Thermal conductivity of rocks from measurements on fragments and its application to heat-flow determinations

热流 热导率 地质学 地球物理学 流量(数学) 矿物学 热的 机械 物理 热力学
作者
J.H. Sass,Arthur H. Lachenbruch,Robert J. Munroe
出处
期刊:Journal of Geophysical Research [Wiley]
卷期号:76 (14): 3391-3401 被引量:409
标识
DOI:10.1029/jb076i014p03391
摘要

Journal of Geophysical Research (1896-1977)Volume 76, Issue 14 p. 3391-3401 Thermal conductivity of rocks from measurements on fragments and its application to heat-flow determinations J. H. Sass, J. H. SassSearch for more papers by this authorArthur H. Lachenbruch, Arthur H. LachenbruchSearch for more papers by this authorRobert J. Munroe, Robert J. MunroeSearch for more papers by this author J. H. Sass, J. H. SassSearch for more papers by this authorArthur H. Lachenbruch, Arthur H. LachenbruchSearch for more papers by this authorRobert J. Munroe, Robert J. MunroeSearch for more papers by this author First published: 10 May 1971 https://doi.org/10.1029/JB076i014p03391Citations: 302AboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Abstract A series of measurements indicates that the thermal conductivity of a rock generally can be estimated adequately for geophysical purposes from simple laboratory measurements on fragments of the rock. The solid-rock conductivity is deduced from a divided-bar measurement of the conductivity of a cylindrical cell containing water-saturated rock fragments. All determinations fall within about ten per cent of conventionally measured solid-rock values for a variety of crystalline and sedimentary rocks with conductivities ranging from about 3 to 14 mcal/cm sec°C. Good agreement is found between values determined from drill cuttings and solid core from the same depth in deep boreholes. The method is illustrated by the determination of heat flow in a 3-km-deep borehole near Tehran, Iran (35°40′N latitude, 51°37′E longitude; elevation, 1710 meters). Contrasting gradients are compensated by conductivity variations determined from drill cuttings. Component heat flows show good agreement with a mean of 2.1±0.1 μcal/cm2 sec. References Birch, F., Flow of heat on the Front Range, Colorado, Bull. Geol. Soc. Amer., 61, 567, 1950. Birch, F., H. Clark, The thermal conductivity of rocks and its dependence on temperature and composition, Amer. J. Sci., 238, 529613, 1940. Combs, J., G. Simmons, Heat-flow measurements in Iowa (abstract), Trans. AGU, 50, 316, 1969. Hashin, Z., S. Shtrikman, A variational approach to the theory of the effective magnetic permeability of multiphase materials, J. Appl. Phys., 33, 3125, 1962. Horai, K., G. Simmons, Thermal conductivity of rock-forming minerals, Earth Planet. Sci. Lett., 6, 359, 1969. Horai, K., S. Uyeda, Studies of the thermal state of the earth, 5, Relation between thermal conductivity of sedimentary rocks and water content, Bull. Earthquake Res. Inst. Tokyo Univ., 38, 199, 1960. Riviere, A., Contribution à l'étude géologique de l'Anti-Elbourz, Bull., Societé Géologique de France, Ser. 5, 6, 277, 1936. Roy, R. F., D. D. Blackwell, F. Birch, Heat generation of plutonic rocks and continental heat-flow provinces, Earth Planet. Sci. Lett., 5, 1, 1968. Sass, J. H., R. J. Munroe, A. H. Lachenbruch, Measurement of geothermal flux through poorly consolidated sediments, Earth Planet. Sci. Lett., 4, 293, 1968. Stocklin, J., Structural history and tectonics of Iran: A Review, Bull. Amer. Ass. Petrol. Geol., 52, 1229, 1968. Venart, J. E. S., C. Krishnamurthy, The thermal conductivity of pure organic liquids, Thermal Conductivity D. R. Flynn, B. A. Peavey, Nat. Bur. Stand. Spec. Publ., 302, 659, 1968. Von Herzen, R., A. E. Maxwell, Measurements of thermal conductivity of deep-sea sediments by a needle-probe method, J. Geophys. Res., 64, 1557, 1959. Walsh, J. B., E. R. Decker, Effect of pressure and saturating fluid on the thermal conductivity of compact rock, J. Geophys. Res., 71, 3053, 1966. Woodside, W., J. H. Messmer, Thermal conductivity of porous media, J. Appl. Phys., 32, 1688, 1961. Citing Literature Volume76, Issue1410 May 1971Pages 3391-3401 ReferencesRelatedInformation

科研通智能强力驱动
Strongly Powered by AbleSci AI
科研通是完全免费的文献互助平台,具备全网最快的应助速度,最高的求助完成率。 对每一个文献求助,科研通都将尽心尽力,给求助人一个满意的交代。
实时播报
姜姜完成签到,获得积分20
1秒前
Liu发布了新的文献求助10
1秒前
1秒前
石博文发布了新的文献求助10
1秒前
区区应助胖虎采纳,获得50
2秒前
2秒前
2秒前
3秒前
完美世界应助小清新采纳,获得10
3秒前
3秒前
猪猪hero发布了新的文献求助10
5秒前
5秒前
5秒前
NexusExplorer应助liumengyuan采纳,获得10
5秒前
轻松狗发布了新的文献求助10
6秒前
asdxsweef完成签到,获得积分10
6秒前
6秒前
7秒前
9秒前
9秒前
9秒前
asdxsweef发布了新的文献求助10
9秒前
zhengzhao发布了新的文献求助10
9秒前
番茄鱼发布了新的文献求助10
9秒前
10秒前
黑色天使完成签到 ,获得积分10
10秒前
量子星尘发布了新的文献求助10
10秒前
天天快乐应助april采纳,获得10
11秒前
标致的香水完成签到,获得积分10
12秒前
科研科发布了新的文献求助10
12秒前
14秒前
美好的夜白完成签到,获得积分20
15秒前
天份完成签到,获得积分10
16秒前
落落发布了新的文献求助30
16秒前
研友_VZG7GZ应助YYQYYQYYQ采纳,获得10
16秒前
彭于晏应助石博文采纳,获得20
16秒前
17秒前
慈祥的丹寒完成签到 ,获得积分10
18秒前
wanci应助wsj采纳,获得10
18秒前
20秒前
高分求助中
(应助此贴封号)【重要!!请各用户(尤其是新用户)详细阅读】【科研通的精品贴汇总】 10000
Binary Alloy Phase Diagrams, 2nd Edition 8000
Encyclopedia of Reproduction Third Edition 3000
Comprehensive Methanol Science Production, Applications, and Emerging Technologies 2000
From Victimization to Aggression 1000
Exosomes Pipeline Insight, 2025 500
Red Book: 2024–2027 Report of the Committee on Infectious Diseases 500
热门求助领域 (近24小时)
化学 材料科学 生物 医学 工程类 计算机科学 有机化学 物理 生物化学 纳米技术 复合材料 内科学 化学工程 人工智能 催化作用 遗传学 数学 基因 量子力学 物理化学
热门帖子
关注 科研通微信公众号,转发送积分 5648614
求助须知:如何正确求助?哪些是违规求助? 4775865
关于积分的说明 15044750
捐赠科研通 4807529
什么是DOI,文献DOI怎么找? 2570836
邀请新用户注册赠送积分活动 1527657
关于科研通互助平台的介绍 1486538