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舟山海域夏季陆源溶解有机质变化特征分析
Variability in the Characteristics of Terrestrial Dissolved Organic Matter in Zhoushan Area of the East China Sea in Summer
投稿时间:2010-01-28  修订日期:2010-09-20
DOI:
中文关键词:  陆源溶解有机质  吸收系数  荧光指数  水团  河口锋  东海
英文关键词:terrestrial dissolved organic matter  absorption coefficient  fluorescence index  water mass  estuarine front  
基金项目:国家自然科学基金项目(面上项目)
作者单位邮编
黄清辉* 同济大学 200092
吴加学中山大学近岸海洋科学与技术研究中心 
蒋愉林同济大学 
李建华同济大学 
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中文摘要:
      2007年夏季在东海舟山海域河口锋区开展了陆源溶解有机质的调查研究。测定了有色溶解有机质(CDOM)在激发波长370 nm/发射波长460 nm处的荧光强度和在λ=355 nm处的吸收系数,用于代表陆源CDOM含量,并测定了荧光指数以指示CDOM来源。结果表明,CDOM的荧光值和紫外吸收系数之间呈显著正相关性,陆源CDOM含量大体有向海方向降低的趋势,但是纵向上存在一些“突跃”现象。在舟山海域东北角不时观测到表层水体含有高浓度的CDOM,但变异性很大,推测可能该海区受到长江口羽状流的影响。在连续观测站发现,陆源CDOM含量在低平潮时往往比高平潮时要高。河海水混合过程中CDOM含量与盐度呈显著的线性负相关关系。在低盐度的悬沙锋区(S <24)CDOM含量明显低于理论稀释值,而在较高盐度的羽状锋区,CDOM含量接近于理论稀释值。在盐度为24 ~ 31范围内,大部分水样的荧光指数在1.50上下波动,表明其中CDOM来源以陆地来源为主;而在较低盐度(S <24)的水样中荧光指数在1.70至1.90以上,表明CDOM以海洋来源为主,这与其陆源组分在高浊度的低盐度区存在显著的去除过程有关。研究表明,舟山海域水质存在着显著的变异性,与近岸羽状流密切相关,陆源溶解有机质的分布特征对此有较好的响应。
英文摘要:
      In the summer of 2007, one cruise survey on terrestrial chromophoric dissolved organic matter (CDOM) was carried out in the Zhoushan Sea Area of the East China Sea. We determined the fluorescence intensities at excitation wavelength 370 nm /emission wavelength 460 nm and the absorption coefficients at wavelength 355 nm, which represent terrestrial CDOM concentrations. The fluorescence indices were also measured as the indicator of CDOM sources. The results showed that CDOM concentrations roughly tended to decrease in the direction from the land to the sea, but there was some phenomenon of vertical jump. High concentrations of CDOM in the surface water were observed in some sites of the northeast of the Zhoushan Sea Area from time to time, but they showed a great variability, which suggesting that the waters may be subject to the impact of estuarine plume of the Yangtze River. It was found in a continuous observation station that the concentrations of CDOM at low tide were often higher than those at high tide. During the mixing process between river water and sea water, the CDOM concentrations and light absorption coefficients at 355 nm had a significant negative linear relationship with the salinity. That is to say, CDOM took on the conservative behavior in general. However, CDOM concentrations were significantly lower than the theoretical dilution values in the low salinity zone (S <24), indicating a non-conservative removal behavior of CDOM in the suspended sediment front. Fluorescence indices were almost fixed at 1.50 in most of water samples with the salinity between 24 and 31, indicating that CDOM could be dominated with terrestrial sources. However, fluorescence indices varied from 1.70 to 1.90 and above in low salinity zone (S <24), indicating that CDOM could be dominated with marine sources; it is related to the significant removal of terrestrial fractions of CDOM in this zone with low salinity and high turbidity. These results prove that terrestrial organic matter can be used as a good tracer and indicate the variability of water quality in the coastal plume.
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