CAPITULO V – SEGUIMIENTO, CONCLUSIONES Y RECOMENDACIONES
5.3 Recomendaciones
The r e gression equa t i o n s d e s c r i b i n g t he cha r a c te r i s t i c s o f the s k im mi l k conc entr a te and the spr a y drier have been combined to form a c omput e r s i mul ation mod e l of the d r y i n g proc e s s. Th i s model may be us e d t o s imul ate a wide v a r i e t y o f drier ope r a t i n g modes a n d i ncorpo r a t e s provi sion for i n troduc ing c ha n g e s i n m i l k compo s i t i o n and pr e he a t treat- ment . The f o l lowing se c t ion e x amine s t he structure o f t h i s mode l whi le t he second sec t ion descr ibes t he s i mu l ation pro g ram .
5 . 1 - The Mod e l Str uc ture
A s t r uc t ural a r r a y s i m i l ar to that in Tab l e 3-3 was used to d e te r
m i n e t h e o r d e r in whi c h t he r e g r e ss i o n e qua t i o n s mus t b e so l v e d t o give t he unknown powde r prope r t i e s r e s ul ting f rom an y given se t of input v a r i ab l e s . T h i s order depe n d s o n whi c h o f t he input s are f i x ed , w h i c h a r e manipu l ate d and wh i c h are dependent o n t h e inputs a l r e a d y spec i f i e d . Some of the po ss i b l e opt ions a r e g i v en in Tab l e 5 - 1 . The V d r l a b l e
s ymbo l s a r e those o f Ta ble 3 - 1 . In b o t h c a s e s t he f o l l owing V d r l ab l e s a r e a s s umed t o have been fixed :
- mi l k compo s i t i o n - pre he a t t e mpe r a t ure - pre he a t ho l di ng time - drier a i r flowrate - the number of no z z l e s - the no z z l e o r i f i c e s i ze
- the no z z l e swi r l chamber or core
The options mar ked wi th a n a s t e r i s k
( * )
are use d in no z z l e a tomis i n g spra y d r ie r s . Re gar d l e s s o f whi c h opt i o n i s cho s e n ,· f i ve ope r a t i n g v a r i ab l e s m us t b e spe c i f ie d b e f o r e the produc t qua l i t y var i a b l e s c a n be c a l cul a ted . There a r e three d i f fe re n t se t s o f dependent var i a b l e s l i s t e d i n Tab l e S - 1 , s o the simulation mod e l s ho ul d have prov i s i o n for t h e f o l l ow i n g c a l c ulation s .TABLE 5 - 1 Options for Operating Spr a y Dr ier s Op tion Deg rees o f Fixed No . F r eedom Variab l e s * 4 2 4 3 4 4 * 3
T
c 5 * 3 T c 6 3T
7 2T ,
T c 8 * 2T ,
T c
Vi sco s i ty sen s i t i v e no z z l e s ( 1 )p
f rom F , p ( 2 )}1
f rom TS , 'I c ( 3 )p
f rom TS ,T
c Vi scosity insensi t i ve ( 4 ) P f r om F ( 5 ) F f r om P and then and then and then nozzles M a n ipul aterl varictbl e sT ,
TS ,
F , p
T ,
TS ,
F , 'rT ,
TS ,
P ,
'I
T ,
TS ,
F T ,TS ,
p
TS ,
P ,
T
cTS ,
FTS ,
p
T
f r omp ,
TS
c p f romp ,
F F fromf '
p
8 1 Depe n d t= n t V a r i a b l e sJ-l t
T c.;Jl t
p cf '
F cf '
pJl t
F'}l t
F}J t
p}J t
FThe conc entrate v i scosity i s a n intermed iate var i a b l e in the c a l c u l ati o n s and may b e c a l c ulate d f rom the concentr ate to tal so l i d s and t empe r a t ur e in the l a st two c a s e s e v en though i t is not r e qui r e d . Th i s s impl i f i e s the programmin g , a s t he n onl y t h e f i r st three c a s e s n e e d be c o n sidered .
The s i mul ation model a l so inc orporate s two out l e t a i r tempe r a t ur e contro l le r s. One man ip ul ate s the i n l e t a i r temperature and the o t he r man ipul ate s t h e conc entrate feedrate or atom i s i n g pre s s ur e .
82
The str ucture o f t he s i mulation prog ram i s i l l u s t r a te d i n F i g ur e 5 . 1 by means of a f l owc hart.
5 . 2
-
The Simulation Pr ogramEac h o f the mod ul e s s hown i n F i gure 5 . 1 w i l l now be con s i le r e d i n deta il. Some o f the regressio n mode l s g i v en i n Chapt e r 4 a r e used directly, but some fur the r a n a l y s i s wa s r e qu i r ed be f o r e all the n e c e s s a r y e qua t i o n s could be derived.
5 . 2 . 1 Th e Press ure , F l owrate , Viscosit y Re l a t i o n
The viscos i t y o f t he c o nc e n t r a te a t t he n o z z l e i s n o t t he same a s tha t me a s ured w i t h t he Contr a v e s v t scome te r a s t h e conc e n t r a t(' l e a ve s
the heat excha nger in t he feed l i n e t o the h i '::J h pressure pump . The a g e
a n d t empe r a tur e o f the conc e n t r a t e a r e d if f e rent, a n d the s h e a r r a te i s 1 0 0 0 t im e s grea te r at t he nozzle. U s i n g t he v i sco s i t y mod e l i n C hapt e r
4 to obta i n the viscosi ty a s a funct i o n o f t he conc e n t r a te tu tal sol i d s
a n d t empe r a ture , and then c a l c uJ a t 1. n g the p r e s s ure a t a g 1.v •2 n f l o<rn ate f rom t he no z z l e e qua tion gives ver y poor agreement with t he expe r i men t a l observations. Instead, a pseudo-visco sity w a s c a l c ul a ted f rom the p r e s s ur e and flowrate readin gs for t he two season's data as fo l l ows.
For the S B 5 4 noz z l e
so
P F 2 • 3 4 5 ( 2 . 3 6 7 9 + 5.3 0334 exp ( - 0 . 0 3 4 64
f ) )
x 1 0 -4l n
( (
1 0 0 0 0 p 1 p 2 . 3 4 5 2.3 67 9) I 5 . 3 0 3 3 4 l-0.03464
for a sugar sol ution with an average density 1 . 1 03 time s that of the concentrate . The pressures mea sured on concentrate wer e mul tipl i e d by 1 . 1 0 3 b e fore being used in this equation , on the assumption that at constant vol umetr ic flowrate , the pre s s ure i s directly proportional to t he fluid density ( Masters , 1 9 7 2 p . 1 7 0 )
MILK COMPO S I T ION
( % Prote i n )
SELECT OPTION
( 1 ) spe c i f y F , P ( 2 ) specif y F , Tc ( 3 ) spe c i f y P , Tc
OPT ION 1
INPUT O PERAT I NG VARIABLES T , F , p ( 2 ) T , F , Tc
( 3 ) T , P , Tc
CHECK E XP L I C IT CONS'l'kA I I'<T� ·rmi n < T < 'lma x Tmin < T < Tmax
Fmi n < F < Fmax ( 2 ) Fm � n < F < Fma x Pmi n < p < Pmax ( 3 ) Pmi n < p < Pma x
SOLVE NOZ ZLE E QUATION SOLVE V I SCOS IT Y E
Q
UATIONGet
p
f r o m F , p G e tp
f r om 1'S ,Tc P r o te l n C HECK IMPL I C IT CONSTIU\ IN'l'S SOLVE NOZZLE E\._!U/\T l UN
p
>}Jlll
i n ( 2 ) Ge t p f romp ,
F ( 3 ) Get F f romp ,
p SOLVE VISCOSITY EQ
UATIONCHECK I l'IP L I C IT CONSTRA I N T S
Ge t Tc f rom
p ,
'l'S I Pr ote i n( 2 ) Pml r1 < p < Pmax ( 3 ) Fmin < F < Fmax
SCALE T , TS , F , P , Tc
SOLVE QUALI T Y EQUATIONS
Ge t moi s ture , S I , bulk densi t y f r om T , ·rs , F ,
ADD MEASUREMENT NOI SE AND ROUND ING
POWDER QUALITY
FIGURE 5 . 1 A Flowc ha r t o f the Drier Simul at ion Mode l P , T
c
8 4
5 . 2 . 2 The V i scosity , To tal So l id s , Tempe ra ture Re l ation
The pse udo- viscosity c al c ul ate d above wa s then regre s s e d against t h e c oncentrate total sol ids , tempe r atur e and prote i n content to g i v e :
P '
1 8 . 4 6 + 7 . 4 0 TS - 8 . 54 T c + 2 . 5 0 T 2 - 0c .8 2 T . TS c- 0 . 4 5 Prot - 1 . 1 9 T S . Pr ot - 1 . 64 Prot 2 cp
w i t h 0 . 6867 and roo t mean square r e s i dua l 5 . 1 cp .
wher e TS total solids - 4 7 . 7
) I
2T H i gh pr e s s ur e cone . temp. - 43 . 7
)
I
1 0 ca n d Prot Prote in - 3 9 . 7 4
Th i s model wa s s i gn i f i c an t l y better tha n one i n wh i c h the natur a l l o ga r i t hm of t h e vi scos i t y wa s used a s the re sponse var i ab l e , but the rms of the r e s i dua l s wa s s t i l l 2 2 % of t he mean pse udo- v i sco s i t y .
Th i s pse udo- vi scosity pa s s e s through a minimum a s t he tempe r ature o f the concentr ate is rai sed . The tempe ranure wh i c h m i n im i s e �. the v i s co s i ty is found by s e t t i n g to zero the f i rst der ivative of t he e qua t i o n with r e spect to tempe r a t ure , g i v in g :
Tc ( min
p'l
( 0 . 82 T S + 8 . 54) I
( 2 X 2 . 5 0 )The min imum v i s c o s i t y may now b e cal cul ate d , and used to check for an impl i c i t constr a i n t violation whe n opt ion 1 of the simul ation pro g ram i s cho s e n. I n thi s option the conc e n tr a te f l owr a te and atom i s i n g pre s s ur e are s pe c i f i e d , so t h a t the pse udo- vi sco s i t y may be c a l c ul ated f rom the noz z l e e qua t ion . F i gure 5 . 2 gives the e qua ti o n s use d in the s i mul ation mod e l for each of t he three opt i on s .
5 . 2 . 3 The Powder Qual i t y Equa t io n s
T h e e quations p r e s e n t e d in Chapter 4 a r e use d to c a l c ul a te the moistur e , So l ub i l i t y In dex , b ul k d en s i t y and othe r qua l i t y v ar i ab l e s . The t hr o ughput o f m i l k sol i d s i s a l so c a l c ul ated at t h i s s t a g e , using t he f o l lowing equa t i o n .
8 5
p
989 + 0 . 0 1 6 6 T S2 - ( 0.0 0 7 6 T - 3 . 7 5)
T Sc c
-
(
0 . 0 64 + 0 . 0 0 2 4 T ) Tc c
where Pc concentrate dens i ty ( k g/m3 )
TS conc entrate total sol i ds
( % )
T c concentrate temperature ( C )
T h i s i s a r e gression e qua tion f i tted to the data o f Ha l l a n d Hed r i c k 3
( 1 9 6 6 ) with t he i
n
te rcept
( 9 89 kg/m ) ad Jus ted to g i ve bette r a g reement w i th data from New Ze a l and s k i m m i l k concen t r a te s . The so l l d s throughputi s then :
G F
( p
/ 1 0 0 0 ) ( T S/ 1 0 0)
c k g / h whe r e F i s i n 1/h.
Thi s quanti ty is needed i f t he proce s s i n g r
a te
s o f t he d r i e r a n de va po r a tor a r e t o b e matched. At the evapor a tor f i n a l e f f e c t temp-
e r at ur e of 44 C , the tota l s o l i d s - d en s i t y e q ua t ion is approx imate l y :