Fluid Phase Equilibria, 53 ( 1989) 207-2 18 Elsevier Science Publishers B.V., Amsterdam - Printed in The Netherlands
UREA-NH,-COz-H.0:
M. BERNHRDIS M.
SRNTINI,
ULE
and
CRLCULATIONS
G. CRRVOLI,
Rgrimont,
Porta
USING
AN EXTENDED
Istituto
Guido
Marghera,
Italy
207
UNIQUAC
Donegani,
EQURTION
Novara,
Italy
RBSTRRCT R
modifi ed
ideaiity
UNIQURC
of the
auaternary
equiii brium
Some
successfuLLy
equation system
equipments
simulatea
is
using
applied
to
caiculate
Liquio
phase
non
URER-NH3-C02-H20.
operating such
in different
an equation
for
ano VLE
strict
conditions
were
calcuiations
INTRODUCTION Correct
VLE
hard
to obtain.
very In
fact,
a
calcutations
unique
different
conditions;
licenced
by Montedison
2) Temperatures to 414
In
Fiqure
the
and
K and same
modei
referring
pressures
7 KPa
0378-3812/89/$03.50
shouid
(Pagani
in the
sections
1 - Partial
for
URER
URER
be abte to
and go
ID9
Mariani,
from
Last
473
simuiation
to treat
and
phase
equilibrium
(Isobaric
Doubte
19841,
Figure
K and
see
optimization
Recycie)
of an
goes
plant
1:
20 MPa,
ciose
from
to
IDR piant
0 1989 Elsevier Science Publishers B.V.
35%
is
in very
to the
react or
flash.
concentration
flowsheeting
plant
100%
by weight
I
208 b)
The URER,
high
In order
section
recovery
ammonia
vacuum
ano
Low
to describe
the
liquid
choose
conditions
we
atready
applied
with
tow concentration
of
temperatures. phase
ternary
ideatity
non LINIQUAC
extended
an
to the
streams
regards
system
in
ecuation
NH,-CO,-H,O
a
Large
(Sande;
(Bernardis
range
et at., al.,
et
of
1988) 1988,
1989).
CHEMICAL The
REACTIONS four
generating The
ions,
comptete
NHs
+ H20
CO2
+ Hz0
H.0
+ OH+ H*
_
HCO;
-
co;
F=
NH,COO-
+ (Nti2)*CO=
We negtect
the
ion
is atways
We
atso
needed
very
is the
foliowing: (1) (II) (IIb) (III) (IV) (V)
+ CO? ion dissociation
is very
(IIb)
so that
low,
the
because
concentration
the of
Last
reaction,
the equitibrium
time
in most
equipments
URER
is thus
treated
because
its
conditions
rate
is much
is so
Longer
tow than
of a IJRER plant.
as an inert
component
of
the
system.
T~IBLE 7. Finat
system
describing
In KX = In ak; tn KXr
In KX,
= In a$+
q
mNu,+
tlB2
q
mCol+ mHcoi+ mNH:=
liquid
In a:H,
aH,P
In a:,--
-In
In auto
mrrw:+ mNH,coc-
muco;+
= l./(l.+
phase
- In aH,P
+ ln a",+- Ln a"cP, - In au,,
= In a9Nulcoo-+Ln
MB,
xw
the
+ In a&--
= In akO;
In KXII
m,++
thermodynamic the carbonate
smait. the
to achieve
reactions
+ HzO
bicarbonate
themselves
react.
+ OH-
2NH,
neglect
dissociate
+ tl'
constant
equilibrium
can
sotution
in
equilibrium
NH+,
G== H*
He0
PHRSE present
in turn
of chemicat
ti
+ HCO;
LIQUID
species
which
set
HCO; NH3
IN THE
motecutar
mNH,coamNu,coo-+
,018 Cm,)
m,,-
aEroj
-In a:, il
that the
the
time
residence
209 Each
remaining
temperature at.,
reaction
dependent.
has Their
a thermodynamic vatues
are
equilibrium
reported
constant
elsewhere
K,,
only
(Pawtikovski
et
1982).
Introducing
the
mass
electroneutraiity fraction The
xw, we get
concentration
moiatity
balances
balance the
final
of
all
system
ammonia
and
equation
to
calculate
the
Liquid
describing
species
but
carbon
water
dioxide, the
phase
are
the
water
(Table
expressed
mote
I).
on
the
scale.
The
corresponding
activities
the
and
moiatities
as pure
The
In this
expressions
appear
paper
by
basea
on the
asymmetric
coefficients
Sander term.
Besides,
the
simultaneous
of activity
in Literature,
we aod
residual
activity
are
activity
convention.
in iabie
1 are
referrer
to
FRHMEWORK
explicit
NH,-CO,-H,O
the
sotvent.
THERMODYNAMIC
done
the
the
Both water
of
and
some
et
concentration
at.
(1986),
expressions presence
of the
of two
coefficients
and
in the
three
of
for
ternary
6,,,
system
as
of activity
2( are
Therefore
expressions
the
(1988).
parameters
calculation
terms
for
Carvoti
dependent
soLvents.
explicit
coefficients
Bernardis
atready
coefficient
modified
now
it's
convenient
the
quaternary
by
to report system
the tSe (see
Rppendix). This
extension
refer
to a mixture
constants the
also
refer
and
(a:,,,,),
=
: ,)1
-
a:,_.U being
and
dilution
VAPOR
(Ra
the
and
that with
activities
water),
URER
and water
respect
of
white
to pure
the components
the
form
equilibrium
an ideal
water
mixture
(a:,,)
or
to
following:
+ 21
(Ra
( I)
+ +&\
(I) an approximation.
XT,,,, are,
in pure
UREA
respectively, and
pure
R, is the moiar the
activity
ratio
water/URER.
coefficients
at
infinite
water
PHASE
URER Only
Supposing activities is the
problem:
CURER
(R,
equation
&'T,_
between
URER
s a,,,
another
solvents
to water.
relationship
water
rises
of
the
volatility three
vapor-liquid
is neglected,
other
motecutar
equitibrium,
since
so it does components ions
not
NH.,
cannot
appear CO2
Leave
and the
in the Hz0
vapor
are
Liquid
phase.
involved
phase.
in the
210 The
relating
phase,
are
Py, 'pz where
expressions, the
taking
= (ti/P!,,.R2.+ H:P),,) m,
i : NH3
into
account
the non-ideatity
of
the
vapor
fotlowing: ,S / (R,il.)
15y:
(2)
or CO?;
for water: Pywy, RLL
= PLY:
fugacity
(Nakamura Henry's
a, exp
:Vw
coefficients
et at.,
(P - Pi) are
/ RTI
catcutated
(3) using
Nakamura's
equation
of
state
19761.
constants
are pressure aependent: cp"z, = in Hi,w + Vi * (P - P:) / RT CP,'I = in Hi,u + U, m fP - P:, / RT
in H:P)w (P> Ln H,,U
(4) (5)
wnere: oiw :: F'$i
1 f:::
The whote
set
TRBLE
!n T + BS~W
T + B4iw
(6)
1 : : ,",,, Ln T + BSLY
T + BLiU
(7)
of B constants
appears
in Table
2.
Henry's
constants
as a function
Electrolyte
B,
of
temperature
NH,
-681.531
28.67202
co,
-8901.728
-22.198746
NH,
-1018.619
28.68392
co1
-3326.2777
-22.27357
NH3
mNH,,
and
COn
moiatities
range
-.0541721
-151.3689
273-423
.OOll3684
156.8756
273-423
(K)
Water
-151.41204
433-453
155.34374
433-453
.0117394 URER
activity
coefficients
are
referred
to
the
of sotvents: PMw
+ xu PM")
(xw PMw
+ xu PM~)
5 = ~,a,>/ (xv,
mco,,a
and
Rpptic.
B,
-.05250941
Sotvent:
mixture
(K).
B.
Ba
Solvent:
The
2.
= xco2/
(9) (3) (IO) (11)
ESTIMFlTION The
(Bernardis 373.15K
OF PRRRMETERS
first
set
et at.,
only.
of
parameters
1998,
In order
1999)
regarding was
to simulate
obtained URER
ptant
the
ternary
reducing equipments
system
experimental the
NH.-COS-HzO data
equitibrium
at must
211 be
retiabty
described
catcuiations
using
temperature To
do
that
new
complete
TRBLE
more
we
had
between
of
data
373.15K
to introduce
set
For
to 473.15K.
experimentat
now
range,
The
up
ternary
this
reason
(Mutter
and
we
revised
our
1968)
et at.,
ternary a
in
wioer
473.15K.
the concentration parameters
dependent
is reported
parameters
in Table
6,,.
3.
3
Complete
set
of ternary
parameters
and
experimental
measurements
used.
Experimental Source: Binary VLE Data i
k
NH.
e.0
CO,
-256~2.10 '107.7931T
P=O.-9.0i?Pa
+.OlEt?211T*
-.108b8171i
m..,, =O.-152.7
H.0
-:272.667
654.7
N&COO-
H.0
-569.5
815.2
HCO;
H,O
-753.5
615.b
NH*
NH:
2500.0
2500.0
NH,COO-
2500
co,
NH,COO-
-1094.0
HCOi
0
-835.3
co,
tico; NH:
NH:
NH,EOO-
NH:
NH.COO-
NH:
uco;
root
and
vapor
The
2500.0
232.6
-1168.2
2500.0
2500.0
mole
from
for
the quaternary
TRBLE
are
between
experimentai
110 data
points
are
between
URER
and
data shown
available
in
TabLe
and
caLcutated
respectively the
other
in Literature.
15.2%
reported
determinations
and
16.3%. were
The
4.
interaction
k
al.
used
parameters
akI
to optimize concerning
Exp.
the URER.
remarks
NH2
URER
-717.3
573.3
COP
UREFl
-957.7
2500.0
H.0
URER
.2982+T
Kawasumi
NH:
UREA
-634.1
-112.9
Durisch
NHnCOO-
URER
-676.9
1293.7
(1979)
(1952,
53,
pressures
components
I.
Experimental
i
o.-9.77
at
6.*
parameters
to be significant
m,,,=
et
(1966)
373887.0
deviations
fractions
O.-Z&.6
-9lEZ.E
LE11.6
squared
m.,,=
16.5
-28661k.0
interaction
optimized found
mean
a:.
2k58.1
6,.
The
nu11er,
2500.0
186.0
co.
et
mcox=O.-1.5
-702.8
NH,
Hough:on, (19571
P=or3.75nPa
at
Data
H,O
NH:
T-273.15.373.15K
-334031.43/T
fxperimental Source. Ternary VLC
References Guiltev~c et (1965) Pawtikowswci et at (:5&i:
1=373.15-503.15K
2282.919
+183ilL.L5/1
NH:
Remarks
a..
a*. 4969.77 -20.832351
SL)
-.53Sl*T et at.
parameters
we
212 We
have
to
comptetely phase
Finally
range
we
solvents,
even
(see
maintained
at every
experimental
are well
In xx
= AH,/R
(I/T
mean
vapor
2).
The
1979).Moreover
K and
constants
keeping
of
453
and
NH3
these
CO,
in
parameters
the mutuat
This
reporting and
vaoor
data
are
URER
as
K).
interaction
in mind
temperature.
comes
awnrER,uREn
ideality
from
the
the
two
solubitity
of
of
of LJRER in water
(Kirk
K and
deviations
and
and
Othmer,
(12)
fractions
8.3%
data
assuming:
Tr = 408
squared
main
Mariani,
Letting
between 22
for
x
= 1.
experimenta:
and
experimental
caLcuLated
quaternary
data
pressures points
are
(Pagani
and
is directly
fed
12.2%.
features
1984)
the
gases
are
the
respectivety
of
can
actually
latter
in the ammonia
Instead
in the
leaving
tne
say
a water/LlRER solution
fixed
or CO=
VLE
D'Rrminio In the
exactly
through
typical
ratio
Like
Monforte, stripper
1987)
were
the stripping
the
from
heart
of
the plant.
carbamate;
missing
and
the
the
in
two phases
flashes.
PATHS
isotherms
azeotropic ternary
to the
calcutated
behaviour
system
goes
due
NH.-C02-HsO.
stoichiometric
is minimum;
pressure
inserted
are
free
five
STRIPPING
boiling
in the
is atso
is set
or
are
stripper.
strippers
four
dioxide
at
20
MPa
and
formation
of
R, = 1.764.
pressure
in solution,
was
plant
is close
component
first
equipments
a characteristic
Nhs/COp
model
two
solution
FIND SIMULATED
motar
shows
temperature,
motecutar
Last
IDR process
of ammonia
carbon
second
the
shown
a part
the
the
the ureic
passed
of an
and
removed.
for
ratio
these
and
traditional
The
molar
that
first
Loop
only
1: part
is quantitatively
2 are
carbamate,
synthesis
in Figure
the
ISOTHERMS
In Figure
the
remaining
former
reactor
EQUILIBRIUM
of
shown
reactor;
In fact
The
633
data
Liquid
IDR PROCESS The
NH3
et at.,
(between
literature of both
- l/T,)
mole
respectiveiy
We
Durisch
sotubitity
reproduced
being Ati, =12050J/mol,
to
avaitabte
compositions
in water. the
root
few
and
Table
calcuiated
1983)
and
found
Henry's
were
URER
In fact,
THE
we
temperature
parameters
auREa,waTEn
solid
of
considered
adjustabLe
The
that
temperature
(Kawasumi,1952,1953,195~;
in a narrow
and
emphasize
pressure,
value
increasing
up because
to
In fact
when
in carbamate,
the
quantities
the concentration
the
at
a
of either of the
free
increasing. in
a
in order
temperature
simulation
computer
to calcuiate slightly
rises
stripping from
program
(Pagani
and
paths. top
to
bottom;
the
213
Fiqufe
2 _
stand
for
- Calculated top
and
isotherms
bottom
of
the
and
concentration
of ammonia
is almost
through
stripper,
removed
excess
the
of ammonia,
reduction In
Table
5 real
comparison TABLE
the
of carbamate
with
stripping
path
of
2nd
stripper.
T and B
equipment.
constant,
by gaseous
reduction
of CO*
while NH..
carbon
dioxide
As there
accompanied
is
decreases
is a stoichiometric by
a
nearly
equal
in solution.
operating
conditions
calculations
of such
an equipment
are
reported:
the
is satisfactory.
5.
Working
conditions
and
outcoming
countercurrent
stripper,
funning
equipment
be quantified
could
Exchanged
heat
Number
theor.
of
No UREA
liquid at
streams
20.
comparison
MPa.
The
gas
phase
for
the
leaving
as difference.
6279. plates
MJ/h
3
hydrolysis
F ""Em Liquid
feed
Gaseous
feed
13355. 0.
Fwas.. 7139. 5.
FNH,
F sn.rtr
FCO,
T
13663.
4306.
0.
455.
2495.
0.
50.
473.
Plant
outlet
13355.
7079.
13754.
3107.
0.
C76.
Calc.
outlet
13355.
7139.
13435.
3205.
0.
476.
lc the
214 The
simulation
reported) at the This
shows
bottom
is due
2nd
of
to both
the the
cold
concentration
has
value
of 4.75
% by weight.
Rgain
the
we
flashes
report
coming
Tables the
agreement
7,
presented
TRBLE
CO*
between
feed
2,
where
stripping with
behaviour,
plant
a plant for
comparisons
where all
are
hydrolysis residence
assumed
and
comparisons
9 that
and
because
We
low.
some
from
6 and
temperature
point
got
Figure
path
the
is also
lowest
value
equipment.
that
at
Moreover
(see
a characteristic
(B) of
especialty
stripper
from
running
calculated
between
are
ptant
data
and
high a
is good
catculated
are missing.
equipments
taking
UREA,
conditions
plant
the strippers
these
of times
It can
(Tabte for
conditions
countercurrent
Exchanged
heat theor.
of
Rssumed
URER
Liquid
feed
Gaseous
feed
and
stripper,
Number
be seen
emerging
in
from
small.
outcoming running
liquid
at 20
streams
comparison
for
the
6120. plates
M3/h
6 1.75%
hydrolysis
F U"EEl
Fwe,,a
13355.
7079.
0.
F
by weight
N*)
FCOt
13754.
0.
0.
F iorrt.
T
3107.
0.
L76.
9245.
65.
383.
Plant
outlet
12720.
6354.
3679.
2912.
0.
653.
outlet
12720.
5684.
4067.
3029.
0.
(62.
TABLE
7.
Working
conditions
and
outcoming
liquid
streams
comparison
for
a flash
running
HPa
Exchanged
heat
Feed
2@
MPa.
Calc.
7
6). some
6.
Working
at
N!i.
hydrotisis
data
the differences
place
and
86671.
F ""LP
FLAX4y.r
65116.
41643.
60171.
F
N*3
tlJ/h
F sn.rt.
T
33487.
318.
b67.
FCD,
Plant
outlet
65116.
35560.
26819.
8645.
0.
b56.
Catc.
outlet
65116.
36732.
28609.
8030.
0.
465. '.'
215 TRBLE
8.
Working at
conditions
and
outcoming
liquid
streams
comparison
for
a flash
running
1.3 MPa
Exchanged
heat
354b3.
Feed
HJ/h
F”llCf3
F WlTL"
F*u,
F,,,
65116.
35560.
26819.
6645.
0.
456.
F lnlrt.
T
Plant
outlet
65116.
30262.
6731.
1676.
0.
b23.
Calc.
outlet
65116.
29250.
8035.
19&O.
0.
42&.
TABLE
9.
Working at
conditions
and
outcoming
liquid
streams
comparison
for
a flash
running
.33 MPa
Exchanged
heat
10664.
Feed
f”“,Cl
FlAWIT.”
65116.
30262.
F
HJ/h
NH)
FCDx
6731.
1676.
F in.rtr 0.
T &23.
Plant
outlet
65116.
25619
2527.
653.
0.
396.
Calc.
outlet
65116.
26530.
2956.
490.
0.
402.
NOTHTION al
= activity
au1
= interaction
of component parameter
= parameters
B,,B,,B,,B, F
= Flow
Ha (V H1 tQ H%
= Henry's
AH,
= heat
KJ
= thermodynamic
m
= molality,
rate,
i between
in equations
component (6 and
k and
constant
7)
of component
i, MPa
kg/mol
constant
of component
i, at pressure
= Henry's
constant
of component
i, evaluated
MB,
= total
MB.
q
P
= pressure,
total
i, K
kg/h
= Henry's
of
component
fusion,
ammonia
MPa
pressure
J/mol
equilibrium
mot/kg
carbon
P at saturation
constant
of solvent
introduced dioxide
in solution,
introduced
mol/kg
in solution,
of solvent moL/kg
of
solvent
216
PL
= saturation
PM
= molecular
91
= surface
ri
= volume
R
= gas
pressure
of water
at system
temperature,
parameter area
parameter
constant, ratio
J/mot
R* T
= temperature,
Tr
= melting
point,
v _ u1
= partial
molar
volume,
= partial
moiar
volume
of molecular
solute
xi
= liquid
fraction
of component
i
mole
Yi
= vapor
2
= coordination
mole
water
K
= molar
Greek
MPa
weight
to URER
K K
fraction
cm3/moL
of component
at
infinite
dilution,
cm3/mot
i
number
letters
21
= activity
6
= concentration
'p
q
vapor
coefficient dependent
phase
fugacity
parameter
coefficient
Superscripts *
= asymmetric
S
= saturation
m
= infinite
V
=
+
= cation
-
= anion
convention
dilution
convention
based
on molality
scale
Subscripts b
= solute
i,k
= component
j
= reaction
m
= single
S
q
solvent
solvents
U
q
URER
W
q
water
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M. and UNIPURC
CarvoCi,
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of Vapour-
Using
an
218 RPPENDIX We
report
here
an extended For et For
the al.
the
expressions
of
the activity
coefficients
caiculated
using
UNIQUACequation.
solvents
there
are
no differences
with
respect
to the
paper
of
Sander
(1966).
the
solutes
you
have
to consider
that: (RI)
and So
now
we
have
a mixture
the Debye-Huckel
term
assumed
concentration
Instead
the
b) and
Besides
:
& = ea
- -
term
changed
at
being
all,
the dielectric
qb a surface number,
taken
area eoual
parameter
(both
referred
xbr./Dx*r*
(R3) (AL)
residual
term
In
L . = q,. 8'
-
expression
C*r Rk
= pc,,
Db
= ;p,2e,6,,,m
is:
Ln Sb - fib + CD, + E,
2B)/T
l
In
Qqwy:;w R,qw
g&f,,
B
FeiEs
(R6) (R7)
Cc*, (Cam
+ cm,)
(A9)
+ C,t¶)
(RIO) (Rll)
: are
referred
+ i
(R6)
Et2 = =
+ qu
qu+R,qwywu ]
= p,
F and
+ quy’Y;,u
(R5)
q”Y.w+%qw
ki Y = yJki 15%
to
to 10.
= x,q,/Ex,qla
being:
constant
is:
parameter,
z a coordination
The
5%
is not
sotvents.
-gzq,.
rb is a volume
solute
two
independent.
combinatorial
In -
where
of
summations
to the
Y *i=
exp
f brn =
e,-;f,,,,e,
(
solvents
-a*,/T)
over
ail
system
species,
expect
where
specified;
only; (R12) (R13)
IZ is _