首页|1987-2022年黄河银川平原段河道演变特征及影响因素

1987-2022年黄河银川平原段河道演变特征及影响因素

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研究黄河银川平原段河道的演变特征,对河道的保护提供理论依据.文中基于1987-2022年8期Landsat卫星影像,利用修正的归一化水体指数对黄河河道进行提取,计算不同时期的河道宽度、河道面积、摆动幅度以及摆动速率,分析35年间黄河银川平原段的摆动特征及变化规律.结果表明:35年间,河道宽度平均减小0.36km,河段面积平均减小0.66km2.河道左岸平均每年向右摆动0.10km,R1、R2、R3河段左岸向左向右的摆动速率之比分别为1∶2.12∶2.53和1∶4.19∶5.33;河道右岸平均每年向右摆动0.004km,R1、RR2、R3段河道右岸向左向右平均摆动速率之比分别为1∶0.82∶2.16和1∶1.90∶3.19.河道整体呈萎缩趋势且向右偏移,黄河银川平原段下游摆动变化程度更为严重.河道在时间上的变化可能与自然因素与人类筑坝蓄水等人类活动相关,在空间上的变化可能受制于河道径流及河岸物质组成的差异.对于黄河银川平原河段,防护建设应重点关注在下游河段.
Evolution characteristics of the river course within Yinchuan Plain section of the Yellow River,from 1987 to 2022
To provide theoretical basis for the protection of the river channel,we study the evolution characteristics of the river channel in the Yinchuan Plain section of the Yellow River.Based on the Landsat satellite images of 8 periods from 1987 to 2022,the channel of the Yellow River is extracted by using the modified normalized water body index,the channel width,channel area,oscillation amplitude and oscillation rate in different periods are calculated,and the oscillation characteristics and the change rule of the Yellow River Yinchuan Plain section during 35 years are analyzed.The results show that the channel width decreased by 0.36 km on average,and the section area decreased by 0.66km2 on average during 35 years.The left bank of the river swings 0.10km to the right every year on average.As to the left bank swing rate,the ratio of the section R1∶R2∶R3 for left bank swinging to left is 1∶2.12∶2.53,and that for the left bank swinging to right is 1∶4.19∶5.33.The right bank of the river swings 0.004km to the right every year on average,and as to the right bank swing rate,the ratio of the section R1∶R2∶R3 for right bank swinging to left is 1:2.12:2.53,and that for the right bank swinging to right is 1∶4.19∶5.33.The river channel as a whole shows a trend of shrinkage and shifts to the right,and the degree of swinging change in the downstream of the Yinchuan plain section of the Yellow River is even more serious.The temporal changes of the river channel may be related to natural factors and human activities such as damming and impoundment,while the spatial changes may be limited by the differences in river runoff and riparian material composition.For the Yinchuan Plain section of the Yellow River,the protection construction should focus on the downstream reach.

river bankchannel swingembankment protection

张伊婧、璩向宁、王磊、王筱平、谭鹏

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宁夏大学生态环境学院,银川 750021

宁夏大学/西北土地退化与生态系统恢复国家重点实验室培育基地,银川 750021

宁夏大学/西北退化生态系统恢复与重建教育部重点实验室,银川 750021

宁夏黄河湿地生态系统国家定位观测研究站,银川 750011

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河岸 河道摆动 堤岸防护 黄河

宁夏重点研发计划项目

2021BEG02013

2024

干旱区资源与环境
中国自然资源学会干旱半干旱地区研究委员会 内蒙古农业大学

干旱区资源与环境

CSSCICHSSCD北大核心
影响因子:1.492
ISSN:1003-7578
年,卷(期):2024.38(3)
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