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Copyright of Uranium Mining & Metallurgy is the property of Uranium Mining & Metallurgy Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

In order to explore the effect of well spacing on the uranium leaching efficiency in acid in-situ leaching, taking the Bayan Ula mining area as an example, and using the finite element method to establish a numerical model for acid in-situ leaching uranium mining, and discuss the coverage and flow rate of the leaching solution. Through the comparison and analysis of 26 schemes, the influence of different well spacing on uranium leaching was discussed from three aspects; well site cost, uranium leaching cycle, and leaching dead angle. The results show that; 1) The fixed cost of the mining area varies with the well. 2) The characteristic flow velocity in the mining area decreases with the increase of the well spacing, and the relative uranium leaching period increases with the increase of the well spacing; 3) With the increase of the well spacing, the volume of the leaching dead angle increases approximately exponentially. Comprehensive consideration, under the simulation conditions in this paper, it is considered that 26 meters to 30 meters is the optimal well spacing for uranium leaching. The results can provide a reference for the reasonable layout of subsequent ground leaching process hoes in this mine area. [ABSTRACT FROM AUTHOR]

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Atomic Energy Science & Technology is the property of Editorial Board of Atomic Energy Science & Technology and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Geology & Exploration is the property of Geology & Exploration Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Geology & Exploration is the property of Geology & Exploration Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

In-situ leaching of uranium is the most predominant method for the current exploitation of sandstone-type uranium deposits. The focus of in-situ leaching of uranium deposits lies in enhancing extraction capacity, and leaching rate, and reducing extraction costs. In order to improve leaching efficiency and reduce costs, the optimization experiments and research on the filter, acidity, and pumping volume were carried out at a uranium in-situ leaching deposit in Inner Mongolia. The research showed that maintaining the length of the filter could be controlled within 4-6 m to ensure its high efficiency and the connection between the upper section of the filter and the rich ore-bearing block with relatively high grade was conducive to the improvement of uranium leaching rate. The leaching efficiency and concentration of uranium in the leaching solution could be improved by controlling the acidity of the solution at about 15 g/L. The pumping volume(single width) was maintained at 0. 75-1.0 mz/h, so that the mining area could maintain a high uranium extraction capacity and a low leaching volume. Through the optimized technical parameters, the optimized peak uranium concentration in the leaching solution was increased from 28.89 mg/L to 59. 72 mg/L. During the initial two years of operation in the mining area, the uranium leaching rate increased from 47.20% to 60. 99%, the average uranium concentration in the leaching solution increased from 17.43 mg/L to 32. 63 mg/L, the acid consumption per ton of uranium decreased by 15. 26%,and the electricity consumption per ton of uranium decreased by 46. 51%. The research had changed the previous "large flow, low concentration" leaching mode, achieving efficient optimization of uranium extraction technology by in-situ leaching. [ABSTRACT FROM AUTHOR]

Uranium extraction by ground leaching is the main mining method for sandstone-type uranium mines, and not only is uranium dissolved after the acidic leach solution reacts with the ore, but a large number of impurity ions are also transferred into the leach solution. This paper takes a pumping unit in the northern part of the C12 mining area of Bayan Wula uranium mine as the research object and carries out systematic research on the evolution characteristics of the chemical composition of leach solution by monitoring the chemical composition of leach solution from its pumping holes. The results show that the increase in ion concentration of leach solution is the result of the interaction between the high acid leach solution and the minerals in the ore-bearing layer, and the evolution of ion concentration goes through three stages, namely, rising, rapidly rising and relatively stable, and the higher the acidity, the faster the rate of increase in concentration, and the order of the reaction between minerals and sulphuric acid is roughly as follows; carbonate, pyrite(iron oxides), silica-alumina, sodium feldspar, and potassium feldspar; the growth rate of the concentration of the cations concerned is similar to the growth rate of SO42- concentration. SO42+ concentration growth rate evolution characteristics have synchronization, SO42- concentration of more than 12 g/L Ca2+ concentration appeared to decrease, indicating that the precipitation of CaSO4 occurred. These research results have important theoretical significance and high academic value for indicating the evolution of mineral dissolution and migration. [ABSTRACT FROM AUTHOR]

Copyright of Coal Science & Technology (0253-2336) is the property of Coal Science & Technology and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Geology & Exploration is the property of Geology & Exploration Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Uranium Geology is the property of Uranium Geology Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Geology & Exploration is the property of Geology & Exploration Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Geology & Exploration is the property of Geology & Exploration Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Ensuring a reliable mine ventilation network is one of the primary strategies to achieve the required air volume at the operating point of a mine quarry. Taking a uranium mine ventilation network as the research object, this paper firstly analyzes the radon concentration distribution in the tunnel under different ventilation parameters and estimates the total ventilation volume required for the ventilation tunnel. Then, using the path entropy theory, air flow transmission path, network flow rate, and radon concentration variation are combined to derive the definition of wind path entropy characterizing the wind performance of uranium mine ventilation. Finally, combined with the maximum entropy theory, a network reliability model that considers the mesoscopic centrality of the network topology to weigh the wind path entropy is proposed, and the model is worked out and analyzed. The experimental results show that the increase of the path length from the human wind entrance makes the probability of transporting radon in each path uneven, the reliability of the end nodes of the network decreases, and the increase of the inlet and return air paths is beneficial to improve the network reliability. [ABSTRACT FROM AUTHOR]

Copyright of Atomic Energy Science & Technology is the property of Editorial Board of Atomic Energy Science & Technology and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Atomic Energy Science & Technology is the property of Editorial Board of Atomic Energy Science & Technology and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Atomic Energy Science & Technology is the property of Editorial Board of Atomic Energy Science & Technology and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Atomic Energy Science & Technology is the property of Editorial Board of Atomic Energy Science & Technology and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Geology & Resources is the property of Geology & Resources Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Hydrogeology & Engineering Geology / Shuiwendizhi Gongchengdizhi is the property of Hydrogeology & Engineering Geology Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Uranium is an efficient and clean fuel for nuclear energy， but it inevitably produces uranium containing wastewater in the nuclear industry. If it is not treated in time and leaked into the environment， it will pose a threat to the health of animals， plants and human beings. Therefore， the separation process of U (Ⅵ) in aqueous solution is urgent based on the perspective of energy recovery and environmental protection. Adsorption techniques have especially attracted attentions because of their advantages on feasibility， efficiency and simple operation. As an ideal adsorbent， functionalized mesoporous silica material has the advantages of large specific surface area， high pore capacity and adsorption capacity. It has a wide range of applications in the field of adsorption and separation for uranium. In this paper， the characterization and adsorption mechanism of U (Ⅵ) adsorption in aqueous solutions at home and abroad are reviewed on the basis of functionalized mesoporous silica preparation methods， combined with X-ray photoelectron spectroscopy， Fourier transform infrared spectroscopy， X-ray absorption fine structure spectroscopy， X-ray energy spectrum analysis and Raman spectroscopy. Although there have been encouraging and potential developments in functionalized mesoporous silica adsorbed uranium， the design and mass production of novel multifunctional adsorbents for applications in actual environments remain challenging. [ABSTRACT FROM AUTHOR]

In situ leaching of sandstone type uranium ore is an economic, green and efficient mining and metallurgy methods The underground sandstone is the seepage channel of leaching solution, the difference of lithology and permeability will affect the migration rule of underground leaching solution. Taking the sandstone type uranium deposits in the northern Or dos basin and northern Erlian basin as an example, the lithology was identified by outcrop drilling logging method, and the stratigraphic correlation was carried out to establish the sequence stratigraphic framework. On the basis of stratigraphic framework comparison, the influence of plane and vertical lithologic structure difference on leaching fluid migration in 2D space is analyzed. Finally, the 3D spatial distribution model of lithologic structure group is established by using 3D geological modeling method to characterize the heterogeneity of lithology of uranium deposit in 3D space. The research results have significance to grasp the seepage law of leaching solution and improve the mining efficiency of in situ leaching. [ABSTRACT FROM AUTHOR]

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of World Nuclear Geoscience is the property of World Nuclear Geoscience Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Remote Sensing for Natural Resources is the property of Remote Sensing for Natural Resources Editorial Office and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Since 1972, China's uranium mining technology has developed from the first generation of technology system to the third generation of technology system, and has gradually played a leading role in the field of uranium mining and metallurgy. This paper reviews the research progress of uranium mining technology such as conventional mining,heap leaching, in-situ blasting leaching and in-situ leaching, and focuses on the mainstream technology of uranium mining-in-situ leaching technology. The ecological restoration technologies of plants, soil, landscape and groundwater microorganisms in uranium mines were reviewed. It is worth noting that microbial leaching and remediation technology will have broad application prospects in uranium mining and remediation technology because of its economic, environmental protection and high efficiency. [ABSTRACT FROM AUTHOR]

It is a major problem to remediate the uranium contaminated groundwater at an acid in-situ leaching uranium mine. In this paper, phytic acid was hydrolyzed by the hydrothermal reaction to obtain phytic acid hydrolyzate, and the simulated uranium contaminated groundwater was prepared according to the physicochemical characteristics of uranium-contaminated groundwater at an acid in-situ leaching uranium mine. The effect of the amount of added phytic acid hydrolyzate and its pH value on the removal performance of U( VI) from the uranium contaminated groundwater was explored, and the concentrations of phosphate anion, calcium ion, total iron ion, manganese ion, zinc ion, and magnesium ion were monitored, and the mechanism for the remediation of uranium contaminated groundwater was analyzed by SEM, TEM, XPS and XRD. The results show that when the amount of the addied phytic acid hydrolyzate was 2 mL, the concentration of phosphate was 24.562 g/L, the initial pH value was 6, the amount of simulated uranium contaminated groundwater was 100 mL, its initial pH value was 3, its uranium concentration was 5 mg/L, and the reaction time was 12 h, the removal rate of uranium reached more than 99%, and the pH value was raised to 5.9. The current research verified that it is feasible to use phytic acid hydrolyzate to remediate the uranium contaminated groundwater at add in-situ leading uranium mine. Since phytic add is cheap and easy to obtain, it can be used as an economical phosphorus source to replace expensive phosphate compounds for the remediation of uranium-contaminated groundwater at the mine. [ABSTRACT FROM AUTHOR]