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Quat Sci Rev 183:1–22 . Prospects for reconstructing paleoenvironmental conditions from organic compounds in polar snow and ice; Giorio C, Marton D, Formenton G, Tapparo A (2017) Formation of Metal–Cyanide Complexes in Deliquescent Airborne Particles: A New Possible Sink for HCN in Urban Environments. Environ Sci Technol 51:14107–14113.
Silane deposits between 300 and 500 °C, dichlorosilane at around 900 °C, and TEOS between 650 and 750 °C, resulting in a layer of low- temperature oxide (LTO). However, silane produces a lower-quality oxide than the other methods (lower dielectric strength, for instance), and it deposits nonconformally. Any of these reactions may be used in ...
In polymer science, dispersion polymerization is a heterogeneous polymerization process carried out in the presence of a polymeric stabilizer in the reaction medium. . Dispersion polymerization is a type of precipitation polymerization, meaning the solvent selected as the reaction medium is a good solvent for the monomer and the initiator, but is a non-solvent for the po
Dispersion is a process by which (in the case of solid dispersing in a liquid) agglomerated particles are separated from each other, and a new interface between the inner surface of the liquid dispersion medium and the surface of the dispersed particles is generated. This process is facilitated by molecular diffusion and convection. [4]
In materials science, dispersion is the fraction of atoms of a material exposed to the surface. In general, D = N S /N, where D is the dispersion, N S is the number of surface atoms and N T is the total number of atoms of the material. [1]
In 1923, Peter Debye and Erich Hückel reported the first successful theory for the distribution of charges in ionic solutions. [7] The framework of linearized Debye–Hückel theory subsequently was applied to colloidal dispersions by S. Levine and G. P. Dube [8] [9] who found that charged colloidal particles should experience a strong medium-range repulsion and a weaker long-range attraction.
The phase velocity is: v p = ω/k. The function ω(k), which gives ω as a function of k, is known as the dispersion relation. If ω is directly proportional to k, then the group velocity is exactly equal to the phase velocity. A wave of any shape will travel undistorted at this velocity.
On the other hand, when the degree of aggregation is polydisperse, then CMC is related to both the method of measurement and the dispersion. [ citation needed ] The common procedure to determine the CMC from experimental data is to look for the intersection ( inflection point ) of two straight lines traced through plots of the measured property ...