ARS Characteristics of Different Uranium Fractions in Sandstone Uranium Deposit and Their Indication for in-situ Leaching of Uranium

被引:0
|
作者
Li C.-G. [1 ]
Tan K.-X. [1 ]
Liu Z.-Z. [2 ]
Xia L.-S. [3 ]
Tan W.-Y. [1 ]
机构
[1] School of Nuclear Resources Engineering, University of South China, Hengyang
[2] School of Environmental Protection and Safety Engineering, University of South China, Hengyang
[3] School of Nuclear Science and Technology, University of South China, Hengyang
关键词
ARS; Chemical fraction; In-situ leching; Sandstone uranium;
D O I
10.7538/yzk.2017.51.08.1358
中图分类号
学科分类号
摘要
In order to study the indicative function of 234U/238U activity ratios (ARS) to in-situ leaching of uranium, taking uranium ore from Xinjiang as an example, sequential extraction test was adopted to separate different uranium chemical fractions, and horizontal column leaching test was applied to obtain pregnant leach solution. ARS in the chemical fractions and the pregnant leach solution were measured by ICP-MS and then uranium concentrations in leaching pregnant solution were measured by TiCl3 reduction-NH4VO3 oxidation titration method. The results show that ARS are higher (1.293-1.348) in exchangeable fraction (F1) and easily acid soluble fraction (F2), which decrease to 1.204-1.229 in acid soluble fraction (F3) and then reduce to the minimum 0.917-0.934 in oxidation fraction (F4). After that ARS increase to 1.018-1.142 in hardly soluble fraction (F5). Three phases of uranium leaching were identified according to the ARS. The first phase was characterized by the relatively high ARS in the range of 1.217-1.318, and the leaching uranium is mainly U(VI) in fraction F1, F2 and F3. The second phase was represented as the decrease of ARS, up to 1.016, and the leaching uranium is mainly U(IV) partly in F3 and primarily in F4. The third phase was characterized by the fluctuant ARS of 1.070-1.118, and the few leaching uranium is mainly the hardly soluble uranium in F5. © 2017, Editorial Board of Atomic Energy Science and Technology. All right reserved.
引用
收藏
页码:1358 / 1363
页数:5
相关论文
共 14 条
  • [1] Maxim S., Alexander Z., Graham J., In situ recovery, an alternative to conventional methods of mining: Exploration, resource estimation, environmental issues, project evaluation and economics, Ore Geology Reviews, 79, pp. 500-514, (2016)
  • [2] Cai Y., Zhang J., Li Z., Et al., Outline of uranium resources characteristics and metallogenetic regularity in China, Acta Geologica Sinica, 89, 6, pp. 1051-1069, (2015)
  • [3] World uranium mining production, (2016)
  • [4] Satybaldiyev B., Lehto J., Suksi J., Et al., Understanding sulphuric acid leaching of uranium from ore by means of <sup>234</sup>U/<sup>238</sup>U activity ratio as an indicator, Hydrometallurgy, 155, pp. 125-131, (2015)
  • [5] Liu J., Sun Z., Shi W., The discussions on some problems of sandstone type uranium ore by using uranium isotopes, Journal of Jilin University: Earth Science Edition, 36, 4, pp. 516-520, (2006)
  • [6] Alfred V.A., Zorana I., Ljudmila B.K., Recent measurements of <sup>234</sup>U/<sup>238</sup>U isotope ratio in spring waters from the Hadzici area, Journal of Environmental Radioactivity, 120, pp. 6-13, (2013)
  • [7] Suksi J., Rasilainen K., Pitkanen P., Variations in <sup>234</sup>U/<sup>238</sup>U activity ratios in groundwater: A key to flow system characterisation, Physics and Chemistry of the Earth, 31, pp. 556-571, (2006)
  • [8] Fredrik L., Andres P.T., Anna V., Et al., <sup>234</sup>U/<sup>238</sup>U in a boreal stream network-relationship to hydrological events, groundwater and scale, Chemical Geology, 420, pp. 240-250, (2016)
  • [9] Kumar A., Karpe P.K., Rout S., Et al., Activity ratios of <sup>234</sup>U/<sup>238</sup>U and <sup>226</sup>Ra/<sup>228</sup>Ra for transport mechanisms of elevated uranium in alluvial aquifers of groundwater in southwestern (SW) Punjab, India, Journal of Environmental Radioactivity, 151, pp. 311-320, (2016)
  • [10] Anirban B., Shaun T., Brown N., Et al., Isotopic and geochemical tracers for U(VI) reduction and U mobility at an in situ recovery U mine, Environmental Science & Technology, 49, pp. 5939-5947, (2015)