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This demonstration shows how the two-phase option of
PHOENICS, library case W249, is extended by PLANT to
permit simulation of the relative movement of water
(rain, or snow) and air. ( Choose the non-shelter variant
when prompted).
PLANT is used to introduce patchwise discontinuity in
interphase friction distribution: the particulate phase
fragments in the bottom part of the domain are much less
influenced by air, than the ones of the upper part. The
inspection of PHOTON pictures show what happened near the
ground: the gravitational sedimentation is increased and
the air becomes purer.
PLANT information :
* Data input groups used: 10
* Ground groups planted : 10
* Headings used : PRPT??
* Functions used : None
* Commands used : PLACE
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LOAD(W429)
TEXT(Rain and snow : effect of interphase friction.
IF(.NOT.ROOF) THEN
LSWEEP=400
mesg(Reduce interface friction at the bottom half of domain ? (y/n)
readvdu(ans,char,y)
if(:ans:.eq.y) then
LG(1)=T
NAMSAT=MOSG
CFIPS=GRND
PLANTBEGIN
INTFRC=9.81*(:RHO2:-:RHO1:)/(:FALLVEL:)*MASS1*LIQ
PLACE(0.0,24.0,5.0,10.0) /LG(1)
INTFRC=9.81*(:RHO2:-:RHO1:)/(7.*:FALLVEL:)*MASS1*LIQ
PLACE(0.0,24.0,0.0,5.0) /LG(1)
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The above two statements provide what is required for
none-shelter (ROOF=F) situation: the first, apllied to
the upper domain part, extended from 5.0 m up to 10.m,
has got the coefficient of 7 times larger than the second
one has. The lattter is applied for the bottom part of
the domain extended up to 5.0 m above the ground. The
both are activated if logical switch LG(1) equals T.
Please note the use of PLACE command with the arguments
being physical distances rather than grid extents in
terms of cell numbers.
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PLANTEND
endif
ENDIF
tstswp=-1
dmpstk=t
DISTIL=T
EX(P1)=2.000E+02; EX(AU1)=2.000E+00; EX(BU2)=1.979E+00
EX(CV1)=5.349E-03; EX(DV2)=2.511E+00; EX(LIQ)=1.079E-05
EX(EPOR)=1.000E+00; EX(NPOR)=1.000E+00
LIBREF=606
STOP