4.7 Article

Early Detection of the Wear of Coriolis Flowmeters Through In Situ Stiffness Diagnosis

Journal

Publisher

IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
DOI: 10.1109/TIM.2021.3091428

Keywords

Coriolis mass flowmeter; erosion; frequency response; slurry flow; tube stiffness; wear detection

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Coriolis flowmeters are widely used in industrial applications, but may face erosion when measuring abrasive fluids. A stiffness diagnosis technique can identify potential wear on the measuring tube through frequency response analysis. Experimental results show that the technique can successfully detect slight tube erosion with a relative change in SRDP of -1%.
Coriolis flowmeters have been widely employed in a variety of industrial applications. There is a potential that the measuring tube of a Coriolis flowmeter may be eroded when it is used to measure abrasive fluid such as slurry flow. However, it is challenging to verify the structural health of the flowmeter without process interruptions or using on-site calibration devices such as meter provers. This article presents an in situ structural health-monitoring technique through stiffness diagnosis to identify the potential wear occurring on the measuring tube. To measure the frequency response of a Coriolis flowmeter, which strongly depends on the structural characteristics of the tube, the tube is not only excited at a resonant frequency but also at two additional off-resonant frequencies. Through digital processing of the drive and sensor signals, the frequency response is obtained and a stiffness-related diagnostic parameter (SRDP) is extracted from a Coriolis flowmeter. The proposed stiffness diagnosis technique was experimentally evaluated on a commercial bent-tube Coriolis flowmeter with dilute sand-water slurry flow. The results illustrate that the slight tube erosion is successfully identified when a relative change in SRDP reaches -1%, showing a good capability for an early detection of tube wear. In addition, the outcomes from recalibration with water suggest that, after the erosion occurs, the flowmeter overestimates the mass flowrate and underestimates the flow density.

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