水团混合及其稳定同位素成分的变化  

SEA WATER MASS MIXING AND THE CHANGE OF THE TOTAL STABLE ISOTOPE COMPONENT

作　　者：张经[1] 

机构地区：[1]山东海洋学院海洋地质学系

出　　处：《山东海洋学院学报》1984年第3期81-85,共5页

摘　　要：水团的概念，一般是指在海洋中由同一源地形成的，物理、化学性质和运动状态基本一致的水体。水团本身是均匀、稳定的，但彼此之问则存在比较明显的差别。When two sea-water masses, A and B, mix each other, the overall stable Isotope component R (D/H, 180/160) changes with the total salinity S and temperature T. This can be shown as follows.Where R1,S1, T1, refers to sea water mass A. and R2, S2, T2 refers to B.It's more complex for three sea-water masses to mingle,but there are still a definite relationship among R. S and T., namely,R= 1/as+b(cS2+dST+eS + fT + g).Where a, b, c, d, e,f and g are constants.

关 键 词：水团混合 稳定同位素 成分变化 运动示踪剂 

分 类 号：P731.16[天文地球—海洋科学]