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DYNAMICS OF SOIL MICROBIAL BIOMASS AND WATER-SOLUBLE ORGANIC C IN BRETON L AFTER 50 YEARS OF CROPPING TO TWO ROTATIONS
Abstract
Amounts and turnover rates of biomass and water-soluble organic C (WSOC) were measured at the Breton plots where records of long-term management of a Gray Luvisolic soil are available. Plots (control, manure, and NPKS) which had been cropped to either a wheat-fallow or a wheat-oats-barley-forage-forage rotation for 50 yr were sampled 13 times during 1981 and 1982. Biomass C and flush of microbial N were measured using the chloroform fumigation technique. Long-term crop yields were used to derive C supply to the plots. Regression analyses were used to relate seasonal fluctuations in environmental conditions to biomass and WSOC dynamics. Reinoculation with soil was unnecessary but Lysobacter sp. formed a greater proportion of isolates following incubation of fumigated soil than of unfumigated samples. Reinoculation with Lysobacter sp. is suggested to provide a more standardized biological assay. The 5-yr rotation contained 38% more N but 117% more microbial N than did the 2-yr rotation, and manured treatments contained twice as much microbial N as did NPKS or control plots. A management effect on soil organic matter quality is indicated. Averge turnover rates of biomass were 0.2–3.9 yr−1; being 1.5–2 times faster in the 2-yr rotation than in the 5-yr rotation. Replenishment of the WSOC component would have to occur 26–39 times yr−1 to supply microbial turnover. Most of the biomass must be dormant because annual C inputs are two orders of magnitude less than maintenance energy requirements. Seasonal variations in biomass were most consistently related to losses during desiccation and regrowth upon moistening. Regrowth appears to be at the expense of native soil organic matter. Management practices and environmental conditions therefore affect amount of organic matter by controlling both input of C and biomass turnover. Key words: Crop rotations, Luvisol, organic matter, biomass, soluble C, Breton plots
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Cites
Burford, J. R., & Bremner, J. M. (1975) · Soil Biology and Biochemistry · doi:10.1016/0038-0717(75)90055-3 · Cited by 742
Cited by
SOM fractionation methods: Relevance to functional pools and to stabilization mechanisms
von Lützow, M., Kögel-Knabner, I., Ekschmitt, K., Flessa, H., Guggenberger, G., Matzner, E., & Marschner, B. (2007) · Soil Biology and Biochemistry · doi:10.1016/j.soilbio.2007.03.007 · Cited by 1,590
Haynes, R. J. (2005) · Advances in Agronomy · doi:10.1016/s0065-2113(04)85005-3 · Cited by 1,010
Chantigny, M. H. (2003) · Geoderma · doi:10.1016/s0016-7061(02)00370-1 · Cited by 819
Current methods for measuring microbial biomass C in soil: Potentials and limitations
Martens, R. (1995) · Biology and Fertility of Soils · doi:10.1007/bf00336142 · Cited by 284
Kaur, T., Brar, B. S., & Dhillon, N. S. (2008) · Nutrient Cycling in Agroecosystems · doi:10.1007/s10705-007-9152-0 · Cited by 254
Metadata
- Authors
- McGILL, W. B., CANNON, K. R., ROBERTSON, J. A., & COOK, F. D.
- Venue
- Canadian Journal of Soil Science
- Publisher
- Canadian Science Publishing
- Published
- 1986-02-01
- Volume
- 66
- Issue
- 1
- Pages
- 1-19
- ISSN
- 0008-4271 (ISSN-L)
- 1918-1841
- OpenAlex
- W2022722465
- Cited by
- 629
- References
- 1
- FWCI
- 15.80
- Type
- journal article
- Language
- en
- Open access
- closed
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- McGILL, W. B., CANNON, K. R., ROBERTSON, J. A., & COOK, F. D. (1986). DYNAMICS OF SOIL MICROBIAL BIOMASS AND WATER-SOLUBLE ORGANIC C IN BRETON L AFTER 50 YEARS OF CROPPING TO TWO ROTATIONS. Canadian Journal of Soil Science. https://doi.org/10.4141/cjss86-001
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