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Stream water quality was stable and had little variation, and pH was always near 7.00. Rainfall contained large proportions of both NO^-_3 and SO^2-_4, and the pH was always below 5.40. Stemflow showed a lower pH than that of rainfall. It was suggested that the chemical compositions in both throughfall and stemflow were mainly caused by the wash-off of dry deposition. Soil water has large proportions of both NO^-_3 and Ca^2+, which were caused by nitrification and base cation exchange. Stream water has large proportions of both Na^+ and HCO^-_3 caused by chemical weathering. The time lag from rainfall to discharge peak in a small catchment was much quicker than that of a large one, and it was suggested to control system of discharge in large catchment. A time series of both discharge and \u03b4^18O had the same changes as in the storm runoff. 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