Coriolis flow meters represent the state-of-the-art in mass flow measurement. While incredibly versatile and accurate, their internal operation can be difficult to understand.
Coriolis Flow Meters
Put into very simple terms, a Coriolis flow meter works by shaking one or more tubes carrying the flowing fluid, then precisely measuring the frequency and phase of that shaking.
The back-and-forth shaking is driven by an electromagnetic coil, powered by an electronic amplifier circuit to shake the tube(s) at their mechanical resonant frequency.
Since this frequency depends on the mass of each tube, and the mass of the tubes depends on the density of the fluid filling the fixed volume of the tubes, the resonant frequency becomes an inverse indication of fluid density (Note 1) , whether or not fluid is flowing through the tubes.
As fluid begins to move through the tubes, the inertia of the moving fluid adds another dimension to the tubes’ motion: the tubes begin to undulate (Note 2) , twisting slightly instead of just shaking back and forth.
This twisting motion is directly proportional to the mass flow rate, and is internally measured by comparing the phase shift (θ) between motion at one point on the tube versus another point on the tube: the greater the undulation, the greater the phase shift between these two points’ vibrations.
Note 1: In fact, this density-measuring function of Coriolis flow meters is so precise that they often find use primarily as density meters, and only secondarily as flow meters!
Note 2 : An interesting experiment to perform consists of holding a water hose in a U-shape and gently swinging the hose back and forth like a pendulum, then flowing water through that same hose while you continue to swing it. The hose will begin to undulate, its twisting motion becoming visually apparent.
The Coriolis force
In physics, certain types of forces are classified as fictitious or pseudo forces because they only appear to exist when viewed from an accelerating perspective (called a non-inertial reference frame).
The feeling you get in your stomach when you accelerate either up or down in an elevator, or when riding a roller-coaster at an amusement park, feels like a force acting against your body when it is really nothing more than the reaction of your body’s inertia to being accelerated by the vehicle you are in.
The real force is the force of the vehicle against your body, causing it to accelerate. What you perceive is merely a reaction to that force, and not the primary cause of your discomfort as it might appear to be.
Centrifugal force is another example of a “pseudo force” because although it may appear to be a real force acting on any rotating object, it is in fact nothing more than an inertial reaction.
Centrifugal force is a common experience to any child who has ever played on a “merry-go-round:” that perception of a force drawing you away from the center of rotation, toward the rim.
The real force acting on any rotating object is toward the center of rotation (a centripetal force) which is necessary to make the object radially accelerate toward a center point rather than travel in a straight line as it normally would without any forces acting upon it. When viewed from the perspective of the spinning object, however, it would seem there is a force drawing the object away from the center (a centrifugal force).
Yet another example of a “pseudo force” is the Coriolis force, more complicated than centrifugal force, arising from motion perpendicular to the axis of rotation in a non-inertial reference frame.
The example of a merry-go-round works to illustrate Coriolis force as well: imagine sitting at the center of a spinning merry-go-round, holding a ball. If you gently toss the ball away from you and watch the trajectory of the ball, you will notice it curve rather than travel away in a straight line.
In reality, the ball is traveling in a straight line (as viewed from an observer standing on the ground), but from your perspective on the merry-go-round, it appears to be deflected by an invisible force which we call the Coriolis force.
In order to generate a Coriolis force, we must have a mass moving at a velocity perpendicular to an axis of rotation:
The magnitude of this force is predicted by the following vector equation :
If we replace the ball with a fluid moving through a tube, and we introduce a rotation vector by tilting that tube around a stationary axis (a fulcrum), a Coriolis force develops on the tube in such a way as to oppose the direction of rotation just like the Coriolis force opposed the direction of rotation of the rotating platform in the previous illustration:
The Coriolis force opposes the direction of rotation. The greater the mass flow rate of water through the hose, the stronger the Coriolis force.
If we had a way to precisely measure the Coriolis force imparted to the hose by the water stream, and to precisely wave the hose so its rotational velocity held constant for every wave, we could directly infer the water’s mass flow rate.