THE EFFECTS OF pH AND Ca/P RATIO ON THE PRECIPITATION OF CALCIUM PHOSPHATE Y. SONG, H. H. HAHN, AND E. HOFFMANN* Institute for Aquatic Environmental Engineering, University of Karlsruhe, Adenauerring 20, Karlsruhe, D-76128, Germany Email: Erhard.Hoffmann@bau-verm.uni-karlsruhe.de ABSTRACT Phosphorus recovery from wastewater accords with the principle of sustainability and meets the needs of phosphate industry and water industry. Studies aiming at understanding of the precipitation of calcium phosphate from wastewater are essential to the technologies of phosphorus recovery. In the present paper, a chemically defined system with a low phosphate concentration of 20 miligrammes phosphorus per liter and an ionic strength, expressed as conductivity of 2.0 milisiemens per centimeter, which was equivalent to wastewater was designed to study the effects of pH value and Ca/P ratio on the precipitation of calcium phosphate. The precipitation experiments were undertaken in a batch system at pH values ranging from 7.50 to 11.00 and initial Ca/P ratios ranging from 1.67 to 6.67 at a constant temperature of 21.5°C. It is found that both the increasing of pH value and the increasing of initial Ca/P ratio of the precipitating system favour the precipitation efficiency and precipitation rate of calcium phosphate. At initial Ca/P ratios of 1.67 and 3.33 the lowest pH values to achieve fast precipitation are 9.00 and 8.50, respectively; at initial Ca/P ratios above 5.00, fast precipitation can be achieved at pH 8.00. At the pH values ranging from 7.50 to 8.00, after a reaction time of 90 minutes a special acceleration phenomenon was also observed, where a fairly high precipitation efficiency could be achieved finally. The effects of pH value and initial Ca/P ratio on the precipitation of calcium phosphate are due to their influences on the supersaturations of the precipitating systems. Keywords: phosphorus recovery, precipitation, pH value, initial Ca/P ratio INTRODUCTION needed to remove carbon dioxide by addition of concentrated (96%) sulphuric acid, accordingly the pH value of the influent is reduced to Phosphorus is an essential element to all living organisms and its 3 to release carbon dioxide and then raised up to about 9 to utilisation has promoted the development of agriculture and precipitate. This is a necessary step to a full process, however this industry, but the modern society does not use phosphorus resources will increase the complexity and the cost of the process, especially in in a sustainable way: phosphates are manufactured from phosphate- the area where the influent contains much carbonate. Besides containing rock, then are consumed in agriculture and industry, carbonate, magnesium, organic matter and other components may finally go into soil, rivers and the sea. This, on one hand, is also affect the precipitation or crystallisation process of calcium exhausting the limited phosphate deposits which are unevenly phosphate. It seems that a thorough understanding of the process distributed in the world, on the other hand, has caused conditions for the precipitation and crystallisation of phosphate is eutrophication of water bodies. With the increasing concern at indispensable to mature technologies for phosphorus recovery. sustainability, more stringent nutrient discharge limits, and more From the viewpoint of industry, to recover phosphorus as calcium restrictions on sludge disposal, both wastewater treatment industry phosphate is promising [2]. The calcium phosphate formation can be and phosphate industry have to consider the alternatives of induced with high calcium concentration and raised pH by adding conventional phosphorus removal technologies and opportunities for lime, phosphorus recovery. environmental problems. Calcium phosphate is just the component Considerable world-wide researches have been undertaken on phosphorus recovery technologies, of which some are already in pilot-scale. From the viewpoint of availability, the crystallisation which is inexpensive, readily available and free of of phosphate rock, so if it is recovered in a suitable physical form it should be a good raw material both to industry and to agriculture. Calcium phosphates occur extensively in natural aquatic processes of calcium phosphate and magnesium ammonium environments, biological fluids, and in processes of technological phosphate hexahydrate (struvite) have been emphatically studied, interests [3], and are studied in several fields: water geochemistry, and a number of technologies such as the DHV CrystalactorTM sedimentary mineralogy, fertilisers and food industry, osteology, Pelletiser, the CSIR Fluidised Bed Crystallisation Column, the Kurita urology, etc [4]. One active field for calcium phosphates studies is Fixed Bed Crystallisation Column etc. have been obtained [1]. In physiology, for these compounds are very important to the biological these technologies, some techniques such as Phostrip are used to systems like bone and teeth which consist mainly of an apatitic extract phosphate from wastewater, then phosphate is precipitated calcium phosphate [5]. Synthetic calcium hydroxyapatite has been and/or crystallised in dedicated reactors such as fluidised bed, fixed taken as an ideal biomaterial because of its bio-compatibility. bed reactors, finally useful end products are obtained. Although Numerous studies have been undertaken on the precipitation and these technologies are successful from the viewpoint of research, crystallisation of calcium phosphates [5-22]. Generally, when calcium many problems on their application and popularization still remain. phosphate precipitates from a system which contains total calcium Taking the DHV CrystalactorTM Pelletiser, one of these technologies and total phosphate each higher than 10 milimoles per liter (mmol.l-1 used to recover phosphate as calcium phosphate as an example, the ) and at pH values greater than 6.8, the precipitation is always presence of carbonate can affect the crystallisation, so a degassifier is preceded by the formation of an amorphous precursor, distinct both Y. SONG, H. H. HAHN, AND E. HOFFMANN chemically and structurally from the final product, hydroxyapatite addition volume was recorded. Aliquots of 15 ml for calcium and (HAP) Ca5(PO4)3OH [18], and this follows the Ostwald Rule of Stages phosphate analyses were removed at frequent intervals after mixing, in Precipitation [23]. Afterwards the precipitate transforms through and filtrated with glassfibre filters (Sartorius AG). The calcium some intermediate states to the thermodynamically stable product, concentration of the filtrate was analysed by complexometric HAP crystal. The formation and transformation may be influenced by method, and the phosphate concentration was analysed by supersaturation, pH values, magnesium [12,16,19], etc. Although so molybdenum many efforts have been made to elucidate the mechanisms of wavelength of 700 nanometers with a Lambda 2 UV/VIS formation, initiation of growth and transformations between Spectrometer (Perkin Elmer). different mineral forms, very few mechanisms have heteropolyphosphate complex method at the been All the above reactant solutions were prepared from Analytical unanimously accepted. Besides, most of these studies focused on the Grade reagents. The water used in the experiments was deionized physiological conditions, i.e. at pH 7.4 and temperatures around water which has a conductivity of 0.7 microsiemens per centimeter. 37°C. All the experiments were performed at 21.5 ± 0.5°C. To recover phosphorus from wastewater as calcium phosphate, the chemical and physicochemical factors which may influence the precipitation process should be investigated. These factors may be: CALCULATION OF SPECIES CONCENTRATION— the compositions of the influent to a recovery process including SUPERSATURATION concentrations of phosphate, calcium, magnesium, organic matter and carbonate, the pH value and temperature of the influent, etc. Under proper physical and chemical environment, different kinds Moreover it is noticeable that the composition of wastewater might of calcium phosphate phases (Table 1) may precipitate from be different in different areas. In the former studies of our group [1, saturated solutions. The supersaturation (S) of a system with respect 24], valuable engineering experiences for phosphorus recovery as to a given calcium phosphate phase indicates the thermodynamically calcium phosphate were obtained and the wastewater characteristics at Darmstadt-Eberstadt Sewage Treatment Works were investigated. Table 1. Calcium phosphate phases It has been found that further understanding of precipitation and Phases crystallisation of calcium phosphate from the system containing 10 to Dicalcium phosphate 50 miligrammes phosphorus per liter (mg P.l-1) is of high importance dihydrate to improve and optimise the recovery process and equipment. The present work has been undertaken in order to study the effects of two operational factors, pH value and initial Ca/P ratio on the Abbreviation Composition Ca/P DCPD CaHPO4.2H2O 1.00 Octacalcium phosphate OCP Ca4H(PO4)3.3H2O 1.33 Tricalcium phosphate TCP Ca3(PO4)2 1.50 Hydroxyapatite HAP Ca5(PO4)3OH 1.67 precipitation of calcium phosphate. Considering the characteristics of wastewaters, a chemically defined system containing 20 mg P.l-1 was driving force of the precipitation reaction. It is defined as designed, within which practical knowledge on precipitation of calcium phosphate has been obtained. Ionic activity product (IP) in solution S = , Solubility product (Ksp) (i) EXPERIMENTS where the following IP’s of different calcium phosphate are defined, The precipitaion of calcium phosphate was initiated by the rapid mixing of CaCl2 and K2HPO4 or KH2PO4 solutions. Experiments were IPHAP performed by adding 500 mililiters (ml) of 2.151, 4.296, 6.450, and = ([Ca2+]f2)5([PO43-]f3)3(Kw/[H+])f1 (ii) 8.600 mmol.l-1 CaCl2 to 500 ml of 1.290 mmol.l-1 K2HPO4 or KH2PO4 IPOCP within 30 seconds, in order to get Ca/P ratios of 1.67, 3.33, 5.00, and = ([Ca2+]f2)4([PO43-]f3)3[H+]f1 (iii) 6.67, respectively. The reverse order of addition was also used with IPTCP no change in results, so the former order of addition was used = ([Ca2+]f2)3([PO43-]f3)2 (iv) throughout the experiments. Prior to mixing, the pH of each of the IPDCPD reagents was adjusted to a value between 7.50 and 11.00 at an = [Ca2+]f2[HPO42-]f2. (v) interval of 0.50 by the addition of NaOH or HCl, as needed. In order to keep the ionic strength of the precipitation system similar to Moreover, a saturation index (SI) is defined as wastewater, 1.01 grammes KNO3 was added to the CaCl2 solution prior to mixing, to arrive at a concentration of 0.01 mole per liter SI = log(S) (vi) (mol.l-1) after mixing. The initial mixing was under strong stirring by a HI 200M magnetic stirrer (Hanna Instruments) for 3 minutes (min), to facilitate further discussion. afterwards solutions were stirred at a constant reproducible rate. The The calculation of ionic activity product necessitates a detailed change in pH with time, after mixing, was monitored with a PH 191 knowledge of the chemical speciation of the ions in solution. pH meter (WTW GmbH) and solutions were maintained at above Assuming that no precipitation has taken place just after mixing, the constant pH values by the addition of 0.45 mol.l -1 NaOH, and the ions, ion-pairs and equilibria listed in Table 2 should be taken into 2 Y. SONG, H. H. HAHN, AND E. HOFFMANN account in the present precipitating system. As an approxiamation, written in FORTRAN, and the activity coefficients were calculated the influence of the dissolved CO2 from atmosphere to the according to Davies equation [5] precipitating system is ignored. The thermodynamic dissociation and -logf z association constants are also given in Table 2. The calculations were = AZ 2 {I 1/2 /(1 + I 1/2 ) – 0.3I}, – 9.221 (vii) performed by an iterative method [5, 35] with a computer program Table 2. Species, equilibria and constants used in the calculation of supersaturation a Equilibrium H3PO4 pK Reference H+ pK = 799.31/T – 4.5535 + 0.013486T [25] H2PO4- HPO42- + H+ pK = 1979.5/T – 5.3541 + 0.019840T [26] HPO42- PO43- + H+ pK = 12.42 0.010 at 20°C [27] H2O H+ + OH- pKw = 4471.33/T + 0.017053T – 6.0846 [28] H2PO4- + pK = -6.462 at 25°C [29] Ca2+ + HPO42- CaHPO40 pK = 148.15 – 22188/T – 0.2554T [30] Ca2+ + H2PO4- CaH2PO4+ pK = 53.335 – 8413.5/T – 0.08660T [30] Ca2+ + OH- CaOH+ pK = -1.356 [31] Ca5(PO4)3OH(s) 5Ca2+ + 3PO43- + OH- pKHAP = 8219.41/T + 1.6657 + 0.098215T [32] Ca4H(PO4)3.3H2O(s) pKOCP = 50.606 at 20°C [13] Ca3(PO4)2(s) 3Ca2+ + 2PO43- pKTCP = 45723.26/T – 287.4536 + 0.546763T [33] CaHPO4.2H2O(s) Ca2+ + HPO42- + 2H2O pKDCPD = 3649.6/T – 18.181 + 0.04203T [34] Ca2+ + PO43- CaPO4- 4Ca2+ + 3PO43- + H+ + 3H2O a T is the temperature (K), Kw is the ionic product of water, and KHAP, KOCP, KTCP, and KDCPD are the solubility products for HAP, OCP, TCP, DCPD, respectively. (pK = - log10K). where I is the ionic strength, and A has a value of 0.505 at 21.5°C. C0 The calculated values for supersaturation help to understand and – Ct = 7.659 ln(t) (ix) interpret the precipition of calcium phosphate where C0 (mmol.l-1) is initial concentration of phosphate in solution and Ct (mmol.l-1) is the concentration of phosphate in solution at RESULTS reaction time t (min). A transformation is obtained by differentiating the above equation The Effect of pH Value on the Precipitation of Calcium Phosphate - dCt/dt = 7.659 1/t (x) For the convenience of discussion, a precipitation efficiency (t), where 0 (t) 100%, is defined as = (C0 – C t) / C0 100% 0.7 Precipitated P (mmol.l-1) (t) where –dCt/dt is the precipitation rate of phosphate, and 7.659 is a (viii) where Ct is the concentration of phosphate at reaction time t and C 0 is the initial concentration of phosphate in solution. This ratio of precipitated phosphate to the initial phosphate in solution also indicates the extent of the precipitation reaction. Figure 1 shows the effect of pH value on the precipitation of 0.6 0.5 pH 11.0 pH 10.5 pH 10.0 pH 9.50 pH 9.00 pH 8.50 pH 8.00 0.4 0.3 0.2 0.1 0 phosphate. In Figure 1a where the initial Ca/P ratio is 1.67, the 0 precipitated phosphate is plotted as a function of reaction time at 30 different pH values ranging from 8.00 to 11.00. At a given pH value the precipitated phosphate increases with the proceeding of the 60 90 120 150 Reaction time (minutes) a. 180 constant related to the reaction conditions including supersaturation, reaction. With the increasing of pH value the (t) improves evidently. Within a reaction time of 180 min, the higher the reaction pH value is, the higher the (t) is. Considering the difference of the precipitation Precipitated P (mmol.l-1) 0.7 processes, three situations can be distinguished. At pH 8.00 the (t) is so low that it is less than 8.0% within a reaction time of 180 min. At pH 8.50 the precipitation reaction can be precisely described by an empirical kinetic equation as 0.6 pH 11.0 pH 10.5 pH 10.0 pH 9.50 pH 9.00 pH 8.50 pH 8.00 pH 7.50 0.5 0.4 0.3 0.2 0.1 0 3 0 30 60 90 120 150 Reaction time (minutes) b. 180 Y. SONG, H. H. HAHN, AND E. HOFFMANN pH value and temperature. It is found that the precipitation rate is Figure 1. The effect of pH value on the precipitation of phosphate. inversely proportional to the reaction time. At pH 9.00, the (a), initial Ca/P ratio 1.67; (b), initial Ca/P ratio 3.33. precipitation of phosphate is very fast at the beginning, but afterwards the precipitation rate slows down although the (t) still increases. Unlike the situation of pH 8.50 where the precipitation reaction advances gradually, the precipitation reactions at pH values from 9.00 to 11.00 are fast reactions, which arrive at high efficiencies 100 10 min Precipitation efficiency (%) Precipitation efficiency (%) within 10 min, and the values of (t) depend on pH values. 180 min 80 60 40 20 0 11 10.5 10 9.5 pH value a. 9 8.5 10 min 100 180 min 80 60 40 20 0 8 11 10.5 10 9.5 9 pH value b. 8.5 8 7.5 Figure 2. The comparison of precipitation efficiencies at reaction time of 10 minutes and 180 minutes. Ca/P ratio of the precipitate Ca/P ratio of the precipitate (a), initial Ca/P ratio 1.67; (b), initial Ca/P ratio 3.33. 4 pH 11.0 pH 10.5 pH 10.0 pH 9.50 pH 9.00 pH 8.50 3 2 1.67 30 60 90 120 150 pH 11.0 pH 10.5 pH 10.0 pH 9.50 pH 9.00 pH 8.50 pH 8.00 3 2 1.67 1 0 4 1 0 180 30 60 90 120 150 180 Reaction time (minutes) b. Reation time (minutes) a. Figure 3. The Ca/P ratios of the precipitate. (a), initial Ca/P ratio 1.67; (b), initial Ca/P ratio 3.33. This can be seen more clearly from Figure 2, in which the values of 11.00. With the increasing of pH value the (t) improves evidently, (t) at reaction times of 10 min and 180 min are compared. Figure 1b too. Here again three different situations can be distinguished. At pH plots the precipitated phosphate as a function of reaction time, where 7.50 the (t) is low, only less than 5.0% within a reaction time of 180 the initial Ca/P ratio is 3.33 and the pH values ranging from 7.50 to min. When pH 8.50, fast precipitation reactions occur and the 4 Y. SONG, H. H. HAHN, AND E. HOFFMANN values of (t) also depend on pH values. An interesting phenomenon Figure 4. The effect of the initial Ca/P ratio of solution on the appears at pH 8.00: at first the precipitation advanced gradually, but precipitation of phosphate. (a), pH 9.00; (b), pH 8.00; (c), pH 7.50. after a reaction time of 90 min the precipitation reaction accelerated, The effect of the initial Ca/P ratio of solution on the Ca/P ratio of at the reaction time of 180 min the (t) became so high that it got close to the reaction where pH value was 9.00. The above phenomenon deserves special attention. 0.70 Precipitated P (mmol.l-1) Besides the precipitated phosphate, the precipitated calcium and the base consumption of the precipitation process versus reaction time also show the same tendency as shown in Figure 1. This, on one hand, confirms the result of the phosphate precipitation, on the other hand, improves our understanding of the precipitation of calcium phosphate. According to the precipitated calcium and phosphate, the Ca/P ratio of the precipitate can be calculated, and the results are 0.60 0.50 0.40 0.30 Ca/P 1.67 Ca/P 3.33 Ca/P 5.00 0.20 0.10 0.00 illustrated in Figure 3. It can be found that both at initial Ca/P ratio 0 of 1.67 and of 3.33, if the pH value is as high as 9.00 and 8.50, 30 respectively, to realise fast precipitation, the precipitates will have Ca/P ratios ranging from 1.2 to 2.0, and at the reaction time of 180 60 90 120 Reaction time (minutes) a. 150 180 150 180 150 180 min will get close to 1.67, the Ca/P ratio of HAP. At a given pH value, with the proceeding of the precipitation reaction, the Ca/P 0.70 Precipitated P (mmol.l-1) ratio of the precipitate has an increasing tendency. But under the pH value of fast precipitation, i.e. where the precipitation reaction advances gradually and where acceleration phenomenon exists, the Ca/P ratio of the precipitate may be higher than 2.0, even above 3.0 at the early stage of the reaction. With the proceeding of the precipitation reaction, the Ca/P ratio goes down, and tends to get close to 1.67. The above evolution phenomenon of Ca/P ratio means that no matter what kind of precipitation process the reaction follows, the final precipitate tends to transform Ca/P Ca/P Ca/P Ca/P 0.60 0.50 1.67 3.33 5.00 6.67 0.40 0.30 0.20 0.10 0.00 to 0 30 thermodynamically stable calcium phosphate, HAP. Precipitated P (mmol.l-1) The Effect of the Initial Ca/P Ratio of Solution on the Precipitation of Calcium Phosphate Figure 4 shows the effect of the initial Ca/P ratio of solution on the precipitation of calcium phosphate at pH values of 9.00, 8.00, and 7.50. In Figure 4a where the pH value is 9.00, the precipitation reactions are all fast. With the increasing of initial Ca/P ratios from 1.67 to 5.00 the precipitated phosphate increases, so the precipitation 60 90 120 Reaction time (minutes) b. 0.70 Ca/P 5.00 0.60 Ca/P 6.67 0.50 0.40 0.30 0.20 0.10 0.00 efficiency (t) improves, but the efficiency is not simply directly 0 proportional to the initial Ca/P ratio. In Figure 4b where the pH value is 8.0, the precipitation reactions show the typical acceleration characteristic which has already been shown in Figure 1b. With the 30 60 90 120 Reaction time (minutes) c. the precipitate is shown in Figure 5. In Figure 5a where pH value is increasing of initial Ca/P ratio the (t) improves. At the initial Ca/P 9.00, it can be found that higher initial Ca/P ratio does not produce ratio of 1.67 the (t) was low; at the initial Ca/P ratios 3.33, precipitate with higher Ca/P ratio, but on the contrary. When the acceleration phenomena appeared in all the reactions after the initial Ca/P ratios are 1.67, 3.33, and 5.00, the corresponding reaction time of 90 min, and finally comparatively high precipitation precipitates at the reaction time of 180 min have Ca/P ratios of 1.85, efficiencies were achieved. The outstanding situation appeared at the 1.73, and 1.51, respectively, which are still in the transformation initial Ca/P ratio of 3.33: at the early stage of the reaction it fell far process to HAP. In Figure 5b where pH value is 8.00, when the initial behind the reactions which have higher initial Ca/P ratios, but after Ca/P ratio is 3.33, the precipitate has the highest Ca/P ratio, and the reaction time of 90 min it accelerated so much that the (t) at 180 when the initial Ca/P ratios are 5.00 and 6.67 the precipitates have min got close to the reactions with higher initial Ca/P ratios. In similar Ca/P ratios. At the reaction time of 180 min, all the Figure 4c where the pH value is 7.50, the situations with initial Ca/P precipitates obtained from reactions with different initial Ca/P ratios ratios of 5.00 and 6.67 are shown. It is worth noticing that at the have Ca/P ratios close to HAP. The above results indicate that initial initial Ca/P ratio of 6.67, an obvious acceleration phenomenon is also Ca/P ratio may influence the precipitation rate and efficiency, but the observed. This is similar to the situation of pH 8.00. final precipitates tend to have stoichiometric compositions of HAP. 5 Y. SONG, H. H. HAHN, AND E. HOFFMANN except DCPD, which has a very low S value and the corresponding SI Ca/P ratio of the precipitate is not shown. The SI with respect to HAP is nearly directly proportional to pH value. The SI with respect to OCP increases with 3 Ca/P 1.67 Ca/P 3.33 Ca/P 5.00 the increasing of pH value until pH 9.50, above which begins to decrease slightly, and so is the situation of TCP, which arrives at a highest SI value at pH 10.50. According to the Ostwald Rule of Stages 2 in Precipitation, although HAP is the most thermodynamically stable 1.67 species, it does not occur first and studies have shown that OCP is the main precipitating phase at medium supersaturations [5]. In the present studies the SI with respect to OCP is taken to discuss the 1 0 30 60 90 120 150 precipitation reactions. Comparing Figure 6a with Figure 1a, at pH 180 8.00 the SI is only 5.95, so (t) is low; at pH 9.00 the SI is 7.49 and fast Reaction time (minutes) a. precipitation occurs; at pH 8.50 where SI is 6.86, precipitation advances gradually. Comparing Figure 6b with Figure 1b, at pH 7.50 Ca/P ratio of the precipitate where SI is 5.81, (t) is low; at pH 8.50 where SI is 7.78, fast precipitation occurs; at pH 8.00 where SI is 6.93, a special acceleration Ca/P 3.33 Ca/P 5.00 Ca/P 6.67 3 phenomenon appears. Figure 6. The effect of pH value on the supersaturation. (a), initial Ca/P ratio 1.67; (b), initial Ca/P ratio 3.33. 2 Through 1.67 the above comparisons, can be found that, occurence and precipitation efficiency of calcium phosphate. It is 1 0 30 60 90 120 150 noticeable that after the fast precipitation of the early stage, the 180 following precipitation becomes very slow (Figure 2), this is because Reaction time (minutes) b. the supersaturation of the solution has decreased to a low level, the driving force is not so strong any more. The present experiment is Figure 5. The effect of the initial Ca/P ratio of solution on the Ca/P only a batch system without phosphate and calcium supplement ratio of the precipitate. (a), pH 9.00; (b), pH 8.00. 25 Saturation index DISCUSSION The Effect of pH Value on the Supersaturation of Calcium Phosphate The precipitation of calcium phosphate from solution is a base uptake process. Because the process is related to the equilibria listed in Table 2, the uptake of base promotes the dissociation of the hydrogen-containing phosphate species, then promotes HA P OCP TCP 20 15 10 5 0 the 7.5 8 8.5 precipitation of calcium phosphate. To a given precipitating system without base addition, the pH value will decrease with the proceeding of the precipitation reaction. In the present experiments, 9 9.5 pH value b. 10 10.5 11 during the reaction, so the fast precipitation rate can not continue. the pH value of the precipitating system is kept constant by base However, at a continuous system the fast precipitation could be kept, addition, so the pH value of the system affects the speciation of provided that suitable pH value and concentrations of phosphate and phosphate and the quantity of the base uptake during the calcium permit. From the above discussion it can be found that the precipitation. The effect of pH value on the precipitation of calcium pH value of the precipitating system influences the supersaturation, phosphate can be analysed by the calculation of the supersaturation then the precipitation rate and efficiency. of the precipitating system. Figure 6 plots the initial SI values with respect to different kinds of The Effect of the Initial Ca/P Ratio on the Supersaturation of Calcium calcium phosphate phases. It is found that the present precipitating Phosphate systems are highly supersaturated with respect to HAP, OCP, TCP, Figure 7. 20The effect of initial Ca/P ratio on the supersaturation. (a), 20 25 HA HAPP HA P OCP TCP 20 pH 8.00; (b), pH 7.50.OCP OCP TCP TCP 15 15 Saturation Saturation index index Saturation index it thermodynamically driving force, supersaturation accounts for the 15 10 5 6 0 7.5 8 8.5 9 9.5 pH value a. 10 10.5 11 10 10 55 00 11 22 33 44 55 Initial Ca/P ratio Initial Ca/P ratio a. b. 66 77 Y. SONG, H. H. HAHN, AND E. HOFFMANN precipitation efficiency can be obtained at low pH values such as 8.00 Figure 7 shows the effect of initial Ca/P ratio of the solution on the and 7.50. supersaturation of calcium phosphate. The SI values are directly proportional to the initial Ca/P ratio. At pH 8.00 the SI values with The Composition of the Precipitate respect to OCP are 5.95, 6.93, 7.45, and 7.77 at initial Ca/P ratios of 1.67, 3.33, 5.00, and 6.67, respectively. Comparing this with Figure 4b, From Figure 3 and 5, it is found that the Ca/P ratio of the it can be found that at initial Ca/P ratios of 5.00 and 6.67, the SI precipitate continuously changes with the proceeding of the values are high enough, so at first fast precipitations occurred, then precipitation. If the reaction is a fast precipitation, the Ca/P ratio of the reaction proceeded slowly until the reaction time of 90 min, after the precipitate will increase slightly to arrive at a value close to 1.67; which the acceleration phenomenon appeared. At pH 7.50 and initial if the reaction advances gradually or accelerates after a second phase Ca/P ratios 3.33, the SI values are so low that the values of (t) are forms, the initial Ca/P ratio of the precipitate may be fairly high, also low; at initial Ca/P ratios of 5.00 and 6.67, where the SI values with the proceeding of the reaction, the Ca/P ratio decreases and has are 6.35 and 6.70, respectively, acceleration phenomena appears, too. the tendency to get to 1.67. The present precipitating system is a The increasing of the initial Ca/P ratio increases the supersaturation complex system, for several mineral phases with different Ca/P of the precipitating system, so the thermodynamically driving force ratios may occur in the precipitation process, and the formed phases of the precipitation becomes stronger. may transform to other phases, so the calculated Ca/P ratio is a comprehensive reflection of the above reactions. For this reason, it is difficult to distinguish the precipitated mineral phases only The Accelaration Phenomena at pH 8.00 and 7.50 according to the Ca/P ratio. In the precipitating process the new As stated before, at a precipitating system with pH 8.00 or 7.50, if precipitates had developed surface area, in the gradually advanced the SI value with respect to OCP is suitable, an acceleration reaction or the reaction containing the acceleration phenomenon, phenomenon will appear after the reaction time of 90 min. In the excessive calcium ions might be adsorbed by the new precipitates, present experiments, at pH 8.00 with initial Ca/P ratios from 3.33 to thus causing the high Ca/P ratios of the precipitates, especially at the 6.67 (SI values from 6.93 to 7.77), and at pH 7.50 with initial Ca/P early stage of the reactions. With the proceeding of the reaction, more ratios from 5.00 to 6.67 (SI values from 6.35 to 6.67), acceleration phosphate was combined to precipitate to the solid phase, then the phenomena are observed after the reaction time of 90 min, and the Ca/P ratio of the precipitate went down to get close to the final precipitation efficiency after a reaction time of 180 min may get stoichiometric value of the HAP. close to or even surpass the reactions with high pH values (Figure 1b). Although the above phenomenon occurs at certain SI value, it CONCLUSIONS seems a characteristic of this special pH range, from 7.50 to 8.00. One evidence is that at initial Ca/P ratio of 1.67, although the SI values In the present paper, a chemically defined system with a low with respect to OCP are 6.86, 7.48, and 7.72 at pH values of 8.50, 9.00, phosphate concentration of 20 mg P.l-1 and an ionic strength and 9.50, respectively, no acceleration phenomena are observed. In a kinetic study on the precipitation of calcium phosphate, Van equivalent to wastewater was designed to study the effects of the pH Kemenade and De Bruyn [5] used a parameter, relaxation time t R, to value and the initial Ca/P ratio of solution on the precipitation of study the precipitation kinetics. To a single growing phase in a calcium phosphate. It is found that both the increasing of solution pH precipitating system, the relaxation time is the time from zero to the value and the increasing of initial Ca/P ratio favour the precipitation inflection point of the sigmoidal kinetic curve, where the efficiency and precipitation rate of calcium phosphate. The precipitating rate reaches its maximum value. In a comlex- precipitating system with an initial Ca/P ratio of 1.67, the precipitating system where the precipitation involves the growth of stoichiometric Ca/P ratio of HAP, will realise fast precipitation at pH more than one phase, the kinetic curve may have more than one value of 9.00; if the initial Ca/P ratio increases to 3.33, the pH value inflection to indicate the formation of different phases, so relaxation to achieve fast precipitation will decrease to 8.50. At a given pH time for each precipitating phase can be defined. To a given value, the increasing of the initial Ca/P ratio increase the precipitating system, the relaxation time of a certain phase is highly precipitation efficiency and the precipitation rate. When the initial reproducible. Analysing the kinetic curve of the present experiments Ca/P ratio attains 5.00, the pH value to achieve fast precipitation can at pH 8.00 or pH 7.50, where an acceleration phenomenon occurs be lowered to 8.00, and at an initial Ca/P ratio of 6.67, the after the reaction time of 90 min, it is found that the precipitation is a precipitation efficiency at pH value of 7.50 can also reach a high two-stages precipitation. The relaxation time for the second phase at value of 83% after a reaction time of 180 min. It is noticeable that at pH 8.00 and initial Ca/P ratio 3.33 is 115 min. The second phase is the pH range from 7.50 to 8.00, the precipitation may accelerate with also a fast growing phase, so the final precipitation efficiency is high. a second phase formation after a reaction time of 90 min, and the It is difficult to identify the phases in the process of precipitation only final precipitation efficiency can reach a fairly high value. Because of by the present Ca/P ratios of the precipitates, for the precipitates this phenomenon, well designed precipitating system at low pH may absorb some calcium and phosphate ions, instrumental methods values could be considered. This, on one hand, can save the base and are needed to distinguish different phases of the precipiates. In the calcium needed for the recovery of phosphate, on the other hand, process of phosphate precipitation, with a proper design the high avoids the problem of the strong basicity of the effluent after the phosphate recovery process. 7 Y. SONG, H. H. HAHN, AND E. HOFFMANN The effects of pH value and initial Ca/P ratio on the precipitation of calcium phosphate are due to their effects on phosphate at defined conditions similar to the phosphate recovery the from wastewater. thermodynamically driving force of the precipitation reactions. No matter how the pH value and the initial Ca/P ratio of the ACKNOWLEDGEMENTS precipitating system vary, after a definite reaction time the final precipitates tend to get close to the Ca/P ratio of HAP, this is the The reflection of the formation of calcium phosphates and transformation authors would like to thank Graduiertenkolleg 366 "Grenzflächenphänomene in aquatischen Systemen und wässrigen to HAP. The present paper focuses on the precipitation of a low phosphate Phasen" for the financial support to Dr. Yonghui Song. Thanks also concentration of 20 mg.l-1 at wide pH values ranging from 7.50 to 11.0 go to Prof. Fritz H. Frimmel of the Engler-Bunte-Institute, and wide initial Ca/P ratio values ranging from 1.67 to 6.67. It differs Department of Water Chemistry of the University of Karlsruhe, Dr. from the traditional studies of the precipitation of calcium phosphate, Dietfried Donnert of the Institute for Technical Chemistry of the which were mainly dedicated to the physiological considerations, i.e. Karlsruhe Research Center Technology and Environment, and Dr. higher temperatures and pH value around 7.4. This study has Ernst Antusch who was formerly a member of the authors’ institute improved the understanding of the precipitaion of calcium for their kind help to the research. REFERENCES 1. Brett S., Guy J., Morse G. K. and Lester J. N., Phosphorus Removal and Recovery Technologies. Selper Publications, London, pp. 31-44 (1997). 2. Driver J., Lijmbach D. and Stehen I., Why recover phosphorus for recycling, and How? Environmental Technology, 20, 651-662 (1999). 3. Golubev S. V., Pokrovsky O. S., Savenko, V. S., Unseeded precipitation of calcium and magnesium phosphates from modified seawater solutions. J. Crystal Growth, 205, 354-360 (1999). 4. Abbona F., Franchini-Angela M., Crystallization of calcium and magnesium phosphates from solutions of low concentration. J. Crystal Growth, 104, 661-671 (1990). 5. Van Kemenade M. J. J. M., De Bruyn P. L., A kinetic study of precipitation from supersaturated calcium phosphate solutions. J. Colloid Interface Sci., 118, 564-585 (1987). 6. Abbona F., Baronnet A., A XRD and TEM study on the transformation of amorphous calcium phosphate in the presence of magnesium. J. Crystal Growth, 165, 98-105 (1996). 7. Iijima M., Kamemizu H., Wakamatsu N., Goto T., Doi Y., Moriwaki Y., Precipitation of octacalcium phosphate at 37°C and at pH 7.4: in relation to enamel formation. J. Crystal Growth, 112, 467-473 (1991). 8. Lundager Madsen H. E. L., Christensson F., Precipitation of calcium phosphate at 40°C from neutral solution. J. Crystal Growth, 114, 613618 (1991). 9. Christoffersen M. R., Christoffersen J. and Kibalczyc W., Apparent solubilities of two amorphous calcium phosphates and of octacalcium phosphate in the temperature range 30-42°C. J. Crystal Growth, 106, 349-354 (1990). 10. Heughebaert J. C., Zawacki S. J., Nancollas G. H., The growth of nonstoichiometric apatite from aqueous solution at 37°C I. Methodology and growth at pH 7.4. J. Colloid Interface Sci., 135, 20-32 (1990). 11. Zawacki S. J., Heughebaert J. C., Nancollas G. H., The growth of nonstoichiometric apatite from aqueous solution at 37°C II. Effects of pH upon the precipitated phase. J. Colloid Interface Sci., 135, 33-44 (1990). 12. Kibalczyc W., Christoffersen J., Christoffersen M. R., Zielenkiewicz A., Zielenkiewicz W., The effect of magnesium ions on the precipitation of calcium phosphates. J. Crystal Growth, 105, 355-366 (1990). 13. Christoffersen J., Christoffersen M. R., Kibalczyc W. and Andersen F. A., A contribution to the understanding of the formation of calcium phosphates. J. Crystal Growth, 94, 767-777 (1989). 14. Lundager Madsen H. E., Thorvardarson G., Precipitation of calcium phosphate from moderately acid solution. J. Crystal Growth, 66, 369376 (1984). 15. De Rooij J. F., Heughebaert J. C., Nancollas G. H., A pH study of calcium phosphate seeded precipitation. J. Colloid Interface Sci., 100, 350358 (1984). 16. Feenstra T. P., Hop J., De Bruyn P. L., The influence of small amount of magnesium on the formation of calcium phosphate in moderately supersaturated solutions. J. Colloid Interface Sci., 83, 583-588 (1981). 17. Koutsoukos P., Amjad Z., Tomson M. B. and Nancollas G. H., Crystallization of calcium phosphates. A constant composition study. J. Am. Chem. Soc., 102, 1553-1557 (1980). 18. Boskey A. L., Posner A. S., Formation of hydroxyapatite at low supersaturation. J. Phys. Chem., 80, 40-45 (1976). 19. Boskey A. L., Posner A. S., Magnesium stabilization of amorphous calcium phosphate: A kinetic study. Mat. Res. Bull., 9, 907-916 (1974). 20. Boskey A. L., Posner A. S., Conversion of amorphous calcium phosphate to microcrystalline hydroxyapatite. A pH-dependent, solutionmediated, solid-solid conversion. J. Phys. Chem., 77, 2313-2317 (1973). 8 Y. SONG, H. H. HAHN, AND E. HOFFMANN 21. Blumenthal N. C., Posner A. S. and Holmes J. M., Effect of preparation conditions on the properties and transformation of amorphous calcium phosphate. Mat. Res. Bull., 7, 1181-1190 (1972). 22. Eanes E. D., Gillessen I. H. and Posner A. S., Intermediate states in the precipitation of hydroxyapatite. Nature, 5008, 365-367 (1965). 23. Feenstra T. P., De Bruyn P. L., The Ostwald Rule of Stages in Precipitation from highly supersaturated solutions: A model and its application to the formation of the nonstoichiometric amorphous calcium phosphate precursor phase. J. Colloid Interface Sci., 84, 66-72 (1981). 24. Hahn H. H., Antusch E., A pilot crystallisation reactor for the recovery of calcium phosphate. Project Report to CEEP, Institute for Aquatic Environmental Engineering, University of Karlsruhe, pp. 28 (1999). 25. Bates R. G., Dissociation constant of phosphoric acid from 0-60°C. J. Res. Natl. Bur. Stand., 47, 125-134 (1951). 26. Bates R. G., Acree S. F., pH values of certain phosphate-chloride mixtures and the second dissociation constant of phosphoric acid from 060°C. J. Res. Natl. Bur. Stand., 30, 129-155 (1943). 27. Vanderzee C. E., Quist A. S., Third dissociation constant of orthophosphoric acid. J. Phys. Chem., 65, 118-123 (1961). 28. Covington A. K., Ferra M. A. and Robinson, R. A., Ionic product and enthalpy of ionization of water from electromotive force measurements. J. Chem. Soc. Faraday Trans. 1, 73, 1721-1730 (1977). 29. Chughtai A., Marshall R. and Nancollas G. H., Complexes in calcium phosphate solutions. J. Phys. Chem., 72, 208-211 (1986). 30. Gregory T. M., Moreno E. C., Brown W. E., Solubility of CaHPO 4.2H2O in the system Ca(OH)2-H3PO4-H2O at 5, 15, 25, and 37°C. J. Res. Natl. Bur. Stand., 74A, 461-475 (1970). 31. Gimblett F. G. R., Monk C. B., E.M.F. studies of electrolytic dissociation. Part 7-Some alkali and alkaline earth metal hydroxides in water. Trans. Faraday Soc., 50, 965-972. (1954). 32. McDowell H., Gregory T. M., Brown W. E., Solubility of Ca 5(PO4)3OH in the system Ca(OH)2-H3PO4-H2O at 5, 15, 25, and 37°C. J. Res. Natl. Bur. Stand., 81A, 273-281 (1977). 33. Gregory T. M., Moreno E. C., Patel J. M. and Brown W. E., Solubility of -Ca3(PO4)2 in the system Ca(OH)2-H3PO4-H2O at 5, 15, 25, and 37°C. J. Res. Natl. Bur. Stand., 78A, 667-674 (1974). 34. Patel J. M., Gregory T. M. and Brown W. E., Solubility of CaHPO4.2H2O in the quaternary system Ca(OH)2-H3PO4-NaCl-H2O at 25°C. J. Res. Natl. Bur. Stand., 78A, 675-681 (1974). 35. Feenstra T. P., A note on the calculation of concentrations in the case of many simultaneous equilibria. J. Chem. Edu., 56, 104-105 (1979). 9