Elsevier

Ore Geology Reviews

Volume 127, December 2020, 103768
Ore Geology Reviews

Petrology, mineralogy, and ore leaching of sandstone-hosted uranium deposits in the Ordos Basin, North China

https://doi.org/10.1016/j.oregeorev.2020.103768Get rights and content

Highlights

  • Injecting H2SO4 + H2O2 solution will produce calcium sulfate precipitate and block ore bed.

  • CO2 + O2 leaching technology was successfully used in laboratory and field uranium leaching tests.

  • Inhibiting ore bed blockage and increasing the amount of injected O2 are important routes for leaching.

Abstract

The Nalinggou–Daying uranium metallogenic belt is situated at the northern Ordos Basin, China. Petrographical, mineralogical and geochemical techniques were used to study the ore-bearing sandstones and host rocks in the Nalinggou–Daying uranium metallogenic belt. The present study shows that uranium minerals, i.e., coffinite, pitchblende, and brannerite, are mostly disseminated around pyrite and detrital particles. The ore-bearing sandstones are enriched in organic matter, with which this reductive environment influenced uranium leaching. The carbonate concentration of the uranium ores is markedly higher than that of the host rocks, and intense carbonatization occurs in the ore-bearing sandstones. In this case, the usage of the classical in-situ leach uranium mining technique by injecting H2SO4 + H2O2 solution produces calcium sulfate precipitate, which can lead to blocking of the ore-bearing strata. For this reason, laboratory and field uranium mining tests were conducted using CO2 + O2 in-situ leaching technology and were demonstrated to be successful, illustrating that this approach is technically feasible. Inhibiting ore bed blockage and increasing the amount of injected O2 are important for uranium leaching in this setting.

Introduction

In the past few years, many large-sized sandstone-hosted uranium deposits in the Yili, Ordos, Erlian, and Kailu basins in North China have been discovered (Feng et al., 2013, Feng et al., 2017b, Shi et al., 2016, Wu et al., 2016a, Wu et al., 2016b, Bonnetti et al., 2017, Hou et al., 2017, Nie et al., 2017, Zhang et al., 2018b, Zhao et al., 2018b). These discoveries have helped China move from 3rd to 1st in reserves of sandstone-hosted uranium deposits (OECD-NEA/IAEA, 2014). Therefore, sandstone-hosted uranium deposits are a major source of uranium prospecting in China (Feng et al., 2017a, He et al., 2017, Jin et al., 2019). Likewise, the economical and environment-friendly in-situ leach uranium mining technique for sandstone-hosted uranium deposits has also been a popular scientific issue (Su et al., 2006, Su and Du, 2012, Xu et al., 2012, Ji et al., 2018).

The Ordos Basin is an important energy basin with abundant gas, oil and coal in China (Feng et al., 2006, Liu et al., 2013, Wang et al., 2018b). The abundance in exploration leads to the discovery of the Huangjingqi and Nalinggou uranium deposits and, importantly, the large-scale Daying uranium deposit (Li and Li, 2011, Chen et al., 2017, Jiao et al., 2018). Both of the Nalinggou and Daying uranium deposits lie in the northeastern Ordos Basin and share many similar features such as in metallogenic setting and ore deposit geology and thus were as a whole for study within this paper, that is, the Nalinggou–Daying uranium metallogenic belt. Mineralization processes and metallogenic models for these two uranium deposits have been extensively studied, with respect to uranium source (Chen et al., 2017b, Feng et al., 2017a), tectonic evolution (Liu et al., 2006, Liu et al., 2007), ore-bearing horizon (Jiao et al., 2005, Chen et al., 2016, Zhao et al., 2018a), ore-forming and hydrocarbon fluids (Peng et al., 2007, Tuo et al., 2010, Xue et al., 2010, Xue et al., 2011) and geochemical behavior of uranium (Hou et al., 2016, Liu et al., 2016, Wu et al., 2016b, Chen et al., 2017b, Tang et al., 2017). However, there are few studies on leaching of uranium from uranium ores according to mineralogical and geochemical aspects. In this study, we analyzed the petrographical and mineralogical characteristics of the ore-bearing sandstones and host rocks in the Nalinggou–Daying uranium metallogenic belt. Based on the results, the application of uranium leaching of the ore is discussed. Furthermore, corresponding leaching tests were designed and performed. Our study provides not only a typical example for in-situ leach mining in the Ordos Basin but also an efficient method for the study of in-situ leach mining in other sandstone-hosted uranium deposits with similar geologic characteristics.

Section snippets

Geological outline

The Ordos Basin lies in the northwestern part of the North China Block and is a large Mesozoic intracontinental depression basin with an area of about 250,000 km2 (Sun and Dong, 2018, Xu et al., 2018). It exhibits a rectangular shape in a north–south orientation, with a steep and narrow west flank, and a gentle and broad east flank (Zhang and Liao, 2006). Its tectonic unit is classified into the Yimeng uplift belt, the Jinxi flexural fold belt, the Northern Shaanxi slope belt, the Weibei uplift

Materials and analytical methods

Imaging characteristics for petrology and mineralogy of the ore-bearing sandstones and host rocks were conducted at the State Key Laboratory of Nuclear Resources and Environment, East China University of Technology based on a JEOL J7600F back-scattered electron (BSE), and a JXA-8100 electron microprobe (EPMA).

Geochemical analysis was performed by the Analysis and Testing Center of Baotou geology and mineral resources, China National Nuclear Corporation. (1) A total of 1018 samples were

Petrological and mineralogical characteristics

Uranium ores of the Nalinggou–Daying uranium metallogenic belt in the Ordos Basin mainly consist of gray medium- to coarse-grained and low-consolidated sandstones. The ore-bearing sandstones are rich in lithic fragments, accounting for 85%–90% of the whole-rock amount. The components of lithic fragments are complex, and are dominated by quartz, followed by feldspar and mica, with minor amounts of heavy minerals (e.g. ilmenite, zircon, apatite, and rutile). Quartz, feldspar, and mica account for

Ores from the Nalinggou mining district

The CO2 + O2 leaching test started with oxidation with O2 as oxidants at a pressure of 2 MPa for 24 h. Then the O2 supply was halted and CO2 at a pressure of 0.2 MPa was introduced for 4 h and dissolved in the ore pulp to increase the concentration of HCO3 in leaching. Thereafter, O2 was introduced to run oxidative leaching at room temperature for 48 h. The liquid to solid ratio was 5:1. The leaching rate on a residue basis was only 25%, which was not ideal. During the CO2 + O2 leaching test,

Petrographical–mineralogical characteristics and choice of leaching scheme

The ore-bearing sandstones in the Nalinggou–Daying uranium metallogenic belt are dominated by medium- to coarse-grained lithic arkose, with the concentration of detrital particles being >85%. In addition, gillaceous cementation and local calcareous cementation are developed in the ore-bearing sandstones. This type of low-consolidated sandstones is favorable for in-situ leach uranium mining (Su et al., 2006). Organic carbon, pyrite, and sulfur are the indicator minerals representing the

Conclusions

In the Nalinggou–Daying uranium metallogenic belt, the uranium ores from horizons of different uranium deposits are similar in chemical composition and mineralogical characteristics. The concentration of carbonate in the uranium ores is significantly higher than that in the host rocks, and intense carbonatization is presented in the ore-bearing sandstones. In this case, leaching uranium from the uranium ores by using classical acidolysis (H2SO4 + H2O2 solution) would result in calcium sulfate

Declaration of Competing Interest

The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Acknowledgments

This research was financially supported by the National Important Basic Research Program of China (Grant No. 2015CB453002), the National Natural Science Foundation of China (Grant No. 41562006, 41862010), and the Sate key laboratory of Nuclear Resources and Environment, East China University of Technology (Grant No. NRE1809). We acknowledge the comments from three anonymous reviewers and the Managing Guest Editor Prof. Deru Xu, which improved the quality of this paper. We are also grateful to

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