地理学报 ›› 2014, Vol. 69 ›› Issue (3): 399-408.doi: 10.11821/dlxb201403011
王随继1, 李玲1,2
收稿日期:
2013-07-15
修回日期:
2013-12-20
出版日期:
2014-03-20
发布日期:
2014-06-10
作者简介:
王随继(1966- ),男,甘肃静宁人,博士,副研究员,中国地理学会会员(S110001472M),主要研究方向为河流沉积学、地貌学及流域地表过程。E-mail:wangsj@igsnrr.ac.cn
基金资助:
WANG Suiji1, LI Ling1,2
Received:
2013-07-15
Revised:
2013-12-20
Online:
2014-03-20
Published:
2014-06-10
Supported by:
摘要: 研究选取黄河银川平原全长196 km的河段,以1975 年、1990 年、2010 年和2011 年四个年份的卫星影像数据绘制的左右河岸线,与设立的平均间隔为1.3 km的153 个河道固定横断面的交点位置的变化,估算了1975-1990 年、1990-2010 年和2010-2011 年三个时期的河岸平均摆动速率。结果表明,该河段左岸以向右摆动为主,在上述时期左岸总的平均摆动速率分别为36.5 m/a、27.8 m/a 和61.5 m/a;右岸在1975-1990 年以向右摆动为主,此后则以向左摆动为主,其摆动速率分别为31.7 m/a、23.1 m/a 和50.8 m/a。在1975-2011 全部36 年间,左右河岸的年均摆动速率分别为22.3 m/a 和14.8 m/a。河岸摆动速率在A、B、C三个河段相差悬殊,在1975-2011 的36 年间,左岸向左和向右的平均摆动速率之比分别为1:7.6:4.6 和1:1.7:3.8;右岸向左和向右的平均摆动速率之比为1:1.8:1.2 和1:5.6:17.7。显然,无论左岸右岸,它们在A段的摆动速率最小,向左摆动速率最大的出现在B段,而向右摆动速率最大的则是C段。河岸摆动速率在时序上的增大现象主要受制于人类筑坝蓄水等引起汛期流量的逐渐减小,而空间变化主要受制于河岸物质组成的区域差异。
王随继, 李玲. 黄河银川平原段河岸摆动速率变化及原因[J]. 地理学报, 2014, 69(3): 399-408.
WANG Suiji, LI Ling. Lateral shift rate variation of the river banks in the Yinchuan Plain reach of the Yellow River and its causes[J]. Acta Geographica Sinica, 2014, 69(3): 399-408.
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