地球科学进展 ›› 2006, Vol. 21 ›› Issue (03): 269 -277. doi: 10.11867/j.issn.1001-8166.2006.03.0269

综述与评述 上一篇    下一篇

海洋N 2O的研究进展
詹力扬 1,2,陈立奇 2,3   
  1. 1.厦门大学海洋系,福建 厦门 361005;2.国家海洋局海洋—大气化学与全球变化重点实验室,福建 厦门 361005;3.国家海洋局第三海洋研究所,福建 厦门 361005
  • 收稿日期:2005-03-07 修回日期:2005-09-19 出版日期:2006-03-15
  • 通讯作者: 詹力扬 E-mail:jumpcut@sohu.com
  • 基金资助:

    国家自然科学基金重点项目“白令海与西北冰洋碳通量及其对北极快速变化的响应”(编号:40531007);国家自然科学基金项目“南大洋PCO2时空变异及其调控因子研究”(编号:40276001);国家社会公益专项“台湾海峡大气污染物的输入及海洋生态效应”(编号:2004DIB5178)和“东南极海洋与空气环境监测研究”(编号:2003DEB5J057)资助.

A Review of the Study on Nitrous Oxide Cycle in the Oceans

Zhan Liyang 1,2,Chen Liqi 2,3   

  1. 1.Department of Oceanography, Xiamen University, Xiamen 361005,China; 2. Key Laboratory of Global Change and Marine-Atmospheric Chemistry, SOA, Xiamen 361005,China; 3 Third Institude of Oceanography, SOA, Xiamen  361005,China
  • Received:2005-03-07 Revised:2005-09-19 Online:2006-03-15 Published:2006-03-15

N2O在大气中的浓度仅为CO2的浓度的千分之一左右,但在同等浓度的情况下温室效应却是CO2的200~300倍;它在大气层中的光化学产物会与臭氧反应,从而损耗平流层的臭氧。N2O的环境效应引起人们的关注,许多国际气候变化研究项目都把其列入重要研究内容。通过对过去40年的相关研究工作进行综合分析,阐述N2O在海洋中的分布规律和其影响因素、产生的机制、它的海气通量及其影响因素,从而揭示N2O的海洋生物地球化学循环过程以及这一过程对全球氮循环的贡献。

The concentration of nitrous oxide in the atmosphere is only two orders of magnitude lower than that of Carbon dioxide, however, its green house effect is about 200-300 times higher than that of carbon dioxide. So it has been considerably concerned in the past decades and lots of work have been carried out. A review of the study on biogeochemical cycle of nitrous oxide in oceans for the past decadets is presented here. The vertical distribution of nitrous oxide in oceans, their impact factors, as formation and removal mechanisms will be discussed in more detail. The N2O cycles in oceans will play a significant role in the global biogeochemical cycle.

中图分类号: 

[1] Khalil M A K, Rasmussen R A, Shearer M J. Atmospheric nitrous oxide: Patterns of global change during recent decades and centuries[J]. Chemosphere,2002, 47: 807-821.

[2] Khalil M A K, Rasmussen R A. Global sources of nitrous oxide[J]. Journal of Geophysical Research,1992, 97(D13):14 651-14 660.

[3] Nevision C D, Weiss R F, Erickson D J. Global oceanic emissions of nitrous oxide[J]. Journal of Geophysical Research,1995, 100 (C8): 15 809-15 820.

[4] Li Ming, Hou Chunmei, Zhang Zhiqiang, et al. The oceanogrophical research in the geological science: Prospection of global oceanographical change of the comeing10 years[J]. Advances in Earth Science,2004, 19(6):918-920.[李明,侯春梅,张志强,.地球系统科学中的海洋学研究:未来10年海洋全球变化研究前景[J]. 地球科学进展, 2004, 19(6):918-920.]

[5] Toyoda S, Yoshida N, Miwa T. Production mechanism and global budget of N2O inferred from its isotopomers in the western north pacific[J]. Geophysical Research Letters, 2002, 29:7-1-7-4.

[6] Craig H, Gordon L I. Nitrous oxide in the ocean and marine atmosphere[J]. Geochimica et Coamochimica Acta,1963, 27:949-955.

[7] Hahn J. The North Atlantic Ocean as a source of atmospheric N2O[J]. Tellus,1974, 26:160-168.

[8] Singh H B, Salas L J, Shigeishi Hisao. The distribution of nitrous oxide (N2O) in the global atmosphere and the Pacific Ocean[J]. Tellus,1979, 31:313-320.

[9] Laws C S, Owens N J P. Significant flux of atmospheric nitrous oxide from the northwest Indian Ocean[J]. Nature,1990,346:826-828.

[10] Naqvi S W A, Noronha R J. Nitrous oxide in the Arabian Sea[J]. Deep-Sea Research,1991, 38:871-890.

[11] Yoshinari T. Nitrous oxide in the sea[J]. Marine Chemistry,1976, 4:189-202.

[12] Cohen Y, Gordon L I. Nitrous oxide in the oxygen minimum of the eastern tropical North Pacific: Evidence for its consumption during dentrification and possible mechanisms for its production[J].Deep-Sea Research,1978, 25:509-524.

[13] Cohen Y, Gordon L I. Nitrous oxide production in the ocean[J]. Journal of Geophysical Researach,1979, 84:347-353.

[14] Cohen Y. Consumption of dissolved nitrous oxide in an anoxic basin, Saanich Inlet, British Columbia[J]. Nature,1978, 272:235-237.

[15] Elkins J W, Wofsy S C, McElroy M B, et al. Aquatic sources and sinks for nitrous oxide[J]. Nature,1978, 275:602-606.

[16] Codispoti L A, Christensen J P. Nitrification, denitrification and nitrous oxide cycling in the eastern tropical south Pacific Ocean[J]. Marine Chemistry, 1985, 16:277-300.

[17] Yoshida N, Hattori A, Saino T, et al. 15N/14N ratio of dissolved N2O in the eastern tropical Pacific Ocean[J]. Nature,1984, 307:442-444.

[18] Yoshida N. 15N depleted as a product of nitrification[J]. Nature, 1988, 335: 528-529.

[19] Yoshida N, Morimoto H, Hirano M, et al. Nitrification rates and 15N abundances of N2O and NO-3 in the western North Pacific[J]. Nature,1989, 342: 895-897.

[20] Kim K, Craig H. Two-isotope characterization of N2O in the Pacific Ocean and constraints on its origin in deep water[J]. Nature,1990, 347:58-61.

[21] Dore J, Popp B N, Karl D M, et al. A large source of atmospheric nitrous xoide from subtropical North Pacific surface waters[J]. Nature,1998,396:63-66.

[22] De Wilde H P J, Helder W. Nitrous oxide in the Somali basin: The role of upwelling[J]. Deep-Sea Research, 1997, 44:1 319-1 340.

[23] Codipoti L A, Elkins J W, Yoshinari T, et al. On the Nitrous Oxide Flux from Productive Regions that Contain Low Oxygen Waters[M]. Oceanography of the Indian Ocean, New Delhi,Oxford,1992:271-284.

[24] Oudot C, Anderie C, Montel Y, et al. Nitrous oxide Production in the Tropical Atlantic Ocean[J]. Deep-Sea Research,1990, 37:183-202.

[25] Carlucci A F, McNally P M. Nitrification by marine bacteria in low concentrations of substrate and oxygen[J]. Limnology and Oceangraphy,1969, 14:736-739.

[26] Goreau I J, Kaplan W A, Wofsey S C, et al. Production of NO-2 and N2O by nitrifying bacteria at reduced contrations of oxygen[J]. Applied Environmental Microbiology, 1980, 40:526-532.

[27] Cline J D, Wisegarver D P, Kelly-Hansenk. Nitrous oxide and vertical mixing in the equatorial Pacific during the 1982-1983 El Niño[J]. Deep-Sea Research,1987, 34:857-873.

[28] Weiss R F, Price B A. Nitrous oxide solubility in water and seawater[J]. Marine Chemistry, 1980, 8:347-359.

[29] Butler J H, Elkins J W, Thompson T M, et al. Tropospheric and dissolved N2O of the west Pacific and east Indian oceans during the El Niño Southern oscillation even of 1987[J]. Journal of Geophysical Research, 1989, 94 (D12): 14 865-14 877.

[30] Rees A P, Owens N J P, Upstill-Goddard R C. Nitrous oxide in the Bellingshausen Sea and Drake Passage[J]. Journal of Geophysical Research, 1997,102 (C2): 3 383-3 391.

[31] Hahn J, Junge C. Atmospheric nitrous oxide: A critical review[J]. Zeitschrift fur Naturforschung, 1977, 32a:190-214.

[32] Goering J J, Dugdale V A. Estimates of the rates of denitrification in a subarctic lake[J]. Limnology and Oceanography, 1966, 11:113-117.

[33] Goering J J. Denitrification in the oxygen minimum layer of the eastern tropical Pacific Ocean[J]. Deep-Sea Research,1968, 15:151-164.

[34] Goering J J, Cline J D. A note on denitrification in seawater[J]. Limnology and Oceanography, 1970, 13:306-309.

[35] Barbaree J M, Payne W J. Products of denitrification by a marine bacterium as revealed by gas chromatography[J]. Marine biology, 1967,1:136-139.

[36] Richards F A. Commnets on the effects of denitrification on the budget of combined nitrogen in the ocean[J]. La Mer, 1971, 9:68-77.

[37] Pierotti D, Rasmussen R A. Nitrous oxide measurements in the eastern tropical Pacific Ocean[J]. Tellus, 1980, 32:56-72.

[38] Hashimoto L K, Kaplan W A, Wofsy S C, et al. Transformations of fixed nitrogen and N2O in the Cariaco Trench[J]. Deep-Sea Research,1983, 30: 575-590.

[39] Kaplan W A. Nitrification[M]Nitrogen in the Marine Environment. New York: Academic Press,1983:155.

[40] McElroy M B, Elkins J W, Wofsky S C, et al. Sources and sinks for atmospheric N2O [J]. Reviews of Geophysics and Space Physics, 1976,14:143-150.

[41] Naqvi S W A, Jayakumar D A, Narvekar P V, et al. Increase marine production of N2O due to intensifying anoxia on the Indian continental shelf[J]. Nature, 2000, 408:346-349.

[42] Nevison C D, Kelling R F, Weiss R F, et al. Southern ocean ventilation inferred from seasonal cycles of atmopheric N2O and O2/N2 at Cape Grim, Tasmania[J]. Tellus, 2005, 57B:218-229.

[43] Popp Brian N, Westley Marian B, Toyoda Sakae, et al. Nitrogen and oxygen isotopomeric constraints on the origins and sea-to-air flux of N2O in the oligotrophic subtropical North Pacific gyre[J]. Global Biogeochemical Cycles, 2002,16:12-1-12-10.

[44] suntharalingam P, Samiento J L. Factors governing the oceanic nitrous oxide distribution: Simulations with an ocean general circulation model[J]. Global Biogeochemical Cycles, 2000, 14:429-454.

[45] Nevison C, Butler J H, Elkins J W. Global distribution of N2O and the ΔN2O-AOU yield in the subsurface ocean[J]. Global Biogeocehmical Cycles,2003, 17(4):1 119-1 136.

[46] Seitzinger S P, Kroeze C, Styles R V. Global distribution of N2O emissions from aquatic systems: Natural emissions and anthropogenic effects[J]. Chemosphere-Global Change Science,2000, 2:267-279.

[47] Oslon R J. Differential photoinhibition of marine nitrifiying bacteria: A possible mechanism for the formation of the primary nitrite maximum[J]. Journal of Marine Research,1981,39: 227-238.

[48] Morell J M, Capella J, Mercado A, et al. Nitrous oxide fluxes in Caribbean and tropical Atlantic waters: Evidence for near surface production[J]. Marine Chemistry, 2001, 74:131-143.

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