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Temperature, critical limiting

Provision of high-temperature alarms and interlocks to shut down reactor feeds, or heating systems, if the temperature exceeds critical limits. [Pg.370]

The level of a measure necessary to ensure that a hazard is fully controlled is determined and called the critical limit. For example, how high the temperature must be to ensure that a pathogen has been eliminated, or how low the humidity must be to prevent the growth of mould fungi. Principle 4 Establish a system to monitor control of the CCP(s). [Pg.492]

On the other hand, samples can be irradiated at constant microwave power over a certain fixed period, for example at 100 W for 10 min. As there is no control over the resulting temperature or pressure, care has to be taken not to exceed the operational limits of the system and this type of program should only be used for well-known reactions with non-critical limits, or under open-vessel (reflux) conditions. Since in this method only the applied energy and not the resulting temperature is controlled, the quality of reaction control is often superior employing a temperature-controlled program. [Pg.96]

Temperature in bulk liquid Temperature in bubble Normal boiling point Temperature of water Superheat-limit temperature Critical temperature Specific volume Distance... [Pg.203]

A typical paper on cryo-crystallographic applications is usually concluded by the author s encouragement to study more and more samples at lower and lower temperature. The message from this chapter is instead somewhat different and can be summarized as follows (1) use temperature critically and think carefully when it is necessary to measure structures or properties of crystals at lower temperature] (2) use all the additional information available when studying the sample at low temperature] (3) do not limit the temperature scans in the range below ambient conditions (even when studying organic crystals). [Pg.62]

Xu and Ruppel (1999) solved the coupled mass, heat, and momentum equations of change, for methane and methane-saturated fluxes from below into the hydrate stability region. They show that frequently methane is the critical, limiting factor for hydrate formation in the ocean. That is, the pressure-temperature envelope of the Section 7.4.1 only represents an outer bound of where hydrates might occur, and the hydrate occurrence is usually less, controlled by methane availability as shown in Section 7.4.3. Further their model indicates the fluid flow (called advection or convection) in the amount of approximately 1.5 mm/yr (rather than diffusion alone) is necessary to produce significant amount of oceanic hydrates. [Pg.566]

Critical limits of phenomena or magnetic states that coincide with phase transitions, for example, magnetic fields or temperatures in spatially ordered, cooperative spin effects. [Pg.70]

LIQUID or SYSTEM IS ALL VAPOR. Make certain you are sufficiently below the critical point for pressure and temperature assumptions. When you find the right temperature, a limited temperature variance will change the system from all liquid to all vapor. [Pg.43]

Temperature is one of the most important variables that determines the distribution and abundance of species (Cossins and Bowler 1987) and imposes critical limits on fitness. As a result of increasing metabolic rate, increasing temperature can increase the uptake and toxicity of contaminants by poikilothermic species, but may also increase rates of detoxification and excretion of toxicants (e.g., pyrethroid insecticides National Research Council of Canada [NRCC] 1987). Temperature extremes in themselves are stressful to organisms, causing induction of various stress proteins, which may be associated with fitness costs (Hoffmann et al. 2003). [Pg.47]

The role of water in governing the upper thermal limits for life also is based on covalent transformations in which water is a reactant. As emphasized earlier in this chapter, the removal of a molecule of water from reactants is common in diverse biosynthetic reactions, including the polymerization of amino acids into proteins and nucleotide triphosphates into nucleic acids. The breakdown of biomolecules often involves hydrolysis, and increased temperatures generally enhance these hydrolytic reactions. The thermal stabilities of many biomolecules, for instance, certain amino acids and ATP, become limiting at high temperatures. Calculations suggest that ATP hydrolysis becomes a critical limiting factor for life at temperatures between 110°C and 140°C (Leibrock et al., 1995 Jaenicke, 2000). Thus, at temperatures near 110°C, both the covalent and the noncovalent chemistries of water that are so critical for life are altered to the extent that life based on an abundance of liquid water ceases to be possible. [Pg.285]

Predictions of theory for rods with axial ratio x = 100 are shown by the curves in Fig. 8. Here % is plotted as ordinate against the volume fractions Vp and Vp in the coexisting phases the ordinate may alternatively, be regarded as an (inverse) measure of temperature. The narrow biphasic gap is httle affected by the interactions for negative values of %, as was noted above. If, however, % is positive, a critical point emerges at = 0.055. For values of % immediately above this critical limit, the shallow concave curve delineates the loci of coexisting anisotropic phases, these being in addition to the isotropic and nematic phases of lower concentration within the narrow biphasic gap on the left. At x = 0.070 the compositions of two of the phases, one from each of the respective pairs, reach the same value. Three phases coexist at this triple point. [Pg.26]

For a given object, the permissible rate of drying can be affected by viscosity of water which depends on temperature. The rate of surface evaporation, which can be controlled over a wide range by humidity, temperature and flow velocity of the air, must not exceed a critical limit, beyond which the rate of evaporation would exceed the rate at which water is supplied from deeper layers. The effect of temperature and air humidity on the distribution of water in the object being dried is illustrated in Fig. 171. The diagram indicates that the drying will proceed at the highest rate and at a minimum water content difference (and thus minimum stress) in case c which corresponds to the conditions in controlled humidity dryers. [Pg.349]

Moreover, the term "breathable" implies that the fabric is actively ventilated. This is not the case. Breathable fabrics passively allow water vapour to diffuse through them yet still prevent the penetration of liquid water. Production of water vapour by the skin is essential for maintenance of body temperature. The normal body core temperature is 37°C, and skin temperature is between 33 and 35°C, depending on conditions. If the core temperature goes beyond critical limits of about 24°C and 45°C then death results. The narrower limits of 34°C and 42°C can cause adverse effects such as disorientation and convulsions. If the sufferer is engaged in a hazardous pastime or occupation then this could have disastrous consequences. [Pg.250]


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See also in sourсe #XX -- [ Pg.233 ]

See also in sourсe #XX -- [ Pg.233 ]




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