Sunday, 29 March 2020

Uranium Minerals



Kadapa district of Andhra Pradesh

Oxidative pressure leaching of uranium from a dolomitic limestone ore:
India has a medium-tonnage, low-grade uranium ore deposit of siliceous dolomitic phosphatic limestone type, in Kadapa district of Andhra Pradesh. Detailed exploration carried out in a stretch of about 9 km in this area, established a resource of 29000 t of U3 O8 with a cut-off grade of 0.025% U3 O8. Mineralogical studies on an exploratory mine ore sample from this area, indicated the occurrence of uranium values predominantly as ultra-fine dissemination, in lighter gangue minerals (specific gravity less than 3.2). It also occurs, albeit to a minor extent, in the form of ultra-fine pitchblende in association with pyrite, as disseminations in collophane-rich parts, coffinite and as U-Ti complex. Carbonate minerals constitute the major gangue present in the form of dolostone (~80%). Siliceous minerals in the ore are quartz, feldspar and chlorite (13%). Collophane (4%) is the only phosphate bearing phase. Pyrite is the predominant sulphide ore mineral, along with few grains of chalcopyrite and galena. The iron bearing oxides are magnetite, ilmenite and goethite. Heavy media separation of various closely-sized feed fractions, using bromoform (BR) and methylene iodide (MI) liquids, have indicated that about 91% of the uranium values are present in lighter minerals (specific gravity <3.2), as ultra-fine disseminations. The remaining 9% of uranium values reported in methylene iodide heavy fraction, are accounted by discrete pitchblende, which is mostly associated with pyrite and collophane. Pitchblende occurring with pyrite is present as fine orbicular cluster, separated by thin disconnected rims of pyrite or as garlands around pyrite.

Leaching Chemistry of Uranium Minerals
The common oxidation states of uranium, in its minerals like uraninite, pitchblende, coffinite and numerous others, are +4 and +6. Amongst the two oxidation states, U+6 is soluble in aqueous media under suitable EH – pH conditions, while U+4 is practically insoluble. The uranium minerals occurring in various ore deposits consist predominantly of uranous ion (U+4), necessitating the use of an oxidant and other lixiviants, for quantitative dissolution during leaching. The type of leaching - acid or alkaline mode depends upon the host rock. Sulfuric acid is the common leachant in acid leaching process, while Na2 CO3 - NaHCO3 , (NH4 ) 2CO3 and NH4 HCO3 are the widely used lixiviants in alkaline leaching of uranium ores. The oxidant reagents could be either chemical or gaseous in nature. A typical chemical reaction in alkaline leaching of UO2 with carbonate ions and oxidant (X) is given in Equation 1, a similar equation can be written for the sulfuric acid leaching process. UO2 + 3CO3 -2 + X  [UO2(CO3) 3 ] -4 + X-2 .
Atmospheric alkaline leaching studies, carried out on this ore sample, by varying important process parameters like mesh-of-grind, temperature, contact time, dosages of leachants - sodium carbonate and sodium bicarbonate, solids concentration and type of oxidant, gave a maximum U3O8 leachability of 65%. Studies with other oxidants like NaOCl, Cu-NH3, oxygen and air gave poor leachability in comparison to KMnO4, emphasizing the need for strong oxidizing conditions during the dissolution process. However, as KMnO4 cannot be used as an oxidant on commercial scale due to its expensive nature, the only alternative is to carryout the leaching reaction in a pressure reactor, using a gaseous oxidant. Since the solubility of oxygen diminishes with increasing temperature, adoption of higher partial pressure aids in increased dissolved oxygen concentration. Detailed analysis of the leach residue obtained in the atmospheric leaching experiments indicated, that uranium values associated with pyrite are not completely leached at temperatures <1000 C. Further, some of the locked-up uranium values in various gangue phases, require more aggressive diffusion conditions for penetration of the leachant to the desired mineral interface. Both these requirements can be realized only at elevated temperature and under sustained oxidizing conditions, possible in an autoclave reactor. Leaching at elevated temperature and pressure was initially carried out in a laboratory, 5 liter S.S. autoclave reactor equipped with necessary instrumentation and control to maintain preset temperature, overpressure and agitation speed of the impeller. All the autoclave leaching experiments were carried out, at optimum dosage combination of sodium carbonate and sodium bicarbonate evolved in atmospheric leaching, that is - 50 kg/ton and - 70 kg/ton respectively. The autoclave leaching studies mainly addressed the dissolution of uranium associated with pyrite and the scope of replacing KMnO4 with industrial oxygen. Figs. 3 and 4, illustrate the effect of temperature and contact time on the leachability of uranium values, observed under aggressive conditions. About 75% of uranium values were leached at a reaction temperature of 125 - 130°C in 3 h of contact time, using a feed ground to 65% weight finer than 200#. Increasing the fineness of grind in -200# to 85% showed, an enhancement in leachability to about 80%. Based on these results, large-scale leaching studies were carried out, both on batch and continuous leach reactor, to generate necessary scale-up and engineering data for industrial scale reactor, besides verifying the reproducibility of results at higher-scale of operation. Both the batch and cigar type continuous reactor were of 850 liter capacity with inconel 600 as material of construction. Largescale studies confirmed the results generated in batch scale experiments. At present, DAE is setting-up a 3000 tpd capacity uranium mill at site, wherein two 720 m3 capacity autoclave reactors with inconel 600 cladding for the wetted parts will be used. This will be the first uranium plant, using autoclave leaching technology in India.

Wednesday, 25 March 2020

Uranium extraction of its ore



Uranium extraction of its ore

Leaching

Roasted uranium ores are leached of their uranium values by both acidic and alkaline aqueous solutions. For the successful operation of all leaching systems, uranium must either be initially present in the more stable hexavalent state or be oxidized to that state in the leaching process.
Acid leaching is commonly performed by agitating an ore-leach mixture for 4 to as long as 48 hours at ambient temperature. Except in special circumstances, sulfuric acid is the leachant used; it is supplied in amounts sufficient to obtain a final leach liquor at about pH 1.5. Sulfuric acid leaching circuits commonly employ either manganese dioxide or chlorate ion to oxidize the tetravalent uranium ion (U4+) to the hexavalent uranyl ion (UO22+). Typically, about 5 kilograms (11 pounds) of manganese dioxide or 1.5 kilograms of sodium chlorate per ton suffice to oxidize tetravalent uranium. In any case, the oxidized uranium reacts with the sulfuric acid to form a uranyl sulfate complex anion, [UO2(SO4)3]4-.
Uranium ores that contain significant amounts of basic minerals such as calcite or dolomite are leached with 0.5 to 1 molar sodium carbonate solutions. Although a variety of reagents has been studied and tested, oxygen is the uranium oxidant of choice. Typically, candidate ores are leached in air at atmospheric pressureand at 75° to 80° C (167° to 175° F) for periods that vary with the particular ore. The alkaline leachant reacts with uranium to form a readily soluble uranyl carbonate complex ion, [UO2(CO3)3]4-.



Treatment of uranium leachates

The complex ions [UO2(CO3)3]4- and [UO2(SO4)3]4- can be sorbed from their respective leach solutions by ion-exchange resins. These special resins—characterized by their sorption and elution kinetics, particle size, stability, and hydraulic properties—can be used in a variety of processing equipment—e.g., fixed-bed, moving-bed, basket resin-in-pulp, and continuous resin-in-pulp. Conventionally, sodium and ammonium chloride or nitrate solutions are then used to elute the sorbed uranium from the exchange resins.
Uranium can also be removed from acidic ore leach-liquors through solvent extraction. In industrial methods, alkyl phosphoric acids—e.g., di(2-ethylhexyl) phosphoric acid—and secondary and tertiary alkyl amines are the usual solvents. As a general rule, solvent extraction is preferred over ion-exchange methods for acidic leachates containing more than one gram of uranium per litre. Solvent extraction is not useful for recovery of uranium from carbonate leach liquors, however.



Precipitation of yellow cake

Prior to final purification, uranium present in acidic solutions produced by the ion-exchange or solvent-extraction processes described above, as well as uranium dissolved in carbonate ore leach solutions, is typically precipitated as a polyuranate. From acidic solutions, uranium is precipitated by addition of neutralizers such as sodium hydroxide, magnesia, or (most commonly) aqueous ammonia. Uranium is usually precipitated as ammonium diuranate, (NH4)2U2O7. From alkaline solutions, uranium is most often precipitated by addition of sodium hydroxide, producing an insoluble sodium diuranate, Na2U2O7. It can also be precipitated by acidification (to remove carbon dioxide) and then neutralization (to remove the uranium) or by reduction to less soluble tetravalent uranium. In all cases, the final uranium precipitate, commonly referred to as yellow cake, is dried. In some cases—e.g., with ammonium diuranate—the yellow cake is ignited, driving off the ammonia and oxidizing the uranium to produce uranium trioxide (UO3) or the more complex triuranium octoxide (U3O8). In all cases, the final product is shipped to a central uranium-purification facility.

Refining of yellow cake

Uranium meeting nuclear-grade specifications is usually obtained from yellow cake through a tributyl phosphate solvent-extraction process. First, the yellow cake is dissolved in nitric acid to prepare a feed solution. Uranium is then selectively extracted from this acid feed by tributyl phosphate diluted with kerosene or some other suitable hydrocarbon mixture. Finally, uranium is stripped from the tributyl phosphate extract into acidified water to yield a highly purified uranyl nitrate, UO2(NO3)2.

Conversion and isotopic enrichment

Uranyl nitrate is produced by the ore-processing operations described above as well as by solvent extraction from irradiated nuclear reactor fuel (described below, see Conversion to plutonium). In either case, it is an excellent starting material for conversion to uranium metal or for eventual enrichment of the uranium-235 content. Both of these routes conventionally begin with calcining the nitrate to UO3 and then reducing the trioxide with hydrogen to uranium dioxide (UO2). Subsequent treatment of powdered UO2with gaseous hydrogen fluoride (HF) at 550° C (1,025° F) produces uranium tetrafluoride (UF4) and water vapour, as in the following reaction:
This hydrofluorination process is usually performed in a fluidized-bed reactor.
Uranium tetrafluoride can also be fluorinated at 350° C (660° F) with fluorine gas to volatile uranium hexafluoride (UF6), which is fractionally distilled to produce high-purity feedstock for isotopic enrichment. Any of several methods—gaseous diffusion, gas centrifugation, liquid thermal diffusion—can be employed to separate and concentrate the fissile uranium-235 isotope into several grades, from low-enrichment (2 to 3 percent uranium-235) to fully enriched (97 to 99 percent uranium-235). Low-enrichment uranium is typically used as fuel for light-water nuclear reactors.
After enrichment, UF6 is reacted in the gaseous state with water vapour to yield hydrated uranyl fluoride (UO2F2 · H2O). Hydrogen reduction of the uranyl fluoride produces powdered UO2, which can be used to prepare ceramic nuclear reactor fuel






Saturday, 15 February 2020

History of chemical industry



Chemical industry

History of chemical industry

Sulfuric Acid
sulfuric acid, chemical compound, H2SO4, colorless, odorless, extremely corrosive, oily liquid. It is sometimes called oil of vitriol.

1749: The Sulfuric Acid began to be produced and manufactured with the use and application of the Leaden Condensing Chambers.


In 1746 John Roebuck developed the lead chamber process for the manufacture of sulfuric acid. Prior to this time, sulfuric acid had been produced in glass bottles several pounds at a time. But the lead chamber process could produce sulfuric acid by the ton.
In the original lead chamber process, sulfur and potassium nitrate are ignited in a room lined with lead foil. Potassium nitrate, or saltpeter is an oxidizing agent oxidizes the sulfur to sulfur trioxide according to the reaction:
6 KNO3(s) + 7 S(s) -----> 3 K2S + 6 NO(g) + 4 SO3(g)
The floor of the room was covered with water. When the sulfur trioxide reacted with the water, sulfuric acid was produced:
SO3(g) + H2O(l) -----> H2SO4(aq)
This process was a batch process and resulted in the consumption of potassium nitrate
In 1835, Joseph Gay-Lussac invented a process for recovering the nitrogen in nitrogen monoxide and recycling it to replace the saltpeter as a source of nitrogen.
4 NO(g) + O2(g) + 2 H2O(l) -----> 4 HNO2(l)
4 HNO2(l) + 2 SO2(g) -----> 2 H2SO4(aq) + 4 NO(g)
This accomplished two things simultaneously: it reduced the dependence on expensive saltpeter and at the same time sharply reduced nitrogen monoxide emissions. The only
requirement now for saltpeter was to make up for the lost nitrogen monoxide.

Lead Chamber Process

In the lead chamber process hot sulfur dioxide gas enters the bottom of a reactor called a Glover tower where it is washed with nitrous vitriol (sulfuric acid with nitric oxide, NO, and nitrogen dioxide, NO 2, dissolved in it) and mixed with nitric oxide and nitrogen dioxide gases; some of the sulfur dioxide is oxidized to sulfur trioxide and dissolved in the acid wash to form tower acid or Glover acid (about 78% H 2SO 4). From the Glover tower a mixture of gases (including sulfur dioxide and trioxide, nitrogen oxides, nitrogen, oxygen, and steam) is transferred to a lead-lined chamber where it is reacted with more water. The chamber may be a large, boxlike room or an enclosure in the form of a truncated cone. Sulfuric acid is formed by a complex series of reactions; it condenses on the walls and collects on the floor of the chamber. There may be from three to twelve chambers in a series; the gases pass through each in succession. The acid produced in the chambers, often called chamber acid or fertilizer acid, contains 62% to 68% H 2SO 4. After the gases have passed through the chambers they are passed into a reactor called the Gay-Lussac tower where they are washed with cooled concentrated acid (from the Glover tower); the nitrogen oxides and unreacted sulfur dioxide dissolve in the acid to form the nitrous vitriol used in the Glover tower. Remaining waste gases are usually discharged into the atmosphere.

Contact Process

In the contact process, purified sulfur dioxide and air are mixed, heated to about 450°C, and passed over a catalyst; the sulfur dioxide is oxidized to sulfur trioxide. The catalyst is usually platinum on a silica or asbestos carrier or vanadium pentoxide on a silica carrier. The sulfur trioxide is cooled and passed through two towers. In the first tower it is washed with oleum (fuming sulfuric acid, 100% sulfuric acid with sulfur trioxide dissolved in it). In the second tower it is washed with 97% sulfuric acid; 98% sulfuric acid is usually produced in this tower. Waste gases are usually discharged into the atmosphere. Acid of any desired concentration may be produced by mixing or diluting the products of this process.


1791: Nicolas LeBlanc patented the Leblac process, which was an industrial process for the production of soda ash (sodium carbonate) from sea salt (sodium chloride). In 1823, production of Soda Ash was started by a British Entrepreneur.


The Leblanc process was a batch process in which sodium chloride was subjected to a series of treatments, eventually producing sodium carbonate. In the first step, the sodium chloride was heated with sulfuric acid to produce sodium sulfate (called the salt cake) and hydrochloric acid gas according to the chemical equation


2 NaCl + H2SO4 Na2SO4 + 2HCl
This chemical reaction had been discovered in 1772 by the Swedish chemist Carl Wilhelm Scheele. Leblanc's contribution was the second step, in which the salt cake was mixed with crushed limestone (calcium carbonate) and coal and fired. In the ensuing chemical reaction, the coal (carbon) was oxidized to carbon dioxide, reducing the sulfate to sulfide and leaving behind a solid mixture of sodium carbonate and calcium sulfide, called black ash.
Na2SO4 + CaCO3 + 2 C → Na2CO3 + CaS + 2 CO2
Because sodium carbonate is soluble in water, but neither calcium carbonate nor calcium sulfide is, the soda ash was then separated from the black ash by washing it with water. The wash water was then evaporated to yield solid sodium carbonate. This extraction process was termed lixiviation.


1804: St. Rollox Chemical Works produced almost 10,000 tons of bleaching powder, improving exponentially its production of 52 tons in 1799. Created by Charles Tennant (who discovered the bleaching powder), it was considered as the first biggest chemical enterprise in the world.


The most common chlorine-based bleaches are:
Sodium hypochlorite (NaClO), usually as a 3–6% solution in water, usually called "liquid bleach" or just "bleach". Historically called "Javel water". It is used in many households to whiten laundry, disinfect hard surfaces in kitchens and bathrooms, treat water for drinking and keep swimming pools free of infectious agents.
Bleaching powder (formerly known as "chlorinated lime"), usually a mixture of calcium hypochlorite(Ca(ClO)
2),
calcium hydroxide (lime, Ca(OH)
2), and
calcium chloride (CaCl
2) in variable amounts.

Sold as a white powder or in tablets, is used in many of the same applications as sodium hypochlorite, but is more stable and contains more available chlorine.

1859: The first oil well is drilled successfully near Titusville, Pennsylvania. This oil well of 70 feet marked the beginning of the Petroleum Industry.

1855: Bejamín Silliman, from New Haven, Conneticut, obtained valuable products from the destillation of petroleum. Between these valuable products were the naphthalene, gasoline, tar and other solvents.

1918: Fritz Haber won and received the Nobel Prize for his work in the synthesis of ammonia.  Nevertheless, this method was adapted for its commercial use until 1930 by the german chemist Carl Bosh

1931: First appearance of the first synthetic rubber.

1933: The Imperial Chemical Industries, England, discovered the polyethylene.

1935: Wallace H. Carothers, Du Pont, discovered the nylon.

1937: Dow Chemical began to commercialize the polystyrene

1940: In United States the first synthetic rubber tire was produced

1943: USA produced the DDT (dichlorodiphenyltrichloroethane), which was used for its insecticidal properties



Sulfuric acid

Sulfuric acid is by far the largest single product of the chemical industry.

Chamber process for Sulphuric acid

When sulfur is burned in air, sulfur dioxide is formed, and this, when combined with water, gives sulfurous acid. To form sulfuric acid, the dioxide is combined with oxygen to form the trioxide, which is then combined with water. A technique to form the trioxide, called the chamber process, developed in the early days of the operation of the Leblanc process. In this technique the reaction between sulfur dioxide and oxygen takes place in the presence of water and of oxides of nitrogen. Because the reaction is rather slow, sufficient residence time must be provided for the mixed gases to react. This gaseous mixture is highly corrosive, and the reaction must be carried out in containers made of lead.


SO 2 + NO 2 + H 2 O → H 2 SO 4 + NO
NO + 1/2 O 2 NO2

Sodium carbonate

In 1775 the French Academy of Sciences offered an award for a practical method for converting common salt, sodium chloride, into sodium carbonate, a chemical needed in substantial amounts for the manufacture of both soap and glass. Nicolas Leblanc, a surgeon with a bent for practical chemistry, invented such a process. His patron, the duc d’Orléans, set up a factory for the process in 1791, but work was interrupted by the French Revolution. The process was not finally put into industrial operation until 1823 in England, after which it continued to be used to prepare sodium carbonate for almost 100 years.

Leblanc process

The first step in the Leblanc process was to treat sodium chloride with sulfuric acid. This treatment produced sodium sulfate and hydrogen chloride. The sodium sulfate was then heated with limestone and coal to produce black ash, which contained the desired sodium carbonate, mixed with calcium sulfide and some unreacted coal. Solution of the sodium carbonate in water removed it from the black ash, and the solution was then crystallized. From this operation derives the expression soda ash that is still used for sodium carbonate.
2 NaCl + H 2 SO 4 Na 2 SO 4 + 2 HCl
followed by conversion of the sulfate to soda with charcoal and chalk
Na 2 SO 4 + 2 C + CaCO 3 Na 2 CO 3 + CaS + 2 CO2
It was soon found that when hydrogen chloride was allowed to escape into the atmosphere, it caused severe damage to vegetation over a wide area. To eliminate the pollutionproblem, methods to convert the dissolved hydrogen chloride to elemental chlorine were developed. The chlorine, absorbed in lime, was used to make bleaching powder, for which there was a growing demand.
Because calcium sulfide contained in the black ash had a highly unpleasant odour, methods were developed to remove it by recovering the sulfur, thereby providing at least part of the raw material for the sulfuric acid required in the first part of the process. Thus the Leblanc process demonstrated, at the very beginning, the typical ability of the chemical industry to develop new processes and new products, and often in so doing to turn a liability into an asset.

The ammonia-soda (Solvay) process

The Leblanc process was eventually replaced by the ammonia-soda process (called the Solvay process), which was first practiced successfully in Belgium in the 1860s. In this process, sodium chloride as a strong brine is treated with ammonia and carbon dioxide to give sodium bicarbonate and ammonium chloride. The desired sodium carbonate is easily obtained from the bicarbonate by heating. Then, when the ammonium chloride is treated with lime, it gives calcium chloride and ammonia. Thus, the chlorine that was in the original sodium chloride appears as calcium chloride, which is largely discarded (among the few uses for this compound is to melt snow and ice from roads and sidewalks). The ammonia thus regenerated is fed back into the first part of the process. Efficient recovery of nearly all the ammonia is essential to the economic operation of the process, the loss of ammonia in a well-run operation being no more than 0.1 percent of the weight of the product.

NH 3 + H 2 O + CO 2 NH 4 HCO 3

NaCl + NH 4 HCO 3 NaHCO 3 + NH 4 Cl

2 NaHCO 3 Na 2 CO 3 + H 2 O + CO2

Electrolytic process

Later in the 19th century the development of electrical power generation made possible the electrochemical industry. This not clearly identifiable branch of the chemical industry includes a number of applications in which electrolysis, the breaking down of a compound in solution into its elements by means of an electric current, is used to bring about a chemical change. Electrolysis of sodium chloride can lead to chlorine and either sodium hydroxide (if the NaCl was in solution) or metallic sodium (if the NaCl was fused). Sodium hydroxide, an alkali like sodium carbonate, in some cases competes with it for the same applications, and in any case the two are interconvertible by rather simple processes. Sodium chloride can be made into an alkali by either of the two processes, the difference between them being that the ammonia-soda process gives the chlorine in the form of calcium chloride, a compound of small economic value, while the electrolytic processes produce elemental chlorine, which has nearly innumerable uses in the chemical industry, including the manufacture of plastic polyvinyl chloride, the plastic material produced in the largest volume. For this reason the ammonia-soda process, having displaced the Leblanc process, has found itself being displaced, the older ammonia-soda plants continuing to operate very efficiently but no new ammonia-soda plants being built.

Contact process

Lead is a material awkward to use in construction, and the process cannot deliver acid more concentrated than about 78 percent without special treatment. Therefore, the chamber process has been largely replaced by the contact process, in which the reaction takes place in a hot reactor, over a platinum or vanadium compound catalyst, a substance that increases the speed of the reaction without becoming chemically involved.

Sulfuric acid is manufactured in three stages

2 SO 2 + O 2 2SO 3

SO 3 + H 2 O → H 2 SO 4

Since the reaction of sulfur with dry air is exothermic, the sulfur dioxide must be cooled to remove excess heat and avoid reversal of the reaction

Carbon disulfide

Carbon disulfide is made by the reaction of carbon and sulfur. Carbon comes from natural gas, and the sulfur may be supplied in the elemental form, as hydrogen sulfide, or as sulfur dioxide. The chief uses of carbon disulfide are for the manufacture of rayon and for regenerated cellulose film. These two products are made in such large quantity that carbon disulfide is a heavy chemical, by any standard.

Nitric acid

By far the most important use of ammonia within the chemical industry is to produce nitric acid (HNO3). Nitrogen and oxygen can be made to combine directly with one another only with considerable difficulty. A process based on such a direct combination, but employing large quantities of electrical power, was in use in the 1920s and 1930s in Norway, where hydroelectric power is readily available. It has not proved economical in modern conditions.
Ammonia burns in air, or in oxygen, causing the hydrogen atoms to burn off, forming water and leaving free nitrogen. With the aid of a catalyst, platinum with a small percentage of the related metal rhodium, ammonia is oxidized to oxides of nitrogen that can be made to react with water to form nitric acid.
Nitric acid treated with ammonia gives ammonium nitrate, a most important fertilizer. Ammonium nitrate, moreover, is also an important constituent of many explosives. Three fundamental explosive materials are obtained by nitrating (treating with nitric acid, often in a mixture with sulfuric acid): cellulose, obtained from wood, gives cellulose nitrate (formerly called nitrocellulose); glycerol gives glyceryl trinitrate (formerly called nitroglycerin); and toluene gives trinitrotoluene, or TNT. Another explosive ingredient is ammonium picrate, derived from picric acid, the relationship of which appears more clearly in its systematic name, 2,4,6-trinitrophenol.
A minor but still important segment of the explosives industry is the production of detonating agents, or such priming compositions as lead azide [Pb(N3)2], silver azide (AgN3), and mercury fulminate [Hg(ONC)2]. These are not nitrates or nitro compounds, although some other detonators are, but they all contain nitrogen, and nitric acid is involved in their manufacture.