JACOBS L, EMERSON S, SKEI J.Partitioning and transport of metals across the O2/H2S interface in a permanently anoxicfjord in Norway[J]. Geochim Cosmochim Acta, 1985, (49): 1 433~1 444.
[2]
JACOBS L, EMERSON S, HUESTED S S. Trace metal geochemistry in the CariacoTrench[J]. Deep-Sca Res, 1987,(34): 965~981.
[3]
KADKO D. Radioisotopic studies of submarine hydrothermal vents[ J ]. Rev Geophys,1996, (34): 349~ 366.
[4]
BACON M P, SPENCER D W, BREWER P G. 210Pb/226Ra and 210Po/210Pb disequilibria insea water and suspended particulate matter[J]. Earth Planet Sci Lett, 1976, (32): 277~296.
[5]
NOZAKI Y, THOMSON J, TUREKIAN K K. The distribution of Pb-210 and Po-210 in thesurface waters of the Pacific Ocean[J]. Earth Planet Sci Lett, 1976, (32): 304~312.
[6]
SOMAYAJULU B L K , CRAIG H. Particulate and soluble 210Pb activities in the deepsea[J]. Earth Planet Sci Lett,1976, (32): 268~276.
[7]
TODDJ F, WONGGTF, REIDDF. The geochemistry of 210Po and 210Pb in waters overlyingand within the Orca Basin, Gulf of Mexico[J]. Deep-Sea Res, 1986, (33): 1 293~1 306.
[8]
ISHIBASHI J, GAMO T, SAKAI H, et al. Geochemical evidence for hydrothermal activityin the Okinawa Trough[J]. G eochen J, 1988, (22): 107~114.
[9]
AOKI M, MATSUMOTO T, KIMURA M, et al. Hydrothermal activity and topographicfeatures in the western part of the Minami - Ensei Knoll, Northern Okinawa Trough[J].JAMSTEC J Deep-Sca Res, 1993, (9): 309~319.
[10]
TANAKAT, MISTUZAWAK, HOTTAH. SHINKAI 2000 diving surveys in the East of IheyaSrall Ridge in the cen tral Okinawa Trough[J]. JAMSTEC J Deep-Sca Res, 1989, (5): 267~281.
[11]
GAMO T, SAKAI H, ISHIBASHI J, et al. Growth mechanism of the hydrothermal moundsat the CLAM Site, Mid-Okinawa Trough, inferred from their morphological, mineralogical,and chemical characteristics[J ]. JAMSTEC J Deep-Sea Res, 1991, (7): 163~184.
[12]
GAMO T, SAKAI H, KIM E-S, et al. Geochemical studies on the hydrothermal activityof the Mid-Okinawa Trough: a report on dive 416 of the SHINKAI 2000 and characterizationof hydrothermal fluids from concentrations of major chemical components[J]. JAMSTEC JDeep-Sea Res, 1990, (6): 51~62.
[13]
SHITASHIMA K. Distribution and behavior of trace metals on the Okinawa Trough[J].JAMSTEC J Deep-Sea Res,1994, (10): 291~298.
[14]
CHIBA H, NAKAJIMA K, GAMO T, et al. Hydrothermal activity at the Minami - EnseiKnoll, Okinawa Trough: chemical characteristics of hydrothermal solutions[J]. JAMSTEC JDeep-Sea Res, 1993, (9): 271 ~282.
[15]
MOORE W S. Sampling Ra-228 in the deep ocean[J]. Deep-Sea Res, 1976, (23): 647~651.
[16]
MOTTL M J, SANSONE F J, WHEAT C G, et al. Manganese and methane in hydrothermalplumes along the East Pacific Rise, 8°40′ to 11°50′N[J]. Geochimi Cosmochimi Acta,1995, (59): 4 147~4 165.
[17]
ELDERFIELD H, SCHULTZ A. Mid-ocean ridge hydrothermal fluxes and the chemicalcomposition of the ocean[J ]. Annu Rev Earth Planet Sci, 1996, (24): 191~224.
[18]
CHUNG Yu-jian, CRAIG H. Pb-210 in the Pacific: the GEOSECS measurements ofparticulate and dissolved concentrations[J]. Earth Planet Sci Lett, 1983, (65): 406~432.
[19]
BACON M P, BREWER P G, SPENCER D W, et al. Lead-210 and polonium-210, manganeseand iron in the Cariaco Trench[J]. Deep-Sea Res, 1980, (27A): 119~135.
[20]
KADKO D. An assessment of the effect of chemical scavenging within submarinehydrothermal plumes upon ocean geochemistry[J]. Earth Planet Sci Lett, 1993, (120): 361~374.
[21]
OKUBO A. Ocean diffusion diagrams[J]. Deep-Sea Res, 1971, (18): 789~802.
[22]
AONO T, YAMADA M, NARITA H. Polonium-210 and lead-210 distributions in the OkinawaTrough and the East Chirna SCa[A]. Global Fluxes of Carbon and Its Related Substances inthe Coastal Sea - Ocean - Atmosphere System[A]. Pro-ceedings of the 1994 Sapporo IGBPSymposium[C]. Zapporo, Hokkaido University, 1994. 232~237.
[23]
NOZAKI Y, IKUTA N, YASHIMA M. Unusually large 210po deficiencies relative to 210pbin the Kuroshio Current of the East China and Philippine Seas[J]. J Geophys Res, 1990,(95): 5 321~5 329.
[24]
NOZAKI Y, TSUBOTA H, KASEMSUPAYA V, et al. Residence time of surface water andpanicle-reactive 210pb and210po in the East China and Yellow Seas[J]. Geochimi CosmochimiActa, 1991, (55): 1 265~1 272.
[25]
KADKO D, BACON M P, HUDSON A. Enhanced scavenging of 210pb and 210po by processesassociated with the East Pacific Rise near 8°45′N[J]. Earth Planet Sci Lett, 1986/87,(81): 349~357.
[26]
YAMADA M, AONO T, NARITA H. 210pb in settling particles on the East China Seacontinental margin: the 1993~1994 MASFLEX[A]. Global Fluxes of Carbon and Its RelatedSubstances in the Coastal Sea - Ocean - Atmosphere System. Proceedings of the 1994 SapporoIGBP Symposium[C]. Hokkaido University, 1994. 226~231.
[27]
TSUNOGAI S, SHINAGAWA T, KURATA T. Deposition of anthropogenic sulfate andlead-210 in the western North Pacific area[J]. Geochem J, 1985, (19): 77~90.
[28]
SHENG Z , KURODA P K. Atmospheric injections of polonium-210 from the recentvolcanic eruptions[J]. Geochem J,1985, (19): 1~10.
[29]
WEI Ching-ling, MURRAY J W. The behavior of scavenged isotopes in marine anoxicenvironments: 210pb and 210po in the water column of the Black Sea[J]. Geochimi CosmochimiActa, 1994, (58): 1 795~1 811.
[30]
HARADA K, BURNETT W, LAROCK P. Polonium in Florida groundwater and its possiblerelationship to the sulfur cycle and bacteria[J]. Geochimi Cosmochimi Acta, 1989, (53):143~150.
[31]
BLAIR N E , ALLER C R. Anaerobic methane oxidation on the Amazon shelf[J].Geochimi Cosmochimi Acta, 1995,(59): 3 707~3 715.