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COLORIMETRIC DETERMINATION OF MANGANESE IN ANOXIC WATERS1

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BREWER, P. G., SPENCER, D. W.·1971·Limnology and Oceanography

Abstract

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.

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Metadata

Authors
BREWER, P. G., & SPENCER, D. W.
Venue
Limnology and Oceanography
Publisher
Wiley
Published
1971-01
Volume
16
Issue
1
Pages
107-110
ISSN
  • 0024-3590 (ISSN-L)
  • 1939-5590
OpenAlex
W1491123067
Cited by
207
References
0
FWCI
3.66
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: COLORIMETRIC DETERMINATION OF MANGANESE IN ANOXIC WATERS1. https://app.cochat.ai/papers/10.4319/lo.1971.16.1.0107
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BREWER, P. G., & SPENCER, D. W. (1971). COLORIMETRIC DETERMINATION OF MANGANESE IN ANOXIC WATERS1. Limnology and Oceanography. https://doi.org/10.4319/lo.1971.16.1.0107

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.