Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

Pressure-release freezing

Direct observations of Tm (P) and AV may be made in a sapphire optical cell with simple screw-press pump by measuring the offset in the pressure versus volume curve. AH can be measured at room pressure using a simple differential calorimeter comprised of two paper nut cups outfitted with kitchen thermistors and containing water in one and a standard solid material in the other for which the heat capacity curve is known. Direct observations of pressure-release freezing of water (as compared to pressure-release melting in silicates) may be observed in such an optical pressure cell by sudden release of pressure. [Pg.293]

Direct observation of pressure-release freezing of water-gas solutions. Pressure release boils out dissolved gas, such as CO2, and raises the melting point over and above that due to pressure release not involving as. This may be directly observed during the pressure release of such solutions in optical cells. [Pg.297]

Figure 9 shows a load-change cycle which is typical for discontinuous SCF extraction. When the pressure release phase following completion of the extraction is considered, the question arises as to the true temperature course. It is wellknown that the pressure-dependent equilibrium temperature of CO2 falls to -79 C under atmospheric conditions. This relationship leads to short-term thermal stresses within the inner surfaces of the pressure vessel, particularly in the lower part where dry ice may form. There is an additional risk to the process that the charge may freeze within the pressure vessel. When designing equipment for the extraction of natural substances, definition of the non-stationary courses of pressure and temperature during pressure release is therefore of especial importance in the choice of materials and for the geometry of the pressure vessel. [Pg.488]

Pore ice plays a particular role for the self-preservation effect in frozen soils Initial hydrate preservation apparently is helped by frozen pore water (not transformed into hydrate). Additional ice formation in the form of a film on the surface of gas-hydrate forming due to hydrate surface dissociation is expected to take place upon gas pressure release. Thus in the sample with 7% of montmorillonite particles (Win=17%), pore hydrate showed a higher stability after pressure release as a consequence of the greater ice content due to the freezing of remaining pore water (Figure 4).Our results clearly indicate that the hydrate content decreases on the expense of an increases of ice (Figure 5). [Pg.152]

After three freeze/pump/thaw cycles, the reaction vessel is fitted with hoses supplying liquid from a constant temperature bath and allowed to equilibrate to the desired temperature. Concurrently, coolant is supplied to the reflux condenser. Upon temperature equilibration, the reaction vessel valve, A4, is opened and the vessel is refilled with hydrogen, through valve Al. Again, excess pressure is released through the pressure release bubbler. The reactant gas, valve, Al, and the pressure release bubbler valve, A6, are then... [Pg.113]

According to the hydraulic pressure theory proposed by Powers [7], water freezes inside the capillary pores and the expanding ice pressurises the remaining liquid. The pressure can only be released if there are (partially) empty pores in the vicinity. This pressure release can be calculated with Darcy s Law [7]. Summarising the pressure increases with decreasing pore diameter with increasing distance over which the water must travel to empty pores or to the outside with increasing flow of pressurised water, proportional to the rate at which ice forms inside the pores themselves. [Pg.51]

FIGURE 8.9 The phase diagram for water and the cooling curve for a sample initially at point A. The sample cools at constant pressure through B to ice at C. The pause in the decline of the cooling curve at B is due to the release of heat when the liquid freezes. [Pg.504]

Pressure relief valves play an important role in LNG piping systems. Any section of LNG piping that can trap LNG must have a pressure relief valve to prevent failure of that section of pipe should all the LNG vaporize. These pressure relief valves are similar to those used on LNG storage tanks. Spring-loaded valves that reseat following a reduction in pressure are preferred to those that do not and vent all the LNG in that line. Pressure relief valves should be protected from water accumulation to prevent freezing in the open position since the LNG vapor that is released will likely be very cold. [Pg.118]


See other pages where Pressure-release freezing is mentioned: [Pg.76]    [Pg.211]    [Pg.212]    [Pg.76]    [Pg.159]    [Pg.127]    [Pg.213]    [Pg.114]    [Pg.68]    [Pg.149]    [Pg.230]    [Pg.243]    [Pg.241]    [Pg.413]    [Pg.631]    [Pg.385]    [Pg.297]    [Pg.68]    [Pg.468]    [Pg.354]    [Pg.2058]    [Pg.2143]    [Pg.110]    [Pg.75]    [Pg.81]    [Pg.181]    [Pg.468]    [Pg.73]    [Pg.108]    [Pg.2]    [Pg.65]    [Pg.369]    [Pg.372]    [Pg.104]    [Pg.51]    [Pg.236]    [Pg.468]    [Pg.468]    [Pg.2]    [Pg.412]    [Pg.354]   
See also in sourсe #XX -- [ Pg.293 , Pg.297 ]




SEARCH



Freeze release

© 2024 chempedia.info