Experimental Study on Pressure Oscillations of Direct-Contact Condensation between Saturated Steam and Droplets at Sub-Atmospheric Pressure
Abstract
:1. Introduction
2. Experimental Apparatus and Procedure
3. Results and Discussion
3.1. The RMS of the Pressure Oscillation
3.2. The Time-Domain Characteristics of the Pressure Oscillation
3.3. The Frequency-Domain Characteristics of the Pressure Oscillation
4. Conclusions
- (1)
- The peak value of the oscillation in the condenser shows pulse fluctuations when pure steam condenses in direct contact with droplets. The energy of the condenser is maximum in the Z direction, and the acceleration RMS value can reach 0.08 m/s2.
- (2)
- When the flow rate is constant, the peak value of the oscillation signal decreases gradually with the increase in absolute pressure, and the time-domain periodic waveform becomes fluctuating. When the absolute pressure is constant, the peak value of the condensation oscillation signal mainly occurs at a low mass flow rate. When the flow rate continues to increase, there is no obvious peak value change.
- (3)
- In the spectrum waterfall diagram, the energy contribution decreases in the range of 20–30 Hz but increases in the range of 5–20 Hz. The range of 0–50 Hz is where the oscillation frequency changes the most in the process of steam condensation. At a low mass flow rate, the RMS of pressure oscillation does not change significantly, and the peak frequency moves towards a high frequency. As the flow rate gradually increases, frequencies with high energy become unconcentrated. The peak frequency decreases continuously from 23.68 Hz to 7.16 Hz, and the oscillation amplitude decreases in a parabolic pattern.
- (4)
- The auto power spectrum of the oscillation shows that the main frequency of oscillation is maintained at 23.04 Hz at a low flow velocity, and gradually decreases to 7.68 Hz when the flow velocity continues to increase.
- (5)
- As the flow rate increases, the main frequency of oscillation is no longer stable and its energy continues to decrease. The auto power spectrum changes from a single peak to a fluctuating characteristic. The amplitude of the first main frequency is approximately 0.00037 (m/s2)2, while the amplitude of other dominant frequencies is between 0.00010 (m/s2)2 and 0.00015 (m/s2)2. Other dominant frequencies may be caused by the formation, aggregation, and rupture of non-condensable gas layers on the surface of droplets.
Author Contributions
Funding
Data Availability Statement
Conflicts of Interest
References
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Parameter | Parameter Symbol | Value | Error |
---|---|---|---|
Pressure, kPa | P | 14–21 | ±0.2% |
Inlet mass flow rate, mL/min | V | 20.067/30.054/35.047/40.040/45.034 | ±0.1% |
Droplet temperature, °C | Ti | 25 | ±0.05% |
Oscillation amplitude, m/s2 | A | ±5% |
V, mL/min | |||||
---|---|---|---|---|---|
20.067 | 30.054 | 35.047 | 40.040 | 45.034 | |
X | 0.05 | 0.04 | 0.03 | 0.03 | 0.04 |
Y | 0.02 | 0.04 | 0.02 | 0.02 | 0.02 |
Z | 0.08 | 0.08 | 0.06 | 0.05 | 0.04 |
P, kPa | |||||
---|---|---|---|---|---|
14 | 16 | 19 | 20 | 21 | |
X | 0.05 | 0.05 | 0.04 | 0.04 | 0.03 |
Y | 0.02 | 0.03 | 0.03 | 0.02 | 0.02 |
Z | 0.08 | 0.06 | 0.05 | 0.04 | 0.04 |
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Jing, Y.; Wang, C.; Huang, Q.; Wang, Y.; Yu, Y. Experimental Study on Pressure Oscillations of Direct-Contact Condensation between Saturated Steam and Droplets at Sub-Atmospheric Pressure. Processes 2024, 12, 516. https://doi.org/10.3390/pr12030516
Jing Y, Wang C, Huang Q, Wang Y, Yu Y. Experimental Study on Pressure Oscillations of Direct-Contact Condensation between Saturated Steam and Droplets at Sub-Atmospheric Pressure. Processes. 2024; 12(3):516. https://doi.org/10.3390/pr12030516
Chicago/Turabian StyleJing, Yuanlin, Chenhao Wang, Qunwu Huang, Yiping Wang, and Yangyang Yu. 2024. "Experimental Study on Pressure Oscillations of Direct-Contact Condensation between Saturated Steam and Droplets at Sub-Atmospheric Pressure" Processes 12, no. 3: 516. https://doi.org/10.3390/pr12030516
APA StyleJing, Y., Wang, C., Huang, Q., Wang, Y., & Yu, Y. (2024). Experimental Study on Pressure Oscillations of Direct-Contact Condensation between Saturated Steam and Droplets at Sub-Atmospheric Pressure. Processes, 12(3), 516. https://doi.org/10.3390/pr12030516