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Comparative Study of Mass Transfer in Wet and Dry Osmotic Dehydration

Peinado Pardo, Irene,Rosa Barbosa, Estela María,Heredia Gutiérrez, Ana Belén,Andrés Grau, Ana María

Abstract

[EN] The differences in the external osmotic medium, dry or dissolved osmotic agent and its concentration (constant or variable) can significantly influence the kinetics of mass transfer. The objective of this work was to compare water and solute transport during the osmotic dehydration of strawberry pieces under different external conditions, wet or dry osmotic agent, with varying types of sugar (sucrose, fructose and isomaltulose). The evolution of the liquid phase concentration as well as the net fluxes under the different scenarios was described and modelled. Results showed that mass transfer kinetics were higher when the concentration of the external medium was variable, in the wet process slightly superior than in the dry process.

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Focusing on Mode n Food Indus y (FMFI) Volume 2 Issue 3, Augus 2013 www. m i-jou nal.o g 111 Compa a i e S udy o Mass T ans e in We and D y Osmo ic Dehyd a ion I ene Peinado*1, Es ela Rosa2, Ana He edia3, Ana And és4 1Depa men o Biology, Food and Nu i ion, Heal h and Li e Sciences, No humb ia Uni e si y, Newcas le Ci y Campus, Ellison Place, Newcas le Upon Tyne, NE1 8ST, UK 2-4Ins i u e o Food Enginee ing o De elopmen , Uni e si a Poli ècnica de València P.O. Box 46022 Valencia, Spain *1i ene.pa do@no humb ia.ac.uk; 2es oba @doc o .up .es; 3anhegu@ al.up .es; 4aand es@ al.up .es Abs ac The di e ences in he ex e nal osmo ic medium, d y o dissol ed osmo ic agen and i s concen a ion (cons an o a iable) can signi ican ly in luence he kine ics o mass ans e . The objec i e o his wo k was o compa e wa e and solu e anspo du ing he osmo ic dehyd a ion o s awbe y pieces unde di e en ex e nal condi ions, we o d y osmo ic agen , wi h a ying ypes o suga (suc ose, uc ose and isomal ulose). The e olu ion o he liquid phase concen a ion as well as he ne luxes unde he di e en scena ios was desc ibed and modelled. Resul s showed ha mass ans e kine ics we e highe when he concen a ion o he ex e nal medium was a iable, in he we p ocess sligh ly supe io han in he d y p ocess. Keywo ds Isomal ulose; F uc ose; Suc ose; Mass T ans e ; Osmo ic Dehyd a ion; S awbe y In oduc ion Many s udies ocused on he in luence o he di e en a iables on mass ans e kine ics du ing osmo ic dehyd a ion o ui s can be ound in he li e a u e. In mos cases, he s udies ha e analysed he in luence o p oduc a iables (cul i a , a ie y, size, shape, e c.), osmo ic solu ion, ui : solu ion a io, ype o osmo ic agen , agi a ion o he medium, e c. (Pani e al., 2008; Nie o e al., 2004; Laza ides, e al., 1999; Maes elli, 1997; Fi o & Pas o , 1994; Le ici e al., 1985; Poin ing, 1973). The osmo ic agen s commonly used in osmo ic dehyd a ion o ui s a e concen a ed suga solu ions, and he kine ic s udies o mass ans e a e pe o med unde in e nal con ol condi ions, ha is, by using solu ion- ui a ios la ge enough o assume ha he concen a ion o he ex e nal solu ion emains cons an du ing dehyd a ion. Unde hese condi ions, in e nal con ol o wa e and soluble solid mig a ion be ween he wo phases, ui and ex e nal solu ion, is ensu ed, easily pe mi ing he es ima ion o he e ec i e di usi i y om Fick’s second law. Ne e heless, a la ge amoun o solu ion is absen in indus ial applica ions due o en i onmen al sus ainabili y, managemen and ope a ing cos s. In some cases, he osmo ic solu ion is eplaced by he use o a d y osmo ic agen as in he case o mea and ish sal ing, in which i is e y common o use d y sal in wha is called he d y sal ing p ocess. Some di e ences ha e been ound be ween we and d y sal ing o cod o ins ance. The we p ocess using b ines a ou s sal up ake, while he d y p ocess maximizes dehyd a ion o wa e ou low (And és e al., 2005; Ba a e al., 2004). Al hough in bo h cases, he same concen a ion o sal can be eached in he inal p oduc , he ope a ion yield and he ex u e o he sal ed p oduc s ongly depend on he sal ing me hod. Howe e , he use o solid suga ins ead o osmo ic solu ion o he osmo ic dehyd a ion o ui s has no been p e iously desc ibed. The di ec con ac be ween he ui and he su ounding solid suga p o okes a wa e ou pu which g adually dissol es he suga gene a ing a supe sa u a ed solu ion which will be dilu ed as dehyd a ion and he di usion o suga o he ui p og esses. The di e ences in he ex e nal osmo ic medium (d y o dissol ed and cons an o a iable concen a ion) can signi ican ly in luence ei he he kine ics o mass ans e o he magni ude o ne luxes o wa e and solu es. Suc ose has been commonly used o he osmo ic dehyd a ion o ui (He edia e al., 2010, He edia e al., 2009; Lomba d e al., 2008; Seguí e al., 2008; Gi aldo e al., 2003; Ga cía e al., 2002; Shi e al., 1995). Ne e heless, i p esen s some disad an ages om he poin o iew o human heal h such as hei high glycemic and ca iogenic indexes (Pe ei a e al., 2005; www. m i-jou nal.o g Focusing on Mode n Food Indus y (FMFI) Volume 2 Issue 3, Augus 2013 112 Zengo & Mandel, 1972; Weidenhagen & Lo enz 1957). Hence, suc ose eplacemen by uc ose and isomal ulose o ins ance, inc easingly becomes in e es ing in he acquisi ion o new heal hie p oduc s by means o osmo ic dehyd a ion. On he one hand, uc ose has a lowe glycemic index bu highe swee ene index han suc ose and glucose (Ma ínez&Ga cía, 2001). Mo eo e , i is impo an o poin ou ha isomal ulose, a suga ob ained om suc ose by means o a ansglucosila ion eac ion (Schiweck e al., 1990), cha ac e ized wi h one o he lowes glycemic and ca iogenic indexes among suga s is especially sui able o diabe ic pa ien s, child en and spo s people (Je e y e al., 2006; Pe ei a e al., 2005; Pawlak e al., 2004; Lina, Jonke & Kozianowski e al., 2002; Ma suyama e al., 1997). Ne e heless, isomal ulose p esen s some echnical handicaps such as 30% lowe solubili y and hal he swee ness o suc ose (Schiweck e al., 1990; Kaga & Mizu ani, 1985). Hence, pa ial o o al eplacemen o suc ose by uc ose and/o isomal ulose as he osmo ic agen in solu ion o solid s a e could p o ide he indus y wi h new possibili ies o de elop heal hie p oduc s by means o osmo ic dehyd a ion. The aim o his s udy was o compa e wa e and solu e anspo du ing he osmo ic dehyd a ion o s awbe y pieces unde di e en ex e nal condi ions, we and d y osmo ic agen , wi h di e en ypes o suga (suc ose, uc ose and isomal ulose), in all cases eaching he same equilib ium concen a ion. Ma e ial and Me hods Raw Ma e ial S awbe ies (F aga ia esca) acqui ed in a local supe ma ke we e so ed o elimina e damage ui s and homogenise he sample o colou , shape and ipening s age. Samples we e imme sed in chlo ina ed wa e o elimina e possible ield esidues, and we e cu in qua e s. Me hodology Samples we e equilib a ed using h ee di e en p ocesses: (1) We Osmo ic Dehyd a ion wi h Va iable concen a ion o he medium (WOD-V): he osmo ic medium used was a 60 B ix suga solu ion (suc ose o uc ose). (2) We Osmo ic Dehyd a ion wi h Cons an concen a ion o he medium (WOD-C): he osmo ic medium used was a 30 B ix suga solu ion (suc ose, uc ose o isomal ulose). (3) D y Osmo ic Dehyd a ion wi h Va iable concen a ion o he medium (DOD-V): he osmo ic medium used was solid suga (suc ose, uc ose o isomal ulose). All he expe imen s we e ca ied ou a 25 ºC. In he h ee p ocesses, he ui : solu ion a io was es ima ed om he mass balance (equa ion 1) o assu e a concen a ion o he ui liquid phase o 30 B ix a equilib ium. 𝑧𝑧𝑒𝑒𝑒𝑒 =𝑚𝑚0 𝑠𝑠·𝑥𝑥0 𝑠𝑠𝑠𝑠+𝑚𝑚0 𝑂𝑂𝑂𝑂 ·𝑦𝑦0 𝑠𝑠𝑠𝑠 𝑚𝑚0 𝑠𝑠·�𝑥𝑥0 𝑠𝑠𝑠𝑠+𝑥𝑥0 𝑤𝑤�+m0 OS (1) Whe e, zeq: Concen a ion o he soluble solu es o he liquid phase a he equilib ium s age (g soluble solids/g liquid phase); m0s: Mass o s awbe y a he beginning o he dehyd a ion p ocess (g s awbe y); m0OS: Mass o he osmo ic solu ion o solid suga a he beginning o he dehyd a ion p ocess (g osmo ic solu ion o g solid suga ); x0ss: Soluble solu e concen a ion o he s awbe y a he beginning o he dehyd a ion p ocess (g soluble solids/g s awbe y); x0w: Wa e concen a ion o he s awbe y a he beginning o he dehyd a ion p ocess (g wa e /g s awbe y); y0ss: Soluble solu e concen a ion o he osmo ic solu ion o solid suga a he beginning o he dehyd a ion p ocess (g soluble solids/g osmo ic solu ion o solid suga ). S awbe y qua e s we e placed in a plas ic baske di ided in o compa men s and imme sed in a plas ic essel con aining he osmo ic solu ion o he solid suga . A di e en p ede e mined imes (0, 30, 60, 90, 120, 150, 180, 240, 300, 420, 540, 900, 1440 1740 and 2880 min), samples (qua e s o s awbe y) we e emo ed om he osmo ic solu ion, gen ly d ied wi h abso ben pape and di ided in o h ee lo s o pe o m he analy ical de e mina ions. Samples used o he con ol o mass a ia ion we e iden i ied. Physicochemic Alanalyses All he physicochemical analyses we e ca ied ou in iplica e on esh ui , and a di e en imes du ing he osmo ic ea men . Fo mass con ol as well as o he physicochemical de e mina ions, analy ical balances wi h 0.0001 g p ecision we e used. Mois u e con en was de e mined g a ime ically by d ying o cons an weigh in a acuum o en a 60ºC (me hod 20.103 AOAC, 1980). The con en o soluble solids (B ix) was measu ed in p e iously homogenized samples wi h a e ac ome e Focusing on Mode n Food Indus y (FMFI) Volume 2 Issue 3, Augus 2013 www. m i-jou nal.o g 113 a 20ºC (ATAGO 3 T). Fo dehyd a ed samples, dilu ion was necessa y a a a io o 4 g wa e o each g am o sample o B ix measu emen s. Mois u e and soluble solid con en we e exp essed as mass ac ion o wa e (xw) and soluble solids (xss), espec i ely. Resul s and Discussion E olu ion o he Liquid Phase Concen a ion Figu e 1 shows he heo e ical ypical e olu ion o he soluble solid concen a ion in he osmo ic medium (yss) and in he liquid phase o he ui (zss) unde he di e en condi ions desc ibed in he ma e ials and me hods sec ion. In he i s case, WOD-V (Fig.1a), he liquid phase o he ui becomes mo e concen a ed due o he wa e ou - low by osmosis and o he di usion o he solu es om he medium o he ui as a consequence o he exis ing concen a ion g adien , while he ex e nal solu ion becomes mo e dilu ed as a consequence o he men ioned luxes. The ui : solu ion sys em eaches he equilib ium concen a ion when he concen a ion o he solu ion (yss) equals he concen a ion o he liquid phase o he ui (zss) (Poin ing, 1973), in his case 30 B ix since he ui : solu ion a io has been es ima ed o each his a ge concen a ion. When he olume o he ex e nal solu ion is la ge enough o assu e ha he concen a ion o he osmo ic medium emains cons an (WOD-C), he ne luxes o wa e and solu es only a ec he concen a ion o he ui liquid phase (Fig.1b). Howe e , when he ex e nal medium is ini ially a solid suga (DOD-V), he wa e om he ui gene a es an ex e nal solu ion whose concen a ion changes in wo s ages (Fig.1c): (1) he o e sa u a ion s age om he beginning un il he suga is comple ely dissol ed and, (2) he a iable concen a ion s age. Figu e 2 shows he esul s ob ained in he equilib ium expe imen s using s awbe y qua e s unde each o he si ua ions p e iously desc ibed (Fig, 1). The esul s poin ou ha he solubili y o he di e en suga s (suc ose, uc ose and isomal ulose) de e mines he du a ion o he o e sa u a ion s age o he medium du ing d y osmo ic dehyd a ion p ocesses. The du a ion o his s ep was 54, 55 and 120 minu es o suc ose, uc ose and isomal ulose espec i ely. These imes ha e been es ima ed om wa e loss da a ( aking in o accoun he solubili y o he di e en suga s) since he ime equi ed o ex ac he necessa y amoun o wa e o dissol e he o al amoun o suga is equi alen o he p ocessing ime, du ing which he ui is in con ac wi h an o e sa u a ed solu ion. FIG 1: EVOLUTION OF SOLUBLE SOLIDS CONCENTRATION IN THE OSMOTIC MEDIUM (YSS) AND IN THE FRUIT LIQUID PHASE (ZSS) UNDER THE DIFFERENT DEHYDRATION PROCESSES: WET OSMOTICDEHYDRATION WITHCONSTANTCONCENTRATION OF THE MEDIUM (WOD- C), WET OSMOTIC DEHYDRATION WITH VARIABLE CONCENTRATION OF THE MEDIUM (WOD-V) AND DRY OSMOTIC DEHYDRATION WITH VARIABLE CONCENTRATION OF THE MEDIUM (DOD-V). a) b) c) www. m i-jou nal.o g Focusing on Mode n Food Indus y (FMFI) Volume 2 Issue 3, Augus 2013 114 FIG. 2.EVOLUTION OF THE SOLUBLE SOLIDS CONCENTRATION IN THE MEDIUM (YSS) AND IN THE STRAWBERRY SAMPLES LIQUID PHASE (ZSS) DURING THE DIFFERENT OSMOTICDEHYDRATION PROCESSES:WET OSMOTIC DEHYDRATION WITH CONSTANT CONCENTRATION OF THE MEDIUM (WOD-C), WET OSMOTIC DEHYDRATION WITH VARIABLE CONCENTRATION OF THE MEDIUM (WOD-V) AND DRY OSMOTIC DEHYDRATION WITH VARIABLE CONCENTRATION OF THE MEDIUM (DOD-V), FOR THE THREE SUGARS (S: SUCROSE; F: FRUCTOSE; I: ISOMALTULOSE). On he o he hand, i is obse ed ha ei he he ype o suga o he ype o p ocess (we o d y me hod) o he concen a ion o he medium in luences he concen a ion a e o he liquid phase. Fo his eason, he e olu ion o he concen a ion o he ui liquid phase unde each o he s udied condi ions has been modelled using equa ion 2: 𝑧𝑧𝑡𝑡 𝑠𝑠𝑠𝑠−𝑧𝑧0 𝑠𝑠𝑠𝑠 𝑧𝑧 ∞ 𝑠𝑠𝑠𝑠−𝑧𝑧0 𝑠𝑠𝑠𝑠 =𝑘𝑘𝑧𝑧·𝑡𝑡0.5 (2) Whe e, z ss: Concen a ion o he soluble solu es in he liquid phase a each ea men ime (g soluble solids/g liquid phase); z0ss: Ini ial concen a ion o he soluble solu es in he liquid phase (g soluble solids/g liquid phase); z∞ss: Equilib ium concen a ion o he soluble solu es in he liquid phase (g soluble solids/g liquid phase); kz: Kine ic pa ame e (min0.5); : T ea men ime (min). Table 1 illus a es he alues o he kine ic pa ame e as well as he equilib ium ime es ima ed using equa ion 2. The concen a ing a e o he liquid phase is highe when he concen a ion o he ex e nal medium is a iable, he we p ocess sligh ly supe io o he d y p ocess. As e e ed o he ype o solu e, i can be said ha he smalle he molecula size and he highe he solubili y a e, he g ea e he dep essing capaci y o wa e ac i i y is, which esul s in as e concen a ion kine ics in he liquid phase. TABLE 1.KINETIC PARAMETER (KZ) FROM THE LIQUID PHASE CONCENTRATION MODEL AND THE ESTIMATED EQUILIBRIUM TIME (T (MIN)). Suga S F I WET C1 kz 0.016 0.024 0.018 3810 1736 3156 R2 0.98 0.99 0.97 V2 kz 0.025 0.032 - 1626 965 - R2 0.96 0.96 - C1 kz 0.023 0.027 0.020 DRY 1842 1324 2268 R2 0.98 0.98 0.92 1 C: Cons an ; 2 V: Va iable Ne Fluxes o Mass, Wa e and Solu es The e olu ion o he p e iously desc ibed liquid phase concen a ion p o ides in e es ing in o ma ion om a he modynamic poin o iew bu insu icien when e alua ion o o he aspec s ela ed o mass ans e is equi ed (Fi o & Chi al , 1997). The e o e, he analysis o he ne luxes o mass, wa e and solu es can be used o imp o e his compa a i e s udy, since he same liquid phase concen a ion can be achie ed wi h di e en combina ions o wa e loss and solu e gain Focusing on Mode n Food Indus y (FMFI) Volume 2 Issue 3, Augus 2013 www. m i-jou nal.o g 115 wi h impo an implica ions o he p ocess yield and p oduc cha ac e is ics (Pani e al., 2008). Figu e 3 shows he co esponding ne luxes o mass, wa e and solu es o he di e en s udied condi ions. The ob ained esul s indica e ha he condi ions in he medium (cons an o a iable concen a ion, we o d y p ocess) do no de e mine he maximum lux alues (maximum soluble solids gain and wa e and o al mass loss); he a e age concen a ion g adien be ween he ui and he medium is he a iable ha de e mines he maximum ne luxes o mass, wa e and solu es. The highe he a e age concen a ion g adien is, he highe he wa e loss and he lowe he gain in solu es a e. The e o e, in he expe imen s pe o med wi h isomal ulose ha dly any di e ences we e seen; p obably because he maximum concen a ion o he solu ion gene a ed in he d y p ocess is nea o he concen a ion o he solu ion used in he we p ocess. FIG.3. NET FLUXES OF MASS (ΔMο), WATER (ΔMW) AND SOLUTES (ΔMSS) EXPERIMENTED BY THE STRAWBERRY SAMPLES DURING THE DIFFERENT OSMOTIC DEHYDRATION PROCESSES: WET OSMOTIC DEHYDRATION WITH CONSTANT CONCENTRATION OF THE MEDIUM (WOD-C), WET OSMOTIC DEHYDRATION WITH VARIABLE CONCENTRATION OF THE MEDIUM (WOD-V) AND DRY OSMOTIC DEHYDRATION WITH VARIABLE CONCENTRATION OF THE MEDIUM (DOD-V), FOR THE THREE SUGARS(S: SUCROSE; F: FRUCTOSE; I: ISOMALTULOSE). Fu he mo e, in he expe imen s ca ied ou wi h suc ose o uc ose, he maximum concen a ion g adien is achie ed in he d y p ocess due o he highe solubili y o hese suga s, which esul s in maximum le els o wa e luxes. Addi ionally, he ne luxes o mass, wa e and solu es we e also modelled acco ding o equa ion 3: ∆𝑀𝑀𝑡𝑡 𝑖𝑖=𝐾𝐾𝑗𝑗·𝑡𝑡0.5 (3) Whe e, ∆M: Ne Flux a ia ion; K: Flux kine ic pa ame e (min0.5); : P ocess ime (min). Supe indexes i and j: (o= mass; w= wa e ; ss= soluble solids). www. m i-jou nal.o g Focusing on Mode n Food Indus y (FMFI) Volume 2 Issue 3, Augus 2013 116 Table 2 shows he alues o he kine ic cons an s ob ained o he di e en s udied condi ions. TABLE 2. VALUES OF THE KINETIC PARAMETER (KJ) FOR THE PREDICTION OF MASS, WATER AND SOLUBLE SOLIDS FLUXES CONCERNING THE DIFFERENT DEHYDRATION PROCESSES (WOD-C) WET OSMOTIC DEHYDRATION WITH CONSTANT CONCENTRATION OF THE MEDIUM, (WOD-V) WET OSMOTIC DEHYDRATION WITH VARIABLE CONCENTRATION OF THE MEDIUM AND (DOD-V) DRY OSMOTIC DEHYDRATION WITH VARIABLE CONCENTRATION OF THE MEDIUM, FORTHE THREE STUDIED SUGARS (S: SUCROSE; F: FRUCTOSE; I: ISOMALTULOSE). Suga WOD DOD Medium Condi ions Medium Condi ions CONSTANT VARIABLE VARIABLE Kο R 2 Kο R 2 Kο R 2 S -0.011 0.97 -0.019 0.97 -0.018 0.94 F -0.017 0.99 -0.022 0.80 -0.018 0.99 I -0.011 0.98 - - -0.012 0.85 K w R 2 K w R 2 K w R 2 S -0.012 0.98 -0.021 0.97 -0.020 0.95 F -0.019 0.99 -0.025 0.83 -0.020 0.98 I -0.014 0.99 - - -0.015 0.85 Kss R2 Kss R2 Kss R2 S 0.0017 0.87 0.0023 0.91 0.0019 0.71 F 0.0021 0.99 0.0053 0.80 0.0020 0.98 I 0.0015 0.92 - - 0.0020 0.99 These kine ic pa ame e s also indica e ha mass ans e is quicke unde condi ions wi h a iable concen a ion o he medium. Besides, when osmo ic dehyd a ion akes place in he we p ocess, he kine ics a e sligh ly supe io , in spi e o he ac ha in he d y p ocess he a e age concen a ion g adien is g ea e . These esul s could be ela ed o a g ea e collapse o he cellula s uc u e a he in e phase du ing he osmo ic d y p ocesses (DOD). I can be obse ed ha he highe capaci y o dep essing he wa e ac i i y o uc ose could explain he highe alues o he kine ic pa ame e s o wa e loss (Kw), while he solubili y and he molecula size o he osmo ic agen a e he main ac o s a ec ing he kine ics o he gain in soluble solu es (Kss). Conclusions Mass ans e kine ics a e highe when he concen a ion o he ex e nal medium is a iable, sligh ly highe in he we p ocesses han he d y ones. The concen a ion o he medium (cons an o a iable), and he ype o p ocess (we o d y) do no de e mine he maximum lux alues. The a iable ha de e mines he maximum ne luxes o mass, wa e and solu es is he a e age concen a ion g adien be ween he ui and he medium. 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