4.5 Article

A solid phase extraction method for isolating HF-extractable soil organic matter for NMR analysis

Journal

ORGANIC GEOCHEMISTRY
Volume 111, Issue -, Pages 1-8

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.orggeochem.2017.04.012

Keywords

Solid phase extraction (SPE); Soil organic carbon (SOC); Nuclear magnetic resonance spectroscopy (NMR)

Funding

  1. Natural Sciences and Engineering Research Council of Canada [341863]
  2. Canada Research Chairs Programme
  3. Forestry and Agrifoods Agency's Centre for Forestry Science and Innovation, Government of Newfoundland and Labrador

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Cross polarization magic angle spinning C-13 nuclear magnetic resonance (CP-MAS C-13-NMR) analysis of soil is an important technique for understanding soil organic carbon (SOC) source, cycling and fate. The low carbon concentration in, and paramagnetic interference from, most mineral soils require that they be extracted and demineralized using HF, generating a residue that is analyzed via CP-MAS C-13-NMR. However, the HF extractable fraction typically represents a significant fraction of the total SOC that cannot be analyzed directly. We describe a method developed for the solid-phase extraction (SPE) of the HF-extractable fraction of SOC from the HF demineralization of mineral soils. Podzolic mineral soils were demineralized with 10% HF, with > 50% of total SOC retained with the existing mineral matrix in the HF-extractable fraction. SPE was utilized to recover and concentrate the HF-extractable SOC as a mineral free extract. Using the approach, 61-73% of the HF extractable SOC was recovered, resulting in a recovery of 73-82% of the total soil SOC. A marked improvement over the 35-51% recovered solely in the HF-insoluble fraction, the soil fraction typically analyzed using CP-MAS C-13-NMR. The increased carbon content and removal of paramagnetic minerals via SPE greatly improved the CP-MAS C-13-NMR signal to noise relative to the HF-insoluble SOC fraction. The composition of the SPE recovered, HF-soluble fraction was rich in aromatic and carboxylic C, in addition to specific alkyl and O-alkyl C types, relative to the HF-insoluble fraction. The method should enable insight into an often significant but poorly studied mineral SOC fraction and, through the decreased matrix effect, should improve comparability among different soil and dissolved organic matter (DOM) samples. (C) 2017 Elsevier Ltd. All rights reserved.

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