A NOTE ON SOURCES OF EXCESS ALKALINITY IN ANOXIC WATERS

被引：10

作者：

KNULL, JR

RICHARDS, FA

机构：

[1] Department of Oceanography, University of Washington, Seattle

来源：

DEEP-SEA RESEARCH | 1969年 / 16卷 / 02期

基金：

美国国家科学基金会;

关键词：

D O I：

10.1016/0011-7471(69)90076-X

中图分类号：

P7 [海洋学];

学科分类号：

0707 ;

摘要：

A model explaining the origin of the excess alkalinity of anoxic waters was tested in Lake Nitinat, a fjord in British Columbia, Canada. The excess alkalinity was nearly all accounted for by the formation of sulfide ions and the solution of alkaline earth metal carbonates. Calcium, magnesium, and strontium concentrations and chlorinity ratios are given. © 1969.

引用

页码：205 / &

共 10 条

[1] DISSOLVED ORGANIC MATTER IN AN ANOXIC FJORD WITH SPECIAL REFERENCE TO PRESENCE OF MERCAPTANS
ADAMS, DD
RICHARDS, FA
[J]. DEEP-SEA RESEARCH, 1968, 15 (04): : 471 - &
[2] RAPID ELECTROMETRIC DETERMINATION OF THE ALKALINITY OF SEA WATER USING A GLASS ELECTRODE
ANDERSON, DH
ROBINSON, RJ
[J]. INDUSTRIAL AND ENGINEERING CHEMISTRY-ANALYTICAL EDITION, 1946, 18 (12): : 767 - 769
[3] CLINE JD, 1967, THESIS U WASHINGTON
[4] DUURSMA EK, 1965, CHEMICAL OCEANOGRAPH, V6, P433
[5] GRIPENBERG STINA, 1960, JOUR CONSEIL PERM INTERNATL EXPLOR MER, V26, P5
[6] SOME CHARACTERISTICS OF NITINAT LAKE, AN INLET ON VANCOUVER ISLAND, BRITISH COLUMBIA
NORTHCOTE, TG
WILSON, MS
HURN, DR
[J]. JOURNAL OF THE FISHERIES RESEARCH BOARD OF CANADA, 1964, 21 (05): : 1069 - 1081
[7] RICHARDS FRANCIS A., 1965, LIMNOL OCEANOGR, V10, pR185
[8] RILEY JP, 1965, CHEMICAL OCEANOGR ED, V6, P433
[9] STRICKLAND JDH, 1965, B FISH RES BD CAN, V125
[10] Wattenberg H., 1933, WISS ERGEBN DT ATLAN, V8, P122

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