잣나무 임분에 있어서 강우수질의 이동 특성 = Water Chemistry Profiles under Korean White Pine (Pinus koraiensis S. et Z.) Stand

다국어 초록 (Multilingual Abstract)

This experiment was conducted to characterize the vertical transport trend of dissolved elements
through throughfall, stemflow, effluent from Ao layer, and leachate out of soil profile on Pinus
koraiensis stand in Experimental Forest of Kyunghee University, located in Kwangju, Kyunggi province for 12 months from July, 1998 to Jun, 1999. In addition, we investigated the content of dissolved elements and the factors influencing the water chemistry concentrations separately collected from the field. Water movement in the process of throughfall and stemflow from precipitation, and rainfall leached from Ao layer into soil water was governed by concentration of throughfall, precipitation, rainfall intensity, seasonal variation, and other factors. Also, smaller changes of pH in soil water than that of dissolved elements in soil water could contribute buffer capacity, as well as balancing the concentration between cations and anions.