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Title: Slash and burn impacts on a Costa Rican wet forest site

Journal Article · · Ecology; (United States)
DOI:https://doi.org/10.2307/1937748· OSTI ID:6456605

Impacts of felling, mulching, and burning on budgets of C, N, S, P, K, Ca, and Mg; rates of CO/sub 2/ evolution from the soil; soil seed storage; and plant growth were evaluated. The felled tropical evergreen forest was 8 to 9 yr old, interspersed with patches of 70-yr-old forest and had a leaf area index of 6 and aboveground biomass of 5.2 kg/m/sup 2/. Harvest of the largest trees removed 18% of the S, and >10% of all other elements except N. During the 11-wk mulching and drying period, 33% of the K and 13% of the P disappeared, but losses of other elements were <6%. Burn temperatures were >620/sup 0/C in surface fuels, but soil temperatures were seldom >100/sup 0/C at 1 cm or >50/sup 0/C at 2 cm. The burn volatilized 1600 g/m/sup 2/ C, 49 g/m/sup 2/ N, and 13 g/m/sup 2/ S. Postburn wind and water erosion of ash, plus leaching, removed 34 g/m/sup 2/ N, 20 g/m/sup 2/ K, 1 g/m/sup 2/ P, 39 g/m/sup 2/ Ca, and 7 g/m/sup 2/ Mg, but insignificant amounts of C and S. After the burn and onset of the rains, 57% of the initial amount of N and 39% of the initial C still remained because of conservation of the organic-rich upper 3 cm of soil. Soil CO/sub 2/ evolution was greater from beneath the 11-wk-old slash (3.6 gC.m/sup -2/.d/sup -1/) than from beneath the forest (2.5 gC.m/sup -2/.d/sup -1/), probably because the slash conserved soil moisture better than the actively transpiring forest. After the burn both the burned field and forest soil evolved CO/sub 2/ at approx. =4.5 gC.m/sup -2/.d/sup -1/. At this rate, 154 d of decomposition and respiration would release as much C into the atmosphere as did the burn.

Research Organization:
Univ. of Florida, Gainesville
OSTI ID:
6456605
Journal Information:
Ecology; (United States), Vol. 62:3
Country of Publication:
United States
Language:
English