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^(226)Ra and ^(228)Ra tracer study on nutrient transport in east coastal waters of Hainan Island,China 被引量:2

^(226)Ra and ^(228)Ra tracer study on nutrient transport in east coastal waters of Hainan Island,China
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摘要 Material fluxes (e.g., nutrients) from coastal waters to offshore areas play an important role in controlling the water quality of the adjacent sea areas not only by increasing nutrient concentration hut also by changing nutrient structures. In this study, naturally occurring isotopes, ^226Ra and ^228Ra, were measured with the alpha spectrometry in the Wenjiao-Wenchang and Wanquan estuaries and adjacent sea areas along the east coast of Hainan Island. The excess ^226Ra and ^228Ra activities were observed by comparison with the values derived from the conservative mixing of freshwater and seawater end-members in both estuaries. Using a one-dimensional diffusion model, the horizontal eddy diffusion coefficient of 3.1 6 × 10^5 cm^2/s, for nutrients diffusing from their sources, was derived from 228Ra activities. Consequently, the corresponding nutrient fluxes flowing into the coastal waters were assessed. The results can provide useful information for the study of the mixing and exchange processes of coastal waters as well as dissoluble pollutant transport in this sea area. Material fluxes (e.g., nutrients) from coastal waters to offshore areas play an important role in controlling the water quality of the adjacent sea areas not only by increasing nutrient concentration hut also by changing nutrient structures. In this study, naturally occurring isotopes, ^226Ra and ^228Ra, were measured with the alpha spectrometry in the Wenjiao-Wenchang and Wanquan estuaries and adjacent sea areas along the east coast of Hainan Island. The excess ^226Ra and ^228Ra activities were observed by comparison with the values derived from the conservative mixing of freshwater and seawater end-members in both estuaries. Using a one-dimensional diffusion model, the horizontal eddy diffusion coefficient of 3.1 6 × 10^5 cm^2/s, for nutrients diffusing from their sources, was derived from 228Ra activities. Consequently, the corresponding nutrient fluxes flowing into the coastal waters were assessed. The results can provide useful information for the study of the mixing and exchange processes of coastal waters as well as dissoluble pollutant transport in this sea area.
出处 《Water Science and Engineering》 EI CAS 2011年第2期157-169,共13页 水科学与水工程(英文版)
基金 supported by the Natural Science Foundation of China (Grant No.41021064) the Sino-German Cooperation Project of Ministry of Science and Technology of China (Grant No.2007DFB20380) the Ph. D. Program Scholarship Fund of East China Normal University (Grant No.2010047)
关键词 Ra isotope ^226Ra and 228Ra tracers horizontal eddy diffusion coefficient nutrient flux east coastal waters of Hainan Island Ra isotope ^226Ra and 228Ra tracers horizontal eddy diffusion coefficient nutrient flux east coastal waters of Hainan Island
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  • 1王颖,吴小根.海平面上升与海滩侵蚀[J].地理学报,1995,50(2):118-127. 被引量:74
  • 2黄奕普,姜德盛,徐茂泉,陈敏,邱雨生.南海东北部表层海水中^(226)Ra的分布[J].热带海洋,1997,16(2):75-81. 被引量:8
  • 3谢永臻,台湾海峡及邻近海域海洋科学讨论会论文集,1995年
  • 4谢永臻,厦门大学学报,1994年,33卷,增刊,86页
  • 5黄奕普,南沙群岛海域的同位素海洋化学,1996年,70页
  • 6黄奕普,南沙群岛海域的同位素海洋化学,1996年,89页
  • 7陈敏,台湾海峡及邻近海域海洋科学讨论会论文集,1995年
  • 8丁国瑜.海南岛第四纪地质的几个问题[A]..见:第四纪地质问题[C].北京:地质出版社,1964.207-233.
  • 9任美锷 张忍顺.潮汐汊道若干问题[J].海洋学报,1984,6(3):352-360.
  • 10Keulegan G H. Tidal flow in entrances, water-level Iluctuations of basins in communication with the sea[C]. TPch. Bulletin, 14. Committee on Tidal Hydraulics. Corps of Engineers,1967.

共引文献40

同被引文献21

  • 1刘衍美.大沽河下游地下水库截渗墙建设前后水质分析与防治对策[J].地下水,2005,27(1):23-24. 被引量:11
  • 2张黎明,魏志远,漆智平.近30年海南不同地区降雨量和蒸发量分布特征研究[J].中国农学通报,2006,22(4):403-407. 被引量:35
  • 3Bumett W C, Cowart J B, Deetae S. Radium in the Suwannee River and estuary[J]. Biodegradation, 1999, 10(3): 237-255.
  • 4Btwnett W C, Bokuniewicz H, Huettel M, et al. Groundwater and pore water inputs to the coastal zone[J]. Biogeochemistry, 2003, 66:3-33.
  • 5Elsinger R J, Moore W S. 224Ra, 228Ra, and 226Ra in Winyah Bay and Delaware Bay[J]. Earth and Planetary Science Letters, 1983, 64(3): 430-436.
  • 6Hwang D W, Kim G Lee Y W, et al. Estimating submarine inputs of groundwater and nutrients to a coastal bay using radium isotopes[J]. Marine Chemistry, 2005, 96:61-71.
  • 7Moore W S. Determining coastal mixing rates using radium isotopes [J]. Continental Shelf Research, 2000, 20(15): 1993-2007.
  • 8Sturchio N C, Banner J L, Binz C M, et al. Radium geochemistry of ground waters in Paleozoic carbonate aquifers, midcontinent, USA[J]. Applied Geochemistry, 2001, 16(1): 109-122.
  • 9Moore W S. The subterranean estuary: a reaction zone of ground water and sea water[J]. Marine Chemistry, 1999, 65:111-125.
  • 10Yang H S, Hwang D W, Kim G. Factors controlling excess radium in the Nakdong River estuary, Korea: submarine groundwater discharge versus desorption from riverine particles[J]. Marine Chemistry, 2002, 78:1-8.

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