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Determination of redox potential of uranium geological samples by potential difference method
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Jianmei ZHANG, Changsheng DENG, Hao QIAO
World Nuclear Geoscience | 2025, 42(3) : 647 - 658
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World Nuclear Geoscience | 2025, 42(3): 647-658
RESEARCH ARTICALS
Determination of redox potential of uranium geological samples by potential difference method
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Jianmei ZHANG, Changsheng DENG, Hao QIAO
Affiliations
  • Geologic Party No.216, CNNC,Urumqi 830011, China
Published: 2025-06-08 doi: 10.3969/j.issn.1672-0636.2025.03.015
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To accurately measure the oxidation-reduction potential of uranium ore geological samples, this study try to explore a better measurement method and experimental conditions by comparing and analyzing the application effects of the acidic potassium dichromate method and the alkaline potassium permanganate method in the measurement of the oxidation-reduction potential of uranium ore geological samples. The potential drop method was used to systematically conduct a multi-dimensional comparison between the acidic potassium dichromate method and the alkaline potassium permanganate method. The aspects of comparison included solution stability, optimal solution concentration, sample soaking time,solid - liquid ratio, and electrode equilibrium time. The sample soaking time and electrode equilibrium time of the alkaline potassium permanganate method are shorter than those of the acidic potassium dichromate method, allowing it to reach a stable and reliable potential value more quickly. For strongly reducing samples,the ΔEh value obtained by the acidic potassium dichromate method is larger. However, the evaluation conclusions of the two methods regarding the reduction ability of the samples are consistent. Nevertheless, the precision of the alkaline potassium permanganate method is better.The optimal experimental conditions for the alkaline potassium permanganate method are as follows: a concentration of 0.03 mol∙L-1, a sample soaking time of 1.5 h,a solid-liquid ratio of 1:25, an electrode equilibrium time of 5 min, a reaction medium of 0.2 % potassium hydroxide solution, and a temperature of (25±1) °C. The ΔEh value measured by this method is basically consistent with the judgment results of the oxidation - reduction environment by the oxidation coefficient method (Fe2+/Fe3+), and is also basically consistent with the color of the samples.Based on comprehensive experimental indicators, the overall performance of the alkaline potassium permanganate method is superior to that of the acidic potassium dichromate method in the measurement of the oxidation - reduction potential of uranium ore geological samples. By adopting the optimal experimental conditions, the accurate measurement of the oxidation - reduction potential of uranium geological samples is achieved, providing reliable technical support for uranium ore geological research.

potential drop method  /  redox potential  /  potassium permanganate  /  potassium dichromate  /  geological samples of uranium ore
Jianmei ZHANG, Changsheng DENG, Hao QIAO. Determination of redox potential of uranium geological samples by potential difference method[J]. World Nuclear Geoscience, 2025 , 42 (3) : 647 -658 . DOI: 10.3969/j.issn.1672-0636.2025.03.015
  • Uranium Investigation Project of China Nuclear Geology“Uranium mineral survey in Dulaota area,Chapchar County,Xinjiang(202305-1)
Year 2025 volume 42 Issue 3
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Article Info
doi: 10.3969/j.issn.1672-0636.2025.03.015
  • Receive Date:2025-04-07
  • Online Date:2025-11-10
  • Published:2025-06-08
Article Data
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History
  • Received:2025-04-07
  • Revised:2025-04-22
Funding
Uranium Investigation Project of China Nuclear Geology“Uranium mineral survey in Dulaota area,Chapchar County,Xinjiang(202305-1)
Affiliations
    Geologic Party No.216, CNNC,Urumqi 830011, China

Corresponding:

DENG Changsheng,male,born in 1984,senior engineer,focusing on the analysis work of rocks and minerals. E-mail:
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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