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Each winter, the researchers determined, surface waters are chilled by winds and become dense enough to cascade into the deep.
The determined surface heat flow can be used to calculate the temperature at depth beyond the logging depth.
Their spatial scale and amplitude determined surface density of nanoscale objects, size variations and component composition, mechanical strain field, random spatial distribution, and population of localized states [7].
This, in turn, determined surface wettability, polymer matrix crystallinity, in vitro bioactivity, and finally antioxidant activity, providing possibilities for modulating these properties in a wide range.
These predictions are confronted with the experimentally determined surface integration kinetics and a good agreement is found between theory and experiment.
The simulations of the self-aggregation of the polyoxyethylene alkyl ether surfactants lead to equilibrium nanoscale structures and computationally determined surface tensions which are in agreement with experimental data for different surfactant concentrations [1]. Figure 1.
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Another powerful force determining surface configuration is erosion, mainly by rivers.
Poisson Boltzmann calculations were used to determine surface electrostatic potential.
It is not necessary to determine surface reflectance first.
Membranes were subjected to X-ray photoelectron spectroscopy (XPS) analysis to determine surface element composition.
Zeta potential (ZP) is a powerful technique used in determining surface charge of NPs.
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