Carbonyl sulfide exchange in soils for better estimates of ecosystem carbon uptake

Whelan, Mary E.; Hilton, Timothy W.; Berry, Joseph A.; Berkelhammer, Max; Desai, Ankur R.; Campbell, J. Elliott

doi:10.5194/acp-16-3711-2016

Title: Carbonyl sulfide exchange in soils for better estimates of ecosystem carbon uptake

Journal Article · Mon Mar 21 04:00:00 UTC 2016 · Atmospheric Chemistry and Physics (Online)

DOI: https://doi.org/10.5194/acp-16-3711-2016 · OSTI ID:1271010

Whelan, Mary E. ^[1]; Hilton, Timothy W. ^[2]; Berry, Joseph A. ^[3]; Berkelhammer, Max ^[4]; Desai, Ankur R. ^[5]; Campbell, J. Elliott ^[2]

Univ. of California-Merced, Merced, CA (United States). Dept. of Environmental Engineering; Carnegie Institution for Science, Stanford, CA (United States); University of California
Univ. of California-Merced, Merced, CA (United States). Dept. of Environmental Engineering
Carnegie Institution for Science, Stanford, CA (United States)
Univ. of Illinois-Chicago, Chicago, IL (United States). Dept. of Earth and Environmental Sciences
Univ. of Wisconsin, Madison, WI (United States). Dept. of Atmospheric and Oceanic Sciences

Carbonyl sulfide (COS) measurements are one of the emerging tools to better quantify gross primary production (GPP), the largest flux in the global carbon cycle. COS is a gas with a similar structure to CO₂; COS uptake is thought to be a proxy for GPP. However, soils are a potential source or sink of COS. This study presents a framework for understanding soil–COS interactions. Excluding wetlands, most of the few observations of isolated soils that have been made show small uptake of atmospheric COS. Recently, a series of studies at an agricultural site in the central United States found soil COS production under hot conditions an order of magnitude greater than fluxes at other sites. To investigate the extent of this phenomenon, soils were collected from five new sites and incubated in a variety of soil moisture and temperature states. We found that soils from a desert, an oak savannah, a deciduous forest, and a rainforest exhibited small COS fluxes, behavior resembling previous studies. However, soil from an agricultural site in Illinois, >800 km away from the initial central US study site, demonstrated comparably large soil fluxes under similar conditions. These new data suggest that, for the most part, soil COS interaction is negligible compared to plant uptake of COS. We present a model that anticipates the large agricultural soil fluxes so that they may be taken into account. Furthermore, while COS air-monitoring data are consistent with the dominance of plant uptake, improved interpretation of these data should incorporate the soil flux parameterizations suggested here.

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Research Organization:: Oregon State Univ., Corvallis, OR (United States)

Sponsoring Organization:: USDOE Office of Science (SC), Biological and Environmental Research (BER) (SC-23); National Science Foundation (NSF)

Grant/Contract Number:: FG02-04ER63917; FG02-04ER63911

OSTI ID:: 1271010

Journal Information:: Atmospheric Chemistry and Physics (Online), Journal Name: Atmospheric Chemistry and Physics (Online) Journal Issue: 6 Vol. 16; ISSN 1680-7324

Publisher:: European Geosciences UnionCopyright Statement

Country of Publication:: United States

Language:: English

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54 ENVIRONMENTAL SCIENCES
atmosphere
cos
dimethyl sulfide
forest soils
gas-exchange
global budget
growing-season
organic-matter
southern great-plains
trace gases

Title: Carbonyl sulfide exchange in soils for better estimates of ecosystem carbon uptake

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