With the polymer, however, ACC always appeared first and
vaterite formed much later.
In this case, the microscope not only identified signatures corresponding to calcium carbonate as forming the crust, but was also able to differentiate between the calcite and
vaterite forms when it was present as a mixture while still attached to the leaf surface.»
Not exact matches
WAXS (wide angle x-ray scattering) analysis of the crystalline particles finally
formed at ambient conditions shows that pure calcite (the stable polymorph of calcium carbonate)
forms at pH - values corresponding to high binding strength in clusters and that predominantly
vaterite (the least stable polymorph) and traces of calcite
form at pH - values corresponding to low binding strength in clusters (fig.
Scientists at Sainsbury Laboratory Cambridge University have found that the mineral
vaterite, a
form (polymorph) of calcium carbonate, is a dominant component of the protective silvery - white crust that
forms on the leaves of a number of alpine plants, which are part of the Garden's national collection of European Saxifraga species.
Without the polymer, they saw crystals of
vaterite and a little calcite
forming randomly under the microscope.
But in some cases, droplet - like particles of uncrystallized material known as amorphous calcium carbonate, or ACC,
formed first and then transformed into either aragonite or
vaterite.
All of the common crystal
forms, including calcite (found in limestone), aragonite (found in mother - of - pearl), and
vaterite (found in gallstones), crystallized from solution, often at the same time.
Multiple
forms often nucleated in a single experiment — at least one calcite crystal
formed on top of an aragonite crystal while
vaterite crystals grew nearby.