920 research outputs found
The Mechanism of Precipitation of Biological Minerals. The Phosphates, Oxalates and Carbonates of Calcium
The precipitation of the phosphates, oxalates, and carbonates
of calcium is complicated by the possible formation of different
precursor phases involving polymorphs, hydrates, and acid salts.
In order to elucidate the mechanisms of the reactions, it is necessary
to study the kinetics under conditions of controlled supersaturation
calculated from the activities of free ionic species. In
general, the rates of formation of the salts are proportional to the
(supersaturation)", where n = 1.25-2.0 suggesting a surface controlled
process. However, in the case of the calcium phosphate
phases, the precipitation of the thermodynamically most stable
hydroxyapatite is often complicated by the formation of precursor
phases which form and subsequently dissolve during the overall
reactions. The sensitivity of the various solid phases to the presence
of crystal growth inhibitors is markedly different. Thus in
the case of calcium carbonate, it is possible to selectively inhibit
calcite and aragonite by adding traces of phosphonate inhibitor,
thereby encouraging the formation of vaterite, the most thermodynamically
unstable phase. Such selective inhibition may explain
the existence of thermodynamically unstable phases in biological
systems
The Kinetics of Growth of Seed Crystals in Solution
The theory of growth of seed crystals in critically supersaturated
electrolyte solutions is discussed. Techniques of studying
crystal growth are reviewed, the application of which yield highly
precise and reproducible data. Effects of added foreign substances
on the rate of crystallization are emphasized and results, obtained
for magnesium oxalate, barium and strontium sulfate crystal
growth, discussed
The Crystal Growth of Sparingly Soluble Salts
The mechanism of crystal growth of sparingly soluble salts
from their supersaturated solutions is discussed in the light of a
number of available growth theories. It is shown that in the case
of both calcium sulphate and calcium carbonate, the observed
quadratic dependence of the rate of crystallization upon the
relative supersaturation is consistent with a surface controlled
reaction. The reaction rates are unaffected by changes in the fluid
dynamics within the crystallization cell, and the activation energy
for both seeded growth and the linear growth of calcium sulphate
is 15.0 ± 0.5 kcal mo1e-1• Evidence is discussed for a screw dislocation
mechanism for calcium sulphate crystal growth. Under
conditions of relatively high supersaturation, secondary nucleation
of both calcium sulphate and calcium carbonate crystals is observed
upon the addition of seed crystals. The striking effect of certain
additives in reducing the rate of crystal growth is discussed in
terms of the important factors involved and in a number of
instances it is shown that a simple adsorption isotherm of the
Langmuir type satisfactory describes the growth data
The Nucleation and Growth of Calcium Phosphate Crystals
The growth of seed crystals in supersaturated solutions of
calcium phosphate at 25° C is discussed. In the pH range 5-6, the
crystallization of dicalcium phosphate follows a second order rate
equation in a process which is surface reaction rather than· diffusion
controlled. Under physiological pH conditions, the growth
of hydroxyapatite seed crystals proceeds through the formation
of a precursor phase which has a calcium : phosphate ratio of
1.45 ± 0.05 and which attains the HAP composition after slow
interaction with the medium; the process again appears to be
interface controlled
The Thermodynamics of Formation of Metal Complexes and Ion-Pairs in Solution
The problem of characterisation of species present at equilibrium
in an electrolyte solution is discussed. Shortcomings of the
free energy approach are shown due to inadmissible neglect of
entropy changes in complex formation. It is shown that complexes
formed with hard ligands are stabilised entirely by entropy
changes. Soft or covalent interactions are always characterized by
exothermic enthalpy changes
The Crystal Growth of Sparingly Soluble Salts
The mechanism of crystal growth of sparingly soluble salts
from their supersaturated solutions is discussed in the light of a
number of available growth theories. It is shown that in the case
of both calcium sulphate and calcium carbonate, the observed
quadratic dependence of the rate of crystallization upon the
relative supersaturation is consistent with a surface controlled
reaction. The reaction rates are unaffected by changes in the fluid
dynamics within the crystallization cell, and the activation energy
for both seeded growth and the linear growth of calcium sulphate
is 15.0 ± 0.5 kcal mo1e-1• Evidence is discussed for a screw dislocation
mechanism for calcium sulphate crystal growth. Under
conditions of relatively high supersaturation, secondary nucleation
of both calcium sulphate and calcium carbonate crystals is observed
upon the addition of seed crystals. The striking effect of certain
additives in reducing the rate of crystal growth is discussed in
terms of the important factors involved and in a number of
instances it is shown that a simple adsorption isotherm of the
Langmuir type satisfactory describes the growth data
The Mechanism of Precipitation of Biological Minerals. The Phosphates, Oxalates and Carbonates of Calcium
The precipitation of the phosphates, oxalates, and carbonates
of calcium is complicated by the possible formation of different
precursor phases involving polymorphs, hydrates, and acid salts.
In order to elucidate the mechanisms of the reactions, it is necessary
to study the kinetics under conditions of controlled supersaturation
calculated from the activities of free ionic species. In
general, the rates of formation of the salts are proportional to the
(supersaturation)", where n = 1.25-2.0 suggesting a surface controlled
process. However, in the case of the calcium phosphate
phases, the precipitation of the thermodynamically most stable
hydroxyapatite is often complicated by the formation of precursor
phases which form and subsequently dissolve during the overall
reactions. The sensitivity of the various solid phases to the presence
of crystal growth inhibitors is markedly different. Thus in
the case of calcium carbonate, it is possible to selectively inhibit
calcite and aragonite by adding traces of phosphonate inhibitor,
thereby encouraging the formation of vaterite, the most thermodynamically
unstable phase. Such selective inhibition may explain
the existence of thermodynamically unstable phases in biological
systems
The Growth of Calcium and Strontium Sulfates on Barium Sulfate Surfaces
The crystallization of calcium sulfate dihydrate (gypsum) and strontium sulfate (celestite) induced by the presence of barium sulfate (barite) surfaces has been studied using a Constant Composition kinetic method. In contrast to calcium sulfate, strontium sulfate appears to grow epitaxially on barium sulfate surfaces. However, barium sulfate induces calcium sulfate dihydrate precipitation from meta stable supersaturated solutions of the salt. Following nucleation, the rate of growth of strontium sulfate was found to be a second order with respect to supersaturation indicating a surface dislocation growth mechanism. The observed epitaxial growth is in agreement with calculations based on crystal lattice mismatch
The Kinetics of Crystallization of Calcium Fluoride. A New Constant Composition Method
A new method is described for studying reproducibly, the
kinetics of crystallization of calcium fluoride under conditions of
constant solution composition. The method can be used even at
very low supersaturation. The rate is proportional to the square of
the supersaturation, over the range of relative supersaturation,
S = 0.20 - 1.66. The results point to a surface controlled crystallization.
The rate is markedly influenced by the presence of phosphate
The Kinetics of Crystallization of Calcium Fluoride. A New Constant Composition Method
A new method is described for studying reproducibly, the
kinetics of crystallization of calcium fluoride under conditions of
constant solution composition. The method can be used even at
very low supersaturation. The rate is proportional to the square of
the supersaturation, over the range of relative supersaturation,
S = 0.20 - 1.66. The results point to a surface controlled crystallization.
The rate is markedly influenced by the presence of phosphate
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