We investigated long-term time variation of dissolved species in the water sampled from the upper stream of Sagami River and its tributaries. The sampling had been done monthly from May 1993 to April 1999 at 14 sampling sites of upper stream of Sagami River water system (Katsura River) . Twenty-four major to trace elements (Li, Mg, Al, Ca, V, Mn, Fe, Co, Ni, Cu, Zn, As, Rb, Sr, Mo, Ag, Cd, Sb, Cs, Ba, W, Tl, Pb, U) were determined using conventional Q-pole ICP-MS with direct nebulization. Electric Conductivity, pH, water flux (from April 1995) were also determined. Long-term interannual trends of dissolved species were examined for the data accumulated for 6 years by 12 months moving average.
Water qualities of uppermost stream area were generally constant and mostly controlled by spring waters, which are located around Mt. Fuji. However, in 1998, some elements such as V Rb, Cs were depleted temporally, which may be caused by dilution effect of over flow from Lake Kawaguchi and Lake Yamanaka.
On the other hand, in the small creeks with minor influence of spring waters, many elements such as Ni, Zn, Cd, Sb showed long-term trends. These trends may be caused by either factory or mining wastewaters. Moving averages of some elements, like V, As, Rb, showed concentration maxima during 1995 to 1996. These trends may correlate with water flux.
In the tributaries of Katsura River with wider catchments, many elements such as V, Mn, Rb, Cs showed seasonal variations. The moving averages of most of the elements were generally constant, however, Mg, Ca showed slight decreasing trend and correlated with water flux. In some cases, Co, Ni, Mo etc.showed spiky increases indicating point source origin.
Because intake and discharge of water utility for electric power plant, water quality of mainstream of upper area alters depending on sampling sites.
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