Green fluid

Bile The yellowish-brown or green fluid secreted by the liver and discharged into the duodenum where it aids in the emulsification of fats, increases peristalsis, and retards putrefaction. 

TO RENDER A GREEN FLUID BLUE AND THEN RED BY BLOWING OR BREATHING INTO IT. 

Electrokinetic/Electrohydrodynamic Flow Instability, Fig. 3 Eiectrohydrodynamic mixing in a DC electric field. The images show the outlet branch of the microchannel after the device has been loaded with two fluids, (a) The initial condition showing a dark green fluid... 

A yellowish-green fluid produced by the liver and stored in the gallbladder, which empties through the bile duct into the duodenum of the small intestine, where it participates in the digestion of fats. It is considered to be one of the digestive juices of the intestinal tract. 

Successive n and n + 1 particle density fiinctions of fluids with pairwise additive potentials are related by the Yvon-Bom-Green (YBG) hierarchy [6]... 

The final result that we wish to present in this connection is an example of the Green-Kubo time-correlation expressions for transport coefficients. These expressions relate the transport coefficients of a fluid, such as... 

Green M S 1954 Markov random processes and the statistical mechanics of time-dependent phenomena. II. Irreversible processes in fluids J. Chem. Phys. 22 398... 

The inverse of the Cauchy-Green tensor, Cf, is called the Finger strain tensor. Physically the single-integral constitutive models define the viscoelastic extra stress Tv for a fluid particle as a time integral of the defonnation history, i.e. 

Initially a gummy green precipitate is formed which is difficult to stir magnetically. Eventually, however, the inorganic by-products become more fluid. The use of a mechanical stirrer may be desirable. 

Sec. 4 is concerned with the development of the theory of inhomogeneous partly quenched systems. The theory involves the inhomogeneous, or second-order, replica OZ equations and the Born-Green-Yvon equation for the density profile of adsorbed fluid in disordered media. Some computer simulation results are also given. 

To the best of our knowledge, there was only one attempt to consider inhomogeneous fluids adsorbed in disordered porous media [31] before our recent studies [32,33]. Inhomogeneous rephca Ornstein-Zernike equations, complemented by either the Born-Green-Yvon (BGY) or the Lovett-Mou-Buff-Wertheim (LMBW) equation for density profiles, have been proposed to study adsorption of a fluid near a plane boundary of a disordered matrix, which has been assumed uniform in a half-space [31]. However, the theory has not been complemented by any numerical solution. Our main goal is to consider a simple model for adsorption of a simple fluid in confined porous media and to solve it. In this section we follow our previously reported work [32,33]. 

Thermodynamic data on fluids can be found in Perry and Green (1984) or Edmister and Lee (1984), among others. The method or determining the thermodynamic data will be explained in detail in Step 3. 

Thermodynamic data are read from a table given in Perry and Green (1984) and interpolated. Subscript f denotes the saturated liquid (fluid) state, and subscript g the saturated vapor (gaseous) state. 

The compound MgGa204, when activated by divalent impurities such as Mn +, is used in ultraviolet-activated powders as a brilliant green phosphor. Another very important application is to improve the sensitivity of various bands used in the spectroscopic analysis of uranium. Minor uses are as high-temperature liquid seals, manometric fluids and heat-transfer media, and for low-temperature solders. 

Chaudhari AM, Woudenberg TM, Albin M, Goodson KE (1998) Transient liquid crystal thermometry of microfabricated PCR vessel arrays. J Microelectromech Sys 7 345-355 Cheng P, Wu WY (2006) Mesoscale and microscale phase heat transfer. In Greene G, Cho Y, Hartnett J, Bar-Cohen A (eds) Advances in heat transfer, vol 39. Elsevier, Amsterdam Choi SB, Barron RF, Warrington RQ (1991) Fluid flow and heat transfer in micro- tubes. ASME DSC 40 89-93... 

The difference in selenium content of acanthite from the different types of ore deposits can, of course, also be explained by the difference in ESe/ES in the ore fluids i.e., the ore fluids responsible for the formation of epithermal Au-Ag vein-type deposits may have had a higher ESe/ES ratio than that for epithermal Pb-Zn vein-type deposits. It is likely that considerable amounts of sulfur were derived from marine rocks (Green tuff) and were incorporated into ore fluids for base-metal veins. 

---