中文摘要：

以中国近海有代表性的陆架区——东海及南黄海为目标，对东海和南黄海中常见的5种挥发性卤代烃（VHCs）的分布及其海．气通量进行了研究。研究表明，在黄海03断面表层海水中CHCl3、C2HCl3、C2C14、CHBrCl2和CHBr2C1的浓度分别为4l（31—54）、53（23—80）、17（6．3—23）、23（7．4—34）和51（3．1—92）pmol／L，东海表层海水中的浓度分别为25（11—83）、54（12—95）、39（9．2—94）、25（5．4—74）和6．4（1_3__41）pmol／L。由于受人为活动、河流输入和黑潮水入侵的影响，VHCs在水平分布上呈现近岸高、远海低的规律；5种VHCs在表层海水中的浓度-9叶绿素a（Chl口）存在相关性；这5种化合物在表层海水中没有完全一致的周日变化规律，CHBrCl2和CHBr2C1的最大值分别在上午10时和下午16时出现，CHCl3、C2HCl3和c2c14均在下午13时出现最大值。根据表层海水中CHCl3、C2HCl3和c2C14的浓度和文献报道的大气浓度，运用Liss和Salter双层模型，估算得到这3种物质在南黄海的海．气通量分别为76（1．97—149）、160（1．07—330）和53（0．70-119）nmol／（m2．d），在东海的海．气通量为46（1．65—223）、171（6．27—495）和135（3．41--484）nmol／（m2．d），东海和南黄海在冬季是大气CHClnC2HCl，和C2C14的源。

英文摘要：

The distributions of five kinds of VHCs in the East China Sea （ECS） and southern Yellow Sea （SYS） were systematically investigated in the present study. The results show that the concentrations of CHC13, C2HC13, C2C14, CHBrC12 and CHBr2C1 in the surface seawater of SYS were 41（31--54）, 53（23--80）, 17（6.3--23）, 23（7.4--34） and 51（3.1--92） pmol/L, and those in ECS were 25（11--83）, 54（12--95）, 39（9.2--94）, 25（5.4--74） and 6.4（1.3---41） pmol/L, respectively. The concentrations of the five VHCs in the surface seawater were higher inshore than offshore, primarily due to anthropogenic influence, potamic input and Kuroshio water. The data presented in this study also show that the concen- trations of VHCs were correlated with [Chl a] in the surface seawater in the study area. The result show that the diurnal variations of VHCs were not the same with each other, but the lowest concentrations of the 5 VHCs appeared at night and the highest concentration of CHBrC12 and CHBr2C1 occurred at 10：00 and 16：00, respectively, while the highest concentra- tions of CHC13, C2HC13 and C2C14 were all present at 13：00. The higher concentrations of VHCs during daytime might be attributed to the light-induced increase in biological production. In addition, tide was found to have a significant impact on the observed diurnal variations of VHCs. On the basis of surface seawater concentrations of VHCs and gas exchange calculations, the mean sea-to-air fluxes of CHCI3, C2HC13 and C2C14 were estimated to be 76 （1.97--149）, 160 （1.07--330） and 53 （0.70--119） nmol/（m2.d） in SYS, and 46 （1.65--223）, 171 （6.27~495） and 135 （3.41 484） nmol/（m2.d） in ECS, respectively. Based on the present observations, we concluded that the study area appeared to be a source of atmospheric CHC13, C2HC13 and C2C14 in winter.