CARBONATE SYSTEM IN THE WESTERN MEDITERRANEAN-SEA

被引：37

作者：

MILLERO, FJ ^{[1
]}

MORSE, J ^{[1
]}

CHEN, CT ^{[1
]}

机构：

[1] OREGON STATE UNIV,SCH OCEANOG,CORVALLIS,OR 97331

来源：

DEEP-SEA RESEARCH PART A-OCEANOGRAPHIC RESEARCH PAPERS | 1979年 / 26卷 / 12期

基金：

美国国家科学基金会;

关键词：

D O I：

10.1016/0198-0149(79)90007-4

中图分类号：

P7 [海洋学];

学科分类号：

0707 ;

摘要：

Measurements of the pH and total alkalinity have been made on waters collected in the western Mediterranean Sea. These results have been used to examine the elements of the carbonate system, HCO3-, CO32-, CO2, ΣCO2, PCO, and specific alkalinity. The saturation of Mediterranean Gibraltar is supersaturated with respect to calcium carbonate. Our results for the saturation state (Ω) for Mediterranean waters are in good agreement with the results of Alekin (Geochemistry, 206, 239-242, 1972) and those calculated from the GEOSECS (Geochemical Ocean Sections) test station in the eastern Mediterranean. The saturation state of calcite and aragonite in deep Mediterranean waters in higher than that of deep North Atlantic waters. © 1979.

引用

页码：1395 / 1404

页数：10

共 19 条

[1]

Alekin O.A., 1972, GEOCHEMISTRY, V206, P239

[2] A METHOD FOR CALCULATING IN-SITU PH OF SEAWATER [J].