海底地下水排泄(Sgd)是海岸带陆海相互作用的一个重要的过程,其重要意义体现在它对海岸带水循环和地球化学循环的影响,以及它对沿岸海域生态环境的影响。国际上自从20世纪90年代中期开始系统研究海底地下水排泄以来,已经研究和开发出一整套较为完善的理论和方法,但Sgd的研究在我国才刚刚起步,相关报道极少见且缺乏不同方法的对比研究。目前,评价Sgd常用的方法有:渗流仪法、数值模拟法和地球化学示踪法。其中以氡和镭为代表的地球化学示踪法成为最具影响力的评价方法。该文详细介绍用氡和镭同位素评价Sgd的理论和方法及其适用条件。Submarine groundwater discharge(SGD) is recognized as an important land-sea interaction in the coastal zone,for it is volumetrically and chemically significant to coastal water and chemical budgets,and it may have an influence on coastal ecological environment.Since the mid 90′s,a set of relatively complete theories and methods has been developed and established due to the systematic researches on SGD internationally.However the study on SGD has just begun in China,its relevant report is rarely available and short of comparison experiments of different methods.The current methods for SGD estimation mainly include: seepage meter measurement,numerical simulation,geochemical tracing method.Among those methods,geochemical tracing method has become one of the most powerful methods,and radium and radon as the representative of geochemical tracers has been extensively used.The methods and applicable conditions of SGD estimation using radon and radium isotopes are introduced in detail.近岸海域的海底地下水排泄及其海洋生态环境效应研究(编号40672166);多种方法研究胶州湾的海底地下水排泄(编号41072174
