Water Properties
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Temperature1 | Density |
0 | 999.8395 |
4 | 999.9720 (density maximum) |
10 | 999.7026 |
15 | 999.1026 |
20 | 998.2071 |
22 | 997.7735 |
25 | 997.0479 |
30 | 995.6502 |
40 | 992.2 |
60 | 983.2 |
80 | 971.8 |
100 | 958.4 |
Water Vapor Pressure at Different Temperatures (°C) | ||
---|---|---|
Temperature | Vapor Pressure (torr) | Vapor Pressure (Pa) |
0 | 4.6 | 613.2812 |
4 | 6.1 | 813.2642 |
10 | 9.2 | 1226.562 |
15 | 12.8 | 1706.522 |
20 | 17.5 | 2333.135 |
22 | 19.8 | 2639.776 |
25 | 23.8 | 3173.064 |
30 | 31.8 | 4239.64 |
35 | 42.2 | 5626.188 |
40 | 55.3 | 7372.707 |
45 | 71.9 | 9585.852 |
50 | 92.5 | 12332.29 |
55 | 118.0 | 15732 |
60 | 149.4 | 19918.31 |
65 | 187.5 | 24997.88 |
70 | 233.7 | 31157.35 |
75 | 289.1 | 38543.39 |
80 | 355.1 | 47342.64 |
85 | 433.6 | 57808.42 |
90 | 525.8 | 70100.71 |
95 | 633.9 | 84512.82 |
100 | 760.0 | 101324.7 |
Water Kw and pKw at Different Temperatures (°C) | ||
---|---|---|
Temperature | Kw 10–14 | pKw2 |
0 | 0.112 | 14.95 |
5 | 0.182 | 14.74 |
10 | 0.288 | 14.54 |
15 | 0.465 | 14.33 |
20 | 0.671 | 14.17 |
25 | 0.991 | 14.00 |
30 | 1.432 | 13.84 |
35 | 2.042 | 13.69 |
40 | 2.851 | 13.55 |
45 | 3.917 | 13.41 |
50 | 5.297 | 13.28 |
55 | 7.080 | 13.15 |
60 | 9.311 | 13.03 |
75 | 19.95 | 12.70 |
100 | 56.23 | 12.25 |
Specific Heat Capacity for Water |
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C°(H2O(l)) = 4184 J∙K−1∙kg−1 = 4.184 J∙g-1∙°C-1 |
C°(H2O(s)) = 1864 J∙K−1∙kg−1 |
C°(H2O(g)) = 2093 J∙K−1∙kg−1 |
Standard Water Melting and Boiling Temperatures and Enthalpies of the Transitions | ||
---|---|---|
Temperature (K) | ΔH (kJ/mol) | |
melting | 273.15 | 6.088 |
boiling | 373.15 | 40.656 (44.016 at 298 K) |
Water Cryoscopic (Freezing Point Depression) and Ebullioscopic (Boiling Point Elevation) Constants |
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Kf = 1.86°C∙kg∙mol−1 (cryoscopic constant) |
Kb = 0.51°C∙kg∙mol−1 (ebullioscopic constant) |
<figure class="ui-has-child-figcaption" id="CNX_Chem_00_EE_LiqWatAbso"> <figcaption>Water full-range spectral absorption curve. This curve shows the full-range spectral absorption for water. The y-axis signifies the absorption in 1/cm. If we divide 1 by this value, we will obtain the length of the path (in cm) after which the intensity of a light beam passing through water decays by a factor of the base of the natural logarithm e (e = 2.718281828).</figcaption> </figure>