Full TGIF Record # 80276
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Web URL(s):https://dl.sciencesocieties.org/publications/aj/pdfs/94/3/455
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https://dl.sciencesocieties.org/publications/aj/articles/94/3/455
    Last checked: 12/15/2016
    Access conditions: Item is within a limited-access website
Publication Type:
i
Refereed
Author(s):Kerek, Mine; Drijber, Rhae A.; Powers, William L.; Shearman, Robert C.; Gaussoin, Roch E.; Streich, Anne Marie
Author Affiliation:Department of Agronomy and Horticulture, University of Nebraska, Lincoln, NE
Title:Accumulation of microbial biomass within particulate organic matter of aging golf greens
Section:Greens management
Other records with the "Greens management" Section
Source:Agronomy Journal. Vol. 94, No. 3, May/June 2002, p. 455-461.
Publishing Information:Madison, WI: American Society of Agronomy
# of Pages:7
Keywords:TIC Keywords: Biomass; Soil microorganisms; Organic matter; Golf greens; Golf courses; Old greens versus young greens; Carbon; Fulvic acid; Humic acid; Phosphates; Humus
Abstract/Contents:"Microbial biomass (MB) is a key variable controlling soil organic matter dynamics in soil. Currently, there is little information on the amount and significance of MB in highly managed golf greens. Our objective was to determine the amount and distribution of MB within soil structural components of golf greens and its relationship to the location of organic substrates. During 1996, 47 greens were sampled from 12 golf courses within Nebraska (USA). Microbial biomass, determined as extractable lipid phosphate on field-moist soils, increased linearly with age of green (Y = 19.39 + 3.54x; r2 = 0.87, P = 0.001). In 1997 and 1999, selected greens were resampled and separated into mineral fraction (MF) and particulate organic matter (POM) fraction using a sodium metatungstate (NMT; r = 2.3 g cm-3). Then, POM was separated into light (L-POM) and heavy (H-POM) fractions using NMT (r = 2.0 g cm-3). Amount of MB of whole soil and POM was linearly related to green age (r2 = 0.76 and 0.68, respectively). Amount of MB in MF was not related to green age. The portion of total soil MB associated with POM increased significantly from 25.6% for an 8-year-old green to 77.8% for a 28-year-old green. Carbon in fulvic acid and humic acid increased with green age from 0.5 to 1.7 and 0.6 to 2.6 g kg-1 soil, respectively. As humus is a relatively stable form of soil organic matter, we hypothesized that humus accumulation within POM renders both POM and associated MB more resistant to degradation; thus, they accumulate."
Language:English
References:48
See Also:Other items relating to: Biostimulants
Note:Figures
Tables
Graphs
ASA/CSSA/SSSA Citation (Crop Science-Like - may be incomplete):
Kerek, M., R. A. Drijber, W. L. Powers, R. C. Shearman, R. E. Gaussoin, and A. M. Streich. 2002. Accumulation of microbial biomass within particulate organic matter of aging golf greens. Agron. J. 94(3):p. 455-461.
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Web URL(s):
https://dl.sciencesocieties.org/publications/aj/pdfs/94/3/455
    Last checked: 12/15/2016
    Requires: PDF Reader
    Access conditions: Item is within a limited-access website
https://dl.sciencesocieties.org/publications/aj/articles/94/3/455
    Last checked: 12/15/2016
    Access conditions: Item is within a limited-access website
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