Theoretical calculation model of heat transfer for deep-derived supercritical fluids with a case study
文献类型:期刊论文
作者 | Hu, WX; Jin, ZJ; Song, YC; Sun, R; Duan, ZH |
刊名 | ACTA GEOLOGICA SINICA-ENGLISH EDITION
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出版日期 | 2004 |
卷号 | 78期号:1页码:221-229 |
关键词 | heat transfer enthalpy theoretical calculation deep-derived fluids a case study |
ISSN号 | 1000-9515 |
文献子类 | Article |
英文摘要 | Based on a set of equations established by Duan et al. (1992,1996) for a geofluid system H2O-CO2-CH4(-N-2), a formula is obtained to calculate the heat changes. Combining the geological T-P conditions (geothermal gradients and. lithostatic and hydrostatic pressures), the enthalpy of some typical geofluids is figured out. Then the principles of heat transfer of deep-derived supercritical fluids are discussed. The result shows that deep-derived geofluids can bring a large amount of thermal heat and release most heat to the shallow surroundings as they move up, because the molar enthalpies vary very greatly from the deep to shallow, increasing with the increases of T and P. Generally, more than tens of kilojoules heat per molar can be released. Furthermore, the molar enthalpy is affected by the compositions of the geofluids, and the molar enthalpy Of CO2, CH4, or N-2 is greater than that of H2O, being twice, more than twice, and about 140% of H2O, respectively. Finally, a case study is conducted by investigating a source rock sequence affected hydrothermally by magmatic fluids in the Huimin depression of Shengli Oilfield. The thermal heat calculated theoretically of the fluids related to a diabase intrusion is quite large, which can increase the temperature near the diabase to about 300degreesC, and that can, to some extent, account for the abnormal rise of the vitrinite reflectance, with the highest of about 3.8% (R-o). |
WOS关键词 | EQUATION ; SYSTEM ; STATE ; PREDICTION ; INCLUSIONS ; MIXTURES ; MANTLE ; CARBON ; EARTH ; BAR |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000221717300028 |
出版者 | GEOLOGICAL SOC CHINA |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/79399] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Hu, WX |
作者单位 | 1.Nanjing Univ, Dept Earth Sci, State Key Lab Mineral Deposits Res, Nanjing 21009, Jiangsu, Peoples R China 2.Petr Univ, Basin & Reservoir Res Ctr, Beijing 102200, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China |
推荐引用方式 GB/T 7714 | Hu, WX,Jin, ZJ,Song, YC,et al. Theoretical calculation model of heat transfer for deep-derived supercritical fluids with a case study[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2004,78(1):221-229. |
APA | Hu, WX,Jin, ZJ,Song, YC,Sun, R,&Duan, ZH.(2004).Theoretical calculation model of heat transfer for deep-derived supercritical fluids with a case study.ACTA GEOLOGICA SINICA-ENGLISH EDITION,78(1),221-229. |
MLA | Hu, WX,et al."Theoretical calculation model of heat transfer for deep-derived supercritical fluids with a case study".ACTA GEOLOGICA SINICA-ENGLISH EDITION 78.1(2004):221-229. |
入库方式: OAI收割
来源:地质与地球物理研究所
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