id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
ap-726	Zítek, P.; Vyhlídal, T.	Model Based Control of Moisture Sorption in a Historical Interior	2005	6	.pdf	application/pdf	5205	191	47	If x is the absolute humidity in kg of water per one kg of dry air, its value, corresponding to a certain given � and T, results, e.g., from the Magnus relationship (Camuffo, 1998), as follows x aT b T� � � �3795 10 103. ( )� , (4) where a � 7.5 and the additive temperature constant b � 237.3 °C. If a considerable change in relative humidity from �0 to � has occurred under x = const., the corresponding temperature change is relatively small, given as follows T T b T a0 0 0� � � �(log log )� � , (6) where, unlike (3), the decimal logarithm is used.	cache/ap-726.pdf	txt/ap-726.txt