The determination of chromium in rocks and minerals

R. Fuge

doi:10.1016/0009-2541(67)90030-7

The determination of chromium in rocks and minerals

R. Fuge^*

^*Corresponding author for this work

Department of Geography and Earth Sciences

Research output: Contribution to journal › Article › peer-review

3 Citations (Scopus)

Abstract

Chromium is determined in rock and mineral samples after a sodium carbonate-magnesium oxide fusion, by colorimetry with diphenylcarbazide, using a Technicon Autoanalyser. The method is rapid, and as many as 50 samples a day can be determined (25 in duplicate). The sensitive procedure was applied to the determination of chromium in the U.S. Geological Survey standard rocks diabase W-1, and dunite DTS-1, and the C.A.A.S. standard rock syenite 1: values of 121; 3,530; and 46 p.p.m. respectively were obtained.

Original language	English
Pages (from-to)	289-296
Number of pages	8
Journal	Chemical Geology
Volume	2
Issue number	C
DOIs	https://doi.org/10.1016/0009-2541(67)90030-7
Publication status	Published - 1967

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title = "The determination of chromium in rocks and minerals",

abstract = "Chromium is determined in rock and mineral samples after a sodium carbonate-magnesium oxide fusion, by colorimetry with diphenylcarbazide, using a Technicon Autoanalyser. The method is rapid, and as many as 50 samples a day can be determined (25 in duplicate). The sensitive procedure was applied to the determination of chromium in the U.S. Geological Survey standard rocks diabase W-1, and dunite DTS-1, and the C.A.A.S. standard rock syenite 1: values of 121; 3,530; and 46 p.p.m. respectively were obtained.",

author = "R. Fuge",

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doi = "10.1016/0009-2541(67)90030-7",

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AU - Fuge, R.

PY - 1967

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N2 - Chromium is determined in rock and mineral samples after a sodium carbonate-magnesium oxide fusion, by colorimetry with diphenylcarbazide, using a Technicon Autoanalyser. The method is rapid, and as many as 50 samples a day can be determined (25 in duplicate). The sensitive procedure was applied to the determination of chromium in the U.S. Geological Survey standard rocks diabase W-1, and dunite DTS-1, and the C.A.A.S. standard rock syenite 1: values of 121; 3,530; and 46 p.p.m. respectively were obtained.

AB - Chromium is determined in rock and mineral samples after a sodium carbonate-magnesium oxide fusion, by colorimetry with diphenylcarbazide, using a Technicon Autoanalyser. The method is rapid, and as many as 50 samples a day can be determined (25 in duplicate). The sensitive procedure was applied to the determination of chromium in the U.S. Geological Survey standard rocks diabase W-1, and dunite DTS-1, and the C.A.A.S. standard rock syenite 1: values of 121; 3,530; and 46 p.p.m. respectively were obtained.

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DO - 10.1016/0009-2541(67)90030-7

M3 - Article

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SP - 289

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JO - Chemical Geology

JF - Chemical Geology

IS - C

ER -

The determination of chromium in rocks and minerals

Abstract

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