Concept:
According to Snell's Law of refraction, when a ray of light passes across multiple parallel plane interfaces separating different media, the product of the refractive index and the sine of the angle of incidence/refraction remains constant throughout the path:
\[ \mu_1 \sin\theta_1 = \mu_2 \sin\theta_2 = \mu_3 \sin\theta_3 = \text{Constant} \]
The critical angle \(\theta_c\) for a boundary separating a denser medium of index \(\mu_d\) and a rarer medium of index \(\mu_r\) is defined by:
\[ \sin\theta_c = \frac{\mu_r}{\mu_d} \]
Step 1: Analyzing the initial glass-air configuration.
Initially, the ray travels in glass (\(\mu_g = \frac{3}{2}\)) and is incident on the glass-air boundary at the critical angle \(\theta_c\). The surrounding medium is air (\(\mu_a = 1\)).
\[ \sin\theta_c = \frac{\mu_a}{\mu_g} = \frac{1}{3/2} = \frac{2}{3} \]
Step 2: Analyzing the system after adding the water layer.
Now, a horizontal layer of water (\(\mu_w = \frac{4}{3}\)) is placed on top of the glass slab. The ray originates with the exact same initial angle of incidence \(\theta_c\) within the glass. It refracts first at the glass-water interface at an angle \(\theta_w\), and then arrives at the water-air interface, finally emerging into the air at an angle \(e\).
Applying continuous parallel layer forms of Snell's Law across all three successive media (Glass \(\rightarrow\) Water \(\rightarrow\) Air):
\[ \mu_g \sin\theta_c = \mu_w \sin\theta_w = \mu_a \sin e \]
Step 3: Calculating the angle of emergence \(e\).
By equating the expression for the first medium (glass) directly with the final medium (air):
\[ \mu_g \sin\theta_c = \mu_a \sin e \]
Substituting our known values (\(\mu_g = \frac{3}{2}\), \(\sin\theta_c = \frac{2}{3}\), and \(\mu_a = 1\)):
\[ \left(\frac{3}{2}\right) \times \left(\frac{2}{3}\right) = 1 \times \sin e \]
\[ 1 = \sin e \]
Since \(\sin e = 1\), the angle of emergence must be:
\[ e = 90^{\circ} \]
This means the ray of light will graze along the final horizontal water-air boundary line as it exits.