摘要
Acid-leachable major elements (K, Na, Ca, Mg)of three riverine sediment cores have been measured. These cores were collected in Oct. 2006 from Daning River which is a major tributary of Yangtze River. The results suggest that the content of acid-leachable major elements in the cores can reflect the characteristics and origin of the sediments. It indicates a differently sedimentary origin from Daning River. As a result, the carbonate content and acid-leachable major elements in the riverine sediments decreased sharply and the color of the sediment changed obviously. Since the first phase of the sluice of Three Gorges Reservoir in December 2004, the sediment thickness around Shuanglong town is about 11 cm, which gives a sedimentary rate of 5.5 cm/a in Daning River.