ViennaVienna Austria;</p> <p>Institute of Soil ScienceLeibniz Universit?t HannoverHerrenh?user Str. 2 30419 Hannover Germany;</p> <p>Agrosphere (IBG-3)Forschungszentrum Jülich GmbH52425 Jülich Germany;</p> <p>Molecular Biology of the RhizosphereUniversit?t BonnNussallee 13 53115 Bonn Germany;</p> <p>Soil Science and Soil EcologyUniversit?t BonnNussallee 13 53115 Bonn Germany;</p> <p>Bodenkunde und Bodenschutz /Martin-Luther-Universit?t Halle-WittenbergVon-Seckendorff-Platz 3 06120 Halle (Saale) Germany;</p> <p>?kologische Agrarwissenschaften (FB11)Universit?t KasselNordbahnhofstr. 1a 37213 Witzenhausen Germany;</p> <p>Applied Mathematics IFriedrich-Alexander University Erlangen-NürnbergCauerstr. 11 91058 Erlangen Germany;</p> <p>Applied Mathematics IFriedrich-Alexander University Erlangen-NürnbergCauerstr. 11 91058 Erlangen Germany;</p> <p>Chair of Soil ScienceTechnical University of Munich85354 Freising 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=aggregation&option=203" rel="nofollow">aggregation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=habitat&option=203" rel="nofollow">habitat;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=organo‐mineral associations&option=203" rel="nofollow">organo‐mineral associations;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=soil functions&option=203" rel="nofollow">soil functions;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=soil structure&option=203" rel="nofollow">soil structure;</a> </p> <div class="translation"> 机译:聚集;栖息地;有机矿物协会;土壤功能;土壤结构; </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="/academic-journal-foreign_pedosphere_thesis/020413995911.html">Characteristics of organo-mineral complexing of microaggregates in paddy soils developed from purple soils.</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wei ChaoFu&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wei ChaoFu,</a> <a 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