Changing tropical hydrologic regimes have been attributed to conversion from tropical forest to agriculturaluse and are a threat to many tropical upland ecosystems. A series of experiments were conducted in headwatercatchments of Matalom, Leyte, Philippines, to quantify the effect on the near-surface hydrology of land uses common tothe steep slopes and thin, calcareous soils. Overland and subsurface runoff were collected to compare the surfacehydrologic response of forested, tilled, slash/mulch, and pasture catchments. The forest site demonstrated the lowestannual runoff response, at less than 3% of rainfall, and the highest rainfall threshold which initiated runoff. Conversely,the pasture site demonstrated the greatest annual runoff response (76%) with the lowest thresholds. A pasture withcontour-hedgerows demonstrated greater infiltration than the pasture without this conservation practice, generatingrunoff at 31% of annual rainfall. The plowed and slash/mulch sites had similar annual runoff responses, at 17% and 13%of rainfall, although the predominant flow pathway differed between these sites. Surface runoff accounted for the majorityof runoff at the plowed and pasture-fallow sites; whereas, interflow provided the largest contribution to runoff at theslash/mulch and forest sites.
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Chandler et al. (1998) studied this question.
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