A new effective thermal conductivity model of methane hydrate-bearing sediments considering hydrate distribution patterns

被引:25
作者
Sun, Shicai [1 ]
Gu, Linlin [1 ]
Yang, Zhendong [1 ]
Li, Yanmin [1 ]
Zhang, Changxing [1 ]
机构
[1] Shandong Univ Sci & Technol, Coll Civil Engn & Architecture, Shandong Prov Key Lab Civil Engn Disaster Prevent, Qingdao 266590, Peoples R China
关键词
Methane hydrate; Distribution pattern; Effective thermal conductivity; Model; Hydrate-bearing sediments; Hydrate content; POROUS-MEDIA; DISSOCIATION;
D O I
10.1016/j.ijheatmasstransfer.2021.122071
中图分类号
O414.1 [热力学];
学科分类号
摘要
In this work, a new effective thermal conductivity (ETC) model considering hydrate distribution patterns was proposed to study the effects of hydrate saturation (n(h)), distribution pattern and pore fluid. The ETC of methane hydrate (MH)-bearing sediments with liquid- saturated state (only water and MH in pores, i.e., "liquid-saturated" sediments), gas saturated state (only methane and MH, i.e., "gas-saturated" sediments) or hydrate-saturated state (only MH in pores, i.e., n(h) = 100%, "hydrate-saturated" sediments) were calculated by the proposed ETC models with the temperature 263.15 similar to 278.15 K, the pressure 6 MPa and the porosity 47.64%. The calculated results show that the ETC of hydrate-saturated sediments is about 1.44 +/- 0.04 W.m(-1) .K-1 ; the ETC of liquid-saturated sediments ranges from 1.42 to 2.2 W.m(-1). K-1, showing a weak negative correlation with n(h), and a positive correlation with temperature. However, the ETC of gas-saturated sediments ranges from 0.15 to 1.45 W.m(-1).K-1, which is positively correlated with n(h), negatively (or positively) correlated with temperature at low n(h) (or high n(h)). Besides, the results suggest that the ETC increment caused by the temperature increase of 1 K is -3.6E-4 similar to 2.34E-3 W.m(-1).K-1 under the three hydrate distribution patterns and three above states, which can be seen as a weak dependence on temperature. The influence of distribution patterns on the ETC of gas-saturated sediments (with the same n(h)) is: cementing model > inclusion model > filling model. Due to the particularity of the structure of the supporting model, the ETC of sediments is mainly affected by sand content (v(s)), but weakly affected by hydrate content (v(h)) and hydrate growth mode. Increasing the same value of v(s) and v(h), the ETC increment of the former is about 10 times that of the latter. Finally, the new ETC models are used to predict hydrate content of natural sea sand and marine soil samples, which provides a new idea for resource evaluation. (C) 2021 Elsevier Ltd. All rights reserved.
引用
收藏
页数:19
相关论文
共 36 条
[1]  
Cheng C., 2015, Study of Heat Transfer Characteristic and the Effects On Exploitation For Natural Gas Hydrate sediments
[2]   Effect of Hydrate Formation Conditions on Thermal Conductivity of Gas-Saturated Sediments [J].
Chuvilin, Evgeny ;
Bukhanov, Boris .
ENERGY & FUELS, 2017, 31 (05) :5246-5254
[3]   Thermal conductivity measurements in unsaturated hydrate-bearing sediments [J].
Dai, Sheng ;
Cha, Jong-Ho ;
Rosenbaum, Eilis J. ;
Zhang, Wu ;
Seol, Yongkoo .
GEOPHYSICAL RESEARCH LETTERS, 2015, 42 (15) :6295-6305
[4]   A NONSTATIONARY METHOD FOR DETERMINING THERMAL CONDUCTIVITY OF SOIL INSITU [J].
DEVRIES, DA .
SOIL SCIENCE, 1952, 73 (02) :83-89
[5]  
[刁少波 DIAO Shaobo], 2008, [岩矿测试, Rock and Mineral Analysis], V27, P165
[6]   Effect of hydrate distribution on effective thermal conductivity changes during hydrate formation in hydrate-bearing quartz sands [J].
He, Juan ;
Li, Xiaosen ;
Chen, Zhaoyang ;
You, Changyu ;
Yan, Kefeng ;
Xia, Zhiming ;
Li, Qingping .
INTERNATIONAL JOURNAL OF HEAT AND MASS TRANSFER, 2021, 174
[7]   Effective thermal conductivity changes of the hydrate-bearing quartz sands in depressurization and soaking [J].
He, Juan ;
Li, Xiaosen ;
Chen, Zhaoyang ;
Li, Qingping ;
Xia, Zhiming ;
Zhang, Yu ;
Wang, Yi ;
You, Changyu .
JOURNAL OF NATURAL GAS SCIENCE AND ENGINEERING, 2021, 89
[8]   In situ thermal conductivity of gas-hydrate-bearing sediments of the Mallik 5L-38 well [J].
Henninges, J ;
Huenges, E ;
Burkhardt, H .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2005, 110 (B11) :1-11
[9]   Measuring and modeling thermal conductivity of gas hydrate-bearing sand [J].
Huang, DZ ;
Fan, SS .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2005, 110 (B1) :1-10
[10]   Series-parallel resistance method based thermal conductivity model for rock-soil with low or high porosity [J].
Jia, G. S. ;
Ma, Z. D. ;
Zhang, Y. P. ;
Zhao, M. ;
Meng, X. Z. ;
Zhang, L. Y. ;
Jin, L. W. .
GEOTHERMICS, 2020, 84