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1.)fumidêy Tatro \omega=0.0136 \mathrm{~kg} / \mathrm{lg} deycis.2) dey ais depontending upon dūndarey to abvo rb wailen Litl abarb catos untel it reachen squilibries at equilibrium the amount of coater absorbed as vaper and arnount of Water $apour Condenous are derme. do thera will be sorne water remaiving (anower &' c^{\prime} )3)\begin{array}{l}\frac{m_{w}}{m_{a}}=\frac{1}{100}=0.01 \quad m \omega=\text { mano of water } \\m_{a}=\text { mano of dy ais } \\\omega=\text { humidita ratio }=\frac{m w}{m a}=0.01 \\\omega=0.622\left(\frac{P_{V}}{P_{t}-P_{V}}\right) \\P_{v}=\text { Partial prosoure } \\\text { of rapour. } \\P_{t}=1 \text { bas } \\0.01=0.622\left(\frac{p_{v}}{1-p_{v}}\right) \\P_{V}=0.01582 \text { bar } \\P_{a}=P_{t}-P_{V}=1-0.01582 \\\text { Pratial Preasme of air 'PA' }=0.984 \mathrm{bas} \\\end{array}(\phi)4) Diltono Model for Noist ailb' * Duy ar and water vapour coecist as ideal gas shoring common volume and Temperatire but contributing pastial pleasue ...