Experimental Investigation of Gas Hydrate Dissociation in Qilian Mountain Permafrost, Qinghai-Tibet Plateau, China

2015 ◽  
Vol 33 (6) ◽  
pp. 664-670 ◽  
Author(s):  
S. Li ◽  
Y. Jin ◽  
J. Li
China Geology ◽  
2020 ◽  
Vol 3 (4) ◽  
pp. 511-523
Author(s):  
Zhen-quan Lu ◽  
◽  
Shi-qi Tang ◽  
Xiao-ling Luo ◽  
Gang-yi Zhai ◽  
...  

2016 ◽  
Vol 72 ◽  
pp. 179-192 ◽  
Author(s):  
Shengqian Liu ◽  
Zaixing Jiang ◽  
Hui Liu ◽  
Shouji Pang ◽  
Zhongyuan Xia ◽  
...  

2009 ◽  
Vol 52 (1) ◽  
pp. 202-213 ◽  
Author(s):  
Zhen-Quan LU ◽  
Nabil SULTAN ◽  
Chun-Shuang JIN ◽  
Zhu RAO ◽  
Xu-Rong LUO ◽  
...  

2013 ◽  
Vol 448-453 ◽  
pp. 1394-1398
Author(s):  
Bin Dou ◽  
Lei Ren ◽  
Hai Sheng Liu

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.


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