Mixing
Added mass
In fluid mechanics, added mass or virtual mass is the inertia added to a system because an accelerating or decelerating body must move (or deflect) some volume of surrounding fluid as it moves through it. Added mass is a common issue because the object and surrounding fluid cannot occupy the same physical space simultaneously. For simplicity this can be modeled as some volume of fluid moving with the object, though in reality "all" the fluid will be accelerated, to various degrees.
The dimensionless added mass coefficient is the added mass divided by the displaced fluid mass – i.e. divided by the fluid density times the volume of the body. In general, the added mass is a second-order tensor, relating the fluid acceleration vector to the resulting force vector on the body.[1]
Contents
1 Background
2 Virtual mass force
3 Applications
3.1 Naval architecture
3.2 Aeronautics
4 See also
5 References
6 External links
Background
Friedrich Bessel proposed the concept of added mass in 1828 to describe the motion of a pendulum in a fluid. The period of such a pendulum increased relative to its period in a vacuum (even after accounting for buoyancy effects), indicating that the surrounding fluid increased the effective mass of the system.[2]
The concept of added mass is arguably the first example of renormalization in physics.[3][4][5]
The concept can also be thought of as a classical physics analogue of the quantum mechanical concept of quasiparticles. It is, however, not to be confused with relativistic mass increase.
It is often erroneously stated that the added mass is determined by the momentum of the fluid. That this is not so becomes clear when considering the case of the fluid in a large box, where the fluid momentum is exactly zero at every moment of time. The added mass is actually determined by the quasi-momentum: the added mass times the body acceleration is equal to the time derivative of the fluid quasi-momentum.[4]
Virtual mass force
Unsteady forces due to a change of the relative velocity of a body submerged in a fluid can be divided into two parts: the virtual mass effect and the Basset force.
The origin of the force is that the fluid will gain kinetic energy at the expense of the work done by an accelerating submerged body.
It can be shown that the virtual mass force, for a spherical particle submerged in an inviscid, incompressible fluid is[6]
- F=ρcVp2(DuDt−dvdt),{displaystyle mathbf {F} ={frac {rho _{mathrm {c} }V_{mathrm {p} }}{2}}left({frac {mathrm {D} mathbf {u} }{mathrm {D} t}}-{frac {mathrm {d} mathbf {v} }{mathrm {d} t}}right),}
- F=ρcVp2(DuDt−dvdt),{displaystyle mathbf {F} ={frac {rho _{mathrm {c} }V_{mathrm {p} }}{2}}left({frac {mathrm {D} mathbf {u} }{mathrm {D} t}}-{frac {mathrm {d} mathbf {v} }{mathrm {d} t}}right),}
where bold symbols denote vectors, u{displaystyle mathbf {u} }
The origin of the notion "virtual mass" becomes evident when we take a look at the momentum equation for the particle.
- mpdvdt=∑F+ρcVp2(DuDt−dvdt),{displaystyle m_{mathrm {p} }{frac {mathrm {d} mathbf {v} }{mathrm {d} t}}=sum mathbf {F} +{frac {rho _{mathrm {c} }V_{mathrm {p} }}{2}}left({frac {mathrm {D} mathbf {u} }{mathrm {D} t}}-{frac {mathrm {d} mathbf {v} }{mathrm {d} t}}right),}
- mpdvdt=∑F+ρcVp2(DuDt−dvdt),{displaystyle m_{mathrm {p} }{frac {mathrm {d} mathbf {v} }{mathrm {d} t}}=sum mathbf {F} +{frac {rho _{mathrm {c} }V_{mathrm {p} }}{2}}left({frac {mathrm {D} mathbf {u} }{mathrm {D} t}}-{frac {mathrm {d} mathbf {v} }{mathrm {d} t}}right),}
where ∑F{displaystyle sum mathbf {F} }
Moving the derivative of the particle velocity from the right hand side of the equation to the left we get
- (mp+ρcVp2)dvdt=∑F+ρcVp2DuDt,{displaystyle left(m_{mathrm {p} }+{frac {rho _{mathrm {c} }V_{mathrm {p} }}{2}}right){frac {mathrm {d} mathbf {v} }{mathrm {d} t}}=sum mathbf {F} +{frac {rho _{mathrm {c} }V_{mathrm {p} }}{2}}{frac {mathrm {D} mathbf {u} }{mathrm {D} t}},}
- (mp+ρcVp2)dvdt=∑F+ρcVp2DuDt,{displaystyle left(m_{mathrm {p} }+{frac {rho _{mathrm {c} }V_{mathrm {p} }}{2}}right){frac {mathrm {d} mathbf {v} }{mathrm {d} t}}=sum mathbf {F} +{frac {rho _{mathrm {c} }V_{mathrm {p} }}{2}}{frac {mathrm {D} mathbf {u} }{mathrm {D} t}},}
so the particle is accelerated as if it had an added mass of half the fluid it displaces, and there is also an additional force contribution on the right hand side due to acceleration of the fluid.
Applications
The added mass can be incorporated into most physics equations by considering an effective mass as the sum of the mass and added mass. This sum is commonly known as the "virtual mass".
A simple formulation of the added mass for a spherical body permits Newton's classical second law to be written in the form
F=ma{displaystyle F=m,a}becomes F=(m+madded)a.{displaystyle F=(m+m_{text{added}}),a.}
One can show that the added mass for a sphere (of radius r{displaystyle r}
All bodies accelerating in a fluid will be affected by added mass, but since the added mass is dependent on the density of the fluid, the effect is often neglected for dense bodies falling in much less dense fluids. For situations where the density of the fluid is comparable to or greater than the density of the body, the added mass can often be greater than the mass of the body and neglecting it can introduce significant errors into a calculation.
For example, a spherical air bubble rising in water has a mass of 43πr3ρair{displaystyle {tfrac {4}{3}}pi r^{3}rho _{text{air}}}
These principles also apply to ships, submarines, and offshore platforms. In the marine industry, added mass is referred to as hydrodynamic added mass. In ship design, the energy required to accelerate the added mass must be taken into account when performing a sea keeping analysis. For ships, the added mass can easily reach ¼ or ⅓ of the mass of the ship and therefore represents a significant inertia, in addition to frictional and wavemaking drag forces.
For certain geometries freely sinking through a column of water, hydrodynamic added mass associated with the sinking body can be much larger than the mass of the object. This situation can occur, for instance, when the sinking body has a large flat surface with its normal vector pointed in the direction of motion (downward). A substantial amount of kinetic energy is released when such an object is abruptly decelerated (e.g., due to an impact with the seabed).
In the offshore industry hydrodynamic added mass of different geometries are the subject of considerable investigation. These studies typically are required as input to subsea dropped object risk assessments (studies focused on quantifying risk of dropped object impacts to subsea infrastructure). As hydrodynamic added mass can make up a significant proportion of a sinking object's total mass at the instant of impact, it significantly influences the design resistance considered for subsea protection structures.
Proximity to a boundary (or another object) can influence the quantity of hydrodynamic added mass. This means that added mass depends on both the object geometry and its proximity to a boundary. For floating bodies (e.g., ships/vessels) this means that the response of the floating body (i.e., due to wave action) is altered in finite water depths (the effect is virtually nonexistent in deep water). The specific depth (or proximity to a boundary) at which the hydrodynamic added mass is affected depends on the body's geometry and location and shape of a boundary (e.g., a dock, seawall, bulkhead, or the seabed).
The hydrodynamic added mass associated with a freely sinking object near a boundary is similar to that of a floating body. In general, hydrodynamic added mass increases as the distance between a boundary and a body decreases. This characteristic is important when planning subsea installations or predicting the motion of a floating body in shallow water conditions.
Aeronautics
In aircraft (other than lighter-than-air balloons and blimps), the added mass is not usually taken into account because the density of the air is so small.
See also
Basset force for describing the effect of the body's relative motion history on the viscous forces in a Stokes flow
Basset–Boussinesq–Oseen equation for the description of the motion of – and forces on – a particle moving in an unsteady flow at low Reynolds numbers
Darwin drift for the relation between added mass and the Darwin drift volume
Keulegan–Carpenter number for a dimensionless parameter giving the relative importance of the drag force to inertia in wave loading
Morison equation for an empirical force model in wave loading, involving added mass and drag
Response Amplitude Operator for the use of added mass in ship design
References
^ Newman, John Nicholas (1977). Marine hydrodynamics. Cambridge, Massachusetts: MIT Press. §4.13, p. 139. ISBN 978-0-262-14026-3..mw-parser-output cite.citation{font-style:inherit}.mw-parser-output q{quotes:"""""""'""'"}.mw-parser-output code.cs1-code{color:inherit;background:inherit;border:inherit;padding:inherit}.mw-parser-output .cs1-lock-free a{background:url("//upload.wikimedia.org/wikipedia/commons/thumb/6/65/Lock-green.svg/9px-Lock-green.svg.png")no-repeat;background-position:right .1em center}.mw-parser-output .cs1-lock-limited a,.mw-parser-output .cs1-lock-registration a{background:url("//upload.wikimedia.org/wikipedia/commons/thumb/d/d6/Lock-gray-alt-2.svg/9px-Lock-gray-alt-2.svg.png")no-repeat;background-position:right .1em center}.mw-parser-output .cs1-lock-subscription a{background:url("//upload.wikimedia.org/wikipedia/commons/thumb/a/aa/Lock-red-alt-2.svg/9px-Lock-red-alt-2.svg.png")no-repeat;background-position:right .1em center}.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration{color:#555}.mw-parser-output .cs1-subscription span,.mw-parser-output .cs1-registration span{border-bottom:1px dotted;cursor:help}.mw-parser-output .cs1-hidden-error{display:none;font-size:100%}.mw-parser-output .cs1-visible-error{font-size:100%}.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration,.mw-parser-output .cs1-format{font-size:95%}.mw-parser-output .cs1-kern-left,.mw-parser-output .cs1-kern-wl-left{padding-left:0.2em}.mw-parser-output .cs1-kern-right,.mw-parser-output .cs1-kern-wl-right{padding-right:0.2em}
^ Stokes, G. G. (1851). "On the effect of the internal friction of fluids on the motion of pendulums". Transactions of the Cambridge Philosophical Society. 9: 8–106. Bibcode:1851TCaPS...9....8S.
^ González, José; Martín-Delgado, Miguel A.; Sierra, Germán; Vozmediano, Angeles H. (1995). Quantum electron liquids and high-Tc superconductivity. Springer. p. 32. ISBN 978-3-540-60503-4.
^ ab Falkovich, Gregory (2011). Fluid Mechanics, a short course for physicists. Cambridge University Press. Section 1.3. ISBN 978-1-107-00575-4.
^ Biesheuvel, A.; Spoelstra, S. (1989). "The added mass coefficient of a dispersion of spherical gas bubbles in liquid" (Submitted manuscript). International Journal of Multiphase Flow. 15 (6): 911–924. doi:10.1016/0301-9322(89)90020-7.
^ Crowe, Clayton T.; Sommerfeld, Martin; Tsuji, Yutaka (1998). Multiphase flows with droplets and particles. CRC Press. p. 81. ISBN 978-0-8493-9469-0.
External links
- MIT OpenCourse Ware
- Naval Civil Engineering Laboratory
- Det Norske Veritas DNV-RP-H103 Modelling And Analysis Of Marine Operations
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