Highlights
Part one: Simple initial value problem
Assignment (please read the problem description before doing the assignment)
Problem description
An energy extraction device includes a cylinder elastically mounted on a spring and the electricity generator. The cylinder vibrates only in a direction parallel to the flow and drives an electricity generator. The electricity generator extracts the energy from the cylinder in the same way as a damper. It is modelled as a damper with a damping constant c when the vibration is studied. The flow velocity is a combined steady and oscillatory flow
u ( t ) = U 0 + U m sin(2p t / T )
where U 0 is the steady flow velocity, U m is the amplitude of the oscillatory flow velocity, T is the period of the oscillatory flow and t is the time.
The KC number is defined as
The electricity generator can modelled by a damper that extract energy from the motion of the cylinder with a constant damping constant of c. The structural damping is considered to be negligibly small. Considering the power given by the fluid should be the same as the power received by the damper, the power can also be calculated using the energy received by the electricity generator (damper) as.
where P is the power of the system, F is the hydrodynamic force on the cylinder, V is the vibration speed of the cylinder. In the numerical simulation, if total computational time step is N , the power can be calculated by
Note, N0 must be a step where the vibration has been fully developed. In addition, the time from step N0 to N0+N must be one or a few whole periods.
The hydrodynamic force on the cylinder can be predicted by the Morison equation
where V r= u - V is the velocity of the flow relative to the cylinder, C A and C D and inertia and drag coefficients, respectively, m d is the displaced fluid mass and A p is the projected area. The calculating parameters are listed in the table below.
Part two: One-dimensional convection diffusion problem
Assignment (please read the problem description before doing the assignment)
Problem description
Note: In the paragraph below, the number j stands for the last digit of your student ID. For example, if your student ID is 2345673, 10+j = 13.
The water on the ground flows into the soil through the pore space of the soil (the space between soil particles). The flow velocity is very small of 0.002×(1+j) m/s and it does not change along the vertical direction. Initially, the temperature is (10+j) °C in the whole soil volume (including soil and the water in the soil). The temperature of the water on top of the ground level is 30°C and remains constant. The warm water moves into the soil and increases the temperature in the soil.
A coordinate x is defined and its origin is on the ground level and pointing downwards. The governing equation is the convection diffusion equation
Where
Boundary condition is T =30°C at the top boundary and 0 at the bottom boundary (at x = 2 m).
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