As previously noted, the largest and most common caves are those formed by dissolution of limestone or dolomite.
Strong weathering is shown by dissolution of quartz and weathering of ilmenite.
Once crystal growth initiated at the seed interface, seed dissolution was stopped and further growth was assisted by dissolution of feed crystal which is at relatively high temperature.
A 50 mM solution of disulfide 4 was prepared by dissolution of disulfide 4 (86 mg, 0.25 mmol) in Tris buffer (500 mM, pH 7.8 8.0, 5.0 mL).
A 40 mM solution of disulfide 4 was prepared by dissolution of disulfide 4 (275 mg, 0.8 mmol) in Tris buffer (500 mM, pH 7.9, 20.0 mL).
Processes occurring during the incubation are most likely autolysis of the cells followed by dissolution of membrane proteins and surface carbohydrates into the aqueous solution.
This solution was prepared by dissolution of Trizma® base (0.303 g, 2.50 mmol) in D2O (5.0 mL) before adjustment to pH* ~9 with DCl (0.5 M in D2O).
A type of topography formed by dissolution of rocks like limestone and gypsum that is characterized by sinkholes, caves, and subterranean passages.
The weight loss of the scaffold increased by dissolution of the degraded products and TCP component, but mainly by dissolution of the glycyl-rich degraded products of the PLGA component.
Carbon is collected from cathodic mixture by dissolution of MnO2 in a solution of oxalic acid.
The hollow spheres are derived by dissolution of the outer shell, therefore the intact shell can be well preserved.
