Assessing the permafrost temperature and thickness conditions favorable for the occurrence of gas hydrate in the Qinghai–Tibet Plateau

2010 ◽  
Vol 51 (4) ◽  
pp. 783-787 ◽  
Author(s):  
Wu Qingbai ◽  
Jiang Guanli ◽  
Zhang Peng
Keyword(s):  
Gas Hydrate ◽  
Tibet Plateau ◽  
Permafrost Temperature ◽  
Qinghai Tibet Plateau

The natural-gas hydrate exploration prospects of the Nayixiong Formation in the Kaixinling-Wuli Permafrost, Qinghai-Tibet Plateau

2016 ◽  
Vol 72 ◽  
pp. 179-192 ◽  
Author(s):  
Shengqian Liu ◽  
Zaixing Jiang ◽  
Hui Liu ◽  
Shouji Pang ◽  
Zhongyuan Xia ◽  
...  
Keyword(s):  
Natural Gas ◽  
Gas Hydrate ◽  
Tibet Plateau ◽  
Natural Gas Hydrate ◽  
Qinghai Tibet Plateau

scholarly journals A natural gas hydrate-oil-gas system in the Qilian Mountain permafrost area, northeast of Qinghai-Tibet Plateau

China Geology ◽  
2020 ◽  
Vol 3 (4) ◽  
pp. 511-523
Author(s):  
Zhen-quan Lu ◽  
◽  
Shi-qi Tang ◽  
Xiao-ling Luo ◽  
Gang-yi Zhai ◽  
...  
Keyword(s):  
Natural Gas ◽  
Gas Hydrate ◽  
Tibet Plateau ◽  
Qilian Mountain ◽  
Natural Gas Hydrate ◽  
Gas System ◽  
Mountain Permafrost ◽  
Qinghai Tibet Plateau ◽  
Oil Gas

scholarly journals Modeling on Gas Hydrate Formation Conditions in the Qinghai-Tibet Plateau Permafrost

2009 ◽  
Vol 52 (1) ◽  
pp. 202-213 ◽  
Author(s):  
Zhen-Quan LU ◽  
Nabil SULTAN ◽  
Chun-Shuang JIN ◽  
Zhu RAO ◽  
Xu-Rong LUO ◽  
...  
Keyword(s):  
Gas Hydrate ◽  
Hydrate Formation ◽  
Tibet Plateau ◽  
Gas Hydrate Formation ◽  
Formation Conditions ◽  
Qinghai Tibet Plateau

Rock Thermal Conductivity of Natural Gas Hydrate Deposits in the Muli Basin of Chinese Qinghai-Tibet Plateau

2013 ◽  
Vol 448-453 ◽  
pp. 1394-1398
Author(s):  
Bin Dou ◽  
Lei Ren ◽  
Hai Sheng Liu
Keyword(s):  
Thermal Conductivity ◽  
Gas Hydrate ◽  
Thermal Conditions ◽  
Tibet Plateau ◽  
Gas Recovery ◽  
Injection Technology ◽  
Heat Injection ◽  
Qinghai Tibet Plateau ◽  
Geological Formations ◽  
Rock Thermal Conductivity

This study reports laboratory measured thermal conductivity values of sandstones from 4 wells (predominantly hydrae exploration boreholes). The objective of the present work is to report the values of the thermal conductivity that were measured in the cores from the borehole that was estimated for the geological formations intercepted by it. The measurements were made on drill cores using the guarded parallel-plate apparatus at a temperature range from 285 to 290 K at Atmospheric pressure. Bulk thermal conductivities of sandstones corrected for in site thermal conditions range between 2.1 and 2.8 W/m/K. In general, the estimated uncertainty of the Effective thermal conductivity measurements is 2%. These data can be used for design of gas recovery form gas hydrate using heat injection technology.

scholarly journals Evidence of natural gas hydrate in Kunlun Pass basin, Qinghai-Tibet Plateau, China

2015 ◽  
Vol 60 (1) ◽  
pp. 68-74
Author(s):  
YuZhong YANG ◽  
YanDong HOU ◽  
BaoGui ZHANG ◽  
YouSheng DENG ◽  
GuanLi JIANG ◽  
...  
Keyword(s):  
Natural Gas ◽  
Gas Hydrate ◽  
Tibet Plateau ◽  
Natural Gas Hydrate ◽  
Qinghai Tibet Plateau

Numerical Simulation of the Change of Gas Hydrate Layer of Qinghai-Tibet Plateau in Global Warming Situation

2011 ◽  
Vol 335-336 ◽  
pp. 302-307
Author(s):  
Yan Chao Qiao ◽  
Zi Qi Guo ◽  
Bao Gang Zhang ◽  
Yao Lin Shi
Keyword(s):  
Global Warming ◽  
Surface Temperature ◽  
Gas Hydrate ◽  
Heat Conduction Equation ◽  
Ground Surface ◽  
Tibet Plateau ◽  
Ground Surface Temperature ◽  
Hydrate Layer ◽  
Major Factors ◽  
Qinghai Tibet Plateau

Using finite element method, we solve the heat conduction equation. In our calculation, we use 0.02 and 0.052 °C/year as temperature rising rate (Gt) in order to get the change of gas hydrate layer of Qinghai-Tibet Plateau (QTP) in global warming situation. Our calculation’s major results are as follows: Our calculation demonstrates the gas hydrate layer’s surface temperature is one of the major factors which influence the thickness of gas hydrate layer (TGH). When Gt=0.02 and 0.052°C/year, the changes of TGH are almost same. The lower the ground surface temperature (GST), the more change of TGH. Therefore we need to monitor the Qiangtang plateau which has low surface temperature and good organic material.

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