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Study On Mechanism Of Uranium Leaching And Solute Migration During The CO2+O2 In-situ Uranium Leach Mining Process In The Mengqiguer Deposit

Posted on:2020-11-02Degree:DoctorType:Dissertation
Country:ChinaCandidate:H B JiFull Text:PDF
GTID:1481306110457654Subject:Geological Resources and Geological Engineering
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The Mengqiguer deposit in XINJIANG is the main production base of natural uranium in China.The content of carbonate and pyrite is high and unevenness.Although using CO2+O2neutral leaching technology,chemical plugging still exist.In order to prevent chemical clogging and improve the uranium leaching effects,this paper study the mechanisms of uranium leaching and element migration during neutral leaching process.It carried out“Groundwater+NH4HCO3+CO2+O2”,“tail liquid+CO2+O2”and“two pumping and six injecting wells”tests.It used Mineralogy,Hydrogeochemistry,Groundwater dynamics and Numerical simulation methods to study the uranium leaching characteristics,influencing factors and migration mechanism of U,C,S,Fe,Ca,Mg between the fluid and minerals.The Uranium ore are mainly pitchblende,little coffinite and brannerite.The mineral form and occurrence state are suitable for CO2+O2neutral leaching.Uranium leaching and migration intensity are positively correlated with ore grade,injection and extraction ratio,oxidation intensity and HCO3-ion concentration.During the solid-liquid-gas interactions in the CO2+O2in-situ leaching system,the migration intensity of various elements is different.49.6%-53.1%of Fe were oxidized,inflowed into solution and finally precipitated from the solution.17.6%of S in uranium ores migrated from mineral to solution and existed in the form of SO42-.The Ca migrated from the mineral phase to the solution under the action of CO2.When the p H value was higher than 6.6,it precipitated again.The migration intensity of K,Na,Mg and Al were weaker than Fe and S.During the field leaching test,HCO3-ion arrived in pumping wells from injecting wells within 14 or 15 days.After 60 days,it can form the stable seepage field controlled by injecting.H-ion arrived in pumping wells within 26 days,which lagged behind the HCO3-ion.It can form stable weakly acidic chemical fields after 110 days.HCO3-and H+ion are good indicators for stability seepage field and weak acidic chemical field.The front line of HCO3-and SO42-arrived at the pumping well at the same time.It shows the migration of these components is unimpeded.The migration of H+,Ca2+and Mg2+lagged behind the solution seepage,reflecting that H+was consumed and Ca2+?Mg2+precipitated in the migration.Controlling the amount of CO2and O2at 550?700 mg/L and 200?300 mg/L,the HCO3-concentration can be kept in 800 mg/L,p H value kept between 6.2 to 6.5,Eh value kept higher than 200 m V.It can satisfy the effective leaching and migration for uranium.It can avoid calcium sulfate and calcium carbonate precipitation.It is a reasonable technological parameter for Mengqiguer deposit.
Keywords/Search Tags:sandstone type uranium deposit, CO2+O2in-situ leach uranium mining, mechanism of uranium leaching, solute migration
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