[1]李志威,王兆印,余国安,等.雅鲁藏布大峡谷水电开发对边坡稳定性的影响[J].山地学报,2015,(03):331.
 LI Zhiwei,WANG Zhaoyin,YU Guoan,et al.Effects on Slope Stability of the Yarlung Tsangbu Grand Canyon under Future Hydropower Development[J].Mountain Research,2015,(03):331.
点击复制

雅鲁藏布大峡谷水电开发对边坡稳定性的影响()
分享到:

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2015年03期
页码:
331
栏目:
山地灾害
出版日期:
2015-06-01

文章信息/Info

Title:
Effects on Slope Stability of the Yarlung Tsangbu Grand Canyon under Future Hydropower Development
作者:
李志威;王兆印;余国安;王旭昭;张晨笛;
清华大学水沙科学与水利水电工程国家重点实验室;中国科学院地理科学与资源研究所;北京矿产地质研究院;
Author(s):
LI Zhiwei WANG Zhaoyin YU Guoan WANG Xuzhao ZHANG Chendi
1. State Key Laboratory of Hydroscience and Engineering, Tsinghua University, Beijing 100084, China; 2. Institute of Geographic Science and Natural Resources Research, Chinese Academy of Science, Beijing 100101, China; 3. Beijing Institute of Geology for Mineral Resource, Beijing 100012, China
关键词:
雅鲁藏布大峡谷水电开发边坡稳定性河床结构消能
Keywords:
Yarlung Tsangbu Grand Canyon hydropower development slope stability river bed structure energy expenditure
分类号:
P642,TV213.2,X141
文献标志码:
A
摘要:
雅鲁藏布大峡谷蕴藏着十分丰富的水能资源,未来水电开发对满足国内能源需求和应对气候变暖都具有重要的战略意义,但可能对其边坡稳定性产生不利影响。野外调查发现,基岩河床下切促使大峡谷内崩塌、滑坡、泥石流等地质灾害频繁发生,大峡谷内巨大水流能量与河床结构消能保持微弱的临界平衡状况,河床结构(瀑布和阶梯深潭系统)的消能作用对维持边坡稳定性起至关重要作用。针对梯级高坝和引水隧洞的两种水电开发方案分析表明,两种方案对边坡稳定性均会产生不利影响,且前一种方案的影响更强烈。只有充分认识未来水电开发对大峡谷边坡的影响,才能将水电工程的不利影响减少到最小。
Abstract:
Yarlung Tsangbo Grand Canyon in southeastern Tibet of China possesses very abundant hydropower resources, where future hydropower development is of strategic importance to meet domestic energy demand and response climate warming, but may adversely affect the slope stability of the canyon. Field investigations indicate that bedrock incision of river bed prompted too many avalanches, landslides and debris flow occurring frequently in the canyon. The interaction between huge flow energy and riverbed structures (e.g. cascades and steppool system) maintains the weak critical balance to hold the stability of the canyon. Two hydropower development schemes which include several steps hydropower plants and long distance diversion tunnels may have direct adverse effects on the canyon stability. Only fully understanding the impact of future hydropower development on the slope stability of the canyon, the adverse effects of the hydropower projects can be reduced to a minimum.

参考文献/References:

[1] Yang Yichou, Gao Dengyi, Li Bosheng. A great geographical discovery in the end of 20th century-Demonstration on the Yarlung Zangbo River valley as the grandest canyon in the world[J]. Geographical Research, 1996, 15(4): 1-9[杨逸畴, 高登义, 李渤生. 20世纪末的一次重大地理发现-雅鲁藏布大峡谷为世界之最的论证[J].地理研究, 1996, 15(4): 1-9]
[2] Guan Zhihua. The water resources exploration of Yarlung Zangbo Grand Canyon, Chinese Water Resources, 1996 , (4): 41-43 [关志华. 雅鲁藏布大峡谷水资源探秘[J].中国水利, 1996, (4): 41-43]
[3] Xu Damao, Chen Chuanyou, Liang Weiyan. Hydropower development at the Yalu Tsangpo River[J]. Engineering Science, 2002, 4(12): 47-52 [徐大懋, 陈传友, 梁维燕. 雅鲁藏布江水电开发[J].中国工程科学, 2002, 4(12): 47-52]
[4] Dai Qinzhong, Yu Xiaobo, Yu Kun. Low carbon economy thrived and expanding industrial situation: Chinese hydropower assumes the task of clean energy[J]. Oriental Motor, 2010, (6): 1-22 [戴庆忠, 余小波, 吕坤. 低碳经济风生水起, 产业拓展审时度势-担纲清洁能源的中国水电[J].东方电机, 2010, (6): 1-22]
[5] Ding Ling, Zhong Dalai, Pan Yusheng, et al. FT evidence for rapid uplift since Pliocene from the east Himalayas[J]. Chinese Science Bulletin, 1995,40(16): 1497-1500 [丁林,钟大赉,潘裕生,等.东喜马拉雅构造结上新世以来快速抬升的裂变径迹证据[J].科学通报, 1995,40(16): 1497-1500]
[6] Yang Yichou. The topographic features and the origin of the great bendvalley at the Yarlung Zangbo River in Tibet[J]. Geographical Research, 1982, 1(1):40-48 [杨逸畴. 雅鲁藏布江大拐弯峡谷的地貌特征和成因[J].地理研究, 1982, 1(1):40-48]
[7] Ji Jianqing, Zhong Dalai, Ding Lin, et al. Genesis and scientific significance of the Yarlung Zangbo Canyon[J]. Earth Science frontiers( China University of Geosciences, Beijing), 1999, 6(4): 231-235 [季建清, 钟大赉, 丁林, 等. 雅鲁藏布大峡谷的地质成因[J].地学科缘, 1999, 6(4): 231-235]
[8] Wang Erchie, Chen Lianzhong, Chen Zhiliang. Tectonic and climatic elementcontrolled evolution of the Yalung Zangbu River in southern Tibet[J]. Quaternary Sciences, 2002, 22(4): 365-373 [王二七, 陈良忠, 陈智樑. 在构造和气候因素制约下的雅鲁藏布江的演化[J].第四纪研究, 2002, 22(4): 365-373]
[9] Chen Jianjun,Ji Jianqing,Gong Junfeng. Formation of the Yarlung Zangbo Grand Canyon,Tibet,China[J].Geological Bulletin of China,2008,27(4):491-499 [陈建军, 季建清, 龚俊峰, 等. 雅鲁藏布大峡谷的形成[J].地质通报,2008,27(4):491-499]
[10] Gao Dengyi. Expeditionary studies on the moisture passage of the Yarlung Zangbo River[J]. Journal of Nature, 2008, 30(5): 301-303 [高登义. 雅鲁藏布江水汽通道考察研究[J].自然杂志, 2008, 30(5): 301-303]
[11] Lei Yongliang, Zhong Dalai, Ji Jianqing, et al. Fission Track evidence for two Pleistocene upliftexhumation events in the eastern Himalayan Syntaxis[J]. Quaternary Sciences, 2008, 28(4): 584-590 [雷永良, 钟大赉, 季建清, 等. 东喜马拉雅构造结更新世两期抬升-剥露事件的裂变径迹证据[J].第四纪研究, 2008, 28(4): 584-590]
[12] Yu Xiangjing, Ji Jianqing, Gong Junfeng, et al. Evidences of rapid erosion driven by climate in the Yarlung Zangbo Great Canyon, the eastern Himalayan syntaxis[J]. Chinese Science Bulletin, 2011, 56(10): 765-773[于祥江, 季建清, 龚俊峰, 等.雅鲁藏布大峡谷气候因素引起地壳剥蚀冷却的证据[J].科学通报, 2011, 56(10): 765-773]
[13] Gong Junfeng, Ji Jianqing, Chen Jianjun, et al. 40Ar/39Ar geochronology studies of rocks in eastern Himalaya syntaxis [J].Acta Petrologica Sinica,2008,24(10): 2255-2272. [龚俊峰, 季建清, 陈建军, 等. 东喜马拉雅构造结岩体冷却的40Ar/3 9Ar年代学研究[J].岩石学报, 2008, 24(10): 2255-2272]
[14] Shang Yanjun, Yang Zhifa, Liao Qiulin, et al. Geological hazard distribution and prevention in North of Yalu Canyon, Tibet[J]. The Chinese Journal of Geological Hazard and Control, 2001, 12(4): 30-40[尚彦军, 杨志法, 廖秋林, 等. 雅鲁藏布江大拐弯北段地质灾害分布规律与防治对策[J].中国地质灾害与防治学报, 2001, 12(4): 30-40]
[15] Jiang ZhongXin. Differential distribution regularity of collapselandslides and debris flows along Palong Zangbu River valley in Tibet[J]. Geographical Research, 2002, 21(4): 495-463 [蒋忠信. 西藏帕隆藏布河谷崩塌滑坡、泥石流的分布规律[J].地理研究, 2002, 21(4): 495-463]
[16] Liu Yuping, Montgomery D R, Hallet B, et al. Quaternary glacier blocking events at the entrance of Yarlung Zangbo Great Canyon, Southeast Tibet[J].Quaternary Sciences, 2006, 26(1): 52-62 [刘宇平, Montgomery D R, Hallet B, 等. 西藏东南雅鲁藏布大峡谷入口处第四纪多次冰川阻江事件[J].第四纪研究, 2006, 26(1): 52-62]
[17] Lv Jietang, Wang, Zhihua, Zhou Chenghu. Discussion on the occurrence of Yigong landslide in Tibet[J]. Earth Science-Journal of China University of Geosciences, 2003, 28(1): 107-110 [吕杰堂, 王治华, 周成虎.西藏易贡大滑坡成因探讨[J]. 地球科学, 2003, 28(1): 107-110]
[18] Stewart R J, Hallet B, Zeitler P K, et al Brahmaputra sediment flux dominated by highly localized rapid erosion from the easternmost Himalaya [J]. Geology, 2008, 36(9): 711-714
[19] Korup O, Montgomery D R. Tibetan plateau river incision inhibited by glacial stabilization of the Tsangpo gorge [J]. Nature, 2008, 456: 786-789
[20] Korup O, Montgomery D R, Hewitt K. Glacier and landslide feedbacks to topographic relief in the Himalayan syntaxes [J]. PANS, 2010, 107: 5317-5322
[21] Jia Jingsheng, Ma Jing, Zhang Zhihui. Vigorously develop hydropower to response climate change [J]. Chinese Hydropower and Electrification, 2010, 1(2): 8-12 [贾金生, 马静, 张志会.应对气候变化必须大力发展水电[J].中国水能及电气化, 2010, 1(2): 8-12]
[22] Chen Fei. Innovation and scientific development of China hydropower[J]. Journal of Hydroelectric Engineering, 2011, 30(4): 1-5[陈飞. 解放思想,推动中国水电事业科学发展[J].水力发电学报, 2011, 30(4): 1-5]
[23] National Bureau of Statistics of People's Republic of China. China Statistical Year Book, 1990—2013[R][中华人民共和国国家统计局. 中国统计年鉴 [R]. 1990—2013]
[24] Yang Yichou. The discovery of Yalu Zangbo Great Canyon and the researches on its characteristics and the cause of its formation[J].Geographical Research, 1999, 18(4): 342-348[杨逸畴.雅鲁藏布大峡谷河床瀑布的发现及其特征和成因[J]. 地理研究, 1999, 18(4): 342-348]
[25] Abrahams A D, Li G, Atkinson J F. Steppool stream: adjustment to maximum flow resistance[J].Water Resources Research, 1995, 10: 2593-2602
[26] Wang Zhaoyin,Xu Jiang,Li Changzhi.Development of steppool sequence and its effects in resistance and stream bed stability[J]. International Journal of Sediment Research,2004,19(5):161-171
[27] Yu Guoan, Wang Zhaoyin, Liu Le, et al. Drainage network and fluvial morphology features of Yarlung Tsangpo River under the impact of neotectonic movement[J]. Advances in Water Science 2012, 23(2): 163-169 [余国安, 王兆印, 刘乐, 等. 新构造运动影响下的雅鲁藏布江水系发育和河流地貌特征[J].水科学进展, 2012, 23(2): 163-169]
[28] Zhang Wenjing, Yang Yichou. A new discoverythe great Polungtsangpo Canyon[J]. Mountain Research, 1999, 17(2): 97-98 [杨文敬, 杨逸畴. 青藏高原考察新发现—帕隆藏布大峡谷[J].山地学报, 1999, 17(2): 97-98]

备注/Memo

备注/Memo:
收稿日期(Received date):2014-03-03;改回日期(Accepted):2014-04-11。
基金项目(Foundation item):水洲科学与水利水电工程国家重点实验室项目(No.SKLHSE-2010-KY-01);科技部国际科技合作计划资助项目(No.2011DFG93160);清华大学自主科研课题(No.20121080027)。[Profect of state kdy Laboratory of Hydroscience and Engineering(No.SKLHSE-2014-KY-01);International Science & Technology Cooperation Program of China (No. 2011DFA20820), Tsinghua University (No. 20121080027). ]
作者简介(Biography):李志威(1984- ),男,湖北云梦人,博士,主要从事河流动力学研究。[Li Zhiwei(19840 ), male, doctor,mainly study on river dynamics.] E - mail:lizw@mail.tsinghua.edu.cn *
通信作者(Corresponding author):王兆印(1951- ),男,教授,主要从事河流动力学研究。[ Wang Zhaoyin(1951- ),male, professor, specialized in river dynamics. ] E - mail:zywang@mail.tsinghua.edu.cn
更新日期/Last Update: 1900-01-01