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U.S. Department of Energy
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Tropical organic soils ecosystems in relation to regional water resources in southeast Asia

Conference ·
OSTI ID:6766882
Tropical organic soils have functioned as natural sinks for carbon, nitrogen, slfur and other nutrients for the past 4000 years or more. Topographic evolution in peat swamp forests towards greater oligotrophy has concentrated storage of the limited nutrient stock in surface soils and biota. Tropical peat systems thus share common ecosystem characteristics with northern peat bogs and certain tropical oligotrophic forests. Organic matter accumulation and high cation-exchange-capacity limit nutrient exports from undisturbed organic soils, although nutrient retention declines with increasing eutrophy and wetland productivity. Peat swamps are subject to irreversible degradation if severely altered because disturbance of vegetation, surface peats and detritus can disrupt nuttrient cycles and reduce forest recovery capacity. Drainage also greatly increases exports of nitrogen, phosphorus and other nutrients and leads to downstream eutrophication and water quality degradation. Regional planning for clean water supplies must recognize the benefits provided by natural peatlands in balancing water supplies and regulating water chemistry.
Research Organization:
Butler Univ., Indianapolis, IN (USA). Holcomb Research Inst.
Sponsoring Organization:
USDOE
DOE Contract Number:
AC02-81EV10725
OSTI ID:
6766882
Report Number(s):
CONF-821118-1; ON: DE83000994
Country of Publication:
United States
Language:
English