EN中文

SCIENTIA GEOGRAPHICA SINICA >

2007 , Vol. 27 >Issue 5: 701 - 706

DOI: https://doi.org/10.13249/j.cnki.sgs.2007.05.701

GIS-based Analysis on Evolutional Process and Stability of Meimaosha Shoal in the Changjiang River Estuary

Expand
  • 1. Tianjin Research Institute of Water Transport Engineering Key Laboratory of Engineening Sediment of Ministry of Communications, Tianjin Research Institute of Water Transport Engineering, Tianjin 300456;
    2. State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062;
    3. The Second Institute of Oceanography, Hangzhou, Zhejiang 310012

Received date: 2006-04-13

  Revised date: 2006-08-11

  Online published: 2007-09-20

Fold

Abstract

Making clear the evolutional process of Meimaosha shoal in the Changjiang(Yangtze) River estuary can provide scientific basis for the construction of a reservoir between the sand ridge and the river bank.Supported by GIS software,15 pieces of charts of the Meimaosha shoal of the South Passage of the Changjiang River etuary were studied.The formation history and evolutional process of the Meimaosha shoal were discussed by the multi-methods.The results showed that,the form and growth of the Meimaosha shoal had undergone three phases which are erosion of local beach,growth of spit and form of sand ridge;the Meimaosha shoal had the character of tidal sand ridge as its middle axes had taken on a good stability along northwest to southeast under the action of steady and driving flood and ebb tides in the passed half century.After 1959,the deposition and erosion of sediment changed very slightly.The volume of 0m sand body change basic invariable,sand body of-2m had been slightly washed out with the erosion rate of 0.07?106m3/a,reflecting the Meimaosha shoal stability is quite good.

Cite this article

ZUO Shu-Hua, LI Jiu-Fa, SHI Lian-Qiang, YING Ming, XU Hai-Gen . GIS-based Analysis on Evolutional Process and Stability of Meimaosha Shoal in the Changjiang River Estuary[J]. SCIENTIA GEOGRAPHICA SINICA, 2007 , 27(5) : 701 -706 . DOI: 10.13249/j.cnki.sgs.2007.05.701

References

[1] 陈吉余,曹勇,刘杰.长江河口淡水资源开发的一个新思路[J].国土资源科技管理,2004,(6):5～8.
[2] 黄胜.长江河口演变特征[J].泥沙研究,1986,(4):1～12.
[3] 陈吉余,沈焕庭,恽才兴,等.长江河口动力过程和地貌演变[M].上海:上海科学技术出版社,1988.
[4] 巩彩兰,恽才兴.应用地理信息系统研究长江口南港底沙运动规律[J].水利学报,2002,4(4):18～22.
[5] 吴华林,沈焕庭,胡辉,等.GIS支持下的长江口拦门沙泥沙冲淤定量计算[J].海洋学报,2002,24(2):84～92.
[6] 张莉莉,李九发,吴华林,等.长江河口拦门沙冲淤变化过程研究[J].华东师范大学学报(自然科学版),2002,(2):73～80.
[7] 薛元忠,何青,李茂田,等.长江口新浏河沙冲淤变化监测及定量分析[J].泥沙研究,2004,(5):56～60.
[8] 吴华林,沈焕庭,茅志昌.长江口南北港泥沙冲淤定量分析及河道演变[J].泥沙研究,2004,(3):75～80.
[9] 李鹏,杨世伦,杜景龙,等.长江口外高桥新港区岸段河槽冲淤GIS分析[J].地理与地理信息科学,2005,21(4):24～27.
[10] 刘权.GIS在河流洪泛区灾害监测中应用研究[J].地理科学,2002,22(6):712～716.
[11] 左书华,李九发,应铭,等.没冒沙水域水沙运动特性及筑库工程对其影响[J].华东师范大学学报(自然科学版),2006,(2):41～48.
[12] 陈述彭,鲁学军,周成虎.地理信息系统导论[M].北京:科学出版社,2000.
[13] 黄杏元,马劲松,汤勤.地理信息系统概论[M].北京:高等教育出版社,2001.
[14] 钱乐样,许叔明,秦奋,等.GIS支持的土壤贫瘠化区域分异研究--以福建为例[J].地理科学,2002,22(1):85～90.
[15] 唐川,朱大奎.基于GIS技术的泥石流风险评价研究[J].地理科学,2002,22(3):300～304.
[16] 范月娇.基于遥感和GIS一体化技术的三峡库区土地利用变化研究[J].地理科学,2002,22(5):593～597.
[17] 汪爱华,张树清,何艳芬.RS和GIS支持下的三江平原沼泽湿地动态变化研究[J].地理科学,2002,22(5):636～641.
[18] 王亚强,王兰民,张小曳.GIS支持下的黄土高原地震滑坡区划研究[J].地理科学,2004,24(2):170～176.
[19] 师长兴.黄河河口延伸与下游淤积关系研究中的问题分[J].地理科学,2005,25(2):183～189.
[20] 第宝锋,杨忠,艾南山,等.基于RS与GIS的金沙江干热河谷区退化生态系统评价--以云南省元谋县为例[J].地理科学,2005,25(4):484～489.
[21] 尹海伟,徐建刚,陈昌勇,等.基于GIS的吴江东部地区生态敏感性分析[J].地理科学,2006,26(1):64～69.
[22] 黎坤,曾彩华,江涛,等.前山河水力排污冲淤联合调度试验及效果分析[J].地理科学,2006,26(1):101～107.
[23] 杨世伦,杜景龙,郜昂,等.近半个世纪长江口九段沙湿地的冲淤演变[J].地理科学,2006,26(3):335～339.
[24] 许炯心.人类活动和降水变化对嘉陵江流域侵蚀产沙的影响[J].地理科学,2006,26(4):432～437.
[25] 陈宁生,张飞.2003年中国西南山区典型灾害性暴雨泥石流运动堆积特征[J].地理科学,2006,26(6):701～705.
[26] 贾铁飞,戴雪荣,张卫国,等.全新世巢湖沉积记录及其环境变化意义[J].地理科学,2006,26(6):706～711.
[27] 杨世伦,贺松林,谢文辉.长江口九段沙的形成演变及其与南北槽发育的关系[J].海洋工程,1998,16(4):55～64.
Options
Outlines

/

〈 〉