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Gases standard atmosphere

Enthalpy of Formation The ideal gas standard enthalpy (heat) of formation (AHJoqs) of chemical compound is the increment of enthalpy associated with the reaction of forming that compound in the ideal gas state from the constituent elements in their standard states, defined as the existing phase at a temperature of 298.15 K and one atmosphere (101.3 kPa). Sources for data are Refs. 15, 23, 24, 104, 115, and 116. The most accurate, but again complicated, estimation method is that of Benson et al. " A compromise between complexity and accuracy is based on the additive atomic group-contribution scheme of Joback his original units of kcal/mol have been converted to kj/mol by the conversion 1 kcal/mol = 4.1868 kJ/moL... [Pg.392]

Entropy of Formation The ideal gas standard entropy of formation (AS°298) of a chemical compound is the increment of entropy associated with the reaction of forming that compound in the ideal gas state from the constituent elements in their standard state definea as the existing phase at a temperature of 298.15 K and one atmosphere (101.325 kPa). Thus ... [Pg.392]

Boiling Point (BP) — the temperature at which a liquid changes to gas under standard atmospheric pressure (760 mm mercury). The BP of water is 100°C, while the BPs of ethyl alcohol and n-hexane are 78.4°C and 68.7°C, respectively. Lowering the atmospheric pressure (e.g., by applying a vacuum) will lower the BP conversely, higher pressures result in elevated boiling points. [Pg.160]

The atmosphere consists of a mixture of dry air and water vapour. Air is itself a mixture of several elemental gases, mainly oxygen and nitrogen, hut the proportions of these are consistent throughout the atmosphere and it is convenient to consider air as one gas. This has a molecular mass of 28.97 and the standard atmospheric pressure is 1013.25 mhar or 101 325 Pa. [Pg.227]

Another unit commonly used to express gas pressure is the standard atmosphere, or simply atmosphere (atm). This is the pressure exerted by a column of mercury 760 mm high with the mercury at 0°C. If we say that a gas has a pressure of 0.98 atm, we mean that the pressure is 98% of that exerted by a mercury column 760 mm high. [Pg.104]

Nernst zero of potential phys chem An electrode potential corresponding to the reversible equilibrium between hydrogen gas at a pressure of 1 standard atmosphere and hydrogen ions at unit activity. nernst zir-o av pa ten chal )... [Pg.257]

Bunsen coefficient 13 (dimensionless) Normal Volume of ozone (calculated for STP) dissolved per volume of water at T, when the partial pressure of ozone in the gas phase is one standard atmosphere (= 101 325 Pa) (273.15 K/T) He... [Pg.85]

VOLUME (Standard). The volume occupied by one gram molecular weight of 3 gas at 0°C and a pressure of 1 standard atmosphere. [Pg.1708]

The vesicles (bubbles) in basaltic lava flows can be used to determine paleoelevation at the time of eruption. In the repertoire of paleoelevation proxies presently available to the research community, it represents one of very few direct proxies of elevation. The technique is based on the sizes of vesicles at the tops and bottoms of lava flows. We assume that bubbles do not know a priori that they will reside in one part of the flow or another when they are erupted from a volcanic vent. As such, the mass of gas is evenly distributed throughout the flow. The volume of the bubbles will therefore depend on pressure, which at the top of the flow is just atmospheric pressure, and at the bottom is atmospheric plus hydrostatic pressure from lava overburden. Since lava thickness can be measured in the field, and bubble size distributions (most notably the modal size) can be measured in the lab, a simple relation can be solved for atmospheric pressure, and using the standard atmosphere, elevation can be determined. [Pg.195]

Of particular interest is the solvation process that takes place between the standard states of the solute in the ideal gas and in the solution. At a given temperature Tthe ideal gas standard state is specified by the standard pressure, P° = 0.1 MPa (formerly 0.101 325 MPa = 1 atmosphere was generally sped-... [Pg.79]

Volumetric flow rates of different gases are often compared to equivalent volumes of air at standard atmospheric temperature and pressure. The ideal gas law works well when used to size fans or compressors. Unfortunately, the gas law relationship, PV/T = constant, is frequently applied to choked gas streams flowing at sonic velocity. A typical misapplication could then be the conversion to standard cubic feet per minute in sizing SRVs. Whether the flow is sonic or subsonic depends mainly on the backpressure on the SRV outlet. In the API calculations, this is taken into account by the backpressure correction factor. [Pg.175]

Standard atmospheric pressure Pressure measurement Standard conditions Gas laws Boyle s law Charles law Gay-Lussac s law Combined gas law Density of an ideal gas Dalton s law of partial pressures Collecting gases over a liquid Deviations from ideal behavior... [Pg.401]

A vacuum chamber is vented using argon at 20 °C and standard atmospheric pressure. It flows into the chamber via a nozzle of 2 mm diameter. Calculate (i) the critical pressure (ii) the critical velocity (v ) and (iii) the mass flux of the gas. [Pg.28]

Area, heat transfer, In milk evaporation process, 311-13 Area, minimum, algorithm, 163 Argon gas, standard exergy In reference to atmosphere, 152t... [Pg.448]


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See also in sourсe #XX -- [ Pg.140 , Pg.141 ]




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Standard atmosphere

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