We first consider the vertical motion of the stone as it falls toward the water. The initial y velocity component of the stone is
vyi=visinθ=–(4.00m/s)sin60.00=–3.46m/s
and its y coordinate is
yf=yi+vyit+12ayt2=h+(visinθ)t−12gt2
yf=2.50−3.46t−4.90t2
where y is in m and t in s. We have taken the water’s surface to be at y=0. At the water,
4.90t2+3.46t–2.50=0
Solving for the positive root of the equation, we get
t=−3.46+√(3.46)2−4(4.90)(−2.50)2(4.90)
t=−3.46+7.819.80
t=0.443s
The y component of velocity of the stone when it reaches the water at this time t is
vyf=vyi+ayt=–3.46–gt=–7.81m/s
After the stone enters to water, its speed, and therefore the magnitude of each velocity component, is reduced by one-half. Thus, the y component of the velocity of the stone in the water is
vyi=(–7.81m/s)/2=–3.91m/s,
and this component remains constant until the stone reaches the bottom. As the stone moves through the water, its y coordinate is
yf=yi+vyit+12ayt2
yf=−3.91t
The stone reaches the bottom of the pool when yf=–3.00m:
yf=–3.91t=–3.00→t=0.767s
The total time interval the stone takes to reach the bottom of the pool is
Δt=0.443s+0.767s=1.21s