CO2 efflux from a Mediterranean semi-arid forest soil. I. Seasonality and effects of stoniness

• Published in: Biogeochemistry 2000-03, Vol.48 (3), p.261-281
• Main Authors: Casals, P, Romanya, J, Cortina, J, Bottner, P, Couteaux, M.M, Vallejo, V.R
• Format: Article
• Language: English
• Subjects: biological activity in soil; Carbon dioxide; Cylinders; Drought; Earth sciences; Earth, ocean, space; Exact sciences and technology; Forest soils; Gravel; Mineral soils; Organic matter; Organic soils; Radiocarbon; Rainstorms; respiration; Seasonal variations; Soil biology; Soil ecology; soil fauna; Soil horizons; soil microorganisms; Soil organic matter; Soil profiles; Soil temperature; Soil water; soil water potential; Soils; Summer; Surficial geology; Water potential
• ISSN: 0168-2563; 1573-515X
• DOI: 10.1023/A:1006289905991

We studied the seasonality of total soil CO2 efflux and labeled C-CO2 released from 14C labeled straw incubated in the H horizon of a semi-arid Mediterranean forest soil. Field measurements were carried out over 520 days in a series of reconstructed soil profiles with and without a gravel layer below the H horizon. We monitored soil climate and related this to soil CO2 efflux. Seasonal variations in soil CO2 efflux in a semiarid Mediterranean forest were mainly related to changes in soil temperature. In spite of drought, high respiration rates were observed in mid summer. High soil CO2 efflux in hot and dry episodes was attributed to increases in soil biological activity. The minimum soil CO2 efflux occurred in late summer also under dry conditions, probably related to a decrease in soil biological activity in deep horizons. Biological activity in organic layers was limited by water potential (Ψ) in summer and by temperature in winter. Rewetting a dry soil resulted in large increases in soil CO2 efflux only at high temperatures. These large increases represented a significant contribution to the decomposition of organic matter in the uppermost horizons. Soil biological activity in the uppermost horizons was more sensitive to changes in soil Ψ and hence to summer rainstorms than the bulk soil microbial activity. The presence of a layer of gravel improved both moisture and temperature conditions for the decomposition of organic matter. As a result, soil CO2 efflux increased in soils containing rock fragments. These effects were especially large for the organic layers.