The rate d t d τ \frac{dt}{d\tau} d τ d t of the change of temperature of the water is given by
d t d τ = k ( t − t e n v ) , \frac{dt}{d\tau}=k(t-t_{env}), d τ d t = k ( t − t e n v ) ,
where k k k is the proportionality coefficient,
t t t - current temperature of the water,
t e n v t_{env} t e n v - environmental temperature.
Let us find the coefficient by solving the equation with initial and final conditions defined by the first case.
d t t − t e n v = k d τ , \frac{dt}{t-t_{env}}=kd\tau, t − t e n v d t = k d τ ,
∫ 70 50 d t t − t e n v = k ∫ 0 3 d τ , \int_{70}^{50}\frac{dt}{t-t_{env}}=k\int_0^3d\tau, ∫ 70 50 t − t e n v d t = k ∫ 0 3 d τ ,
l n ( t − t e n v ) ∣ 70 50 = k τ ∣ 0 3 , ln(t-t_{env})\Big\rvert_{70}^{50}=k\tau\Big\rvert_0^3, l n ( t − t e n v ) ∣ ∣ 70 50 = k τ ∣ ∣ 0 3 ,
k = 1 3 l n ( 70 − 30 50 − 30 ) = 0.23105. k=\frac{1}{3}ln\Bigg(\frac{70-30}{50-30}\Bigg)=0.23105. k = 3 1 l n ( 50 − 30 70 − 30 ) = 0.23105. Substitution the conditions defined by the second case lets us find the final temperature t f t_f t f of the water after 5 minutes of the cooldown
l n ( t − t e n v ) ∣ 70 t f = k τ ∣ 0 5 , ln(t-t_{env})\Big\rvert_{70}^{t_f}=k\tau\Big\rvert_0^5, l n ( t − t e n v ) ∣ ∣ 70 t f = k τ ∣ ∣ 0 5 ,
l n ( 70 − 30 t f − 30 ) = 5 k , ln\Bigg(\frac{70-30}{t_f-30}\Bigg)=5k, l n ( t f − 30 70 − 30 ) = 5 k ,
40 t f − 30 = e 5 k , \frac{40}{t_f-30}=e^{5k}, t f − 30 40 = e 5 k ,
t f = 40 e 5 ⋅ 0.23105 + 30 = 42.6 0 o C . t_f=\frac{40}{e^{5\cdot0.23105}}+30=42.60^oC. t f = e 5 ⋅ 0.23105 40 + 30 = 42.6 0 o C .