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Isotopic and Elemental Hydrogeochemistry of the Han River, South Korea

机译:韩国汉江的同位素和元素水文地球化学

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摘要

The Han River is the largest river in South Korea and supports a variety of industrial, agricultural and human activities, including water supply for a metropolitan city, Seoul. It consists of two major rivers (the North and South Han Rivers) and many tributaries. The river originates at altitudes of more than 1,300 meters above sea level in the Taeback Mountains, which run subparallel to the eastern coast of South Korea, and traverse the mid-western parts of the Korean peninsula before flowing into the Yellow Sea. The North Han River drains a basin consisting of the Precambrian gneissic basements and Mesozoic granites, whereas the South Han River drains a basin consisting of the Paleozoic sedimentary rocks (mostly carbonates) and Mesozoic granites
机译:汉江是韩国最大的河流,支持各种工业,农业和人类活动,包括为大城市首尔供水。它由两条主要河流(北汉江和南汉江)和许多支流组成。这条河发源于Taeback山脉海拔1300多米,该山脉与韩国东海岸平行,并横穿朝鲜半岛中西部,然后流入黄海。北汉江流域由前寒武纪片麻质基底和中生代花岗岩组成,而南汉江流域由古生代沉积岩(主要为碳酸盐岩)和中生代花岗岩组成

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