Fertilizer material from apatite

Abstract

Apatite is conventionally made into a fertilizer material by treatment with a strong acid, requiring capital-intensive industry. Hydroxyapatite is treated above 1100 C. with alkali but world reserves are problematic. The invention treats apatite at 900 C. with sodium aluminosilicate/carbonate and siliceous material in quantities to keep the composition in terms of CaO, SiO.sub.2, Na.sub.2 O and P.sub.2 O.sub.5 in or near the ternary system Ca.sub.2 SiO.sub.4 --Ca.sub.3 (PO.sub.4).sub.2 --CaNaPO.sub.4.

Description

This invention relates to making a fertilizer material from apatite. Apatite is an insoluble phosphorus-containing mineral, approximating to Ca.sub.5 (PO.sub.4).sub.3 (F,OH,CI,1/2CO.sub.3), and the phosphate content must be rendered soluble for fertilizer use.

Apatite, the most abundant terrestial form of phosphorus, is conventionally treated with a strong acid such as nitric or sulphuric acid to render the phosphate soluble. This requires a capital-intensive industry.

Another known way of treating apatite is the `Rhenania process` described in British Patent Specification 301022. The apatite is mixed with Na.sub.2 CO.sub.3 to give a molar ratio of Na.sub.2 CO.sub.3 /P.sub.2 O.sub.5 .perspectiveto.1.0, while at the same time sufficient SiO.sub.2 is also added to combine with excess CaO. The reactants are ground together and calcined in a rotary kiln at 1100 C.-1200 C. for approximately 2 hours. Fluorine is said to be retained in the process, although steam is sometimes admitted to the kiln before 1000 C. is reached in an attempt to remove at least part of the fluorine. The sintered product may be used directly as a slow-release source of P or it may be subsequently extracted with hot aqueous Na.sub.2 CO.sub.3 solution, giving either Na.sub.3 PO.sub.4 or Ca.sub.3 (PO.sub.4).sub.2. This process requires high temperatures, and hydroxy-rich apatite, which is indigenous to central Europe and occurs in a few other regions of the world, some of which are of questionable reliability.

Hard mineral apatite (richer in chlorine/fluorine) is widely available in Sri Lanka, India and East Africa and is often a by-product from other mining operations. The present invention seeks to make fertilizer material from such apatite at a lower temperature than the 1100 C.-1200 C. required in the Rhenania process and without using acid. Sri Lanka is understood to have an indigenous alkali (NaOH) industry. (While it does also produce hydrochloric acid, this is not a suitable acid for treating apatite). The alkali is readily convertible to sodium carbonate. To make fertilizer material from apatite according to the present invention requires siliceous material, and this is also widely available as quartz, sand or potash felspar (an alkali metal aluminosilicate). Addition of the last-named in small proportions also has the advantage of introducing available K.sub.2 O, and the same might be said of mica.

Accordingly, the present invention is a method of making a fertilizer material from apatite, by roasting apatite at up to 1100 C. with a carbonate and/or aluminosilicate of an alkali metal in an amount such that the molar ratio apatite (as P.sub.2 O.sub.5): alkali metal is 1: at least 3 and in the presence of sufficient siliceous material to keep the free-lime content of the fertilizer material below 2 weight % and to inhibit formation of tetracalcium phosphate.

The molar ratio apatite:alkali metal is preferably from 1:3 to 1:10, more preferably 1:3 to 1:5, for example 1:4.

The molar ratio apatite:siliceous material (as SiO.sub.2) is preferably from 1:0.75 to 1:1.0.

The roasting temperature is preferably below 1000 C., and desirably at least 800 C., more preferably at least 850 C., most preferably from 880 C., to 950 C., for example 900 C. The duration of roasting need not exceed 2 hours, and is preferably at least 1 hour.

Preferably the apatite, the siliceous material and the carbonate and/or aluminosilicate are pressed together (e.g. pelletised) before the roasting. This appears to enhance the rate of reaction.

The invention extends to the fertilizer material made as set forth above, optionally admixed with other agriculturally acceptable components.

The reasons for avoiding excessive free lime and tetracalcium phosphate (i.e. why siliceous material is added) are as follows: Free lime is capable of causing skin burns, reacts with moisture thereby causing caking and may make the fertilizer, and hence the soil, too alkaline. The phosphate in tetracalcium phosphate Ca.sub.4 P.sub.2 O.sub.9 is all soluble, i.e. it is at first sight an ideal fertilizer material. However, Ca.sub.4 P.sub.2 O.sub.9 is liable to conversion in the presence of water vapour, which is likely in a fossilfuel-fired tunnel kiln, to CaO (or Ca(OH).sub.2) plus insoluble hydroxyapatite, one of the very materials which the present invention was devised to solubilise.

In practice, the quantities of Na.sub.2 O/K.sub.2 O and SiO.sub.2 (which must be added in order to eliminate the above undesirable phases) are desirably the minimum, as an excess would result in too much dilution of the phosphate phases. A way of determining these is to consider the CaO- and P.sub.2 O.sub.5 -rich regions of the system CaO-Na.sub.2 O-P.sub.2 O.sub.5 -SiO.sub.2. The plane of compositions lying between Ca.sub.2 SiO.sub.4, Ca.sub.3 (PO.sub.4).sub.2 and CaNaPO.sub.4 just fulfils the condition that CaO and Ca.sub.4 P.sub.2 O.sub.9 should be absent and, furthermore, we find that this plane of compositions constitutes a true ternary system at subsolidus temperatures. Its position within the quaternary system is shown in the accompanying drawing.

Table 1 records the results of solubility determinations made on pure single-phase preparations. For present purposes availability is defined by the relation: ##EQU1## The experimental method for determining the 2%-citric-acid-soluble P.sub.2 O.sub.5 is given in the Appendix. Ground mineral apatite is poorly soluble: typically only 17-18% of its P.sub.2 O.sub.5 content is `available`.

Amongst the phases having 100% available P.sub.2 O.sub.5 are Ca.sub.4 P.sub.2 O.sub.9, nagelschmidtite, silicocarnotite, rhenanite (a range of solid solutions around CaNaPO.sub.4), and an .alpha. Ca.sub.2 SiO.sub.4 solid solution containing typically 30 wt % Ca.sub.3 (PO.sub.4).sub.2. The presence of silica in solid solution in rhenanite appears to activate the dissolution of phosphate. Moreover, phase A is not completely soluble unless it too contains silica in solid solution; Phase A is explained in the footnote to Table 3. Both .alpha. and .beta. Ca.sub.3 (PO.sub.4).sub.2 give less than 100% available P.sub.2 O.sub.5. Moreover, while Ca.sub.4 P.sub.2 O.sub.9 has 100% availability, it is (as already mentioned) readily converted to hydroxyapatite by annealing in air, whereby the available P.sub.2 O.sub.5 falls to 20%. Attempts to form a solid solution, substituting two Na.sup.+ ions for Ca.sup.++ ions, in the hope that Ca.sub.4-x Na.sub.2x P.sub.2 O.sub.9 would be less reactive to water vapour than the Ca.sub.4 P.sub.2 O.sub.9, were unavailing.

CaNa.sub.6 P.sub.2 O.sub.9 was found to be 100% extractable, but is hygroscopic and therefore undesirable.

TABLE 1______________________________________RESULTS OF SOLUBILITY STUDIES P.sub.2 O.sub.5 SOLUBLE SOLUBILITY IN 2% AS PERCENT CITRIC OF TOTALSAMPLE ACID P.sub.2 O.sub.5______________________________________.beta. Ca.sub.3 (PO.sub.4).sub.2 34.0 74.alpha. Ca.sub.3 (PO.sub.4).sub.2 36.6 80Ca.sub.4 P.sub.2 O.sub.9 38.9 100Ca.sub.4 P.sub.2 O.sub.9 heated at 1000.degree. C. in air 7.8 20Ca.sub.5 (SiO.sub.4) (PO.sub.4).sub.2 30.1 100Ca.sub.7 (SiO.sub.4).sub.2 (PO.sub.4).sub.2 21.9 100.alpha.-Ca.sub.2 SiO.sub.4 ss containing Ca.sub.3 (PO.sub.4).sub.2[Composition = 70.0 wt % Ca.sub.2 SiO.sub.4 ] 14.0 100Phase A - Ca.sub.5 Na.sub.2 (PO.sub.4).sub.4 40.1 90Phase A ss containing SiO.sub.2[Composition = 20 wt % Ca.sub.2 SiO.sub.4,40% Ca.sub.3 (PO.sub.4).sub.2, 40% CaNaPO.sub.4 ] 36.4 100.beta. CaNaPO.sub.4 45.0 100.alpha. CaNaPO.sub.4 ss containing SiO.sub.2[Composition = 10 wt % Ca.sub.2 SiO.sub.4,10% Ca.sub.3 (PO.sub.4).sub.2, 80% CaNaPO.sub.4 ] 40.5 100CaNa.sub.6 P.sub.2 O.sub.9 36.9 100Sri Lanka Apatite Sample (1) 6.3 17Sri Lanka Apatite Sample (2) 6.2 18______________________________________ Note: ss = solid solution; Sri Lanka apatite sample (1) is a sample of pure apatite from the "leached zone" in the deposit at Eppawela, Sri Lanka. Sample (2) is a commercially beneficiated sample of apatite from Eppawela Sri Lanka. For explanation of Phase A, see footnote to Table 3.

As for the influence of halogens, chlorine is almost entirely eliminated during the firing of apatite-containing batches, although most of the fluorine is retained. The fluorine is believed to be present in solid solution in phases which are soluble in citric acid. When these phases are dissolved in citric acid, fluorine is probably present in the solution in the form of fluorosilicate complexes.

The invention will now be described by way of example. The accompanying drawing shows a corner of the quaternary system CaO-Na.sub.2 O-P.sub.2 O.sub.5 -SiO.sub.2. The plane Ca.sub.3 (PO.sub.4).sub.2 -Ca.sub.2 SiO.sub.4 -CaNaPO.sub.4 has been marked out. Compositions on this plane contain neither CaO nor Ca.sub.4 P.sub.2 O.sub.9, and accordingly are desirable.

Mineral apatite (minus 100 mesh BS) was reacted with Na.sub.2 CO.sub.3 and SiO.sub.2 (quartz, minus 120 mesh). The apatite was taken from the "leached zone" of the deposit: Table 2 gives a complete analysis typical of the concentrate as well as partial analysis of the particular batch of apatite concentrate used in this study. Microscopically, the apatite occurs as anhedral grains, most of which are monocrystals.

TABLE 2______________________________________CHEMICAL COMPOSITION OF SRI LANKA APATITE Sample EP/N/J Sample used inwt % from the leached zone.sup.(a) the Examples______________________________________CaO 55.30 --SrO 1.18 --MgO 0.01 --MnO 0.01 --Fe.sub.2 O.sub.3 0.08 --SiO.sub.2 0.40 --P.sub.2 O.sub.5 40.75 38.10F 1.78 1.70CI 2.29 2.20______________________________________ .sup.(a) Analysis reported by the Geological Survey Department, Colombo 2 Sri Lanka (1973). The two samples were believed to be essentially identical. Reaction batches were prepared by blending these raw materials and firing following a heating rate of 5 C./min at a constant temperature for 2 hours. Table 3 records the results of the annealing treatments. The phases present were determined by X-ray powder diffraction but the limit of detection of unreacted apatite was as high as 5%.

In the absence of SiO.sub.2, mixtures of apatite and Na.sub.2 CO.sub.3 react to produce large amounts of free CaO. Therefore, as free CaO is deemed to be an undesirable constituent, it is essential to add something to combine with it: SiO.sub.2 fulfils this role.

Much of the reaction is completed swiftly, even though this apatite is comparatively coarse-grained. As a rough guide, batches having a molar ratio of apatite to Na.sub.2 CO.sub.3 from 1:1.5 to 1:2.0 (i.e. apatite:alkali metal=from 1:3 to 1:4) gave the most rapid reaction at low temperatures. These batch proportions correspond to a weight percentage of Na.sub.2 CO.sub.3 between 20 and 27%. Some excess sodium carbonate was tolerable. If the optimum proportions of all three components are considered, molar ratios of apatite:Na.sub.2 CO.sub.3 :SiO.sub.2 close to 1:2:1 are favourable for reaction. If the SiO.sub.2 content is reduced slightly below this optimum, for example to 1:2:3/4, a high yield of available phosphorus is obtained, but free CaO is also developed. Similarly, reduction of the sodium carbonate content leads to incomplete reaction and the appearance of unreacted apatite which can only be removed by sintering at 1100.degree.-1300.degree. C.

Table 3 shows the various compositions tried. Examples 1 to 3 are according to the invention. Examples A to K are not according to the invention. Example 1 is shown prior to Example K. It will be seen that few of Examples A to K gave any significant reaction below 1100.degree. C., and of those which did, either inadequate phosphate was solubilised (as H) or free lime and sometimes a hygroscopic product resulted (as C and D). The phases present are given roughly in the order: most first.

TABLE 3______________________________________AVAILABLE P.sub.2 O.sub.5 CONTENT OF SINTERSMADE WITH APATITE______________________________________ COMPOSITION Molar ratio Weight percentExample No Apatite:Na.sub.2 CO.sub.3 :SiO.sub.2 Apatite Na.sub.2 CO.sub.3 SiO.sub.2______________________________________A 1:1:0 82.9 17.1 0.0B 2:3:0 76.3 23.7 0.0C 1:2:0 71.0 29.0 0.0D 1:10:0 32.9 67.1 0.0E 5:2:8 78.6 6.5 14.9F 4:2:3 85.1 8.1 6.8G 10:8:3 82.9 14.2 2.9H 13:10:11 79.4 12.7 7.9J 1:1:1 75.5 15.6 8.91 4:6:3 71.5 22.2 6.3K 2:3:3 67.3 20.9 11.82 4:8:3 66.6 27.5 5.93 1:2:1 65.3 27.0 7.7______________________________________ 2% CITRIC ACID SOLUBILITY Wt Per- Percent PHASES PRESENTEX. TEMP. cent out of (See abbreviationsNO. .degree.C. P.sub.2 O.sub.5 Total P.sub.2 O.sub.5 below)______________________________________A 1100 20.5 55 .beta. R + CaO + F ap 1300 28.5 76 .beta. R + .alpha.R + CaO + F apB 900 23.0 67 .beta. R + .alpha.R + CaO + F ap 1100 27.8 81 .beta. R + .alpha.R + CaO + F ap 1300 29.5 86 .beta. R + .alpha.R + CaO + F apC 900 31.4 90 .beta. R + CaNa.sub.6 P.sub.2 O.sub.9 + CaO + tr. F ap 1100 35.0 100 .beta. R + CaO 1300 34.7 100 .beta. R + CaOD 900 16.6 100 CaO + CaNa.sub.6 P.sub.2 O.sub.9E 1100 8.0 23 F ap + .alpha.R + .beta.R 1300 14.4 42 F ap + AF 1100 9.8 27 F ap + .alpha.R + .beta.R 1300 15.8 43 F ap + AG 1100 18.1 49 .beta. R + F ap + CaO 1300 18.8 51 .beta. R + F ap + CaOH 900 10.0 36 F ap + .beta. R 1100 16.5 59 .beta. R + F ap 1300 20.4 73 A + .beta.C.sub.3 P + F apJ 1100 18.8 55 .beta. R + F ap 1300 25.1 74 A + .beta.R + F ap1 900 21.7 67 .beta. R + .alpha.R + F ap 1100 29.7 91 .beta. R + .alpha.R + F ap 1300 30.0 92 .beta. R + .alpha.R + F apK 1100 21.8 70 .beta. R + F ap 1300 24.9 80 .beta. R + F ap2 900 27.0 92 .alpha.R + .beta.R + CaO + tr. F ap 1100 30.4 100 .beta.R + .alpha.R + CaO 1300 31.1 100 .beta.R + .alpha.R + CaO3 900 25.5 91 .alpha.R + .beta.R + tr. F ap 1100 28.1 100 .alpha.R 1300 28.6 100 .alpha.R______________________________________ Abbreviations: R = Rhenanite, CaNaPO.sub.4 ; F ap = Fluorapatite, Ca.sub. (PO.sub.4).sub.3 F (all remaining apatite having this composition); tr. = trace. .alpha. and .beta. are the high and low temperature forms respectively. C.sub.3 P = tricalcium phosphate. Phase A is believed to approximate to Ca.sub.5 Na.sub.2 (PO.sub.4).sub.4 and is the crystalline phase defined b Ando and Matsuno (J. Ando and S. Matsuno, Bull. Chem. Soc. Japan 41 (1968 342.) In the present context, Phase A solid solutions may also contain th silicon.

APPENDIX

Determining the 2%-citric-acid-soluble P.sub.2 O.sub.5 in a sample:

The sample is ground to pass a 100 mesh BS sieve. A 1.0 g sample is extracted with 100 ml of 2% citric acid in a mechanical shaker operating at 260 oscillations per minute for 30 minutes at 18 C. The resultant solution is filtered under vacuum using a sintered glass crucible (porosity No. 4) and the filtrate P.sub.2 O.sub.5 content is determined by the vanadomolybdate method, in which the following reagents are used:

(i) Ammonium metavanadate solution, prepared by dissolving 1.12 g of ammonium metavanadate in a mixture of 240 ml of concentrated HClO.sub.4 acid and 260 ml of water. (ii) Ammonium molybdate solution, prepared by dissolving 35 g of ammonium molybdate in 500 ml of water. (iii) Standard phosphate solution, 0.2 mg/ml P.sub.2 O.sub.5, prepared by dissolving 0.3835 g of dried potassium dihydrogen phosphate in 1 liter of water. Solutions (i) and (ii) are stable and will keep for some months.

To a 2 ml aliquot of sample filtrate are added 10 ml of the vanadate solution (i) and 10 ml of the molybdate solution (ii) successively, mixing well after the addition of each reagent. The resultant solution is diluted with water in a 100 ml volumetric flask.

After 30 minutes the absorbance is measured at 460 nm using a Unicam SP 600 colorimeter against a reagent blank solution. The standard phosphate solution (iii) is used in calibration.

Claims

1. A method of making a fertilizer material from hard mineral apatite rich in chlorine and/or fluorine, by roasting apatite at from about 880.degree. C. to about 900.degree. C. as a final temperature with a carbonate and/or aluminosilicate of an alkali metal in an amount such that the molar ratio apatite (as P.sub.2 O.sub.5):alkali metal is 1: at least 3 and in the presence of sufficient siliceous material to keep the free-lime content of the fertilizer material below 2 weight % and to inhibit formation of tetracalcium phosphate.

2. A method according to claim 1, wherein the molar ratio apatite:alkali metal is from 1:3 to 1:10.

3. A method according to claim 2, wherein the molar ratio apatite:alkali metal is from 1:3 to 1:5.

4. A method according to claim 1, wherein the molar ratio apatite:siliceous material (as SiO.sub.2) is from 1:0.75 to 1:1.0.

5. A method according to claim 1, wherein the duration of the roasting does not exceed 2 hours.

6. A method according to claim 1, wherein the duration of the roasting is at least 1 hour.

7. A method according to claim 1, further comprising pressing together the apatite, the siliceous material and the carbonate and/or aluminosilicate before the roasting.