4.5 Article

Permafrost soil complexity evaluated by laboratory imaging Vis-NIR spectroscopy

Journal

EUROPEAN JOURNAL OF SOIL SCIENCE
Volume 72, Issue 1, Pages 114-119

Publisher

WILEY
DOI: 10.1111/ejss.12927

Keywords

Alaska; HySpex; mineral associated organic matter; occluded particulate organic matter; particulate organic matter; pedogenic iron oxides; supervised image classification

Categories

Funding

  1. Deutsche Forschungsgemeinschaft [MU 3021/2-1, MU 3021/8-1]
  2. Deutsches Zentrum fur Luftund Raumfahrt [50 EE 1530]
  3. National Science Foundation [0852036]
  4. Directorate For Geosciences
  5. Division Of Polar Programs [0852036] Funding Source: National Science Foundation

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This study introduces a new method using Vis-NIR spectroscopy and resin-embedded soil core sections to determine microscale soil structure arrangement through image classification, including quantification of soil organic matter fractions. This approach helps to scale up from microscale spectromicroscopic techniques to the centimeter and possibly pedon scale.
The biogeochemical functioning of soils (e.g., soil carbon stabilization and nutrient cycling) is determined at the interfaces of specific soil structures (e.g., aggregates, particulate organic matter (POM) and organo-mineral associations). With the growing accessibility of spectromicroscopic techniques, there is an increase in nano- to microscale analyses of biogeochemical interfaces at the process scale, reaching from the distribution of elements and isotopes to the localization of microorganisms. A widely used approach to study intact soil structures is the fixation and embedding of intact soil samples in resin and the subsequent analyses of soil cross-sections using spectromicroscopic techniques. However, it is still challenging to link such microscale approaches to larger scales at which normally bulk soil analyses are conducted. Here we report on the use of laboratory imaging Vis-NIR spectroscopy on resin embedded soil sections and a procedure for supervised image classification to determine the microscale soil structure arrangement, including the quantification of soil organic matter fractions. This approach will help to upscale from microscale spectromicroscopic techniques to the centimetre and possibly pedon scale. Thus, we demonstrate a new approach to integrate microscale soil analyses into pedon-scale conceptual and experimental approaches. Highlights Quantification of soil constituents using Vis-NIR spectroscopy. New approach to use resin embedded soil core sections with intact structure. Reproducible quantification of soil constituents important for soil carbon storage. Vis-NIR as promising tool for upscaling from microscale to pdeon scale.

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