uranium balancing in narwaphar ore leaching

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Uranium balancing in Narwaphar ore leaching Y S Ladola 1 , S V Kadam 1 , K N Hareendran 1 , S Chowdhury 1 , S Biswas 1 S B Roy 1 , A B Pandit 2 1. Uranium Extraction Division, BARC, Mumbai 2. Institute of Chemical Technology (ICT), Mumbai Abstract Sulfuric acid is the most preferred leachant for the recovery of uranium from ores as it is cheap, less corrosive and produces anionic uranyl complex which makes the separation of uranium from other cationic gangue mineral easy using an anionic exchanger subsequently. Sulphuric acid leaching of Narwaphar (INDIA) uranium ore assisted with acoustic cavitation and without cavitation has been studied. The primary uranium minerals of Narwaphar ore are uraninite and pitchblende with minor presence of brannerite, allanite, xenotime and davidite. In this paper we have discussed selective leaching of uranium using sulphuric acid from Narwaphar uranium ore relative to other leachable compounds and material balance has been carried out around each of the leaching experiments. Material balance of uranium ore and also that of uranium leaching for with and without cavitation could be established within ±10%. Keywords: Uranium; Leaching; Material balance; Ore 1. Introduction Sulfuric acid leaching is the most commonly used practice for the recovery of uranium from its ores. The major disadvantage of nitric acid is that it dissolves considerable amount of gangue material along with uranium. Further nitric acid is 1

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Page 1: Uranium Balancing in Narwaphar Ore Leaching

Uranium balancing in Narwaphar ore leaching Y S Ladola 1, S V Kadam 1, K N Hareendran 1, S Chowdhury 1, S Biswas 1

S B Roy 1, A B Pandit 2

1. Uranium Extraction Division, BARC, Mumbai

2. Institute of Chemical Technology (ICT), Mumbai

Abstract Sulfuric acid is the most preferred leachant for the recovery of uranium

from ores as it is cheap, less corrosive and produces anionic uranyl complex which makes

the separation of uranium from other cationic gangue mineral easy using an anionic

exchanger subsequently. Sulphuric acid leaching of Narwaphar (INDIA) uranium ore

assisted with acoustic cavitation and without cavitation has been studied. The primary

uranium minerals of Narwaphar ore are uraninite and pitchblende with minor presence of

brannerite, allanite, xenotime and davidite. In this paper we have discussed selective

leaching of uranium using sulphuric acid from Narwaphar uranium ore relative to other

leachable compounds and material balance has been carried out around each of the

leaching experiments. Material balance of uranium ore and also that of uranium leaching

for with and without cavitation could be established within ±10%.

Keywords: Uranium; Leaching; Material balance; Ore

1. Introduction Sulfuric acid leaching is the most commonly used practice for the recovery of

uranium from its ores. The major disadvantage of nitric acid is that it dissolves

considerable amount of gangue material along with uranium. Further nitric acid is

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expensive compared to sulphuric acid. Sulfuric acid reacts with hexavalent uranium and

produces anionic uranyl sulphate complex which makes its separation easy from other

cationic gangue mineral in subsequent anion type ion exchange. Hydrochloric acid is not

preferred due its highly corrosive nature. Though carbonate leaching is more selective, it

is used mostly for treatment of ores, which contain higher acid consuming carbonate

minerals. Kinetics of carbonate leaching is slow and also carbonate does not attack

calcareous materials, which may be encapsulating uranium, necessitating fine grinding of

ore to achieve reasonable leaching rate [1] adding to grinding energy cost. In general

carbonates are costlier compared to acid.

Uranium was discovered in 1789 by Klaproth but it was only in the middle of the

nineteenth century it could find industrial application as pigment for glass, porcelain and

enamel. For about fifty years this remained the only field of uranium application. After

discovery of radium by the Curies at the end of the nineteenth century uranium ores were

treated more for their radium content and uranium itself was obtained as byproduct.

Exploration of the rich ores of the Belgian Congo and upper Katanga resulted in a

reduction of radium prices and closing down of the small uranium mines of Austria,

Portugal etc. in 1921. Discovery of rich ores in other countries reduced the monopoly of

Belgium to a considerable extent. By 1942 the Canadian mine operators were also

considering closure due to the depletion of high grade ore but the prospect of utilizing

nuclear fission for military purposes gave new impetus to uranium production here and

an extensive exploration program was undertaken which revealed several uranium

deposits in the Eldorado mining area as well as other parts of Canada. The phenomenal

increase in the demand for uranium in the post war period, for military and civilian

nuclear programs encouraged many countries to launch extensive prospecting for

uranium ores and rework the economics of reutilizing lean ore deposit. The result has

been, the discovery of extensive, though relatively poor, deposits but also new methods

of ore processing. Enhancement in the final uranium recovery and also the rate of

recovery of metal leaching by acoustic cavitation has been well documented [2, 3, 4].

From geological data it is known that uranium is as abundant as lead, about 4

ppm, in the earths crust. But because of the chemical reactivity of its ions and relative

solubility of many of its hexavalent compounds in aqueous solution it is found that

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uranium is widely dispersed and significant concentrations in the form of high grade

deposits are exceptional or rarity.

Uranium Ores can roughly be classified into five categories based on the chemical nature

of the embedded uranium minerals and their response to leaching

1) Ores containing tetravalent uranium: most of the world’s important deposits

contain a significant proportion of their uranium in the tetravalent form. The

important examples of this type are primary minerals like uraninite, pitchblende,

coffinite and uranothorite.

2) Ores containing hexavalent uranium: These minerals are the hydrated oxides like

gummite, phosphates like autonite and torbernite and vanadates like carnotite and

silicate.

3) Refractory uranium minerals: These ores are characterized by their resistance to

chemical attack. Davadite and brannerite are the examples of such ores.

4) Carbon associated uranium ore: Uranium occurs as an organo complex in

minerals

5) Phosphate associated uranium: Uranium is a common constituent of the phosphate

rocks. [5]

Narwaphar ore is uraninite type ore. Petrology of a lean Uranium ore sample from

Narwaphar is shown in Figure 1. Uranium is hosted in chlorite-sericite-quartz schist and

feldspathic schist. Sulphides are very low in this deposit. The primary uranium minerals

uraninite and pitchblende with minor presence of brannerite, allanite, xenotime and

davidite. Two types of uraninite are found in ore, one is irregular particles and aggregates

and the other as pore fillings in chlorite and sericite schists [6].

2. Experimental Procedure Uranium leaching experiments have been conducted with mechanical agitation

(Experiment No. 1) and with acoustic cavitation supported mechanical agitation

(Experiment No. 2 and 3). For Experiment 1 and 3, 30µm average particle size

Narwaphar ore is used and 200µm average particle size Narwaphar ore is used for

Experiment 2. Iron as FeSO4•7H2O was added at the beginning of experiment 2 and 3,

465g and 410g respectively. Experiments have been conducted under simulated plant

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conditions in a 30 liter batch reactor as shown in Figure 2. Ore slurry was prepared using

ore and water. Ore slurry was kept in suspension using 4 pitched blades down pumping

impeller (diameter 0.2m) rotating at 100 rpm in the reactor. Incase of experiment 2 and 3

slurry was circulated through the ultrasonic flow cell using a piston pump at a rate of

1.5m3/hr, giving pipe slurry velocity of 0.8 m/s ensuring no sedimentation during the

hydraulic transport. Cavitation was generated by 1kW radial ultrasonic horn arranged as a

flow cell. Concentrated H2SO4 and laboratory grade MnO2 were added in a controlled

manner in slurry mass to maintain required pH and Oxidation Reduction Potential (ORP).

pH and ORP were monitored using pH and ORP probes. These probes were attached to a

2 channel display. pH was maintained at 2.0 during initial 2 hr of experiment and at 1.8

for the rest of leaching period. ORP was maintained between 480-510 mV during the

experiment. At the end of experiment slurry was discharged through bottom valve and

collected in bucket. Leached liquor was decanted after settling of solid particles. Water

washes were given to the settled solids and the washings were filtered. For uranium

balance washing filters and residual solid was analyzed in addition to the leached liquor.

Particle size is measured by laser diffraction particle size analyzer CILAS 1180.

3. Analytical Methods 3.1 Uranium in ore and residue: Uranium content in the ore and residue samples have

been carried out as per the procedure followed by UCIL [7]. Weighed quantity of sample

is digested with hydrofluoric acid -nitric acid mixture and uranium in the resultant

solution is extracted with tri-n-butyl phosphate diluted with kerosene. Uranium from the

organic is stripped with sodium sulphate and the solution is made alkaline with sodium

hydroxide. Colour development is achieved by adding hydrogen peroxide and the

absorabance of this complex is measured at 380nm. The overall precision of this method

is within ±5% for analyzing the Uranium in ore and residue is also determined using

bromo-PADAP as the colour forming reagent [8]. In this procedure the sample is digested

with a mixture of nitric acid-hydrofluoric acid and the uranium is extracted using tri-octyl

phosphineoxide diluted with cyclohexane. Colour is developed in the organic phase using

1% solution of bromo-PADAP. Absorbance measurement is carried out at 574nm. The

precision of this method is also within ±5%.

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3.2 Uranium in leached liquor: Uranium in leached liquor is measured by

spectrophometric method using dibenzoyl methane as the chromogenic reagent [9].

Uranium is extracted into ethyl acetate medium using aluminium nitrate as a salting out

agent. Absorbance measurement is carried out at 395nm using 1 cm cells. The precision

of this method is known to be within ±3%.

3.3 Uranium in wash: Due to the low concentration of uranium in the washings the

above methods were not used for determination. A sequential ICP AES (Induction

Coupled Plasma Atomic Emission Spectroscopy) with a radial plasma and PMT detector

is used for this purpose. Two interference free lines of uranium (385.465nm and

409.014nm) are used for determination. The precision of this method is within ±5%.

3.4 Iron: Iron content of all the samples is carried out by o-phenanthroline

spectrophotmetric method. Absorbance measurements were carried out at 515nm. The

precision of the method is within ±5%.

Determination of uranium in ore and residue samples were also carried out by

neutron activation technique (NAA). For ore samples, the result of duplicate samples

differed significantly. In the case of residue samples the uranium values were found to be

significantly less than that obtained by other methods used. The analysis of uranium in

leached liquor did not match with uranium in leached liquor calculated based on ore and

residue analyses by NAA. Considering all this drawback result of NAA is not used for

material balance.

4. Results and discussion Material balance sheets show the uranium concentration and uranium content at

different stages of processing. It can be seen from the material balance sheets that

material balance is agreed within ±10% of uranium content in the ore. The unaccounted

uranium for Experiment 1 is 4.81%, for Experiment 2 is 9.43% and for Experiment 3 is

9.36%. This is attributed to the error in sampling, analysis and handling loss during the

experiments. Precision of analytical methods do not include sampling error. As ore and

residue are solid powder there is uncertainty in the draw of representative sample.

Considering the precision of different analytical methods used for uranium content

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estimation and sampling uncertainty the balance of uranium in all three experiments are

quite satisfactory. Leaching efficiency for Experiment 1 is 48%, for Experiment 2 is 58%

and for Experiment 3 is 61% on basis of overall material balance. Significant uranium is

recovered in washing in all experiments. Percentage recovery of uranium at each stage of

washing is summarized in Table 1. Though average particle size of residue is 30µm for

all experiments, the distribution of particle size is different. There is small peak in

submicron range in experiment 2 and 3; this peak shows the presence of finer particles.

Recovery of uranium during washes is different in all three experiments and total

recovery of uranium is varies from 10 to 20%. Balance of Fe is summarized in Table 2.

Unaccounted Fe is less than 15% in these experiments. This unaccountability is due to

sampling and analysis error as well as loss of material during experiments. Concentration

of Fe in Ore is 11-11.25% and leaching of Fe is less than 1% during experiments. Fe in

washing was not analyzed and this has resulted in the increase of unaccounted Fe. It has

been observed that when Fe concentration in the leached liquor is less, leaching of

uranium is also less. More than 80% of Fe added as FeSO4•7H2O has come out with the

solid residue. This may be due to precipitation of iron during settling of slurry mass in

settler. It has been observed that pH of decanted leached liquor is more than 3 even

though pH is maintained during experiment is 1.8. Rise of pH may be due to

consumption of acid by gangue minerals. These three experiments were conducted to

establish the uranium partitioning during leaching. Further studies are being continued to

quantify the effect of cavitation on uranium leaching and parameter optimization in

recovery of uranium from low grade ore.

5. Conclusion

Material balance of uranium ore leaching is found to agree within ±10% of

uranium content in ore. This is attributed to solid sample inhomogeneity, to the material

handling during experiment and washing inefficiency for finer. Methods used for analysis

of various samples are found to suffice the purpose, in respect of their precision.

Significant amount of uranium recovered in washing stages shows the importance of

washing for uranium recovery from the leached out ore. Uranium recovered by washes is

up to 19% of total input uranium. Material balance of iron in ore leaching operation is

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found to agree within 15% of input iron. Total recovery of uranium is 47%, 58% and

61%.

6. Acknowledgement The authors would like to thank Dr A K Suri, Director Material Group, BARC for

allowing to do this work. The authors would also like to acknowledge Uranium

Corporation of India Ltd. for providing ore material. First author would like to

acknowledge Shri A K Sarangi, Chief Superintendent (Geology) UCIL for providing

valuable literatures as well as Dr. P Sengupta, MSD, BARC for providing petrology of

the ore sample collected from Narwaphar mine and UED staff members for their help

and support for this work.

7. Reference 1. R C Merrit, ‘The extractive metallurgy of uranium’ Colorado Schools of mines

Research Institute, United States Atomic Energy Commission, Colorado (1971)

2. Balasubrahmanyam Avvaru, S.B. Roy, Yogesh Ladola, Sujit Chowdhury, K.N.

Hareendran and Aniruddha B. Pandit, ‘Sono-chemical leaching of uranium’,

Chemical engineering and processing: Process intensification, vol. 47 (2008) pp

2107-2113

3. K M Swamy, K S Rao, K L Narayana, J S Murthy and H S Ray, ‘Application of

ultrasound in leaching’, Min. Pro. Ext. Metal. Rev. 14, (1995) pp 179-192

4. V S Shastri and D J Mackinnon, ‘Some effects of ultrasonic and their applications in

metallic ore processing’ J. Scient. Ind. Res. Vol. 36, (1977) pp 379-385

5. K D Kamat and T K S Murthy, ‘Extraction of uranium from its ores – A Review’

proceedings of Symposium on uranium, held at Jaduguda, India, 18-20 January 1971

6. Personal communication with Shri A K Sarangi, Chief superintendent (Geology)

UCIL, India.

7. Departmental Quality Control Manual, UCIL/DQM/CR&D/ANALYSIS

8. T.M.Florence and D.A.Jhonson, ‘Analytical procedure for determination of uranium’

Anal.Chim.Acta, 53 (1971) pp 73-79

9. “Analytical techniques in uranium exploration and ore processing” IAEA TecDoc

314 (1992)

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Lower grade ore (E3 Stope ore)

Feldspar

Magnetite

Uraninite

Figure 1: Narwapahar Uranium ore: Petrography (Reflected light)

Piston pump

Flow cell

Reactor

Agitator

Figure 2: Experimental set up for ore leaching with acoustic cavitation

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U: 1.65 g

Residue

Separation

Water/Acid Volume: 12 liter

Leach Solution Volume: 8.9 L U: 0.185 g/L

Reactor

ORE Weight: 10.7 kg U: 0.0466%

Wash-1

Wash-1 liquorVolume: 3.6 LU: 0.0783g/L

Residue

Wash-2

Wash-2 liquorVolume: 4.0 LU: 0.0525g/L

Residue

Wash-3

Wash-3 liquorVolume: 4.1 LU: 0.0258g/L

Residue

Residue

Wash-5

Wash-5 liquorVolume: 4.2 LU: 0.0074g/L

Residue

Residue

Wash-4

Wash-4 liquor Volume: 4.75 L U: 0.012g/L

Dry Residue 10.7 kg U: 0.027%

U: 4.99 g

U: 0.28 g

U: 0.21 g

U: 0.11 g

U: 0.06 g

U: 0.03 g

U: 2.89 g Input U: 4.99 g Output U: 1.65 g+0.28 g+0.21 g+0.11 g+ 0.06 g+0.03 g+ 2.89 g = 5.23 g Unaccounted : 4.99 g – 5.23 g = -0.24 g % Unaccounted : (0.24÷4.99)X100 = 4.81%

33%

5.6%

4.2%

2.2%

1.2%

0.6%

Figure 3: Material balance sheet for experiment 1

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Residue

Separation

Water/Acid Volume: 17 L

Leach Solution Volume: 17.5 L U: 0.20 g/l

Reactor

ORE Weight: 17 kgU: 0.043%

Wash-1

Wash-1 liquorVolume: 4.9 LU: 0.10g/L

Residue

Wash-2

Wash-2 liquor Volume: 5.05L U: 0.043g/L

Residue

Wash-3

Wash-3 liquor Volume: 4.95 LU: 0.005g/L

Residue Residue

Dry Residue 17 kg U: 0.014%

Input: U: 7.31 g

U: 3.50 g

U: 0.49 g

U: 0.22 g

U: 0.03 g

U: 2.38 g

Input U: 7.31 g Output U: 3.50 g+0.49 g+0.22 g+0.03 g+2.38 g = 6.62 g Unaccounted : 7.31 g – 6.62 g = 0.69 g % Unaccounted : (0.69÷7.31)X100 = 9.43%

6.7%

47.9%

3.0%

0.4%

Figure 4: Material balance sheet for experiment 2

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U: 1.705 g

Residue

Separation

Water/Acid Volume: 12.9 liter

Leach Solution Volume: 8.4L U: 0.203 g/L

Reactor ORE

Weight: 12 kg U: 0.034%

Wash-1

Wash-1 liquor Volume: 4.95 LU: 0.100g/L

Residue

Wash-2

Wash-2 liquor Volume: 4.65 L U: 0.043g/L

Residue

Wash-3

Wash-3 liquorVolume: 5.0 LU: 0.005g/L

Residue

Residue

Wash-5

Wash-5 liquorVolume: 3.6 LU: 0.005g/L

Residue

Residue

Wash-4

Wash-4 liquor Volume: 4.95 L U: 0.008g/L

Dry Residue 12 kg U: 0.01%

U: 4.080 g

U: 0.495 g

U: 0.200 g

U: 0.025 g

U: 0.040 g

U: 0.018 g

U: 1.2 g Input U: 4.080 g Output U: 1.705 g+0.495 g+0.20 g+0.025 g+ 0.040 g+0.018 g+0.015 g+ 1.2 g = 3.698 g Unaccounted : 4.080 g – 3.698 g = 0.382 g % Unaccounted : (0.382÷4.080) X100= 9.36%

Residue

Wash-5

Wash-5 liquorVolume: 5.0 LU: 0.003g/L

U: 0.015 g

41.8%

12.1%

4.9%

0.6%

1.0%

0.4%

0.4%

Figure 5: Material balance sheet for experiment 3

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Table 1: Recovery of uranium during washing at each stage Experiment 1 Experiment 2 Experiment 3 % recovery % recovery % recovery

Leached Liquor 33 47.9 41.8 Wash 1 5.6 6.7 12.1 Wash 2 4.2 3.0 4.9 Wash 3 2.2 0.4 0.6 Wash 4 1.2 ------ 1.0 Wash 5 0.6 ------ 0.4 Wash 6 ------ ------ 0.4

Total of wash 13.8 10.1 19.1 Table 2: Iron Balance (without accounting for washes)

Experiment 1 Input (g) Output (g)

Fe in Ore 1204.8 Fe in Residue 1177.0

Fe added as FeSO4 7H2O 0.0 Fe in leached liquor 0.1

Total 1204.8 Total 1177.1 Difference in input and Output 2.3%

Experiment 2 Input (g) Output (g)

Fe in Ore 1912.5 Fe in Residue 1740.8

Fe added as FeSO4 7H2O 92.3 Fe in leached liquor 11.4

Total 2004.8 Total 1752.2 Difference in input and Output 12.6%

Experiment 3 Input (g) Output (g)

Fe in Ore 1320.0 Fe in Residue 1584.1

Fe added as FeSO4 7H2O 81.4 Fe in leached liquor 14.3

Total 1401.4 Total 1598.4 Difference in input and Output 14.1%

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