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COLORIMETRIC DETERMINATION OF MANGANESE IN ANOXIC WATERS 1
Author(s) -
BREWER P. G.,
SPENCER D. W.
Publication year - 1971
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.4319/lo.1971.16.1.0107
Subject(s) - manganese , anoxic waters , reagent , chemistry , sulfide , environmental chemistry , precipitation , seawater , black sea , geology , oceanography , physics , organic chemistry , meteorology
In the reducing environment of anoxic basins manganese (III) or (IV) is reduced to soluble Mn (II); the deep waters of the Black Sea contain up to 500 µ g Mn (II)/ liter, about 100 times the oceanic average. When this manganese was measured with formaldoxime, color development was erratic if the reagents were added separately. Rapid and reproducible color development was achieved by using a mixed ammonia/formal‐doxime reagent added singly to the sample. Precipitation was avoided by maintaining the pH in the range 8.8–8.9. No interferences from sulfide or dissolved salts were observed. A small correction was made for interference due to iron. Dissolved manganese values in the Black Sea ranged from a midwater maximum of ca. 460 µ g Mn/liter to ca. 250 µ g/ liter in deep water.