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Flash evaporation

From Wikipedia, the free encyclopedia
Partial vapor due to reduction in pressure
A typical flash drum

Flash evaporation (orpartial evaporation) is the partial vapor that occurs when asaturated liquid stream undergoes a reduction in pressure by passing through athrottling valve or other throttling device. This process is one of the simplestunit operations. If the throttling valve or device is located at the entry into apressure vessel so that the flash evaporation occurs within the vessel, then the vessel is often referred to as aflash drum.[1][2]

If the saturated liquid is a single-component liquid (for example,propane or liquidammonia), a part of the liquid immediately "flashes" into vapor. Both the vapor and the residual liquid are cooled to thesaturation temperature of the liquid at the reduced pressure. This is often referred to as "auto-refrigeration" and is the basis of most conventionalvapor compression refrigeration systems.

If the saturated liquid is a multi-component liquid (for example, a mixture ofpropane,isobutane and normalbutane), the flashed vapor is richer in the morevolatile components than is the remaining liquid.

Uncontrolled flash evaporation can result in a boiling liquid expanding vapor explosion (BLEVE).

Flash evaporation of a single-component liquid

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The flash evaporation of a single-component liquid is anisenthalpic process and is often referred to as anadiabatic flash. The following equation, derived from a simple heat balance around the throttling valve or device, is used to predict how much of a single-component liquid is vaporized.

X=HuLHdLHdVHdL{\displaystyle X={\frac {H_{u}^{L}-H_{d}^{L}}{H_{d}^{V}-H_{d}^{L}}}}[3]
where: 
X{\displaystyle X}=   weight ratio of vaporized liquid / total mass
HuL{\displaystyle H_{u}^{L}}=  upstream liquid enthalpy at upstream temperature and pressure, J/kg
HdV{\displaystyle H_{d}^{V}}
 
=  flashed vapor enthalpy at downstream pressure and corresponding saturation
    temperature, J/kg
HdL{\displaystyle H_{d}^{L}}
 
=  residual liquid enthalpy at downstream pressure and corresponding saturation
    temperature, J/kg

If the enthalpy data required for the above equation is unavailable, then the following equation may be used.

X=cp(TuTd)Hv{\displaystyle X={\frac {c_{p}(T_{u}-T_{d})}{H_{v}}}}
where: 
X{\displaystyle X}=  weight fraction vaporized
cp{\displaystyle c_{p}}=  liquidspecific heat at upstream temperature and pressure, J/(kg °C)
Tu{\displaystyle T_{u}}=  upstream liquid temperature, °C
Td{\displaystyle T_{d}}=  liquidsaturation temperature corresponding to the downstream pressure, °C
Hv{\displaystyle H_{v}}
 
=  liquidheat of vaporization at downstream pressure and corresponding saturation
    temperature, J/kg

Here, the words "upstream" and "downstream" refer to before and after the liquid passes through the throttling valve or device.

This type of flash evaporation is used in thedesalination ofbrackish water or ocean water by "Multi-Stage Flash Distillation." The water is heated and then routed into a reduced-pressure flash evaporation "stage" where some of the water flashes into steam. This steam is subsequently condensed into salt-free water. The residual salty liquid from that first stage is introduced into a second flash evaporation stage at a pressure lower than the first stage pressure. More water is flashed into steam which is also subsequently condensed into more salt-free water. This sequential use of multiple flash evaporation stages is continued until the design objectives of the system are met. A large part of the world's installed desalination capacity uses multi-stage flash distillation. Typically such plants have 24 or more sequential stages of flash evaporation.

Equilibrium flash of a multi-component liquid

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Theequilibrium flash of a multi-component liquid may be visualized as a simpledistillation process using a singleequilibrium stage. It is very different and more complex than the flash evaporation of single-component liquid. For a multi-component liquid, calculating the amounts of flashed vapor and residual liquid in equilibrium with each other at a given temperature and pressure requires a trial-and-erroriterative solution. Such a calculation is commonly referred to as an equilibrium flash calculation. It involves solving theRachford-Rice equation:[4][5][6][7]

izi(Ki1)1+β(Ki1)=0{\displaystyle \sum _{i}{\frac {z_{i}\,(K_{i}-1)}{1+\beta \,(K_{i}-1)}}=0}

where:

  • zi is the mole fraction of componenti in the feed liquid (assumed to be known);
  • β is the fraction of feed that is vaporised;
  • Ki is the equilibrium constant of componenti.

The equilibrium constantsKi are in general functions of many parameters, though the most important is arguably temperature; they are defined as:

yi=Kixi{\displaystyle y_{i}=K_{i}\,x_{i}}

where:

  • xi is the mole fraction of componenti in liquid phase;
  • yi is the mole fraction of componenti in gas phase.

Once the Rachford-Rice equation has been solved forβ, the compositionsxi andyi can be immediately calculated as:

xi=zi1+β(Ki1)yi=Kixi.{\displaystyle {\begin{aligned}x_{i}&={\frac {z_{i}}{1+\beta (K_{i}-1)}}\\y_{i}&=K_{i}\,x_{i}.\end{aligned}}}

The Rachford-Rice equation can have multiple solutions forβ, at most one of which guarantees that allxi andyi will be positive. In particular, if there is only oneβ for which:

11Kmax=βmin<β<βmax=11Kmin{\displaystyle {\frac {1}{1-K_{\text{max}}}}=\beta _{\text{min}}<\beta <\beta _{\text{max}}={\frac {1}{1-K_{\text{min}}}}}

then thatβ is the solution; if there are multiple suchβ's, it means that eitherKmax<1 orKmin>1, indicating respectively that no gas phase can be sustained (and thereforeβ=0) or conversely that no liquid phase can exist (and thereforeβ=1).

It is possible to useNewton's method for solving the above water equation, but there is a risk of converging to the wrong value ofβ; it is important to initialise the solver to a sensible initial value, such as (βmax+βmin)/2 (which is however not sufficient: Newton's method makes no guarantees on stability), or, alternatively, use a bracketing solver such as thebisection method or theBrent method, which are guaranteed to converge but can be slower.

The equilibrium flash of multi-component liquids is very widely utilized inpetroleum refineries,petrochemical andchemical plants andnatural gas processing plants.

Contrast with spray drying

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Spray drying is sometimes seen as a form of flash evaporation. However, although it is a form of liquid evaporation, it is quite different from flash evaporation.

In spray drying, aslurry of very small solids is rapidly dried by suspension in a hot gas. The slurry is firstatomized into very small liquid droplets which are then sprayed into a stream of hot dry air. The liquid rapidly evaporates leaving behind dry powder or dry solid granules. The dry powder or solid granules are recovered from the exhaust air by usingcyclones,bag filters orelectrostatic precipitators.

Natural flash evaporation

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Natural flash vaporization or flash deposition may occur duringearthquakes resulting in deposition of minerals held insupersaturated solutions, sometimes even valuableore in the case of auriferous, gold-bearing, waters. This results when blocks of rock are rapidly pulled and pushed away from each other byjog faults.[8]

See also

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References

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  1. ^Stanley M. Walas (1988).Chemical Process Equipment:Selection and Design. Butterworth-Heinemann.ISBN 0-409-90131-8.
  2. ^Gas Processing Suppliers Association (GPSA) (1987).Engineering Data Book (10th Edition, Vol. 1 ed.). Gas Processing Suppliers Association,Tulsa,Oklahoma.
  3. ^Vic Marshall; Steve Ruhemann (2001).Fundamentals of Process Safety. IChemE. p. 46.ISBN 9780852954317.
  4. ^Harry Kooijman and Ross Taylor (2000).The ChemSep Book(PDF) (2nd ed.). H.A. Kooijman and R. Taylor.ISBN 3-8311-1068-9. See page 186.
  5. ^Analysis of Objective Functions (Pennsylvania State University)
  6. ^Flash Calculations using the Soave-Redlich-Kwong equation of state (view full-size image)
  7. ^Curtis H. Whitson, Michael L. Michelsen,The Negative Flash, Fluid Phase Equilibria, 53 (1989) 51–71.
  8. ^Richard A. Lovett; Nature magazine (March 18, 2013)."Earthquakes Make Gold Veins in an Instant: Pressure changes cause the precious metal to deposit each time the crust moves, a new study finds. The insight suggests that remote sensing could be used to find new deposits in rocks where fault jogs are common".Scientific American. RetrievedMarch 18, 2013.

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