Titlebook: Gas Transfer at Water Surfaces; Wilfried Brutsaert,Gerhard H. Jirka Book 1984 Springer Science+Business Media Dordrecht 1984 Entrainment.a

褻瀆

Turbulence Structure of Wavy Stratified Air-Water Flowole of the transport in turbulent kinetic energy (TKE) and shear stress balance is shown: it is considered as responsible of the secondary flow generation. When secondary flows are not important a diffusive length scale can be determined linked with wave characteristics.

Slit-Lamp

Nuance

Absorption of Gases at Condensing and Evaporating Water Surfacesncentration of gas transferred to the water which was always less than that at thermal equilibrium. The rate of mass transfer was controlled by heat transfer to the droplets. A mechanism is proposed whereby hydrate formation at the water surface explains the results observed.

Encapsulate

Interfacial Motion Observed during Experiments on Air-Water Gas Transferaves dominate the wave field. Their effects on gas transfer could be analyzed thru a linear hydrodynamic stability model. Otherwise, the mass transfer would be influenced by the observed mixed non-linear processes such as the gravity wave breaking, the wave-wave and the wind-wave interactions.

exostosis

Schaltzeichen (Auswahl DIN 40 900)compared with literature values and with Henry’s constants measured in a bubble column. The results indicate that the technique is accurate. In addition, the technique is unencumbered by equilibration problems which limit the utility of other methods for determining Henry’s constant.

SPALL

disparage

https://doi.org/10.1007/978-3-322-88922-5and countercurrent packed columns. Hence the gas-phase resistance has been underestimated, which can lead to the overestimation of overall mass transfer rate constants. Also, k./k. varies for a given process depending on the hydrodynamic conditions.

LITHE

腐蝕

Sebastian W?rwag,Alexandra Clootsertically oscillating grid whose stroke length, frequency, and distance from the interface are adjustable. Preliminary results using five gases (O., N., CH., CO., and Rn) indicate that the data are consistent with surface renewal and energy dissipation models of gas exchange.

GROSS