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Title: Association with pedogenic iron and aluminum: effects on soil organic carbon storage and stability in four temperate forest soils

Journal Article · · Biogeochemistry
 [1];  [1];  [2];  [3];  [1]
  1. Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States). Climate and Ecosystem Sciences Division
  2. Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States). Center for Accelerator Mass Spectroscopy
  3. Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). Climate Change SCience Inst. and Environmental Sciences Division

Soil organic carbon (SOC) can be stabilized via association with iron (Fe) and aluminum (Al) minerals. Fe and Al can be strong predictors of SOC storage and turnover in soils with relatively high extractable metals content and moderately acidic to circumneutral pH. Here we test whether pedogenic Fe and Al influence SOC content and turnover in soils with low Fe and Al content and acidic pH. In soils from four sites spanning three soil orders, we quantified the amount of Fe and Al in operationally-defined poorly crystalline and organically-complexed phases using selective chemical dissolution applied to the soil fraction containing mineral-associated carbon. We evaluated the correlations of Fe and Al concentrations, mean annual precipitation (MAP), mean annual temperature (MAT), and pH with SOC content and14C-based turnover times. We found that poorly crystalline Fe and Al content predicted SOC turnover times (p < 0.0001) consistent with findings of previous studies, while organically-complexed Fe and Al content was a better predictor of SOC concentration (p < 0.0001). Greater site-level MAP (p < 0.0001) and colder site-level MAT (p < 0.0001) were correlated with longer SOC turnover times but were not correlated with SOC content. Our results suggest that poorly crystalline Fe and Al effectively slow the turnover of SOC in these acidic soils, even when their combined content in the soil is less than 2% by mass. However, in the strongly acidic Spodosol, organo-metal complexes tended to be less stable resulting in a more actively cycling mineral-associated SOC pool.

Research Organization:
Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States); Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States); Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
Sponsoring Organization:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
Grant/Contract Number:
AC52-07NA27344; AC05-00OR22725; AC02-05CH11231
OSTI ID:
1366910
Alternate ID(s):
OSTI ID: 1400180; OSTI ID: 1471031
Report Number(s):
LLNL-JRNL-708394
Journal Information:
Biogeochemistry, Vol. 133, Issue 3; ISSN 0168-2563
Publisher:
SpringerCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 47 works
Citation information provided by
Web of Science

References (39)

Deep soil carbon dynamics are driven more by soil type than by climate: a worldwide meta-analysis of radiocarbon profiles journal October 2015
AN EVALUATION OF 0.1  M PYROPHOSPHATE AND PYROPHOSPHATE-DITHIONITE IN COMPARISON WITH OXALATE AS EXTRACTANTS OF THE ACCUMULATION PRODUCTS IN PODZOLS AND SOME OTHER SOILS journal June 1967
Temperature sensitivity of soil carbon decomposition and feedbacks to climate change journal March 2006
The Effective Removal of Suspended Materials from Pyrophosphate Extracts of Soils from Tropical and Temperate Regions1 journal January 1983
Temperature and soil organic matter decomposition rates - synthesis of current knowledge and a way forward journal August 2011
Weathering controls on mechanisms of carbon storage in grassland soils: WEATHERING CONTROLS ON CARBON STORAGE journal December 2004
The adsorption of molybdenum on oxide surfaces journal January 1983
Mineral control of soil organic carbon storage and turnover journal September 1997
Simultaneous Inference in General Parametric Models journal June 2008
Describing the adsorption of phosphate, citrate and selenite on a variable-charge mineral surface journal January 1980
Adsorption of aquatic humic substances on colloidal-size aluminum oxide particles: Influence of solution chemistry journal October 1994
Differenzierung der Eisenoxide des Bodens durch Extraktion mit Ammoniumoxalat-Lösung journal January 1964
Proton-binding study of standard and reference fulvic acids, humic acids, and natural organic matter journal January 2003
Catechol derivatives and anion adsorption onto alumina surfaces in aqueous media: influence on the electrokinetic properties journal July 2001
Deglaciation of the northwestern White Mountains, New Hampshire journal January 1999
Comparison of soil organic matter dynamics at five temperate deciduous forests with physical fractionation and radiocarbon measurements journal May 2012
Competitive Sorption of Dissolved Organic Matter Fractions to Soils and Related Mineral Phases journal January 1997
The Iron Oxides book July 2003
Mineral Assemblage and Aggregates Control Carbon Dynamics in a California Conifer Forest journal January 2005
Application of surface complexation models to anion adsorption by natural materials: Surface complexation modeling of anion adsorption by soils journal August 2014
The retention of organic matter in soils journal February 1988
Surface Charge Characteristics of Amorphous Aluminosilicates journal January 1977
The adsorption of aquatic humic substances by iron oxides journal February 1981
pH-dependent surface charging of metal oxides journal January 2009
Sorptive stabilization of organic matter in soils by hydrous iron oxides journal January 2007
Properties and Quantitative Estimation of Poorly Crystalline Components in Sesquioxidic Soil Clays* journal January 1977
Adsorption of natural dissolved organic matter at the oxide/water interface journal November 1982
Soil carbon storage controlled by interactions between geochemistry and climate journal August 2015
Stable metal-organic frameworks containing single-molecule traps for enzyme encapsulation journal January 2015
Sorptive stabilization of organic matter by microporous goethite: sorption into small pores vs. surface complexation journal February 2007
Long-term controls on soil organic carbon with depth and time: A case study from the Cowlitz River Chronosequence, WA USA journal June 2015
Differentiation of Forms of Extractable Iron and Aluminum in Soils1 journal January 1971
The sorption of humic acids to mineral surfaces and their role in contaminant binding journal May 1992
Geologic controls of soil carbon cycling and microbial dynamics in temperate conifer forests journal September 2009
Mineral control of organic carbon mineralization in a range of temperate conifer forest soils journal May 2006
Generalized Model for Anion and Cation Adsorption at Oxide Surfaces journal October 1973
Determination of Noncrystalline Soil Components by Weight Difference after Selective Dissolution journal January 1980
Influence of mineral-bound humic substances on the sorption of hydrophobic organic compounds journal October 1990
Composition of Organic Matter Fractions for Explaining Wettability of Three Forest Soils journal January 2005

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Faster redox fluctuations can lead to higher iron reduction rates in humid forest soils journal February 2018
Lithology controlled soil organic carbon stabilization in an alpine grassland of the Peruvian Andes journal January 2020
What do we know about soil carbon destabilization? journal July 2019
Drivers of postfire soil organic carbon accumulation in the boreal forest journal July 2018
Examining mineral-associated soil organic matter pools through depth in harvested forest soil profiles journal November 2018
Age distribution, extractability, and stability of mineral-bound organic carbon in central European soils journal July 2020
Boreal-forest soil chemistry drives soil organic carbon bioreactivity along a 314-year fire chronosequence journal May 2020