A vacuum tube connecting Earth and space would create a significant pressure differential when opened, leading to complex interactions between water and atmospheric pressure. The atmospheric pressure would initially prevent water from rushing into the tube, as it exerts a force that keeps the water level stable. Once opened, water may rise into the tube, but it would likely not reach space due to vaporization at lower pressures along the tube. The pressure gradient would stabilize, balancing the water column with atmospheric pressure, but the exact height the water could reach before turning into vapor remains uncertain. Overall, the dynamics of pressure and vaporization would dictate the behavior of water in this hypothetical scenario.