Abstract
The heat capacity, Cp, of synthetic hydroxyapatite [Ca5(PO4)3OH–OH-Ap], as well as of ten compositions along the OH-Ap-chlorapatite (Cl-Ap) join and 12 compositions along the OH-Ap-fluorapatite (F-Ap) join have been measured using relaxation calorimetry (heat capacity option of the Physical Properties Measurement System—PPMS) and differential scanning calorimetry (DSC) in the temperature range of 5–764 K. Apatites along the Cl-OH and F-OH joins were synthesized at 1100 °C and 300 MPa in an internally heated gas pressure vessel via an exchange process between synthetic fluorapatite or chlorapatite crystals (200–500 μm size) and a series of Ca(OH)2-H2O solutions with specific compositions and amounts relative to the starting apatite. The standard third-law entropy of OH-Ap, derived from the low-temperature heat capacity measurements, is S° = 386.3 ± 2.5 J mol−1 K−1, which is ~ 1% lower than that resulting from low-temperature adiabatic calorimetry data on OH-Ap from the 1950’s. The heat capacity of OH-Ap above 298.15 K shows a hump-shaped anomaly centred around 442 K. Based on published structural and calorimetric work, this feature is interpreted to result from a monoclinic to hexagonal phase transition. Super ambient Cp up to this transition can be represented by the polynomial: C_{p}^{{text{OH - Ap}}} {}_{{298K - 442K}}left( {{text{J mol}}^{ - 1} {text{K}}^{- 1}} right) = {1013.7-13735.5T^{{ - 0.5}}} + 2.616718,10^{7} T^{{ - 2}} - 3.551381,10^{9} T^{{ - 3}} .. The DSC data above this transition were combined with heat capacities computed using density functional theory and can be given by the Cp polynomial: C_{p}^{{text{OH - Ap}}} {}_{{ >,442K}}left( {{text{J mol}}^{ - 1} {text{K}}^{- 1}} right) = {877.2-11393.7 T^{ - 0.5}} + {5.452030,10^{7}} ,T^{- {2}} - {1.394125,10^{10}} ,T^{- {3}}. Positive excess heat capacities of mixing, ∆Cpex, in the order of 1–2 J mol−1 K−1, occur in both solid solutions at around 70 K. They are significant at these conditions exceeding the 2σ-uncertainty of the data. This positive ∆Cpex is compensated by a negative ∆Cpex of the same order at around 250 K in both binaries. At higher temperatures (up to 1200 K), ∆Cpex is zero within error for all solid solution members. As a consequence, the calorimetric entropies, Scal, show no deviation from ideal mixing behaviour within a 2σ-uncertainty for both joins. Excess entropies of mixing, ∆Sex, are thus zero for the OH-Ap–F-Ap, as well as for the OH-Ap–Cl-Ap join. The Cp–T behaviour of the OH-Ap endmember is discussed in relation to that of the F- and Cl-endmembers.
Highlights
Apatite [Ca10(PO4)6(F,Cl,OH)2] is the most common and widespread phosphate mineral in the Earth’s crust and lithospheric mantle
To this end an earlier study measuring the Cp with regard to F-Cl mixing on the halogen site over a broad temperature range has been
The sample couplings in the PPMS measurements ranged between 99.0–99.4% around room temperature, increased with falling temperature to a maximum between 99.5% and 99.8% around 150 K, and decreased to values between 95 and 98% at the lowest temperatures
Summary
Apatite [Ca10(PO4)6(F,Cl,OH)2] is the most common and widespread phosphate mineral in the Earth’s crust and lithospheric mantle. As a major host for F, Cl, and OH, apatite in equilibrium with another major halogen carrier, biotite, can be used as a halogen exchange thermometer (Zhu and Sverjensky 1992; Sallet 2000). It can be used as a F, Cl, and OH barometer in equilibrium with a fluid (Zhu and Sverjensky 1991). There is an underlying importance in understanding the thermodynamics of F, Cl, and OH mixing on the halogen site in apatite To this end an earlier study measuring the Cp with regard to F-Cl mixing on the halogen site over a broad temperature range has been
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