Organic carbon and nitrogen mineralization under Mediterranean climatic conditions: The effects of incubation depth

• Published in: Soil biology & biochemistry Vol. 29; no. 9; pp. 1509 - 1520
• Main Authors: Rovira, P., Vallejo, V.R.
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier Ltd 01.09.1997; New York, NY Elsevier Science
• Subjects: Agronomy. Soil science and plant productions; Biological and medical sciences; Chemical, physicochemical, biochemical and biological properties; Fundamental and applied biological sciences. Psychology; Organic matter; Physics, chemistry, biochemistry and biology of agricultural and forest soils; Soil science; Southern Europe; Europe; Spain; Organic carbon; Eucalyptus globulus; Decomposition; Forest soil; Depth; Climatic condition; Soil climate; Luvisols; Organic matter cycle; Mineralization; Dicotyledones; Angiospermae; Softwood forest tree; Gymnospermae; Myrtaceae; Hardwood forest tree; Pinus halepensis; Alfisols; Quercus ilex; Fagaceae; Carbon cycle; Nitrogen cycle; Soil horizons; Coniferales; Spermatophyta; Mediterranean climate
• ISSN: 0038-0717; 1879-3428
• DOI: 10.1016/S0038-0717(97)00052-7

In a soil profile, temperature and humidity regimes change with depth. Under Mediterranean conditions, upper horizons are more affected by water deficits and drying-rewetting cycles than deep horizons. Our aim was to study how carbon and nitrogen mineralization are affected by depth, and special attention is paid to separating the effects of pedoclimate fromthe effects of other constraints like amount and quality of organic matter. To this end, mixtures of plant + soil material were exposed by incorporation in the field, at depths of 5, 20 and 40 cm, in nylon mesh bags. Mineralization of C and N was studied for 2 y. For all types of plant material studied ( Eucalyptus globulus, Quercus ilex and Pinus halepensis), mineralization of both carbon and nitrogen was lower at 5 cm. No differences were between 20 and 40 cm. This result, probably as a result of the higher drying of the upper-most horizons, contrasts with the usual findings on this topic. The amounts of both C and N mineralized were lower than expected, probably because plant materials were finely ground, allowing stabilization in the mineral matrix of soil. With the possible exception of Pinus, depth affected the rate of mineralization, not the relation between C and N. It is concluded that, at least under Mediterranean conditions, the pedoclimate in deep layers is more favourable to microbial activity than in upper layers, in which drought is a strong limiting factor. Reduced oxygen availability in the subsoil layers did not inhibit decomposition and mineralization to the same extent as did desiccation in the surface layer. The higher mineralization of C and N usually found in upper horizons may be attributed to the higher amount and quality of organic matter in these horizons, rather than to pedoclimatic constraints.