Soil indicators of C and N transformations under pure and mixed grass-clover swards

Citation
G. Alvarez et al., Soil indicators of C and N transformations under pure and mixed grass-clover swards, EUR J AGRON, 9(2-3), 1998, pp. 157-172
Citations number
46
Categorie Soggetti
Agriculture/Agronomy
Journal title
EUROPEAN JOURNAL OF AGRONOMY
ISSN journal
11610301 → ACNP
Volume
9
Issue
2-3
Year of publication
1998
Pages
157 - 172
Database
ISI
SICI code
1161-0301(199811)9:2-3<157:SIOCAN>2.0.ZU;2-M
Abstract
The changes occurring in the soil organic status under grassland swards aft er 3 years were examined as a function of the initial soil nitrogen supplyi ng capacity (SNSC: 135 or 225 kg N ha(-1) year(-1)) and of the soil cover: bare soil, pure white clover, pure rye-grass or a mixture of both species. The amounts of C and N of the coarse particle size OM, the microbial biomas s-C, the C and N in water extracts (microbial metabolites) and the C and N mineralization in 28-day incubation tests were used as indicators of the tr ansformation of the organic C and N inputs to the soil under these contrast ing managements. The part of the Variation of these indicators explained by the initial soil N supplying capacity decreased from the metabolite-C to t he coarse plant residues-C to the microbial biomass-C (MB-C) soil compartme nts. The part of the variation explained by plant cover increased in the sa me order. For each variable, the effect of soil fertility was maintained un der pure grass and was reduced or suppressed under pure legume. The soil or ganic status under the mixed stand was similar to that of the pure clover a nd intermediate between that of the pure clover and the pure grass stands. The amount of N mineralization was similar with similar N amounts in the pl ant residues, whereas amounts of C in the plant residues and MB-C were in t he order; pure clover<mixed stand<pure grass. Higher soil respiration and m icrobial specific respiration in incubation tests were seen in the pure gra ss stand. Soil organic status was examined as a function of the amounts of C and N and the C:N ratio of the organic inputs and from their impact on th e microbial activity in situ. The ratio of C mineralization to N mineraliza tion in laboratory incubations is proposed as an indicator of the dry matte r and N harvests, of the degree of accumulation of the non-harvested C and N in the plant residues, and of the risk of nitrate leaching. The optimum v alue of this indicator, about 14, was obtained under the mixed award. (C) 1 998 Elsevier Science B.V. All rights reserved.