本文分析GEOSECS計畫中取得之南冰洋氚及碳14數據。將GEOSECS於大西洋之測站76,77,82,85,87,89,9l及SOMOV-8l航次之所有測站所得之過量二氧化碳與碳14資料作對比後發現,這些資料與氚一樣,均顯示於深水中之分佈不平均。本文最後計算出南極底層水當形成時,其中所含表層水中碳14之原始値爲-139.3×10^(-3)。
The tritium and radiocarbon measurements taken at the Southern Ocean GEOSECS stations were analyzed. Excess CO2 for the Atlantic GEOSECS stations 76,77,82,85,87,89,91 and for all the stations of the SOMOV-81 cruise were correlated with the radiotracer data. Radiocarbon and excess CO2 support the tritium data showing that these tracers are not homogeneously distributed in the deep-water column. The preformed radiocarbon value of the Antarctic Surface water component in the Antarctic Bottom Water was estimated to be-139.3×10^(-3).