4.7 Article

Fe(II)-catalyzed transformation of Fe (oxyhydr )oxides across organic matter fractions in organically amended soils

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 748, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2020.141125

Keywords

EXAFS; Linear combination fitting; Physical fractionation; Organic amendments

Funding

  1. Spanish State Plan for Scientific and Technical Research and Innovation [AGL201675762-R]
  2. AEI/FEDER
  3. Spanish State Plan for Scientific and Technical Research and Innovation 2013-2016 (AEI/FEDER, UE) [AGL201675762-R]

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The Fe(II)-catalyzed transformation of ferrihydrite into highly crystalline forms may represent an important pathway for soil organic matter (SOM) destabilization under moderately reducing conditions. However, the link between redox-driven changes in soil Fe mineral composition and crystallinity and SOM chemical properties in the field remains elusive. We evaluated abiotic Fe(II)-catalyzed mineralogical transformation of Fe (oxyhydr) oxides in bulk soils and two particle-size SOM fractions, namely the fine silt plus clay (<20 mu m, FSi + Cl) and fine sand (50-200 mu m, FSa) fractions of an agricultural soil unamended or amended with biochar, compost, or the combination of both. After spiking with Fe(II) and incubating for 7 days under anoxic and sterile conditions at neutral pH, the FSa fractions (Fe(II):Fe(III) molar ratios approximate to 3.3) showed more significant ferrihydrite transformations with respect to FSi + Cl fractions (Fe(II):Fe(III) molar ratios approximate to 0.7), with the consequent production of well-ordered Fe oxides in most soils, particularly those unamended or amended with biochar alone. Nonetheless, poorly crystalline ferrihydrite still constituted about 45% of the FSi + a fractions of amended soils after reaction with Fe(II), which confirms that the higher SOM and clay mineral content in this fraction may possibly inhibit atom exchange between aqueous Fe(II) and the solid phase. Building on our knowledge of abiotic Fe(II)-catalyzed mineralogical changes, the suppression of ferrihydrite transformation in FSi + Cl fractions in amended soils could ultimately lead to a slower turnover of ferrihydrite, possibly preserving the carbon sequestration potential associated with this mineral. Conversely, in both bulk soils and FSa fractions, the extent to which mineral transformation occur seemed to be contingent on the quality of the amendment used. (C) 2020 Elsevier B.V. All rights reserved.

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