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The Role of Soil Characteristics on Temperature Sensitivity of Soil Organic Matter
Author(s) -
Haddix Michelle L.,
Plante Alain F.,
Conant Richard T.,
Six Johan,
Steinweg J. Megan,
Magrini-Bair Kim,
Drijber Rhae A.,
Morris Sherri J.,
Paul Eldor A.
Publication year - 2011
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj2010.0118
Subject(s) - soil water , decomposition , organic matter , chemistry , pyrolysis , environmental chemistry , soil organic matter , soil respiration , cycling , soil science , environmental science , fraction (chemistry) , chromatography , organic chemistry , history , archaeology
The uncertainty associated with how projected climate change will affect global C cycling could have a large impact on predictions of soil C stocks. The purpose of our study was to determine how various soil decomposition and chemistry characteristics relate to soil organic matter (SOM) temperature sensitivity. We accomplished this objective using long‐term soil incubations at three temperatures (15, 25, and 35°C) and pyrolysis molecular beam mass spectrometry (py‐MBMS) on 12 soils from 6 sites along a mean annual temperature (MAT) gradient (2–25.6°C). The Q 10 values calculated from the CO 2 respired during a long‐term incubation using the Q 10‐q method showed decomposition of the more resistant fraction to be more temperature sensitive with a Q 10‐q of 1.95 ± 0.08 for the labile fraction and a Q 10‐q of 3.33 ± 0.04 for the more resistant fraction. We compared the fit of soil respiration data using a two‐pool model (active and slow) with first‐order kinetics with a three‐pool model and found that the two and three‐pool models statistically fit the data equally well. The three‐pool model changed the size and rate constant for the more resistant pool. The size of the active pool in these soils, calculated using the two‐pool model, increased with incubation temperature and ranged from 0.1 to 14.0% of initial soil organic C. Sites with an intermediate MAT and lowest C/N ratio had the largest active pool. Pyrolysis molecular beam mass spectrometry showed declines in carbohydrates with conversion from grassland to wheat cultivation and a greater amount of protected carbohydrates in allophanic soils which may have lead to differences found between the total amount of CO 2 respired, the size of the active pool, and the Q 10‐q values of the soils.