Structure and properties
Thermodynamic properties
Liquid physical properties
Water/steam equilibrium properties
Vapor pressure formula for steam in equilibrium with liquid water: : where ''P'' is equilibrium vapor pressure in k Pa, and ''T'' is temperature inMelting point of ice at various pressures
Data obtained from ''CRC Handbook of Chemistry and Physics'' 44th ed., p. 2390Table of various forms of ice
‡Ice XI triple point is theoretical and has never been obtainedPhase diagram
Water with dissolved NaCl
Self-ionization
:Spectral data
Self-diffusion coefficients
Additional data translated from German "Wasser (Stoffdaten)" page
The data that follows was copied and translated from the German language Wikipedia version of this page (which has moved tPhysical and thermodynamic tables
In the following tables, values are temperature-dependent and to a lesser degree pressure-dependent, and are arranged by state of aggregation (s = solid, lq = liquid, g = gas), which are clearly a function of temperature and pressure. All of the data were computed from data given in "Formulation of the Thermodynamic Properties of Ordinary Water Substance for Scientific and General Use" (1984). This applies to: * ''T'' – temperature in degrees Celsius * ''V'' – specific volume in cubicStandard conditions
In the following table, material data are given for standard pressure of 0.1 M Pa (equivalent to 1 bar). Up to 99.63 °C (the boiling point of water at 0.1 MPa), at this pressure water exists as a liquid. Above that, it exists as water vapor. Note that the boiling point of 100.0 °C is at a pressure of 0.101325 MPa (1 atm), which is the average atmospheric pressure. ::Triple point
In the following table, material data are given with a pressure of 611.7 Pa (equivalent to 0.006117 bar). Up to a temperature of 0.01 °C, the triple point of water, water normally exists as ice, except forSaturated vapor pressure
The following table is based on different, complementary sources and approximation formulas, whose values are of various quality and accuracy. The values in the temperature range of −100 °C to 100 °C were inferred from D. Sunday (1982) and are quite uniform and exact. The values in the temperature range of the boiling point of water up to the critical point (100 °C to 374 °C) are drawn from different sources and are substantially less accurate; hence they should be used only as approximate values.Klaus Scheffler (1981): ''Wasserdampftafeln: thermodynam. Eigenschaften von Wasser u. Wasserdampf bis 800°C u. 800 bar'' (''Water Vapor Tables: Thermodynamic Characteristics of Water and Water Vapor to 800°C and 800 bar''), Berlin .a. Ulrich Grigull, Johannes Staub, Peter Schiebener (1990): ''Steam Tables in SI-Units – Wasserdampftafeln.'' Springer-Verlagdima gmbh To use the values correctly, consider the following points: * The values apply only to smooth interfaces and in the absence other gases or gas mixtures such as air. Hence they apply only to pure phases and need a correction factor for systems in which air is present. * The values were not computed according formulas widely used in the US, but using somewhat more exact formulas (see below), which can also be used to compute further values in the appropriate temperature ranges. * The saturated vapor pressure over water in the temperature range of −100 °C to −50 °C is only extrapolated ranslator's note: Supercooled liquid water is not known to exist below −42 °C">Supercool.html" ;"title="ranslator's note: Supercool">ranslator's note: Supercooled liquid water is not known to exist below −42 °C * The values have various units (Pa, hPa or bar), which must be considered when reading them.Formulas
The table values for −100 °C to 100 °C were computed by the following formulas, where ''T'' is in kelvins and vapor pressures, ''Pw'' and ''Pi'', are in pascal (unit)">pascals. Over liquid water :loge(''Pw'') = −6094.4642 ''T''−1 + 21.1249952 − 2.724552×10−2 ''T'' + 1.6853396×10−5 ''T''2 + 2.4575506 loge(''T'') For temperature range: 173.15 K to 373.15 K or equivalently −100 °C to 100 °C Over ice :loge(''Pi'') = −5504.4088 ''T''−1 − 3.5704628 − 1.7337458×10−2 ''T'' + 6.5204209×10−6 ''T''2 + 6.1295027 loge(''T'') For temperature range: 173.15 K to 273.15 K or equivalently −100 °C to 0 °C At triple point An important basic value, which is not registered in the table, is the saturated vapor pressure at the triple point of water. The internationally accepted value according to measurements of Guildner, Johnson and Jones (1976) amounts to: :''Pw''(''ttp'' = 0.01 °C) = 611.657 Pa ± 0.010 Pa at (1 − ''α'') = 99% :Magnetic susceptibility
Accepted standardized value of the magnetic susceptibility of water at 20 °C (room temperature) is −12.97 cm3/mol. Accepted standardized value of the magnetic susceptibility of water at 20 °C (room temperature) is −0.702 cm3/g.See also
* Properties of waterReferences
Bibliography
* * * *External links