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大规模采沙后赣江河道外洲站断面冲淤变化分析
引用本文:邓坤,郭纯青,史小玲.大规模采沙后赣江河道外洲站断面冲淤变化分析[J].桂林工学院学报,2007,27(3):333-336.
作者姓名:邓坤  郭纯青  史小玲
作者单位:1. 桂林工学院,资源与环境工程系,广西,桂林,541004;南昌市水文局,南昌,330006
2. 桂林工学院,资源与环境工程系,广西,桂林,541004
3. 南昌市水文局,南昌,330006
摘    要:根据赣江外洲水文站近40年实测大断面资料和沙量资料,分析了大规模和无序河道采沙前后断面的冲淤变化情况,以及对各方面产生的影响.大规模采沙前,外洲河沙站断面变化幅度很小,河床变化不大,河势稳定;20世纪90年代中期大规模采沙以来,断面面积平均每年增大380 m2,河床平均每年下切0.26 m,河床严重变形.尽管河道加深,增强了输水能力,降低了洪水位,提高了防洪标准,但该河段的河势恶化,已影响到河势稳定和堤防安全.

关 键 词:河道  采沙  含沙量  大断面  河底高程  赣江  南昌
文章编号:1006-544X(2007)03-0333-04
修稿时间:2006-06-09

Analysis on Scour and Sedimention of Ganjiang Section at Waizhou Hydrologic Station by Large Scale Sand Extraction
DENG Kun,GUO Chun-qing,SHI Xiao-ling.Analysis on Scour and Sedimention of Ganjiang Section at Waizhou Hydrologic Station by Large Scale Sand Extraction[J].Journal of Guilin University of Technology,2007,27(3):333-336.
Authors:DENG Kun  GUO Chun-qing  SHI Xiao-ling
Affiliation:1. Department of Resources and Environmental Engineering, Guilin University of Technology, Guilin 541004, China; 2. Nanchang Hydrologic Office, Nanchang 330006, China
Abstract:According to nearly 40 year's sectional and sedimentary data of Waizhou hydrologic station,the riverbed and river regime kept stable before 1990;the area of the channel has developed by 380 m2,and the riverbed is downcut by 0.26 m every year since 1990s.Although the channel is deepened,with more supply of water,lower flood stage and higher flood-prevention standards,the riverbed is deteriorating which will influence the stability of the river regime and security of the dams.
Keywords:channel  sand extraction  sediment concentration  section  bed level of the river  Ganjiang River  Nanchang
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