Comparative study of the modern flood slackwater deposits in the upper reaches of Hanjiang and Weihe River Valleys, China

详细信息    查看全文

• 作者：Yuzhu Zhang ; Chun Chang Huang ; ^{cchuang@snnu.edu.cn} ; Jiangli Pang ; Xiaochun Zha ; Yali Zhou ; Shuyan Yin ; Juan Wang
• 刊名：Quaternary International
• 出版年：2012
• 出版时间：19 December, 2012
• 年：2012
• 卷：282
• 期：Complete
• 页码：184-191
• 全文大小：1059 K

文摘

Modern flood slackwater deposits (SWD) were investigated and sampled in the upper reaches of Hanjiang River and the Weihe River valleys, China. Magnetic susceptibility and grain-size distribution were analyzed in the laboratory. The results show that the magnetic susceptibility values of the modern flood SWD vary between 20?¡Á?10^?8?m³?kg^?1 and 60?¡Á?10^?8?m³?kg^?1, very close to that of the Malan Loess over the Weihe River basin. These sediments were newly deposited and uninfluenced by weathering and pedogenesis. The grain-size distribution of the modern flood SWD is dominated by silt, with sand and clay, indicating that these sediments were sourced from the suspended sediment load of floodwater. However, the grain-size distribution of the modern flood SWD has more sand-sized sediments in the upper reaches of Hanjiang River valley than that in the Weihe River valley. The modern flood SWD are defined as sandy silt and silty sand in the upper reaches of Hanjiang River valley, whereas the modern flood SWD are defined as silt, sandy silt and clayey silt in the Weihe River valley. The modern flood SWD have different sediment sources and transporting forces. The modern flood SWD are sourced mainly from the Qinling and the Bashan bedrock mountains and the related residual deposits, slopewash and mud-rock flow deposits in the upper reaches of Hanjiang River valley. During rainstorms, torrential tributary rivers can bring much coarse deposits into the mainstream of the Hanjiang River. However, the sources of the modern flood SWD are the eolian loess and the related surface soil in the Weihe River valley. Comparative study shows different sedimentary features between the modern flood SWD in the upper reaches of Hanjiang River valley and that in the Weihe River valley. These results give insight into the different sediment sources and transporting force of the modern flood SWD, which provide a basic reference to mitigate flood disasters, and to soil and water conservation.