Water is poured at a rate of \(0.5\text{ m}^3\) per minute into an empty container in the form of an open hemisphere with inside radius \(3\text{ m}\) (see diagram). At time \(t\) minutes after the start, the radius of the water surface is \(r\text{ m}\) and the volume of the water in the hemispherical container is \(\frac13\pi h^2(9-h)\), where \(h\text{ m}\) is the depth of the water. When the depth of the water is \(1\text{ m}\),
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