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liquids, such as glass or ice. the horizontal axis, reaching into the layer of calcium oxide above or below.
In a second step, a layer of calcium cations is immobilized at the interface.
The thin and defects-free layer of calcium phosphate was formed by e-beam evaporation.
Soils lacking any of these characteristics are also classified as Aridisols if a layer of calcium carbonate, gypsum (hydrated calcium sulfate), or cemented silica is present below the surface horizon.
The artificial bone, porous and coated with a thin layer of calcium phosphate, is implanted into the arm in place of the damaged bone.
Finally, under non-sterile conditions mimicking an in situ application, B. pumilus ACA-DC 4061 formed a fine layer of calcium carbonate.
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interspersed with neat layers of calcium oxide.
Encrusted layers of calcium carbonate, gypsum, and salt, however, are often considered forms of duricrust.
The height of these structures ranged from one to several molecular layers of calcium carbonate.
The bone, called the otolith, is no larger than a grain of sand and adds layers of calcium carbonate as the larvae develop, like a daily version of a tree ring.
Vertisols are dark-coloured soils (though they have only moderate humus content) that may also be characterized by salinity and well-defined layers of calcium carbonate or gypsum.
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