Full TGIF Record # 81347
Item 1 of 1
DOI:10.2134/agronj2002.9300
Web URL(s):https://dl.sciencesocieties.org/publications/aj/pdfs/94/4/930
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https://dl.sciencesocieties.org/publications/aj/articles/94/4/930
    Last checked: 12/15/2016
    Access conditions: Item is within a limited-access website
Publication Type:
i
Refereed
Author(s):Qian, Yaling; Follett, Ronald F.
Author Affiliation:Qian: Dep. of Hortic. and Landscape Architecture, Colorado State Univ.; Follett: USDA-ARS, Soil-Plant-Nutrient Res. Unit, Fort Collins, CO
Title:Assessing soil carbon sequestration in turfgrass systems using long-term soil testing data
Section:Turfgrass
Other records with the "Turfgrass" Section
Source:Agronomy Journal. Vol. 94, No. 4, July/August 2002, p. 930-935.
Publishing Information:Madison, WI: American Society of Agronomy
# of Pages:6
Keywords:TIC Keywords: Application rates; Carbon sequestration; Golf fairways; Golf greens; Organic matter; Soil chemistry; Soil pH; Soil testing; Soil texture
Abstract/Contents:"As part of the urbanization process, an increasing percentage of land throughout the USA is being converted into turfgrass. Because of high productivity and lack of soil disturbance, turfgrass may be making substantial contributions to sequester atmospheric C. To determine the rate and capacity of soil C sequestration, we compiled historic soil-testing data from parts of 15 golf courses that were near metropolitan Denver and Fort Collins, CO, and one golf course near Saratoga, WY. In addition, we compiled a total of about 690 data sets on previous land use, soil texture, grass species and type, fertilization rate, irrigation, and other management practices. The oldest golf course was 45 yr old in 2000, and the newest golf course was 1.5 yr old. Nonlinear regression analysis of compiled historic data indicated a strong pattern of soil organic matter (SOM) response to decades of turfgrass culture. Total C sequestration continued for up to about 31 yr in fairways and 45 yr in putting greens. However, the most rapid increase occurred during the first 25 to 30 yr after turfgrass establishment, at average rates approaching 0.9 and 1.0 t ha-1 yr-1 for fairways and putting greens, respectively. Our study also found that past land use imparted a strong control of SOM baseline; fairways converted from agricultural lands exhibited 24% lower SOM than fairways converted from native grasslands. We concluded that C sequestration in turf soils occurs at a significant rate that is comparable to the rate of C sequestration reported for USA land that has been placed in the Conservation Reserve Program."
Language:English
References:21
See Also:See also related article "Assessing soil carbon sequestration in turfgrass systems using long-term soil testing data" United States Department of Agriculture Agricultural Research Service Web Site, January 20 2002, p. [1-2], R=135864. R=135864
See Also:Other items relating to: Carbon sequestration of turf
Note:Tables
Graphs
ASA/CSSA/SSSA Citation (Crop Science-Like - may be incomplete):
Qian, Y., and R. F. Follett. 2002. Assessing soil carbon sequestration in turfgrass systems using long-term soil testing data. Agron. J. 94(4):p. 930-935.
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DOI: 10.2134/agronj2002.9300
Web URL(s):
https://dl.sciencesocieties.org/publications/aj/pdfs/94/4/930
    Last checked: 12/15/2016
    Requires: PDF Reader
    Access conditions: Item is within a limited-access website
https://dl.sciencesocieties.org/publications/aj/articles/94/4/930
    Last checked: 12/15/2016
    Access conditions: Item is within a limited-access website
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