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Testing Os Staining Approach for Visualizing Soil Organic Matter Patterns in Intact Samples via X-ray Dual-Energy Tomography Scanning

机译:测试OS染色方法,用于通过X射线双能断层扫描可视化完整样品中的土壤有机物质图案

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摘要

Challenges with in situ visualization of nonparticulate organics in porous materials limit understanding and modeling processes of transport, decomposition, and storage of organic compounds. In particular, it impedes deciphering the mechanisms driving accumulation and protection of soil organic matter (SOM), processes crucial for sustaining soil fertility and mitigating effects of global climate change. A recently proposed method of staining soil organics by OsO_4 vapors with subsequent dual-energy X-ray computed microtomography scanning (jiCT) offers new opportunities to visualize SOM within intact soil matrix. Our objective was to test the method's performance in staining different organic materials located in media with contrasting pore characteristics: (1) roots of switchgrass (Panicum virgatum L.), either placed within fine and coarse sands or grown within soil microcores, (2) biochar fragments, and (3) soils with relatively low and high C contents. We found that the method was effective in staining organic materials of root origin and the organics associated with fine soil particles, but not the biochar. The estimated percent of total C that reacted with OsO_4 vapors ranged from 0.7% in plant roots to 3.2% in sand-free fraction of the high C soil and was only 0.2% in the studied biochar. Total soil C and Os concentrations were strongly linearly related, suggesting a potential for future method development. However, we would recommend caution when interpreting the results in cases when gas diffusion through the soil matrix is limited.
机译:在多孔材料中原位可视化对多孔材料中的非氨素有机物的挑战限制了有机化合物的运输,分解和储存的理解和建模过程。特别地,它阻碍了驾驶驾驶积聚和保护土壤有机物质(SOM)的机制,对维持土壤肥力和全球气候变化的缓解影响至关重要。最近提出的染料方法通过随后的双能X射线计算的MicrotoMography扫描(JICT)的染料蒸汽染色的土壤有机物提供了新的机会,可在完整的土壤基质中可视化SOM。我们的目的是测试该方法在染色中染色的孔隙特性染色的不同有机材料的性能:(1)切换(Panicum Virgatum L.)的根部,无论是在细小的砂砂中或在土壤微征内种植,(2)生物炭片段,(3)含有相对较低和高C含量的土壤。我们发现该方法有效地染色根源的有机材料和与细土颗粒相关的有机物,但不是生物炭。与OSO_4蒸汽反应的总C的估计百分比范围从植物根部的0.7%范围为3.2%,在高C土壤的无砂级分中的3.2%,并且在研究的生物炭中仅为0.2%。总土壤C和OS浓度强烈线性相关,表明未来方法开发的潜力。但是,我们建议在解释通过土壤基质的气体扩散有限时解释结果时谨慎行事。

著录项

  • 来源
    《Environmental Science & Technology》 |2020年第14期|8980-8989|共10页
  • 作者单位

    Department of Plant Soil and Microbial Sciences Michigan State University East Lansing Michigan 48824 United States Research Institute of Agricultural Resources and Environment Jilin Academy of Agricultural Science Changchun 130033 China;

    Department of Plant Soil and Microbial Sciences Michigan State University East Lansing Michigan 48824 United States;

    Department of Plant Soil and Microbial Sciences Michigan State University East Lansing Michigan 48824 United States;

    Argonne National Lab Center for Advanced Radiation Sources The University of Chicago Chicago Illinois 60637 United States;

    Department of Plant Soil and Microbial Sciences Michigan State University East Lansing Michigan 48824 United States;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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  • 正文语种 eng
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