Carbon residence times obtained from labelled ryegrass decomposition in soils under contrasting environmental conditions

Citation
A. Parshotam et al., Carbon residence times obtained from labelled ryegrass decomposition in soils under contrasting environmental conditions, SOIL BIOL B, 32(1), 2000, pp. 75-83
Citations number
23
Categorie Soggetti
Environment/Ecology
Journal title
SOIL BIOLOGY & BIOCHEMISTRY
ISSN journal
00380717 → ACNP
Volume
32
Issue
1
Year of publication
2000
Pages
75 - 83
Database
ISI
SICI code
0038-0717(200001)32:1<75:CRTOFL>2.0.ZU;2-J
Abstract
Thc rate of decomposition of ryegrass in New Zealand soils was studied. Six soils from contrasting New Zealand environments were amended with C-14-lab elled ryegrass (Lolium hybridum Hausskn), which was allowed to decompose in micro-lysimeters under field conditions for 2 yr. Periodically, the micro- lysimeters were destructively sampled, and the amount of C-14 remaining in the soil and the fraction of C-14 incorporated into microbial biomass measu red. After 2 yr of exposure, 18 to 32% of the labelled C-14 was retained by the soils. Decomposition was initially rapid, with almost one-half of the labelled C-14 being lost after 2 months. Thereafter, the rate of decomposit ion was much reduced. During the initial phase of decomposition (2 months), a larger portion of the C-14 was retained by one soil which had major wate r deficits. The influence of environmental factors on decomposition rate wa s assessed by assuming a three compartment model and calculating the mean a nd variances of residence times of biomass-C-14 and residual-C-14. Analytic al solutions are presented to the model equations. The C-14 residence times , adjusted for soil surface area, were related to rainfall. The residence t imes were compared with times obtained in our earlier study on soils varyin g in clay content and mineralogy. This provides a range of C-14 residence t imes for decomposition of ryegrass in New Zealand soils. These results may be used to validate rate-reduction factors in soil organic matter models. ( C) 2000 Elsevier Science Ltd. All rights reserved.