Titration Calculations: Weak Acid - Strong Base
Titration of a Polyprotic Acid
Factors Affecting Solubility
Solution Composition During Acid/Base Titrations
Composition of Polyprotic Acid Solutions as a Function of pH
Titration of Polyprotic Acids with a Strong Base
You might also read
Articles linked to this work by shared authors, journal, and citation graph.
Updated: Jul 11, 2026

Separation of Single-stranded DNA, Double-stranded DNA and RNA from an Environmental Viral Community Using Hydroxyapatite Chromatography
Published on: September 29, 2011
1Dental Materials Science, The University of Hong Kong, Hong Kong.
This study investigated the solubility of hydroxyapatite, a mineral found in teeth and bones, over a broader pH range than previously studied. Using a solid titration method, the researchers confirmed a previously reported solubility isotherm but extended it from pH 2.9 to 5.2. They observed an abrupt change in the solubility curve at pH 3.9 and found that calcium-deficient hydroxyapatite formed instead of brushite, a mineral previously thought to form under acidic conditions. The study validated the reliability of the solid titration method and suggested that the chemistry of calcium phosphates in biological systems may need to be reevaluated. These findings could help improve models of tooth mineral stability in saliva and related environments.
05:41Rapid Mix Preparation of Bioinspired Nanoscale Hydroxyapatite for Biomedical Applications
Published on: February 23, 2017
08:21Optimized Procedure for Determining the Adsorption of Phosphonates onto Granular Ferric Hydroxide using a Miniaturized Phosphorus Determination Method
Published on: May 18, 2018
Area of Science:
Background:
The solubility of hydroxyapatite (HAp) is a central topic in saliva chemistry and dental caries research. Prior studies have suggested that the solubility isotherm of HAp is lower than commonly reported and has a different slope, possibly due to incongruent dissolution. This discrepancy introduces uncertainty in understanding how HAp behaves in biological fluids. While previous work has established a baseline, the exact behavior of HAp in a broader pH range remains unclear. The absence of a definitive solubility profile limits the ability to predict HAp stability in oral environments. Earlier studies have focused on narrower pH ranges, leaving gaps in the full spectrum of HAp solubility behavior. The formation of secondary phases, such as brushite, is also poorly characterized in this context. This gap motivated the current investigation to expand the pH range and identify precipitates formed during HAp dissolution. The goal is to refine the solubility isotherm for more accurate applications in dental and biological systems.
Purpose Of The Study:
The primary aim of this study was to determine the solubility isotherm of hydroxyapatite (HAp) over a broader pH range than previously investigated. The researchers sought to validate and extend prior findings by confirming the reproducibility of the solubility isotherm and identifying the precipitate formed at equilibrium. By expanding the pH range from approximately 2.9 to 5.2, the study aimed to provide a more comprehensive understanding of HAp's solubility behavior. This work also aimed to clarify whether brushite forms under these conditions, as suggested in earlier literature. The study focused on the chemical stability of HAp and its transformation into other phases during dissolution. The motivation for this research stems from the need to refine models of calcium phosphate chemistry in biological systems. By using the solid titration method, the researchers aimed to produce reliable and reproducible data on HAp solubility. The ultimate goal was to contribute to a more accurate understanding of HAp behavior in saliva and related contexts.
Main Methods:
The study employed the solid titration technique developed by Leung and Darvell to investigate the solubility of hydroxyapatite (HAp) in 100 mM aqueous KCl at a controlled temperature of 37.0+/-0.1 degrees Celsius. The pH range was extended from approximately 2.9 to 5.2 to capture a broader spectrum of solubility behavior. X-ray diffraction (XRD) and energy-dispersive X-ray spectroscopy (EDX) were used to identify the precipitates formed during dissolution. Scanning electron microscopy (SEM) and transmission electron microscopy (TEM) were utilized to examine the morphology of the precipitates. The experimental setup was designed to ensure reproducibility and accuracy in measuring solubility isotherms. The researchers focused on confirming the presence or absence of brushite and calcium-deficient HAp at different pH levels. The solid titration method allowed for precise control of pH and temperature during the dissolution process. The combination of analytical techniques provided a comprehensive characterization of the precipitates and their structural properties.
Main Results:
The study confirmed the solubility isotherm of hydroxyapatite (HAp) previously reported by Chen et al., extending the pH range from 2.9 to 5.2. An abrupt change in the slope of the solubility isotherm was observed at pH approximately 3.9, indicating a shift in dissolution behavior. No other phase than HAp was detected at pH 3.2, 3.6, and 4.1, suggesting that the dissolution process remained congruent within this range. Brushite (dicalcium phosphate dihydrate) was not detected, even below pH 3.9, where calcium-deficient HAp was consistently formed. The solid titration method was validated as reproducible across the tested pH range. The formation of calcium-deficient HAp was observed as a stable phase under the experimental conditions. The absence of brushite challenges previous assumptions about its formation in acidic environments. These findings suggest a need to reevaluate the chemistry of calcium phosphates in biological systems.
Conclusions:
The study reconfirmed the solubility isotherm of hydroxyapatite (HAp) as previously reported, extending the pH range to 2.9–5.2. The abrupt change in slope at pH approximately 3.9 was consistently observed, indicating a shift in dissolution behavior. The researchers did not detect brushite formation, even below pH 3.9, where calcium-deficient HAp was the only precipitate identified. This finding challenges prior assumptions about the formation of brushite in acidic conditions. The solid titration method was validated as reproducible and reliable for measuring HAp solubility. The consistent formation of calcium-deficient HAp suggests a need to reevaluate the chemistry of calcium phosphates in biological systems. The absence of brushite indicates that the dissolution process may be more complex than previously understood. These results contribute to a more accurate understanding of HAp solubility in oral and biological environments.
The study found an abrupt change in the solubility isotherm of hydroxyapatite at pH approximately 3.9, with calcium-deficient HAp forming instead of brushite.
X-ray diffraction (XRD), energy-dispersive X-ray spectroscopy (EDX), scanning electron microscopy (SEM), and transmission electron microscopy (TEM) were used.
The pH range was extended to capture a broader spectrum of solubility behavior and validate prior findings in a wider context.
The solid titration method was used to measure hydroxyapatite solubility and confirm the reproducibility of the solubility isotherm.
Calcium-deficient HAp was consistently formed instead of brushite, suggesting a need to reevaluate calcium phosphate chemistry in biological systems.
The study provides a more accurate solubility isotherm for hydroxyapatite, which is essential for modeling its behavior in saliva and related contexts.