HALOCARBON RATIO AND TRITIUM HE-3 DATING OF WATER MASSES IN THE NANSEN BASIN, ARCTIC-OCEAN

被引：40

作者：

WALLACE, DWR

SCHLOSSER, P

KRYSELL, M

BONISCH, G

机构：

[1] COLUMBIA UNIV,LAMONT DOHERTY GEOL OBSERV,PALISADES,NY 10964

[2] COLUMBIA UNIV,DEPT GEOL,PALISADES,NY 10964

[3] CHALMERS UNIV TECHNOL,DEPT ANALYT & MARINE CHEM,S-41296 GOTHENBURG,SWEDEN

[4] GOTHENBURG UNIV,S-41296 GOTHENBURG,SWEDEN

[5] UNIV HEIDELBERG,INST UMWELTPHYS,W-6900 HEIDELBERG,GERMANY

来源：

DEEP-SEA RESEARCH PART A-OCEANOGRAPHIC RESEARCH PAPERS | 1992年 / 39卷 / 2A期

关键词：

D O I：

10.1016/S0198-0149(06)80015-4

中图分类号：

P7 [海洋学];

学科分类号：

0707 ;

摘要：

Three separate tracer ratio-based water mass ages (CCl4/F11, tritium/He-3 and F11/F12) are calculated for the 1987 oceanographic section by R.V. Polarstern across the Nansen Basin, Arctic Ocean. The CCl4/F11 ratio ages are shown to be in good agreement with the apparent tritium/He-3 ages throughout the age range studied (5-30 years) and with F11/F12 ages in the age range for which such comparisons can be made (16-30 years). A simple box model (integrated to 1987) shows that for CCl4/F11 and tritium/He-3 ages less than 12 years, the apparent ages should be close to the mean age of the water sampled. The distribution of the tracer ages is discussed with respect to the circulation of water masses in the Nansen Basin.

引用

页码：S435 / S458

页数：24

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