, °geen verandering in 𝜔 wel in 𝜑 à horizontale lijn in psychrometrisch diagram
°bij hogere T, hogere capaciteit à relatief vochtgehalte daalt t.o.v. begintoestand
°massabalans: droge lucht: 𝑚̇Q; = 𝑚̇Q• = 𝑚̇Q water: 𝜔) = 𝜔f
°energiebalans: 𝑄̇ = 𝑚̇Q (ℎf − ℎ) ) of 𝑞 = ℎf − ℎ)
1.3.3 verwarmen met bevochtiging (ZIE VB SLIDE 39)
°door stoom vocht en temperatuur verhogen (𝑇f > 𝑇f )
°verstuiven van water à vochtgehalte stijgt en temperatuur daalt (𝑇z < 𝑇f )
1.3.4 koelen met ontvochtiging (ZIE VB SLIDE 41)
°ontvochtiging door koeling lucht tot onder dauwpunt
1.3.5 evaporatieve koeling
°als water verdampt latente verdampingswarmte onttrokken van omgeving
°lijnen constante natteboltemperatuur die ≈ 𝑠amenvallen met lijnen van constante enthalpie
°lucht komt binnen, water wordt verneveld à druppels verdampen en ontrekken E van lucht
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