In this study, the samples were collected from the selected locations (Fig.1) in Sumiyoshi River; the geology of whose drainage basin consists mostly of biotite granite region; water quality of which is not contaminated with human life and mineral spring. The variations of the various soluble components have been measured over three years.
To investigate the seasonal variations, the surveys were made every ten days at the four locations in Juneecember, 1975. The results, given in Table 1, show that the concentrations of Mg, K, F, PO
4, NO
2, Fe, Mn, Cu and Zn are higher in the hot season than in the cold one, while those of Ca, Na, HCO
3, Cl, SO
4 and SiO
2 do not show such a variation.
To make clear the influence of rainfall, the daily investigations in September, 1975, in December, 1976, and in May and June, 1977 were carried out and also the surveys in June 2nd, 1977 were performed every two hours at the main stream, the location No.4. From the results shown in Table 2 and Figs.2-4, it is shown that the concentrations of Ca, Mg, Na, HCO
3, Cl and F vary with almost definite propotion, and the concentrations move in a little inverse way to the flow rate of the stream, But the concentrations of K, SO
4, SiO
2, PO
4, NO
2, Fe, Mn, Cu and Zn vary independently and change with relatively large extent.
Based on these experimental results and the relationship between the correlation coefficients given in Table 3 and the concentration correlations from the upper stream to the lower stream, shown in Fig.5, it is considered that the soluble components in the stream arise mostly from CO, weathering, fall-out, and humus decomposition products.
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