# The Identification and Synthesis of Lead Apatite Minerals Formed in Lead Water Pipes

Authors: Jeremy D. Hopwood; Glyn R. Derrick; David R. Brown; Christopher D. Newman; John Haley; Richard Kershaw; Mike Collinge
Journal: Journal of Chemistry
 (2016)

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## Abstract

Phosphate is added to drinking water in the UK to minimise the release of lead from lead water pipes. The phosphate encourages the formation of insoluble lead apatites on the walls of the pipe. Hydroxylpyromorphite Pb5(PO4)3OH is the lead apatite that is most often used to model lead levels in tap water; however, its presence has not been confirmed. Our aims were to identify the lead pipe apatite and synthesise it. The synthetic mineral would then be used in future solubility studies to produce better predictions of lead levels in tap water. XRD and FTIR were used to characterise the minerals on a range of lead pipes. Pyromorphite and hydroxylpyromorphite were absent and instead a range of mixed calcium lead apatites were present. For every five lead ions in the general formula Pb5(PO4)3X between one and two ions were replaced with calcium and there was evidence of substitution of P
O
4
3
- by either C
O
3
2
- or H
P
O
4
2
-. Calcium lead apatites with similar unit cell dimensions to those found on lead water pipes were then synthesised. The calcium : lead ratio in these reaction mixtures was in excess of 500 : 1 and the resulting crystals were shown by TEM to be nanosized rods and flakes. The synthetic apatites that most closely resembled the unit cell dimensions of the apatites on lead water pipes were shown to be Pb3.4Ca1.3(PO4)3Cl0.03OH0.97, Pb3.6Ca1.2(PO4)3Cl0.07OH0.93, and Pb3.6Ca1.2(PO4)3Cl0.27OH0.73.


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## Body

## 1. Introduction

Lead is a harmful heavy metal that is associated with poor cognitive performance at low levels of exposure [1, 2] and organ failure at high levels of exposure [3, 4]. Environmental lead levels have fallen in the UK over the last 30 years due to the discontinuation of lead in petrol and paints [5], although a historical legacy remains [6]. Many homes built before 1970 are connected to the mains water pipe in the street by a lead pipe [1, 7–9]. Although lead pipe replacement is the best option it is costly and therefore rarely undertaken by the homeowner. Recently the issue of lead in tap water has been highlighted by events taking place in Flint, Michigan, USA, where high levels of lead have been recorded [10].Research by Colling in the 1980s showed that low levels of phosphate (1–3 mg/L as P) added to tap water can reduce the concentration of soluble lead [11, 12]. This practice has been adopted by water utilities worldwide and in the UK has enabled water utilities to compliant with lead levels [9]. Recently the focus of UK water utilities has been on complying with the new European Union 2013 legal limit of 10 μg/L. For some, this has meant identifying supply zones that do not respond as well to phosphate dosing. These so-called “lead hot spots” are <98% compliant with the 10 μg/L limit. Understanding why these occur has led to renewed interest in optimising phosphate dosing procedures and in understanding the chemistry of lead water pipes.The corrosion of lead pipes results in the formation of a thin mineralised corrosion layer [11, 13–17]. This layer typically contains lead oxide (litharge) overlaid with lead carbonates (cerussite and hydrocerussite). In the case of phosphate dosing a further layer containing lead apatite is thought to occur. In phosphate-dosed tap water, the lead apatites are the least soluble form of lead [18] and it is thought that these are the minerals that control the concentration of dissolved lead in tap water.Lead apatite is the name used in this paper to describe minerals of general formula M5(PO4)3X, where M is either Pb2+ or a mixture of Pb2+ and one other cation such as Ca2+ and X is a monovalent anion such as OH− or Cl−. Examples include pyromorphite Pb5(PO4)3Cl, hydroxylpyromorphite Pb5(PO4)3OH, and phosphohedyphane Pb3Ca2(PO4)3Cl. Lead apatites are closely related in formula and crystal structure to calcium apatites [19], which have been extensively studied because they form the mineral component of bones and teeth. Examples of the calcium apatites include hydroxylapatite Ca5(PO4)3OH, chlorapatite Ca5(PO4)3Cl, and fluoroapatite Ca5(PO4)3F.There is uncertainty about the chemical formulae of the lead apatites found on lead water pipes. Hydroxylpyromorphite (Pb5(PO4)3OH) is the phase that is most often used in solubility studies [20]. However, Grimes et al. identified a calcium containing lead apatite on new lead pipes exposed to phosphate-dosed tap water and analysis by electron diffraction implied that the structure of the mineral was between hydroxylapatite (Ca5(PO4)3OH) and hydroxylpyromorphite (Pb5(PO4)3OH) [21]. Davidson et al. have also shown by secondary ion mass spectrometry that a correlation exists between calcium and phosphorus in the mineral scale and have interpreted this as evidence for a mixed calcium lead apatite [15, 22]. Recently, a new geological lead apatite mineral called phosphohedyphane Ca2Pb3(PO4)3Cl has been identified and its crystallography determined [23].The lead apatites belong to a large group of minerals having the apatite crystal structure (space groupP63/m). The different members are usually described in terms of their unit cell data obtained from X-ray diffraction. Figure 1 shows published unit cell data as a plot of thec dimension versus thea,b dimension for five minerals hydroxylapatite [24, 25], chlorapatite [26], phosphohedyphane [23], hydroxylpyromorphite [27, 28], and pyromorphite [29–32]. The graph shows that the calcium lead apatite unit cell dimensions exist within a quadrilateral. The fact that phosphohedyphane, Pb3Ca2(PO4)3Cl, is 3
/
5 of the way along the line from Ca5(PO4)3Cl to Pb5(PO4)3Cl is consistent with a linear dependence of the unit cell dimensions on the ratio of Pb : Ca.Figure 1
Unit cell graph for apatites containing calcium, lead, hydroxide, and chloride ions (see text for references).Identifying the lead apatites present on the lead water pipes and knowing their solubility products would enable much better predictions to be made of lead levels in tap water of different water quality. Unfortunately, it is difficult to do this directly on thein situ lead apatites. This is because the mineral corrosion layer is a mixture of cerussite, hydrocerussite, and lead apatite. It would be difficult to physically separate the lead apatites for solubility studies without contaminating the mineral with cerussite or hydrocerussite or chemically separate them without altering the surface structure of the apatites. Similar problems have beset those trying to understand the solubility of bones and teeth as these are mixtures of different calcium apatites [33]. In the case of bones and teeth synthetic calcium apatites have been prepared and these have then been used in solubility studies [34]. A similar strategy of identifying and making synthetic copies of the lead apatites is used in this study. The long term aim is to produce better predictions of lead levels in tap water, which can be used to optimise phosphate dosing and to shed light on the occurrence of “lead hot spots.” The ability to make synthetic copies of the lead apatites found on the walls of lead water pipes is a crucial first step.The results presented here will also be of interest to those studying the immobilisation of lead in contaminated soil [35–38] and the immobilisation of lead in the ash produced from municipal solid waste incineration (MSWI) plants [39–41]. In both cases, phosphate has been used to produce lead apatites, the low solubility of which reduces the bioavailability of lead. Calcium is likely to be a coprecipitant in these apatites.In this study, powder XRD was used to identify the minerals present in the lead pipe corrosion layer and to show which peaks corresponded to lead apatite. FTIR was used to support the XRD work and to show whether or not foreign anions such as carbonate were incorporated in the apatite structure. Synthetic calcium lead apatites were then prepared from solutions containing different ratios of Ca : Pb and OH : Cl and samples analysed by powder XRD and FTIR. Transmission electron microscopy (TEM) was used to determine the size and morphology of the synthetic lead apatites. The unit cell dimensions of the apatites formed on the lead pipes and the synthetic apatites were then calculated and their positions on the unit cell graph compared. Finally, three target minerals (T1, T2, and T3) were prepared whose unit cell dimensions were similar to the apatites formed on the lead pipes. The chemical formulae of these target minerals, the synthetic copies of the lead apatites found on the walls of lead water pipes, were then determined chemically by elemental analysis.


## 2. Materials and Methods

### 2.1. Extraction of Lead Pipes and Preparation of Mineral Scale

Lead communication pipes were extracted by Yorkshire Water. They were taken from properties within Yorkshire, UK, in 2010 and were thought to be between 60 and 80 years old.Eight pipes (P2, P4, P5, P8, P11, P12, P13, and P14) came from compliance zones with moderate alkalinity,100
±
20 mg/L CaCO3, and an average pH of 7.2. Four pipes (P1, P3, P7, and P9) came from compliance zones with high alkalinity (250
±
50 mg/L CaCO3) and average pH range of 7.2–7.6. Two pipes (P6 and P10) were not supplied with water quality data. The pipes, P1 to P14 (internal diameter 10–15 mm), were drained on-site and their ends covered in plastic bags before being sent to the laboratory. They were then dried at room temperature, cut into 5–7 cm long lengths using a ratchet PVC and HDPE pipe cutter, and stored at room temperature. Samples of mineral scale from pipes P1 to P14 were removed in a beaker of tap water by scraping the internal surface of the lead pipes with a stainless steel spatula. The resulting solution was then centrifuged and the powder collected and dried overnight at 80°C.


### 2.2. Synthesis of Lead Apatites

Calcium nitrate tetrahydrate, sodium phosphate dibasic dihydrate, sodium chloride, and lead(II) nitrate were obtained from Sigma Aldrich. Ultrapure water was produced using a Thermo Scientific Nanopure Ultrapure Water System.Initial work established that a Ca : Pb ratio of the order 500 : 1 was needed to make the calcium lead apatites. The synthetic minerals, S1–S10, were produced by mixing a phosphate-chloride solution (solution 1) with a lead-calcium solution (solution 2). All the solutions were bubbled with nitrogen gas to remove dissolved CO2 gas. This was undertaken because carbonate ions are known to substitute for up to 3.6% of the phosphate ions in lead apatites [42]. The phosphate-chloride solution (pH 8.4–9.2) was made by mixing dibasic sodium phosphate (0.100 M, 10.0 mL) with sodium chloride (1.67 M–1.67 × 10−4M, 15 mL) and made up to 100 mL with ultrahigh purity water. The lead-calcium solution (pH 5.2–5.4) was made by mixing lead(II) nitrate (0.040 M, 12.5 mL) with solid calcium nitrate tetrahydrate (0.00–295 g) and made up to 1000 mL with ultrahigh purity water. Solution 1 (100 mL) was added dropwise, over a period of 10 minutes, to solution 2 (1000 mL). The resulting cloudy white suspension was centrifuged (Eppendorf 5702, 2500 rpm, 2.5 mins) and washed five times with ultrapure water to remove any remaining calcium nitrate. The remaining solid was then filtered and dried overnight at 80°C. Samples S1, S2, S3, S4, and S6 were used to investigate the effect of increasing the chloride concentration. Samples S5–S10 were used to investigate the effect of increasing the calcium concentration. The solution compositions are shown in Table 1.Table 1
Composition of solutions 1 and 2 used to make the synthetic calcium lead apatites, S1–S10 and T1–T3.
Code
Solution 1, 100 mL
Solution 2, 1000 mL
Mix
Na2HPO4  (mM)
NaCl (mM)
pH
Ca(NO3)2 (mM)
Pb(NO3)2 (mM)
Ca/Pb
pH
pH
Chlorideexperiments
S1
10
250
8.44
250
0.5
500
5.37
5.69
S2
10
25
—
250
0.5
500
5.37
—
S3
10
2.5
9.22
250
0.5
500
5.37
—
S4
10
0.25
9.14
250
0.5
500
5.37
—
Calciumexperiments
S5
10
0.025
9.2
zero
0.5
0
5.43
7.16
S6
10
0.025
9.2
250
0.5
500
5.37
—
S7
10
0.025
9.2
500
0.5
1000
5.37
—
S8
10
0.025
9.2
750
0.5
1500
5.30
—
S9
10
0.025
9.2
1000
0.5
2000
5.23
—
S10
10
0.025
9.2
1250
0.5
2500
5.20
—
Targetminerals
T1
10
0.025
9.2
940
0.5
1880
—
—
T2
10
0.025
9.2
690
0.5
1380
5.18
4.98
T3
10
0.50
9.1
660
0.5
1320
5.23
5.26The target minerals T1, T2, and T3 were prepared in the same manner as minerals S1–S10. The solution compositions were those that gave synthetic minerals whose unit cell dimensions were similar to those of the lead pipe apatites. Each target mineral was prepared three times and elemental analysis was undertaken on all nine samples.It should be noted that the synthetic minerals S1–S10 and T1–T3 were made at a much higher supersaturation than those of the lead apatites found on the water pipes. The higher supersaturations were necessary in order to produce sufficient material for sample analysis and for future solubility experiments. The concentrations of lead and phosphate (as P) in the synthetic experiments were 28 mg/L and 93000μg/L, respectively, whereas the concentration of lead and phosphate (as P) in the lead water pipes would have been 1–3 mg/L and 2–20 μg/L, respectively.


### 2.3. Analytical Methods

X-ray powder diffraction was carried out using a Bruker D2 PHASER fitted with a LYNXEYE™ detector and CuKα radiation (λ
=
1.5418 Å). Samples for XRD were ground to a fine powder and loaded into the centre of a mirror sample holder using ethanol. Peak positions were identified using XFIT 2 and the patterns refined using Chekcell [43]. The diffracted peaks of minerals other than those from lead apatite were removed prior to calculating the unit cell parameters. The initial values used as a starting point for the assignment were the unit cell parameters of hydroxylpyromorphite. FTIR spectra of the minerals were recorded on a Nicolet 380 spectrometer from 4000 to 400 cm−1 with a diamond ATR accessory. Transmission electron microscopy of synthetic minerals was undertaken using a JEOL 3010 TEM operated at 300 kV. The minerals for TEM analysis were dispersed in deionised water and a small drop was transferred to a Formvar-carbon coated copper grid and allowed to air dry. ICPMS data were recorded using an Agilent 7700e ICP-MS. Yttrium and lead single element standards for ICP-MS were obtained from VWR. Elemental analysis of the three target minerals was carried out by an external contractor Medac Ltd. The minerals were digested in 5 mL conc. HNO3 and 1 mL (30% w/v) H2O2 and made up to 100 mL. The resulting solutions were then analysed for Ca, P, and Pb using a Varian Vista MPX ICP_OES. The Cl analysis was carried out by combustion of the sample in oxygen and absorption, followed by titration with mercuric nitrate solution.


## 2.1. Extraction of Lead Pipes and Preparation of Mineral Scale

Lead communication pipes were extracted by Yorkshire Water. They were taken from properties within Yorkshire, UK, in 2010 and were thought to be between 60 and 80 years old.Eight pipes (P2, P4, P5, P8, P11, P12, P13, and P14) came from compliance zones with moderate alkalinity,100
±
20 mg/L CaCO3, and an average pH of 7.2. Four pipes (P1, P3, P7, and P9) came from compliance zones with high alkalinity (250
±
50 mg/L CaCO3) and average pH range of 7.2–7.6. Two pipes (P6 and P10) were not supplied with water quality data. The pipes, P1 to P14 (internal diameter 10–15 mm), were drained on-site and their ends covered in plastic bags before being sent to the laboratory. They were then dried at room temperature, cut into 5–7 cm long lengths using a ratchet PVC and HDPE pipe cutter, and stored at room temperature. Samples of mineral scale from pipes P1 to P14 were removed in a beaker of tap water by scraping the internal surface of the lead pipes with a stainless steel spatula. The resulting solution was then centrifuged and the powder collected and dried overnight at 80°C.


## 2.2. Synthesis of Lead Apatites

Calcium nitrate tetrahydrate, sodium phosphate dibasic dihydrate, sodium chloride, and lead(II) nitrate were obtained from Sigma Aldrich. Ultrapure water was produced using a Thermo Scientific Nanopure Ultrapure Water System.Initial work established that a Ca : Pb ratio of the order 500 : 1 was needed to make the calcium lead apatites. The synthetic minerals, S1–S10, were produced by mixing a phosphate-chloride solution (solution 1) with a lead-calcium solution (solution 2). All the solutions were bubbled with nitrogen gas to remove dissolved CO2 gas. This was undertaken because carbonate ions are known to substitute for up to 3.6% of the phosphate ions in lead apatites [42]. The phosphate-chloride solution (pH 8.4–9.2) was made by mixing dibasic sodium phosphate (0.100 M, 10.0 mL) with sodium chloride (1.67 M–1.67 × 10−4M, 15 mL) and made up to 100 mL with ultrahigh purity water. The lead-calcium solution (pH 5.2–5.4) was made by mixing lead(II) nitrate (0.040 M, 12.5 mL) with solid calcium nitrate tetrahydrate (0.00–295 g) and made up to 1000 mL with ultrahigh purity water. Solution 1 (100 mL) was added dropwise, over a period of 10 minutes, to solution 2 (1000 mL). The resulting cloudy white suspension was centrifuged (Eppendorf 5702, 2500 rpm, 2.5 mins) and washed five times with ultrapure water to remove any remaining calcium nitrate. The remaining solid was then filtered and dried overnight at 80°C. Samples S1, S2, S3, S4, and S6 were used to investigate the effect of increasing the chloride concentration. Samples S5–S10 were used to investigate the effect of increasing the calcium concentration. The solution compositions are shown in Table 1.Table 1
Composition of solutions 1 and 2 used to make the synthetic calcium lead apatites, S1–S10 and T1–T3.
Code
Solution 1, 100 mL
Solution 2, 1000 mL
Mix
Na2HPO4  (mM)
NaCl (mM)
pH
Ca(NO3)2 (mM)
Pb(NO3)2 (mM)
Ca/Pb
pH
pH
Chlorideexperiments
S1
10
250
8.44
250
0.5
500
5.37
5.69
S2
10
25
—
250
0.5
500
5.37
—
S3
10
2.5
9.22
250
0.5
500
5.37
—
S4
10
0.25
9.14
250
0.5
500
5.37
—
Calciumexperiments
S5
10
0.025
9.2
zero
0.5
0
5.43
7.16
S6
10
0.025
9.2
250
0.5
500
5.37
—
S7
10
0.025
9.2
500
0.5
1000
5.37
—
S8
10
0.025
9.2
750
0.5
1500
5.30
—
S9
10
0.025
9.2
1000
0.5
2000
5.23
—
S10
10
0.025
9.2
1250
0.5
2500
5.20
—
Targetminerals
T1
10
0.025
9.2
940
0.5
1880
—
—
T2
10
0.025
9.2
690
0.5
1380
5.18
4.98
T3
10
0.50
9.1
660
0.5
1320
5.23
5.26The target minerals T1, T2, and T3 were prepared in the same manner as minerals S1–S10. The solution compositions were those that gave synthetic minerals whose unit cell dimensions were similar to those of the lead pipe apatites. Each target mineral was prepared three times and elemental analysis was undertaken on all nine samples.It should be noted that the synthetic minerals S1–S10 and T1–T3 were made at a much higher supersaturation than those of the lead apatites found on the water pipes. The higher supersaturations were necessary in order to produce sufficient material for sample analysis and for future solubility experiments. The concentrations of lead and phosphate (as P) in the synthetic experiments were 28 mg/L and 93000μg/L, respectively, whereas the concentration of lead and phosphate (as P) in the lead water pipes would have been 1–3 mg/L and 2–20 μg/L, respectively.


## 2.3. Analytical Methods

X-ray powder diffraction was carried out using a Bruker D2 PHASER fitted with a LYNXEYE™ detector and CuKα radiation (λ
=
1.5418 Å). Samples for XRD were ground to a fine powder and loaded into the centre of a mirror sample holder using ethanol. Peak positions were identified using XFIT 2 and the patterns refined using Chekcell [43]. The diffracted peaks of minerals other than those from lead apatite were removed prior to calculating the unit cell parameters. The initial values used as a starting point for the assignment were the unit cell parameters of hydroxylpyromorphite. FTIR spectra of the minerals were recorded on a Nicolet 380 spectrometer from 4000 to 400 cm−1 with a diamond ATR accessory. Transmission electron microscopy of synthetic minerals was undertaken using a JEOL 3010 TEM operated at 300 kV. The minerals for TEM analysis were dispersed in deionised water and a small drop was transferred to a Formvar-carbon coated copper grid and allowed to air dry. ICPMS data were recorded using an Agilent 7700e ICP-MS. Yttrium and lead single element standards for ICP-MS were obtained from VWR. Elemental analysis of the three target minerals was carried out by an external contractor Medac Ltd. The minerals were digested in 5 mL conc. HNO3 and 1 mL (30% w/v) H2O2 and made up to 100 mL. The resulting solutions were then analysed for Ca, P, and Pb using a Varian Vista MPX ICP_OES. The Cl analysis was carried out by combustion of the sample in oxygen and absorption, followed by titration with mercuric nitrate solution.


## 3. Results and Discussion

### 3.1. The Lead Pipe Apatites

Peaks belonging to lead apatite were present in all the powder XRD patterns of the lead water pipes (Figure2). Litharge PbO, cerussite PbCO3, and hydrocerussite Pb3(CO3)2(OH) were also present as were a small number of peaks that could not be assigned. The predominance of these minerals varied from pipe to pipe as evidenced by the variation in the profile of the XRD patterns. The presence of cerussite and hydrocerussite is consistent with previous studies [14]. However, unlike previous studies, plattnerite PbO2 [13, 44], scrutinyite PbO2 [44], laurionite Pb(OH)Cl [14], lead phosphate Pb9(PO4)6 [14], and plumbonacrite Pb10(CO3)6(OH)6O [14] were not observed.Figure 2
Lead mineral scale. X-ray powder diffraction patterns of lead pipes P1–P14 together with published reference spectra of oxide, carbonate, and phosphate minerals taken from the JCPDS and RRUFF databases. The prominent apatite peaks are shaded and the pattern for pyromorphite is indexed.The positions of the lead apatite peaks varied slightly, which was consistent the presence of lead apatites of different formulae. Previous studies on hydroxylpyromorphite, pyromorphite, and phosphohedyphane have shown that there are eight X-ray diffraction peaks in the 2θ region 20°–35° that are associated with lead apatite minerals. These are the (200), (111), (002), (102), (210), (121), (112), and (300) peaks. Typically, the pipes P1–P14 showed between three and five of the eight peaks. The easiest peaks to identify were the (111) peaks at 21.5–22.5° 2θ and the (121) and (112) peaks at 30.0–31.0° 2θ.The unit cell dimensions of the apatites formed on lead pipes, as determined from powder XRD using XFIT and Chekcell, are shown in Figure3. Each data point represents one sample. The errors due to curve fitting are shown by the error bars and were generated by Chekcell.Figure 3
Unit cell graph for apatites from lead water pipes.The apatites fall within a region of the quadrilateral bounded by the points Pb3Ca2(PO4)3OH-Pb3Ca2(PO4)3Cl-Pb4Ca(PO4)3Cl-Pb4Ca(PO4)3OH. In this region, one to two of the lead atoms are substituted by calcium and both chloride and hydroxide are present.Only one of the lead apatites had similar unit cell dimensions on the unit cell graph to phosphohedyphane. This was the apatite from pipe P4. However, most of the lead apatites were located away from the phosphohedyphane Pb3Ca2(PO4)3Cl point on the quadrilateral. Five of the lead apatites (P1, P3, P5, P7, and P10) were close to the hydroxylphosphohedyphane Pb3Ca2(PO4)3OH point on the unit cell graph. None of the lead apatites were located near the hydroxylpyromorphite and pyromorphite points on the unit cell graph. Therefore, the data showed that the corrosion scale of the lead pipes contained more than one type of mixed calcium lead apatite and neither hydroxylpyromorphite nor pyromorphite was present.The FTIR spectra of the corrosion scales of lead pipes P1–P14 are shown in Figure4.Figure 4
Lead mineral scale. Comparison of the FTIR spectra of lead pipes P1–P14 with spectra of carbonate and phosphate minerals. The spectra for phosphohedyphane was obtained from [23] and the other carbonate and phosphate standards were obtained from samples prepared in the laboratory.Peaks for carbonate and phosphate were observed that were consistent with the presence of cerussite, hydrocerussite, and lead apatite. The precise identity, peak positions, and the modes of vibration were determined from published FTIR data on cerussite [17], hydrocerussite [17], hydroxylpyromorphite [42, 45], pyromorphite [42, 46–48] calcium lead apatite [45], and hydroxylapatite [33, 45, 49, 50]. The broad peaks at 1300 to 1500 cm−1, the less intense but sharper peak at 670–685 cm−1, and the small peak at 1045–1051 cm−1 are typical of the carbonate vibrations in either cerussite or hydrocerussite. The small peak at 839 cm−1 is characteristic of cerussite only. The intense peaks at 1000–1070 cm−1, the shoulder peak at 920 cm−1, and the medium sized peaks at 540 cm−1 and 570 cm−1 are typical of the ν
3, ν
1, and ν
4 phosphate vibrations, respectively, in pyromorphite, hydroxylpyromorphite, and mixed calcium lead apatites.Four of the lead pipes P9, P10, P12, and P14 had a peak at 870–880 cm−1 (marked ∗ in Figure 4). A peak at this position has been observed in spectra of hydroxylapatite and has been attributed either to the incorporation of carbonate into the hydroxylapatite structure, where carbonate occupies the phosphate position (type B substitution) [51] or to the substitution of phosphate ions for H
P
O
4
2
- ions [33, 50]. Carbonate peaks at 850 cm−1 have also been reported in calcium lead apatites grown in the presence of sodium carbonate [42], although we have observed the peak at 870 cm−1 (unpublished work). Alternatively, a peak at this position could also be due small amounts of calcite.


### 3.2. The Synthetic Apatites

The powder XRD patterns of the synthetic apatites S1 to S10 are shown in Figure5. All the patterns could be indexed for lead apatite and no other mineral was observed. Changes were observed in the degree of separation of the (121) and (112) peaks, which are the peaks most easily visible on patterns of the lead mineral scale. In sample S1, produced at high chloride concentration, the peaks were separate and appeared as a doublet, whereas in sample S4 produced at a low chloride concentration the peaks coincided and appeared as a singlet. A similar change from a doublet to a singlet can be seen in the diffraction patterns of pyromorphite and hydroxylpyromorphite. In other words, the doublet implies that the lead apatite is rich in chloride ions and the singlet implies that the lead apatite is rich in hydroxide ions. Varying the calcium concentration also affected the position of the (121) and (112) singlet peak. The peak shifted to higher 2θ values and smaller interplanar d-spacings at higher calcium concentrations. This change is consistent with the incorporation of a smaller cation such as calcium into the crystal structure. XRD line broadening, which was a feature of the lead pipe apatites was also a feature for the synthetic apatites.Figure 5
Synthetic apatites. X-ray powder diffraction patterns of synthetic calcium lead apatites S1–S10. The Miller indices are shown for sample S1.The positions of the synthetic lead apatites on the unit cell graph, as determined from powder XRD using XFIT and Chekcell, are shown in Figure6. The error bars are smaller than those of the lead pipe apatites because only lead apatite was present, which made the curve fitting easier. The graph clearly shows that it is possible to move from the chloride side of the quadrilateral to the hydroxide side by decreasing the concentration of chloride in the reaction mixture (S1–S4, S6). Likewise, it is possible to move from the lead side of the quadrilateral to the calcium side by increasing the concentration of calcium in the reaction mixture (S5–S10). It is clear from the unit cell graph that a solid solution series exists for calcium lead apatite.Figure 6
Unit cell graph for synthetic apatites S1–S10.The FTIR spectra of samples S1–S10 are shown in Figure7. The spectra were consistent with the presence of lead apatite. Phosphate vibrations accounted for the peaks at 950–1100 cm−1, 920 cm−1, 590 cm−1, and 540 cm−1. Carbonate vibrations accounted for the low intensity peaks at 1250–1500 cm−1. The carbonate ions must have been incorporated on the surface of the lead apatite crystals when they were exposed to the atmosphere during the washing, centrifuging, and drying processes. The carbonate vibrations were not due to the presence of cerussite or hydrocerussite as these minerals were absent in the XRD patterns nor were they due to the incorporation of carbonate in the bulk crystal structure as the lead apatite minerals were synthesised under nitrogen gas.Figure 7
Synthetic apatites. FTIR spectra of the synthetic calcium lead apatites S1–S10 together with spectra for hydroxylpyromorphite (HPM), pyromorphite (PM), and hydroxylapatite (HA).The FTIR spectra from S1, S2, S3, S4, and S6 were similar to each other indicating that the positions of the phosphate peaks are unaffected by the Cl : OH ratio in the lead apatite structure. In contrast, the spectra for S5, S6, S7, S8, S9, and S10 were different from each other. In particular, theν
4
P
O
4
3
- peaks at 530–590 cm−1 shifted to the to higher wavenumbers as the Ca : Pb ratio in the lead apatite structure increased.The small peaks at 870–880 cm−1 observed on lead pipes P9, P10, P12, and P14 (Figure 4) were absent and instead the samples containing calcium, S6–S10, exhibited small peaks at 820 cm−1.TEM images of the synthetic samples S1–S10 (Figure8) showed particles ranging in size from 10 to 200 nm. Most of the samples comprised well faceted rod-shaped crystals of length 50–200 nm and width 10–20 nm. However, samples S8 and S10 comprised flakes that were aggregated together. Although there were changes in crystal size and shape it was not possible to correlate this with changes in chloride concentration or calcium concentration in the reaction mixture. Hydroxylapatite typically forms rods that are elongated along the c axis [49] and the same axis of elongation has been reported for pyromorphite crystals [18]. Rod-shaped crystals of lead apatite have also been observed in new lead pipes exposed to phosphate-dosed tap water [14].Figure 8
TEM images showing the morphology and size of synthetic lead apatites. The effect of increasing the chloride is shown in S1–S4, S6 and the effect of increasing the calcium concentration is shown in S5–S10. Bar markers = 50 nm.


### 3.3. The Target Minerals

The information from Figures3 and 6 was used to identify the reaction conditions needed to make the target minerals. Powder XRD patterns, unit cell graph, FTIR spectra, and TEM images of the three target minerals are shown in Figures 9(a)–9(d).Figure 9
Characterisation of the target minerals, (a) XRD, (b) unit cell graph, (c) FTIR, and (d) TEM (bar markers = 50 nm).
(a)
(b)
(c)
(d)Table2 shows the elemental analysis of the three target minerals, each synthesised in triplicate. The mole ratio of Pb2+ : Ca2+ : P
O
4
3
- : Cl− in each mineral was determined from percentage weight data (not shown). The ratio was normalised by setting the P
O
4
3
- value to 3.0, this being the number of P
O
4
3
- groups expected in each formula unit. The mole ratio of OH− ions was determined by subtracting the number of moles of Cl− ions from 1.00. Average values were then determined.Table 2
Composition of the target minerals determined from elemental analysis.
Min.
Repeat
Composition in moles
Pb + Ca
Divalent cation deficiency
(Pb + Ca)/P
Pb/Ca
±0.1
±0.01
% Ca [Ca/(Ca + Pb)] × 100
Pb2+
Ca2+
P
O
4
3
-
Cl−
(OH−)
T1
A
3.5
1.2
3.0
0.03
0.97
4.7
0.3
1.6
26
2.9
B
3.4
1.4
3.0
0.00
1.00
4.8
0.2
1.6
29
2.4
C
3.4
1.3
3.0
0.06
0.94
4.7
0.3
1.6
28
2.6
Av
3.4
1.3
3.0
0.03
0.97
4.7
0.3
1.6
28
2.6
T2
A
3.6
1.1
3.0
0.03
0.97
4.7
0.3
1.6
23
3.3
B
3.4
1.4
3.0
0.03
0.97
4.8
0.2
1.6
29
2.4
C
3.8
1.0
3.0
0.16
0.84
4.8
0.2
1.6
20
3.8
Av
3.6
1.2
3.0
0.07
0.93
4.8
0.2
1.6
25
3.2
T3
A
3.6
1.2
3.0
0.25
0.75
4.8
0.2
1.6
25
3.0
B
3.4
1.3
3.0
0.27
0.73
4.7
0.3
1.6
28
2.6
C
3.8
1.0
3.0
0.29
0.71
4.8
0.2
1.6
28
3.8
Av
3.6
1.2
3.0
0.27
0.73
4.8
0.2
1.6
25
3.1The formulae of the three target minerals, as determined from the average mole ratios in Table2, were(1)
P
b
3.4
C
a
1.3
P
O
4
3
C
l
0.03
O
H
0.97
T
1
P
b
3.6
C
a
1.2
P
O
4
3
C
l
0.07
O
H
0.93
T
2
P
b
3.6
C
a
1.2
P
O
4
3
C
l
0.27
O
H
0.73
T
3The formulae show that between one and two lead ions are replaced by calcium. This was consistent with the results from the unit cell diagram (Figure 9(b)). The closest fit was for minerals T2 and T3. Mineral T1 was predicted from the unit cell diagram to have two lead ions replaced by calcium ions but the actual figure was lower at 1.3. The reason for this discrepancy is not yet known. Mineral T3 had the highest amount of chloride ions. The results show that calcium is incorporated into the lead apatite structure when the Ca : Pb ratio in the reaction solution is equal to or greater than 500 : 1.In all three minerals, the total number of lead and calcium ions was less than 5.0, indicating that the minerals were deficient in calcium and/or lead. Apatites that have a total of 5.0 divalent cations are said to be stoichiometric and have M2+/P ratio of 1.7. Samples T1, T2, and T3 were therefore slightly nonstoichiometric, with M2+/P ratio of 1.6 (Table 2).The cationic deficiency implied that species other than Pb2+, Ca2+, P
O
4
3
-, Cl−, and OH− were present in the target minerals. In calcium deficient hydroxylapatite, it is thought that some of the Ca2+ ions are missing or replaced with Na+ ions. The loss of positive charge is then balanced by the substitution of P
O
4
3
- ions with H
P
O
4
2
- or C
O
3
2
- ions or by the substitution of OH− ions with H2O molecules. Lead apatites are likely to show similar changes and therefore Na+, H
P
O
4
2
-, C
O
3
2
-, and H2O may all be present as minor components in the target minerals. Their actual formulae might be rather complex as has been proposed for hydroxylapatite [51]. Possible formulae for mineral T1 are shown in Table 3.Table 3
Possible formulae of target mineral T1 together with general formulae. Divalent cation vacancies are denoted by the symbol □. Formulae containing carbonate are more complex and are not shown.
Possible formulae of the charge balanced target mineral T1
General formula
Pb3.4Ca1.3□0.3(PO4)2.4(HPO4)0.6OH0.03Cl0.95
Pb5
-
y
-
x
/
2Cay□x
/
2(PO4)3
-
x(HPO4)xOHwCl1
-
w
Pb3.4Ca1.3Na0.3(PO4)2.7(HPO4)0.3OH0.03Cl0.95
Pb5
-
y
-
xCayNax(PO4)3
-
x(HPO4)xOHwCl1
-
w
Pb3.4Ca1.3□0.6(PO4)3(H2O)0.6OH0.4
Pb5
-
y
-
x
/
2Cay□x(PO4)3(H2O)xOH1
-
x
Pb3.4Ca1.3Na0.3(PO4)3(H2O)0.3OH0.7
Pb5
-
y
-
xCayNax(PO4)3(H2O)xOH1
-
x
Any combination of the above formulaeTaken together, all the data for the target minerals show that synthetic copies of the lead apatites found on lead water pipes can be made. We hypothesise that the synthetic calcium lead apatites produced in this study (target minerals T1–T3) are similar to apatites found on lead water pipes and that these synthetic apatites can be used in solubility studies to determine their solubility products (Ksp values).


## 3.1. The Lead Pipe Apatites

Peaks belonging to lead apatite were present in all the powder XRD patterns of the lead water pipes (Figure2). Litharge PbO, cerussite PbCO3, and hydrocerussite Pb3(CO3)2(OH) were also present as were a small number of peaks that could not be assigned. The predominance of these minerals varied from pipe to pipe as evidenced by the variation in the profile of the XRD patterns. The presence of cerussite and hydrocerussite is consistent with previous studies [14]. However, unlike previous studies, plattnerite PbO2 [13, 44], scrutinyite PbO2 [44], laurionite Pb(OH)Cl [14], lead phosphate Pb9(PO4)6 [14], and plumbonacrite Pb10(CO3)6(OH)6O [14] were not observed.Figure 2
Lead mineral scale. X-ray powder diffraction patterns of lead pipes P1–P14 together with published reference spectra of oxide, carbonate, and phosphate minerals taken from the JCPDS and RRUFF databases. The prominent apatite peaks are shaded and the pattern for pyromorphite is indexed.The positions of the lead apatite peaks varied slightly, which was consistent the presence of lead apatites of different formulae. Previous studies on hydroxylpyromorphite, pyromorphite, and phosphohedyphane have shown that there are eight X-ray diffraction peaks in the 2θ region 20°–35° that are associated with lead apatite minerals. These are the (200), (111), (002), (102), (210), (121), (112), and (300) peaks. Typically, the pipes P1–P14 showed between three and five of the eight peaks. The easiest peaks to identify were the (111) peaks at 21.5–22.5° 2θ and the (121) and (112) peaks at 30.0–31.0° 2θ.The unit cell dimensions of the apatites formed on lead pipes, as determined from powder XRD using XFIT and Chekcell, are shown in Figure3. Each data point represents one sample. The errors due to curve fitting are shown by the error bars and were generated by Chekcell.Figure 3
Unit cell graph for apatites from lead water pipes.The apatites fall within a region of the quadrilateral bounded by the points Pb3Ca2(PO4)3OH-Pb3Ca2(PO4)3Cl-Pb4Ca(PO4)3Cl-Pb4Ca(PO4)3OH. In this region, one to two of the lead atoms are substituted by calcium and both chloride and hydroxide are present.Only one of the lead apatites had similar unit cell dimensions on the unit cell graph to phosphohedyphane. This was the apatite from pipe P4. However, most of the lead apatites were located away from the phosphohedyphane Pb3Ca2(PO4)3Cl point on the quadrilateral. Five of the lead apatites (P1, P3, P5, P7, and P10) were close to the hydroxylphosphohedyphane Pb3Ca2(PO4)3OH point on the unit cell graph. None of the lead apatites were located near the hydroxylpyromorphite and pyromorphite points on the unit cell graph. Therefore, the data showed that the corrosion scale of the lead pipes contained more than one type of mixed calcium lead apatite and neither hydroxylpyromorphite nor pyromorphite was present.The FTIR spectra of the corrosion scales of lead pipes P1–P14 are shown in Figure4.Figure 4
Lead mineral scale. Comparison of the FTIR spectra of lead pipes P1–P14 with spectra of carbonate and phosphate minerals. The spectra for phosphohedyphane was obtained from [23] and the other carbonate and phosphate standards were obtained from samples prepared in the laboratory.Peaks for carbonate and phosphate were observed that were consistent with the presence of cerussite, hydrocerussite, and lead apatite. The precise identity, peak positions, and the modes of vibration were determined from published FTIR data on cerussite [17], hydrocerussite [17], hydroxylpyromorphite [42, 45], pyromorphite [42, 46–48] calcium lead apatite [45], and hydroxylapatite [33, 45, 49, 50]. The broad peaks at 1300 to 1500 cm−1, the less intense but sharper peak at 670–685 cm−1, and the small peak at 1045–1051 cm−1 are typical of the carbonate vibrations in either cerussite or hydrocerussite. The small peak at 839 cm−1 is characteristic of cerussite only. The intense peaks at 1000–1070 cm−1, the shoulder peak at 920 cm−1, and the medium sized peaks at 540 cm−1 and 570 cm−1 are typical of the ν
3, ν
1, and ν
4 phosphate vibrations, respectively, in pyromorphite, hydroxylpyromorphite, and mixed calcium lead apatites.Four of the lead pipes P9, P10, P12, and P14 had a peak at 870–880 cm−1 (marked ∗ in Figure 4). A peak at this position has been observed in spectra of hydroxylapatite and has been attributed either to the incorporation of carbonate into the hydroxylapatite structure, where carbonate occupies the phosphate position (type B substitution) [51] or to the substitution of phosphate ions for H
P
O
4
2
- ions [33, 50]. Carbonate peaks at 850 cm−1 have also been reported in calcium lead apatites grown in the presence of sodium carbonate [42], although we have observed the peak at 870 cm−1 (unpublished work). Alternatively, a peak at this position could also be due small amounts of calcite.


## 3.2. The Synthetic Apatites

The powder XRD patterns of the synthetic apatites S1 to S10 are shown in Figure5. All the patterns could be indexed for lead apatite and no other mineral was observed. Changes were observed in the degree of separation of the (121) and (112) peaks, which are the peaks most easily visible on patterns of the lead mineral scale. In sample S1, produced at high chloride concentration, the peaks were separate and appeared as a doublet, whereas in sample S4 produced at a low chloride concentration the peaks coincided and appeared as a singlet. A similar change from a doublet to a singlet can be seen in the diffraction patterns of pyromorphite and hydroxylpyromorphite. In other words, the doublet implies that the lead apatite is rich in chloride ions and the singlet implies that the lead apatite is rich in hydroxide ions. Varying the calcium concentration also affected the position of the (121) and (112) singlet peak. The peak shifted to higher 2θ values and smaller interplanar d-spacings at higher calcium concentrations. This change is consistent with the incorporation of a smaller cation such as calcium into the crystal structure. XRD line broadening, which was a feature of the lead pipe apatites was also a feature for the synthetic apatites.Figure 5
Synthetic apatites. X-ray powder diffraction patterns of synthetic calcium lead apatites S1–S10. The Miller indices are shown for sample S1.The positions of the synthetic lead apatites on the unit cell graph, as determined from powder XRD using XFIT and Chekcell, are shown in Figure6. The error bars are smaller than those of the lead pipe apatites because only lead apatite was present, which made the curve fitting easier. The graph clearly shows that it is possible to move from the chloride side of the quadrilateral to the hydroxide side by decreasing the concentration of chloride in the reaction mixture (S1–S4, S6). Likewise, it is possible to move from the lead side of the quadrilateral to the calcium side by increasing the concentration of calcium in the reaction mixture (S5–S10). It is clear from the unit cell graph that a solid solution series exists for calcium lead apatite.Figure 6
Unit cell graph for synthetic apatites S1–S10.The FTIR spectra of samples S1–S10 are shown in Figure7. The spectra were consistent with the presence of lead apatite. Phosphate vibrations accounted for the peaks at 950–1100 cm−1, 920 cm−1, 590 cm−1, and 540 cm−1. Carbonate vibrations accounted for the low intensity peaks at 1250–1500 cm−1. The carbonate ions must have been incorporated on the surface of the lead apatite crystals when they were exposed to the atmosphere during the washing, centrifuging, and drying processes. The carbonate vibrations were not due to the presence of cerussite or hydrocerussite as these minerals were absent in the XRD patterns nor were they due to the incorporation of carbonate in the bulk crystal structure as the lead apatite minerals were synthesised under nitrogen gas.Figure 7
Synthetic apatites. FTIR spectra of the synthetic calcium lead apatites S1–S10 together with spectra for hydroxylpyromorphite (HPM), pyromorphite (PM), and hydroxylapatite (HA).The FTIR spectra from S1, S2, S3, S4, and S6 were similar to each other indicating that the positions of the phosphate peaks are unaffected by the Cl : OH ratio in the lead apatite structure. In contrast, the spectra for S5, S6, S7, S8, S9, and S10 were different from each other. In particular, theν
4
P
O
4
3
- peaks at 530–590 cm−1 shifted to the to higher wavenumbers as the Ca : Pb ratio in the lead apatite structure increased.The small peaks at 870–880 cm−1 observed on lead pipes P9, P10, P12, and P14 (Figure 4) were absent and instead the samples containing calcium, S6–S10, exhibited small peaks at 820 cm−1.TEM images of the synthetic samples S1–S10 (Figure8) showed particles ranging in size from 10 to 200 nm. Most of the samples comprised well faceted rod-shaped crystals of length 50–200 nm and width 10–20 nm. However, samples S8 and S10 comprised flakes that were aggregated together. Although there were changes in crystal size and shape it was not possible to correlate this with changes in chloride concentration or calcium concentration in the reaction mixture. Hydroxylapatite typically forms rods that are elongated along the c axis [49] and the same axis of elongation has been reported for pyromorphite crystals [18]. Rod-shaped crystals of lead apatite have also been observed in new lead pipes exposed to phosphate-dosed tap water [14].Figure 8
TEM images showing the morphology and size of synthetic lead apatites. The effect of increasing the chloride is shown in S1–S4, S6 and the effect of increasing the calcium concentration is shown in S5–S10. Bar markers = 50 nm.


## 3.3. The Target Minerals

The information from Figures3 and 6 was used to identify the reaction conditions needed to make the target minerals. Powder XRD patterns, unit cell graph, FTIR spectra, and TEM images of the three target minerals are shown in Figures 9(a)–9(d).Figure 9
Characterisation of the target minerals, (a) XRD, (b) unit cell graph, (c) FTIR, and (d) TEM (bar markers = 50 nm).
(a)
(b)
(c)
(d)Table2 shows the elemental analysis of the three target minerals, each synthesised in triplicate. The mole ratio of Pb2+ : Ca2+ : P
O
4
3
- : Cl− in each mineral was determined from percentage weight data (not shown). The ratio was normalised by setting the P
O
4
3
- value to 3.0, this being the number of P
O
4
3
- groups expected in each formula unit. The mole ratio of OH− ions was determined by subtracting the number of moles of Cl− ions from 1.00. Average values were then determined.Table 2
Composition of the target minerals determined from elemental analysis.
Min.
Repeat
Composition in moles
Pb + Ca
Divalent cation deficiency
(Pb + Ca)/P
Pb/Ca
±0.1
±0.01
% Ca [Ca/(Ca + Pb)] × 100
Pb2+
Ca2+
P
O
4
3
-
Cl−
(OH−)
T1
A
3.5
1.2
3.0
0.03
0.97
4.7
0.3
1.6
26
2.9
B
3.4
1.4
3.0
0.00
1.00
4.8
0.2
1.6
29
2.4
C
3.4
1.3
3.0
0.06
0.94
4.7
0.3
1.6
28
2.6
Av
3.4
1.3
3.0
0.03
0.97
4.7
0.3
1.6
28
2.6
T2
A
3.6
1.1
3.0
0.03
0.97
4.7
0.3
1.6
23
3.3
B
3.4
1.4
3.0
0.03
0.97
4.8
0.2
1.6
29
2.4
C
3.8
1.0
3.0
0.16
0.84
4.8
0.2
1.6
20
3.8
Av
3.6
1.2
3.0
0.07
0.93
4.8
0.2
1.6
25
3.2
T3
A
3.6
1.2
3.0
0.25
0.75
4.8
0.2
1.6
25
3.0
B
3.4
1.3
3.0
0.27
0.73
4.7
0.3
1.6
28
2.6
C
3.8
1.0
3.0
0.29
0.71
4.8
0.2
1.6
28
3.8
Av
3.6
1.2
3.0
0.27
0.73
4.8
0.2
1.6
25
3.1The formulae of the three target minerals, as determined from the average mole ratios in Table2, were(1)
P
b
3.4
C
a
1.3
P
O
4
3
C
l
0.03
O
H
0.97
T
1
P
b
3.6
C
a
1.2
P
O
4
3
C
l
0.07
O
H
0.93
T
2
P
b
3.6
C
a
1.2
P
O
4
3
C
l
0.27
O
H
0.73
T
3The formulae show that between one and two lead ions are replaced by calcium. This was consistent with the results from the unit cell diagram (Figure 9(b)). The closest fit was for minerals T2 and T3. Mineral T1 was predicted from the unit cell diagram to have two lead ions replaced by calcium ions but the actual figure was lower at 1.3. The reason for this discrepancy is not yet known. Mineral T3 had the highest amount of chloride ions. The results show that calcium is incorporated into the lead apatite structure when the Ca : Pb ratio in the reaction solution is equal to or greater than 500 : 1.In all three minerals, the total number of lead and calcium ions was less than 5.0, indicating that the minerals were deficient in calcium and/or lead. Apatites that have a total of 5.0 divalent cations are said to be stoichiometric and have M2+/P ratio of 1.7. Samples T1, T2, and T3 were therefore slightly nonstoichiometric, with M2+/P ratio of 1.6 (Table 2).The cationic deficiency implied that species other than Pb2+, Ca2+, P
O
4
3
-, Cl−, and OH− were present in the target minerals. In calcium deficient hydroxylapatite, it is thought that some of the Ca2+ ions are missing or replaced with Na+ ions. The loss of positive charge is then balanced by the substitution of P
O
4
3
- ions with H
P
O
4
2
- or C
O
3
2
- ions or by the substitution of OH− ions with H2O molecules. Lead apatites are likely to show similar changes and therefore Na+, H
P
O
4
2
-, C
O
3
2
-, and H2O may all be present as minor components in the target minerals. Their actual formulae might be rather complex as has been proposed for hydroxylapatite [51]. Possible formulae for mineral T1 are shown in Table 3.Table 3
Possible formulae of target mineral T1 together with general formulae. Divalent cation vacancies are denoted by the symbol □. Formulae containing carbonate are more complex and are not shown.
Possible formulae of the charge balanced target mineral T1
General formula
Pb3.4Ca1.3□0.3(PO4)2.4(HPO4)0.6OH0.03Cl0.95
Pb5
-
y
-
x
/
2Cay□x
/
2(PO4)3
-
x(HPO4)xOHwCl1
-
w
Pb3.4Ca1.3Na0.3(PO4)2.7(HPO4)0.3OH0.03Cl0.95
Pb5
-
y
-
xCayNax(PO4)3
-
x(HPO4)xOHwCl1
-
w
Pb3.4Ca1.3□0.6(PO4)3(H2O)0.6OH0.4
Pb5
-
y
-
x
/
2Cay□x(PO4)3(H2O)xOH1
-
x
Pb3.4Ca1.3Na0.3(PO4)3(H2O)0.3OH0.7
Pb5
-
y
-
xCayNax(PO4)3(H2O)xOH1
-
x
Any combination of the above formulaeTaken together, all the data for the target minerals show that synthetic copies of the lead apatites found on lead water pipes can be made. We hypothesise that the synthetic calcium lead apatites produced in this study (target minerals T1–T3) are similar to apatites found on lead water pipes and that these synthetic apatites can be used in solubility studies to determine their solubility products (Ksp values).


## 4. Conclusions

This study shows that lead water pipes from the county of Yorkshire in Northern England, fed with phosphate-dosed tap water, contain a range of apatite minerals of slightly different chemical formulae, in which both calcium and lead are present. Hydroxylpyromorphite which is the mineral used in solubility studies was not observed. The presence of calcium lead apatites instead of hydroxylpyromorphite implies that current solubility models do not give an accurate prediction of lead levels in tap water from Yorkshire.Analysis of the lead apatites from the walls of the lead pipes showed that for every five lead ions in the general formula Pb5(PO4)3X between one and two ions were replaced with calcium. There were also differences in the amounts of hydroxide and chloride ions (X = OH and/or Cl) with most of the calcium lead apatites being richer in hydroxide ions. Phosphohedyphane, in which all the monovalent anions are chloride ions, was not observed although the hydroxyl form of phosphohedyphane Pb3Ca2(PO4)3OH may have been present. There was evidence for the substitution of P
O
4
3
- by either C
O
3
2
- or H
P
O
4
2
- ions.Synthetic calcium lead apatites that had similar unit cell dimensions to those found on lead water pipes were successfully made having the formulae Pb3.4Ca1.3(PO4)3Cl0.03OH0.97, Pb3.6Ca1.2(PO4)3Cl0.07OH0.93, and Pb3.6Ca1.2(PO4)3Cl0.27OH0.73. In other words, 20–29% of the lead ions were replaced with calcium (Table 2). These synthetic calcium lead apatites were slightly nonstoichiometric having M2+/P ratio of 1.6 as opposed to the stoichiometric value of 1.7. This nonstoichiometry can be explained by the presence of small amounts of Na+, H
P
O
4
2
-, C
O
3
2
-, and H2O species or by cation vacancies. The synthetic calcium lead apatite crystals appeared as nanosized rods and flakes and were less crystalline than synthetic lead apatites.


## 5. Future Work

Future work will focus on the solubility products and modelling of the solution chemistry using the ion speciation software PHREEQC [52]. These models will be used to optimise phosphate dosing and to shed light on the occurrence of “lead hot spots,” where the concentration of lead in tap water is >10 μg/L, which is the current European Union limit for lead. We will also investigate whether there is a correlation between the predicted formulae of the lead pipe apatites and the composition and origin of the tap water flowing through the pipes. Table 3 suggests that H
P
O
4
2
- ions are H2O molecules which may be present within the calcium lead apatites and we will use spectroscopic techniques to see whether this is true. The distribution of Ca and Pb within the apatite structure has important implications for the minerals stability and solubility and we are currently investigating this using atomistic simulations.



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*Source: 9074062-2016-03-24.xml*