黃登花崗巖의 風化에 따른 化學組成의 變化와 主要元素의 相對的 移動

Variation of chemical composition and relative movement of major elements on the weathering of Hwang-Dung granite

The writer intended to observe the relative mobility of elements in weathering process of granite, on the outskirts of IRI city at Jeollabukdo KOREA. He analysed fresh granites and weathered ones of Hwang-Dung granite mass and had following conclusions by the triangular diagrams and the oxidized variation diagrams of the analysis. 1) The increasing phenomena of H₂O observed clearly in early and late stage of weathering processes. 2) Granites was weathered by physical weathering in early stage, and it was weathered by chemical weathering in late stage. 3) The ratio of FeO/Fe₂O₃, FeO/MgO, and SiO₂/Al₂O₃ decreased uniformly from early to late stage of weathering processes. 4) It was proved that weathering potential of granite was larger than that of basaltic rock. 5) The order of mobility in major elements was Ca, Na, K＞Si＞Mg＞Fe, Al.