热液系统输向大洋的热通量估算

栾锡武; 赵一阳; 秦蕴珊; 初凤友

热液系统输向大洋的热通量估算

1.
中国科学院海洋研究所, 山东, 青岛, 266071
2.
国家海洋局, 第二海洋研究所, 浙江, 杭州, 310012

基金项目: 973"项目;国家自然科学基金资助项目(40006004;G20000467);中国科学院院长基金资助项目

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- 文章访问数: 734
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出版历程
- 收稿日期: 2000-09-01
- 修回日期: 2001-09-03

Heat flux estimates from hydrothermal system to the ocean

摘要

摘要: 从四个方面对现代海底热液活动输向大洋的热通量进行了初步估算.热液系统通过集中、高温的热液烟囱和低温、大面积漫溢热水的形式向海洋输送的热通量为357GW;由底热异常边界层计算出的热通量为32GW;根据Baker提出的扩张洋脊的扩张速率和扩张洋脊热液柱覆盖率之间的线性关系,推算的热液通量为1086GW;根据扩张洋脊岩墙冷却和扩张推算的热通量为592GW.不同的方法给出的结果有较大的差异.一方面这些结果反映了热液系统向大洋的供热水平,另一方面反映了目前对现代海底热液活动的认识水平.虽然热液系统向大洋的热输出比太阳的热辐射小,但由于其特殊的供热方式,这部分热能仍有可能对全球气候带来影响,应在今后的研究中给予重视.
- 现代海底热液活动 /
- 分布 /
- 热通量估算
Abstract: Four methods are used to estimate the heat flux from the hydrothermal system to the ocean.The heat flux from high temperature vents and low temperature warm water diffusion fields is about 357 GW.The heat flux from bottom thermal boundary layer is 32 GW.Based on Baker's linear relationship between spreading rate and plume incidence,the possibly total hydrothermal fields on the whole world ocean are calculated and then their heat flux estimate is about 1 086 GW.Based on the spreading axiscrust cooling model the result is about 592 GW.From the results it can be seen that the heat flux from the hydrot hermal system to the world ocean may be tens to thousands giga-watt on one hand,and on the other hand it is well known that it is not easy to estimate it actually now.The great differ ence comes mainly from limited knowledge about the distribution of the hydrothermal fields on the world ocean.The abovementioned analysis is shown that though the heat flux from the hydrothermal system to the ocean is much smaller than the heat flux from the solar radiation to the ocean,but concerning the different ways of supplying the world ocean with heat,much attention should be paid to the effects of the hydrothermal activity on the world ocean current and world climate.
- modern hydrothermal activity /
- distribution /
- heat flux estimate

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参考文献(30)

RISE Project Group. East Pacific Rise:hot spring and geophysical experiments[J]. Science, 1980, 207:1 421-1 444.

BAKER E T. The relationship between near axis hydrothermal cooling and the spreading rate of mid-ocean ridges[J]. EPSL,1996, 142:137-145.

LOWELL R P, RONA P A, VON HERZEN R P. Scafloor hydrothermal systems[J]. JGR, 1995, 100:327-352.

STEIN C A, STEIN S. Constraints on hydrothermal heat flux through the oceanic lithospheric from global heat flow [J].JGR, 1994, 99:3 081-3 095.

FOUQUET Y, BARRIGA F. FLORES diving cruise with the Nautile near the Azores first dives on the Rainbow Field:hydrothermal sea water/mantle interaction[J]. InterRidge News, 1998, 2:1 154-1 162.

OOSTING S E, VON DAMM K L. Bromide/chloride fractionation in sea floor hydrothermal fluids from 9'～10°N, EPR[J].EPSL, 1996, 144:133-145.

CHARLOUJ L, FOUQUET Y. Axineral and gas chemistry of hydrothermal fluids on an ultrafast spreading ridge:EPR17°～19°S (Nautile cruise, 1993) phase separation processes controlled by volcanic and tectonic activity[J].JGR, 1996, 101:15 899-15 919.

GERMAN C R, BAKER E T, MEVEL C. Hydrothermal activity along the Southwest Indian Ridge[J]. Nature, 1998, 395:490-493.

SCHEIER D S, BAKER E T, JOHNSON K T. Detection of hydrothermal plumes along the Southeast Indian Ridge near theAmsterdam-St. Plateau[J]. Geoph Res Lett, 1998, 25:97-100.

吴世迎.世界海底热液硫化物资源[M].北京:海洋出版社,2000.1-290

CONVERSE D R. Flow rates in the axial hot springs of the East Pacific Rise (21°N):implications for the heat budget andthe formation of massive sulfide deposits[J]. EPSL, 1984, 69:159-175.

DELANEY J R. Geology of a vigorous hydrothermal system on the Endeavor segment Juan de Fuca Ridge[J]. JGR, 1992,97:19 663-19 682.

RONA P A, VON HERZEN R P. Introduction to special section on measurements and monitoring at the TAGhydrothermal field, MAR 26°N, 45°W[J]. Geophysical Research Letters, 1996, 23:3 427-3 430.

RONA P A. Black smoker and massive sulfides at the TAG hydrothermal field, Mid-Atlantic Ridge, 26°N[J]. EOS, 1985,66:936.

GOODFELLOW W D, FRANKLIN J M. Geology, minerology and chemistry of sediment hosted elastic massive sulfides inshallow core, Middle Valley, North Juan de Fuca Ridge[J]. Economic Geology, 1993, 88:2 037-2 069.

RONA P A. An Atlantic hydrothermal plume:TAG area, Mid-Atlantic Ridge crest near 26°N[J]. JGR, 1989, 94:13 879-13 893.

RONA P A. Hydrothermal circulation, serpentinization, and degassing at a rife valley fracture zone intersection, MAR near15°N, 45°W[J]. Geology, 1992, 20:783-786.

Tamayo Tectonic Team. Tectonies at the intersection of theEast Pacific Rise with the Tamayo transform fault[J]. MarineGeophysicalResearch, 1984, 6:159-185.

WOODRUFF L G. Sulfur isotope study of chimney minerals and vent fluids from 21°N, EPR:hydrothermal sulfur sourcesand disequilibrium sulfate reduction[J]. JGR, 1988, 93:4 562-4 572.

THOMSON R E, DAVIS E E. Hydrothermal venting and geothermal heating in Cascadia Basin [J]. JGR, 1995, 100:6121-6 141.

MURTON B J, KLINKHAMMER G, BECKER K, et al. Direct evidence for the distribution and occurrence ofhydrothermal activity between 27°and 30°N on the MAR[J]. EPSL, 1994, 125:119-128.

GERMAN C R, PARSON L M, Heat Scientific Team. Hydrothermal exploration at the Azores Tripple Junction:tectoniccontrol of venting at slow-spreading ridge[J]? EPSL, 1996, 138:93-104.

GERMAN C R, BRIEM J, CHIN C, et al. Hydrothermal activity on the Reykjanes Ridge:the Steinaholl Vent-Field at 63°06°N[J]. EPSL, 1994, 121:647-654.

DETRICK R S, MUTTER J C. No evidence from multichannel reflection data for a crustal magma chamber in the MARKarea on the Mid-Atlantic Ridge[J]. Nature, 1990, 347:61-64.

LOWELL R P, RONA P A. Hydrothermal models for the generation of massive sulfide are deposits[J]. JGR, 1985, 90:8 769-8 783.

KENT G M. Evidence for a smaller magma chamber beneath the East Pacific Rise at 9°30'N [J]. Nature, 1990, 344:650-653.

SINTON, DETRICK. Mid-ocean ridge magma chambers[J]. JGR, 1992, 97:197-216.

RUBIN A M. On the thermal variability of dikes leaving magma chambers[J]. Geopysical Res Lett, 1993, 20(4):257-260.

HENSTOCK T J. The accretion of oceanic crust by episodic sill injection[J]. JGR, 1993, 98:4 143-4 161.

DETR1CK R S, BUHL P, VERA E, et al. Multi-seismic imaging of a crustal magma chamber along the East Pacific Rise[J]. Nature, 1987, 326:35-41.

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