Factors influencing thermokarst lake development in Beiluhe basin, the Qinghai-Tibet Plateau

被引:11
作者
Wang, Huini [1 ]
Liu, Hongjia [2 ]
Ni, Wankui [3 ]
机构
[1] Wuhan Univ Technol, Intelligent Transport Syst Res Ctr, Engn Res Ctr Transportat Safety, Minist Educ,Natl Engn Res Ctr Water Transport Saf, 1040 Heping Ave, Wuhan 430063, Hubei, Peoples R China
[2] Jiujiang Univ, Sch Civil Engn & Urban Construct, 551 East Qianjin Rd, Jiujiang 332000, Peoples R China
[3] Changan Univ, Geol Engn & Survey Inst, Xian 710054, Shaanxi, Peoples R China
关键词
Frozen soil; Qinghai-Tibet Plateau; Sensitivity analysis; Thermokarst lake; RIVER-BASIN; PERMAFROST; HIGHWAY; RAILWAY;
D O I
10.1007/s12665-017-7143-2
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Thermokarst lake is a significant indicator of permafrost degradation. However, the evaluation of thermokarst lake development is very difficult through physical mechanism analysis because the development is influenced by many factors. In the present study, the factors influencing thermokarst lake development were investigated from the perspective of frozen soil and the geographical environment. The influences of six factors on thermokarst lake development in Beiluhe basin, located in the hinterland of the Qinghai-Tibet Plateau, were analyzed: permafrost type, ground temperature, vegetation type, soil type, hydrogeological type, and slope. Sensitivity coefficients were calculated for these factors using statistical methods. The results show that thermokarst lake development was influenced by the analyzed factors as follows: permafrost > soil type > ground temperature > hydrogeological type. Furthermore, 80.1% of the study area was highly sensitive to thermokarst lake development. Overall, thermokarst lake development in the Beiluhe basin was thoroughly evaluated based on sensitivity factors and an established statistical evaluation method. The method detailed in this paper provides a reference for evaluating the likelihood and severity of thermokarst lake development.
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页数:15
相关论文
共 32 条
[21]   Morphological characteristics of thermokarst lakes along the Qinghai-Tibet engineering corridor [J].
Niu, Fujun ;
Luo, Jing ;
Lin, Zhanju ;
Liu, Minhao ;
Yin, Guoan .
ARCTIC ANTARCTIC AND ALPINE RESEARCH, 2014, 46 (04) :963-974
[22]   Characteristics of thermokarst lakes and their influence on permafrost in Qinghai-Tibet Plateau [J].
Niu, Fujun ;
Lin, Zhanju ;
Liu, Hua ;
Lu, Jiahao .
GEOMORPHOLOGY, 2011, 132 (3-4) :222-233
[23]   Disappearing Arctic lakes [J].
Smith, LC ;
Sheng, Y ;
MacDonald, GM ;
Hinzman, LD .
SCIENCE, 2005, 308 (5727) :1429-1429
[24]   Thermokarst lakes as a source of atmospheric CH4 during the last deglaciation [J].
Walter, K. M. ;
Edwards, M. E. ;
Grosse, G. ;
Zimov, S. A. ;
Chapin, F. S., III .
SCIENCE, 2007, 318 (5850) :633-636
[25]   Impacts of permafrost changes on alpine ecosystem in Qinghai-Tibet Plateau [J].
Wang Genxu ;
Li Yuanshou ;
Wu Qingbai ;
Wang Yibo .
SCIENCE IN CHINA SERIES D-EARTH SCIENCES, 2006, 49 (11) :1156-1169
[26]  
Wang SL, 2000, PERMAFROST PERIGLAC, V11, P43, DOI 10.1002/(SICI)1099-1530(200001/03)11:1<43::AID-PPP332>3.0.CO
[27]  
2-H
[28]   Ground temperature monitoring and its recent change in Qinghai-Tibet Plateau [J].
Wu, QB ;
Liu, YZ .
COLD REGIONS SCIENCE AND TECHNOLOGY, 2004, 38 (2-3) :85-92
[29]   A review of recent frozen soil engineering in permafrost regions along Qinghai-Tibet Highway, China [J].
Wu, QB ;
Liu, YZ ;
Zhang, JM ;
Tong, CJ .
PERMAFROST AND PERIGLACIAL PROCESSES, 2002, 13 (03) :199-205
[30]   Permafrost temperatures and thickness on the Qinghai-Tibet Plateau [J].
Wu, Qingbai ;
Zhang, Tingjun ;
Liu, Yongzhi .
GLOBAL AND PLANETARY CHANGE, 2010, 72 (1-2) :32-38