Thermodynamics: Vertical pipe flow of geothermal water

In summary, the problem involves water at T1=240 C and P1=16 MPa at a depth of 2 km with a mass flow rate of 2 kg/s through a 0.2 m diameter adiabatic drilling hole. The goal is to find the enthalpy, temperature, pressure, and steam percentage at the top of the hole, where there is a throttling valve and further piping. The initial velocity can be calculated using the mass flow rate and the pressure gradient can be calculated using the water density and gravity. Approximations may be needed for the density of water and the behavior of water and steam in the pipe.
  • #1
mr.learnmore
1
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1. Water at T1=240 C and P1=16 MPa is at 2 km depth. A drilling hole with diameter 0.2 m has the water flowing up with mass flow rate at 2 kg/s. The hole is considered adiabatic(no heat transfer).
I need to find the following values at the top of the hole:
Enthalpy(h), temperature(T2), pressure(P2) and steam percentage(x) of the water.

There is no pipe friction. At the top of the hole there is a throttling valve which leads to further piping(so the pressure can not be considered to be 1 atm).



3. The Attempt at a Solution
The water is a compressed liquid in the beginning, so using saturated liquid values at T1 gives(from table):
v1=0.001229 m^3/kg
h1=1037.5 kJ/kg

The initial velocity is V =0.078241 m/s, using massflowrate = ρ*A*V.

The mass flow is steady, but as pressure drops with elevation the specific volume changes (I would think).
I'm not sure how to begin solving this, any ideas/hints are very welcome.

 
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  • #2
The pressure gradient can be calculated with the density of your water and gravity. This should allow to calculate the system up to the point where water begins to boil, probably with approximations for the water density. Afterwards, I don't know how water and steam behave in the pipe.
 

1. What is the significance of studying the vertical pipe flow of geothermal water in thermodynamics?

The vertical pipe flow of geothermal water is an important aspect of thermodynamics as it allows us to understand the transfer of energy and heat in geothermal systems. This knowledge is crucial for the development of renewable energy sources and the efficient use of geothermal resources.

2. How does the flow rate of geothermal water affect the efficiency of a geothermal system?

The flow rate of geothermal water is directly related to the efficiency of a geothermal system. A higher flow rate means that more energy can be extracted from the geothermal source, leading to a more efficient system. However, a very high flow rate can also result in a decrease in efficiency due to the increased pressure drop and friction in the pipes.

3. What are the key factors that influence the vertical pipe flow of geothermal water?

The key factors that influence the vertical pipe flow of geothermal water include the temperature difference between the geothermal source and the surface, the properties of the geothermal fluid, the diameter and length of the pipe, and the presence of any obstructions or bends in the pipe.

4. How is the energy transfer in the vertical pipe flow of geothermal water calculated?

The energy transfer in the vertical pipe flow of geothermal water can be calculated using the Bernoulli's equation, which takes into account the kinetic, potential, and pressure energy of the fluid. The frictional losses in the pipe can also be calculated using the Darcy-Weisbach equation.

5. What are some practical applications of understanding the vertical pipe flow of geothermal water in thermodynamics?

Understanding the vertical pipe flow of geothermal water has various practical applications, such as in the design and optimization of geothermal power plants, heating and cooling systems, and geothermal wells. It can also help in predicting the rate of heat transfer in geothermal systems and ensuring their sustainable use.

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