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Interactions between cations and water molecule bridges in soil organic matter

机译:阳离子与土壤有机质中水分子桥的相互作用

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摘要

Purpose Nutrient release, soil wettability, water binding, and matrix rigidity of soil organic matter (SOM) can be affected by cross-links between segments of SOM, cations, and water molecule bridges (WaMB). Not all cation effects on SOM can be explained with the currently accepted idea that multiva-lent cations cross-link organic matter segments via direct cation bridges (CaB). The objective was to understand these interactions and their effect on SOM matrix rigidity and wettability. Materials and methods We modified cation composition of two peats and an organic surface layer (OSL) using cation exchange resin to remove cations and solutions of Na~+, Ca~(2+), or Al~(3+) to enrich samples with cations. SOM matrix rigidity was determined at 4 and >8 weeks after treatment via the WaMB transition temperature T*, using differential scanning calorimetry. Wettability was measured via sessile drop contact angle (CA). Results and discussion The effect of cation removal on T* depended on cation exchange capacity and initial cation content. Cation addition to OSL increased 7*. This effect increased with increasing cation loading and valency, and T* correlated with CA. Classical cross-linking can neither explain the higher heterogeneous matrix of Ca-treated than Al-treated samples nor the aging-induced convergence of T* for different cations and concentrations. The latter is likely due to interaction between CaB and WaMB in SOM. Conclusions Associations of CaB and WaMB evolve slowly and form a supramolecular network in SOM. Those dynamic associations can fix molecular arrangements inducing water repellency and increase kinetic baRR_1ers for the release and uptake of water and nutrients from aged soil.
机译:目的养分释放,土壤润湿性,水结合力和土壤有机质(SOM)的基质刚度会受到SOM,阳离子和水分子桥(WaMB)片段之间的交联的影响。并非所有阳离子对SOM的影响都可以用目前公认的想法来解释,即多价阳离子通过直接阳离子桥(CaB)交联有机物片段。目的是了解这些相互作用及其对SOM基体刚度和润湿性的影响。材料和方法我们通过使用阳离子交换树脂去除阳离子和Na〜+,Ca〜(2+)或Al〜(3+)的溶液来修饰两个泥炭和一个有机表面层(OSL)的阳离子组成,以富集样品。阳离子。使用差示扫描量热法通过WaMB转变温度T *在处理后4周和> 8周确定SOM基质的刚性。通过无滴液滴接触角(CA)测量润湿性。结果与讨论阳离子去除对T *的影响取决于阳离子交换容量和初始阳离子含量。 OSL中的阳离子增加了7 *。随着阳离子负载量和化合价的增加,该效应增加,并且T *与CA相关。经典的交联既不能解释比铝处理的样品更高的钙处理基质,也不能解释不同阳离子和浓度的T *的老化诱导的收敛。后者可能是由于SOM中CaB和WaMB之间的相互作用。结论CaB和WaMB的协会发展缓慢,并形成SOM中的超分子网络。这些动态关联可以固定诱导疏水的分子排列,并增加动力学baRR_1,以从老化的土壤中释放和吸收水分和养分。

著录项

  • 来源
    《Journal of soil & sediments》 |2013年第9期|1579-1588|共10页
  • 作者单位

    Institute for Environmental Sciences, Department of Environmental and Soil Chemistry, University Koblenz-Landau,Fortstr. 7, 76829 Landau, Germany;

    Institute for Environmental Sciences, Department of Environmental and Soil Chemistry, University Koblenz-Landau,Fortstr. 7, 76829 Landau, Germany;

    Institute for Environmental Sciences, Department of Environmental and Soil Chemistry, University Koblenz-Landau,Fortstr. 7, 76829 Landau, Germany;

    Institute for Environmental Sciences, Department of Environmental and Soil Chemistry, University Koblenz-Landau,Fortstr. 7, 76829 Landau, Germany,Institute of Integrated Natural Sciences, University Koblenz-Landau, Universitatsstr. 1, 56070 Koblenz, Germany;

    Institute for Environmental Sciences, Department of Environmental and Soil Chemistry, University Koblenz-Landau,Fortstr. 7, 76829 Landau, Germany;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Cross-links; Differential scanning calorimetry; Matrix rigidity; Multivalent cation; Soil organic matter; Water molecule bridges (WaMB); Water repellency;

    机译:交叉链接;差示扫描量热法;基质刚度;多价阳离子;土壤有机质;水分子桥(WaMB);防水性;

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