Remote Sensing Interpretation and early Warning System Designing of Geohazards along Transmission Lines - A Case Study of the Danba - Kangding 500 kV Double Circuit Transmission Line

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Abstract:

The landslide and debris flow investigation area for Danba ~ Kangding 500 kv double-circuit transmission line route selection is within Ganzi in Tibetan autonomous prefecture, with the area of about 440 km2. The topography, geomorphology, geologic structure, stratum lithology, natural factors, social and economic conditions have great influences on the transmission lines route selection and its construction. For comprehensive evaluation engineering rationality and construction convenience, remote sensing technology (RS) and geographic information system (GIS) technology are taken to implement geological environment survey. With field investigation, remote sensing images interpretation method is used to determine basic characteristics of the geo-hazards.

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Periodical:

Advanced Materials Research (Volumes 986-987)

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1647-1650

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July 2014

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© 2014 Trans Tech Publications Ltd. All Rights Reserved

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[1] Huang RQ, Li WL. A Study on the Development and Distribution Rules of Geo-hazards Triggered by 5. 12, Wenchuan Earthquake [J]. Science in China (Edition E), 2009a, 52(4): 810-819.

Google Scholar

[2] Huang RQ, Li WL. Analysis of the geo-hazards triggered by the 12 May Wenchuan Earthquake, China [J]. Bull of Engineering Geology and the Environment, 2009b, 68(2): 363–371.

DOI: 10.1007/s10064-009-0207-0

Google Scholar

[3] Huang RQ, Li WL. Research On Development And Distribution Rules Of Geohazards Induced By Wenchuan Earthquake On 12th[J]. Chinese Journal of Rock Mechanics and Engineering, 2008, 27(12): 2585-2592.

Google Scholar

[4] Huang RQ, Li WL. Fault effect analysis of geo-hazard triggered by wen-chaun earthquake [J]. Journal of Engineering Geology, 2009, 17(1): 19- 28.

Google Scholar

[5] Parker RN, Densmore A, Rosser NJ, Michele M, Li Y, Huang RQ, et al. Mass wasting triggered by the 2008 Wenchuan earthquake is greater than organics growth [J]. Nature Geoscience, 2011, 4 (2): 449–452.

DOI: 10.1038/ngeo1154

Google Scholar

[6] Tang C, Zhu J, Li WL. Rainfall triggered debris flows after Wenchuan earthquake [J]. Bull Eng Geol Environ, 2009, 68(4): 187–194.

DOI: 10.1007/s10064-009-0201-6

Google Scholar

[7] Tang C, Liang JT. Characteristics of debris flows in Beichuan epicenter of the Wenchuan earthquake triggered by rain storm on sep-tember[J]. Journal of Engineering Geology, 2008, 16(6): 751-758.

Google Scholar

[8] Xie H, Zhong DL, Zhang JS. Debris Flow in Wenchuan Quake-hit Area in 2008[J]. Journal of Mountain Science, 2009, 5(4): 501-509.

Google Scholar

[9] Chang M, Tang C, Fu R. Application of mike11 model in water diversion and flushing pollutants of urban river network in sihong city[J]. Water Resources and Power, 2012, 30(8): 103-106.

Google Scholar

[10] Feng HF, Zhang ZM, Qian JP. Disaster characteristics and countermeasures of Huili county, Sichuan geological[J]. The Chinese Journal of Geological Hazard and Control, 2007, 18(4): 111-114.

Google Scholar

[11] Xu Q, Liu HX. Large-scale shaking table test study of acceleration dynamic responses characteristics of slopes [J]. Chinese Journal of Rock Mechanics and Engineering, 2010, 29(12): 2420-2428.

Google Scholar

[12] Liu HX, Xu Q, Fan XM. Influence of ground motion intensity on dynamic response laws of slope accelerations [J]. Rock and Soil Mechanics, 2012, 3(5): 1357-1365.

Google Scholar