Initially, water velocity had two components, y and x. The range (37 m) is defined by both:
The time required for a mass of water to go up:
It is easy to understand that the time for the water to reach the ground level again is
"t=2t_\\text{up}=2\\frac{v_y}{g}=\\frac{2v\\text{ sin}\\theta}{g}."
The range is determined by the horizontal component only:
Express and calculate the initial velocity:
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