Full TGIF Record # 279674
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DOI:10.2136/sssaj2016.03.0061
Web URL(s):https://acsess.onlinelibrary.wiley.com/doi/10.2136/sssaj2016.03.0061
    Last checked: 02/26/2024
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https://acsess.onlinelibrary.wiley.com/doi/epdf/10.2136/sssaj2016.03.0061
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Publication Type:
i
Refereed
Author(s):Wang, Jiaping; Monger, Curtis; Wang, Xiujun; Serena, Matteo; Leinauer, Bernhard
Author Affiliation:Jiaping Wang: College of Agronomy, Shihezi Univ, Shihezi, China and State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, China; Monger: New Mexico State Univ., Las Cruces, NM and National Soil Survey Center, USDA, Lincoln, NE; Xiujun Wang: State Key Laboratory of Desert and Oasis Ecology and Xinjiang Institute of Ecology and Geography Chinese Academy of Sciences, Urumqi, China and Earth System Sci. Interdisciplinary Center, Univ. of Maryland, College Park, MD; Serena and Leinauer: New Mexico State Univ., Las Cruces, NM
Title:Carbon sequestration in response to grassland-shrubland-turfgrass conversions and a test for carbonate biomineralization in desert soils, New Mexico, USA
Section:Pedology
Other records with the "Pedology" Section
Source:Soil Science Society of America Journal. Vol. 80, No. 6, November/December 2016, p. 1591-1603.
Publishing Information:Madison, Wisconsin: Soil Science Society of America
# of Pages:13
Keywords:TIC Keywords: C-4 plant; Carbon sequestration; Chemical soil analysis; Conversion; Grassland soils; Isotopes; Microbiological soil analysis; Organic soils; Pedology
Abstract/Contents:"This study uses an experimental pedology approach to examine (i) how the conversion of native C4 grassland to C3 woody shrubs then to irrigated C4 turfgrass affects both soil organic C (SOC) and soil inorganic C (SIC) and (ii) whether SIC can be enhanced by microbial biomineralization. Three sites were studied in the Chihuahuan Desert of New Mexico. At each site, SOC, SIC, and their δ13C values were measured on control soil samples and compared to samples treated with liquid growth medium and Ca(OH)2 at 10 and 40 cm. The treated samples were left to react for 1 mo in February, May, and August of 2014. Using a space-for-time substitution, soil organic C decreased when native grasslands converted to desert shrubs, then sharply increased after desert shrubs were converted to irrigated turfgrass. Most surprising, however, was the increase of SIC in the turfgrass site, which doubled in 6 yr. The δ13C values of both SOC and SIC reflected the change from C4 to C3 then back to C4 vegetation and showed how rapidly SOC and SIC can change their isotopic signatures. Soil inorganic C formation was slightly higher for the liquid growth medium, but no statistically significant differences were observed between the treatments and control samples. In addition, no biomineralization was observed with microscopy, perhaps because the 1-mo reaction time was too short and the amount applied was too small. Although SIC is typically viewed as a soil mineral that requires centuries to accumulate, our study indicate that SIC can be generated in months to years if the soil environment is suitable."
Language:English
References:67
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ASA/CSSA/SSSA Citation (Crop Science-Like - may be incomplete):
Wang, J., C. Monger, X. Wang, M. Serena, and B. Leinauer. 2016. Carbon sequestration in response to grassland-shrubland-turfgrass conversions and a test for carbonate biomineralization in desert soils, New Mexico, USA. Soil Science Society of America Journal. 80(6):p. 1591-1603.
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DOI: 10.2136/sssaj2016.03.0061
Web URL(s):
https://acsess.onlinelibrary.wiley.com/doi/10.2136/sssaj2016.03.0061
    Last checked: 02/26/2024
    Access conditions: Item is within a limited-access website
https://acsess.onlinelibrary.wiley.com/doi/epdf/10.2136/sssaj2016.03.0061
    Last checked: 02/26/2024
    Requires: PDF Reader
    Access conditions: Item is within a limited-access website
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