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Erschienen in: Environmental Earth Sciences 6/2017

01.03.2017 | Thematic Issue

Geothermal resources in Tibet of China: current status and prospective development

verfasst von: Siqi Wang, Chuan Lu, Dawa Nan, Xiancai Hu, Jingli Shao

Erschienen in: Environmental Earth Sciences | Ausgabe 6/2017

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Abstract

Tibet boasts many huge geothermal reserves and resource exploitation potential. However, as the geothermal resource is relatively scattered, it is hard to be exploited. The scope of work includes assessments of geothermal and ground water storage capacity, and the amount of exploitable heat and water and the fluid quality are evaluated in separate geothermal districts (fields) on the basis of the former investigation on geothermal wells, springs and geothermal field. Considering the low degree of general survey in Tibet and less information available, the amount of geothermal water in Tibet is calculated by natural heat flux method (SPA). The exploited amount of geothermal fluid (SPA) in Tibet mountainous area is 7.65 × 107 m3/a, and the exploitable geothermal resources (SPA) are 1700.77 × 1013 J/a, equivalent to 51.1 × 104 T of standard coal. A single interception of natural heat flow (SPA) shows that there is a huge potential for the development and utilization of geothermal resources in Tibet mountainous areas. Hot dry rock resources evaluation is conducted as well. Statistics show that this region’s base temperature is greater than 150 °C, and 19 zones are found with surface thermal fluid above boiling point. It is calculated that the thermal reserve 3–5 km below amounts to 145,367.93 × 1015 J, equivalent to 49.68 × 108 tons of standard coal. In south Tibet, the currently developed and utilized geothermal resources are mainly from Yangbajing thermal field. Early exploited amount of shallow geothermal resources amounts to 1512 t/h. Other geothermal active areas are basically unexploited. In middle Tibet, the geothermal active zones are still in natural forms without any exploitation. The total amount of geothermal liquid resources in north Tibet is 8.3 × 104 m3/a. East Tibet area’s geothermal resources are basically unexploited. The total amount of geothermal liquid resources is 3.77 × 105 m3/a. According to the results of geothermal resources evaluation in each area of Tibet, most geothermal active zones are in their natural state and not utilized, and are exploitation zones with high potential, especially in south and east Tibet uplifted zones.

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Literatur
Zurück zum Zitat China Geological Survey (2014) The geothermal resource investigation and evaluation division technical requirements. Internal report China Geological Survey (2014) The geothermal resource investigation and evaluation division technical requirements. Internal report
Zurück zum Zitat Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1984) Report on geothermal field resources of shallow geothermal reservoir of Yangbajing in Dangxiong County, Tibet Autonomous Region Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1984) Report on geothermal field resources of shallow geothermal reservoir of Yangbajing in Dangxiong County, Tibet Autonomous Region
Zurück zum Zitat Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1987) Geological report on detailed inspection on Naqu geothermal field in Naqu County, Tibet Autonomous Region Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1987) Geological report on detailed inspection on Naqu geothermal field in Naqu County, Tibet Autonomous Region
Zurück zum Zitat Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1991) Geothermal resource regionalisation in Tibet Autonomous Region. Internal report Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1991) Geothermal resource regionalisation in Tibet Autonomous Region. Internal report
Zurück zum Zitat Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1995a) Geological report on general inspection on gothermal resources of North Yangbajing geothermal field in Dangxiong County, Tibet Autonomous Region Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1995a) Geological report on general inspection on gothermal resources of North Yangbajing geothermal field in Dangxiong County, Tibet Autonomous Region
Zurück zum Zitat Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1995b) Hydrogeological report on general inspection on geochemistry study of high temperature thermal fluid in Tibet Autonomous Region Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (1995b) Hydrogeological report on general inspection on geochemistry study of high temperature thermal fluid in Tibet Autonomous Region
Zurück zum Zitat Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (2015) Tibetan geothermal resources evaluation and regionalisation research report Geothermal and Geological Institute, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau (2015) Tibetan geothermal resources evaluation and regionalisation research report
Zurück zum Zitat Institute of Geochemistry, Chinese Academy of Sciences, Guiyang (1977) Concise geochemical manual. Science Press Institute of Geochemistry, Chinese Academy of Sciences, Guiyang (1977) Concise geochemical manual. Science Press
Zurück zum Zitat Jin C, Zhou Y (1978) The magmatic rock zone in Himalayan mountains and Gangdise arc mountains and the genetic models. Geol Sci 13(4):297–312 Jin C, Zhou Y (1978) The magmatic rock zone in Himalayan mountains and Gangdise arc mountains and the genetic models. Geol Sci 13(4):297–312
Zurück zum Zitat Liao Z (1988) Yunnan–Burma–Thailand tectonic domain and special cenozoic volcanic activity. J Peking Univ (Nat Sci Edn)(4):111–120 Liao Z (1988) Yunnan–Burma–Thailand tectonic domain and special cenozoic volcanic activity. J Peking Univ (Nat Sci Edn)(4):111–120
Zurück zum Zitat Liao Z, Zhao P (1999) Yunnan-Tibet geothermal belt: geothermal resources and typical geothermal system. Science Press, Beijing Liao Z, Zhao P (1999) Yunnan-Tibet geothermal belt: geothermal resources and typical geothermal system. Science Press, Beijing
Zurück zum Zitat Lin W, Liu Z, Wang W, Wang G (2013) Geothermal resources and potential evaluation in China. Geol China 40(1):312–321 Lin W, Liu Z, Wang W, Wang G (2013) Geothermal resources and potential evaluation in China. Geol China 40(1):312–321
Zurück zum Zitat Liu Y, Wang Q, Wu C (1977) Crustal structure and geological significance in the central region of Himalayan mountains. Chin J Geophys 20:143–149 Liu Y, Wang Q, Wu C (1977) Crustal structure and geological significance in the central region of Himalayan mountains. Chin J Geophys 20:143–149
Zurück zum Zitat Pan Y, Wang Y, Chang C (1980) Evidence of Himalayan tectonic activity and Qinghai–Tibet plateau formation model. Seismol Geol 2:1–10 Pan Y, Wang Y, Chang C (1980) Evidence of Himalayan tectonic activity and Qinghai–Tibet plateau formation model. Seismol Geol 2:1–10
Zurück zum Zitat Sandong Z, Wang D (1980) The seismic activity around the Himalayas. Seism Geol Transl (2):3–8 Sandong Z, Wang D (1980) The seismic activity around the Himalayas. Seism Geol Transl (2):3–8
Zurück zum Zitat The Geological and Mineral of the People’s Republic of China (1985) Method for geothermal resource assessment The Geological and Mineral of the People’s Republic of China (1985) Method for geothermal resource assessment
Zurück zum Zitat The Tibet Autonomous Region Geological Survey Institute (2009) Geothermal resource evaluation and regionalization in Tibet The Tibet Autonomous Region Geological Survey Institute (2009) Geothermal resource evaluation and regionalization in Tibet
Zurück zum Zitat Tian T, Li M, Bai Y (2006) Geothermal resources development and utilization in China. China Environmental Science Press, Beijing Tian T, Li M, Bai Y (2006) Geothermal resources development and utilization in China. China Environmental Science Press, Beijing
Zurück zum Zitat Toksöz MN, Bird P (1977) Modelling of temperatures in continental convergence zones. Tectonophysics 41:181–193CrossRef Toksöz MN, Bird P (1977) Modelling of temperatures in continental convergence zones. Tectonophysics 41:181–193CrossRef
Zurück zum Zitat Tong W, Zhang M, Zhang Z (1981) Geothermal in Tibet. Science Press, Beijing Tong W, Zhang M, Zhang Z (1981) Geothermal in Tibet. Science Press, Beijing
Zurück zum Zitat Wei W et al (1997) Magnetotelluric deep exploration of the Tibetan plateau—crust–mantle electrical structure in Yadong–Bamucuo area. Modern Geol 11(3):366–374 Wei W et al (1997) Magnetotelluric deep exploration of the Tibetan plateau—crust–mantle electrical structure in Yadong–Bamucuo area. Modern Geol 11(3):366–374
Zurück zum Zitat Xu Z, Yang J, Li H, Ji S, Zhang Z, Liu Y (2011) On the tectonics of the India–Asia collision. Acta Geol Sin 1:1–33 Xu Z, Yang J, Li H, Ji S, Zhang Z, Liu Y (2011) On the tectonics of the India–Asia collision. Acta Geol Sin 1:1–33
Zurück zum Zitat Xu Z et al (2013) Three dimensional extrusion model of high Himalaya. Geol China 40(3):671–680 Xu Z et al (2013) Three dimensional extrusion model of high Himalaya. Geol China 40(3):671–680
Zurück zum Zitat Zhang Z, Li L (2005) China groundwater resources (Tibet part). China Cartographic Publishing House, Beijing Zhang Z, Li L (2005) China groundwater resources (Tibet part). China Cartographic Publishing House, Beijing
Zurück zum Zitat Zhang X, Teng J, Sun R, Romanelli F, Zhang Z, Panza GF (2014) Structural model of the lithosphere–asthenosphere system beneath the Qinghai–Tibet plateau and its adjacent areas. Tectonophysics 634:208–226. doi:10.1016/j.tecto.2014.08.017 CrossRef Zhang X, Teng J, Sun R, Romanelli F, Zhang Z, Panza GF (2014) Structural model of the lithosphere–asthenosphere system beneath the Qinghai–Tibet plateau and its adjacent areas. Tectonophysics 634:208–226. doi:10.​1016/​j.​tecto.​2014.​08.​017 CrossRef
Metadaten
Titel
Geothermal resources in Tibet of China: current status and prospective development
verfasst von
Siqi Wang
Chuan Lu
Dawa Nan
Xiancai Hu
Jingli Shao
Publikationsdatum
01.03.2017
Verlag
Springer Berlin Heidelberg
Erschienen in
Environmental Earth Sciences / Ausgabe 6/2017
Print ISSN: 1866-6280
Elektronische ISSN: 1866-6299
DOI
https://doi.org/10.1007/s12665-017-6464-5

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