It seems clear that the pipe will drain in two stages.
In the first stage, water will squirt from the nozzle under a net pressure of 9 bars and declining to 0 bars as the pipe drains from 100 meters full to only 10 meters full. There will be a partial vacuum inside the pipe above the surface of the water filled only with water vapor. At room temperature, the vapor pressure will be negligible.
At the end of the first stage, the system is in an equilibrium. Water pressure at the bottom of the pipe is equal to atmospheric pressure. Water no longer squirts. But a 1.125" opening is large enough to allow air bubbles to enter the pipe and for water to "glug" out.
The first stage is easy to model. The exit velocity of the water stream will depend on the water pressure at the bottom of the pipe. Let P be the current pressure difference between the bottom of the pipe and atmospheric pressure. Let V be an incremental volume of water. Let ##\rho## be the density of water and v be the exit velocity. Then we can equate the kinetic energy of the water (##\frac{mv^2}{2} = \frac{V{\rho}v^2}{2}##) with the pressure energy of the water ##PV##. That yields:
##PV = \frac{V{\rho}v^2}{2}##
Simplify that, solve for v and multiply by nozzle cross-section to get flow rate. Express the pressure difference P as a function of the height of water in the column. Express the change in water height in terms of flow rate and you have a differential equation for water height in terms of time. Solve that and you have the time required to get through stage one.
Stage two is tougher.