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Intensifying glycerol steam reforming on a monolith catalyst: a reaction kinetic model

Abstract

In this work, a structured monolithic catalyst has been tested under a wide range of conditions (partial pressure, residence time, temperature and time-on-stream), with the aim of modeling its kinetic behavior and assessing its economic and upscaling potential. We have developed a sequential model to help us interpret both main trends and salient features. Unexpected behavior was found for certain parameter values, which led us to consider kinetic parasitic effects such as mass or heat transfer limitations. By independently invoking these effects, a conciliatory view of the results observed could not be reached. A combined explanation may prove successful, although overfitting could not be ruled out at this point. More importantly, however, the observed salient features of this stable and selective monolith catalyst may hold potential for process intensification of glycerol steam reforming, thus contributing to a more sustainable industry.

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Intensifying glycerol steam reforming on a monolith catalyst: a reaction kinetic model

Author: Bobadilla Baladrón, Luis Francisco; Blay, V.; Domínguez Leal, María Isabel; Romero Sarria, Francisca; Centeno Gallego, Miguel Ángel; Odriozola Gordón, José Antonio
Publisher: Elsevier
Year: 2016
DOI: 10.1016/j.cej.2016.08.021
Source: https://idus.us.es/bitstreams/53364e66-71cd-4914-b43a-5c471c99807b/download
In ensi ying glyce ol s eam e o ming on a monoli h ca alys :
a eac ion kine ic model
L.F. Bobadilla1, V. Blay2, A. Ál a ez 1,†, M.I. Domínguez1, F. Rome o-Sa ia1, M.A.
Cen eno1,* and J.A. Od iozola1
1 Ins i u o de Ciencia de Ma e iales de Se illa, Uni e sidad de Se illa-Consejo Supe io
de In es igaciones Cien í icas, A enida Amé ico Vespucio s/n, 41092 Se illa, España
2 Ins i u o de Tecnología Química (UPV-CSIC), Uni e si a Poli ècnica de València,
Consejo Supe io de In es igaciones Cien í icas, A enida de los Na anjos s/n, 46022
Valencia, España
AUTHOR INFORMATION
Co esponding Au ho
To whom co espondence should be add essed:
* D . Miguel A. Cen eno ([email p o ec ed])
P esen Add esses
† Ins i u e o Chemical Resea ch o Ca alonia (ICIQ), The Ba celona Ins i u e o Science
and Technology, A . Països Ca alans 16, 43007 Ta agona, Spain
ABSTRACT. In his wo k, a s uc u ed monoli hic ca alys has been es ed unde a
wide ange o condi ions (pa ial p essu e, esidence ime, empe a u e and ime-on-
s eam), wi h he aim o modeling i s kine ic beha io and assessing i s economic and
upscaling po en ial. We ha e de eloped a sequen ial model o help us in e p e bo h
main ends and salien ea u es. Unexpec ed beha io was ound o ce ain pa ame e
alues, which led us o conside kine ic pa asi ic e ec s such as mass o hea ans e
limi a ions. By independen ly in oking hese e ec s, a concilia o y iew o he esul s
obse ed could no be eached. A combined explana ion may p o e success ul, al hough
o e i ing could no be uled ou a his poin . Mo e impo an ly, howe e , he obse ed
salien ea u es o his s able and selec i e monoli h ca alys may hold po en ial o
p ocess in ensi ica ion o glyce ol s eam e o ming, hus con ibu ing o a mo e
sus ainable indus y.
Keywo ds: Ni monoli h ca alys , kine ic modeling, mass and hea ans e
1. In oduc ion
In ecen yea s, biodiesel has a ac ed a conside able a en ion wo ldwide as an
al e na i e enewable uel o eplace adi ional pe oleum diesel p oduc because o
limi ed ese es o adi ional ossil esou ces, he ins abili ies o c ude oil p ice and he
conce ns o e g eenhouse gases emissions [1, 2]. Du ing he p oduc ion o biodiesel by
ca aly ic anses e i ica ion eac ion om ege able oils o animal a s, a la ge amoun
o glyce ol is o med as byp oduc . As a esul o he inc eased biodiesel p oduc ion
du ing he las yea s, a sa u a ed ma ke o glyce ol has p o oked an expec ed all in
glyce ol p ices; he e o e, inding e ec i e and economical ways o con e sion o
glyce ol in o use ul p oduc s is necessa y. Recen s udies ha e sugges ed ha an
a ac i e idea would be o p oduce hyd ogen om glyce ol ia ca aly ic e o ming
p ocesses, hus adding alue o he glyce ol su plus [3, 4].
Glyce ol s eam e o ming (SR) has been demons a ed o be an e ec i e me hod o
hyd ogen p oduc ion wi h high selec i i y, and i can be pe o med in gas o aqueous
phase depending on he eac ion condi ions, mainly empe a u e and p essu e [5]. S eam
e o ming, al hough highly endo he mic, is p e e able since he low p essu e a ou s
selec i i y o hyd ogen. Nickel is he mos used ac i e me al o glyce ol s eam
e o ming because o i s good ac i i y o C-C, C-O and C-H bond clea age, as well as
o i s abili y o emo e he adso bed CO by wa e gas shi (WGS) eac ion [6-17]. In
addi ion o hei op imal pe o mance, Ni-based ca alys s a e p e e ed due o he low
cos and high a ailabili y. Howe e , he supp ession o coke deposi ion o enhance
ca aly ic s abili y s ill emains a majo challenge. Di e en s udies ha e sugges ed ha
he combina ion o basic p omo e s (Mg, Ce) and a g oup IV alloying elemen such as
Sn a o s coke- esis ance o Ni ca alys s in he SR o hyd oca bons [18-21]. Typically
hese addi i es help o a oid ca bon deposi ion and enhance hei ca aly ic s abili y.
In a p e ious pape [22], we demons a ed ha a Ni-based monoli h ca alys is e y
ac i e and s able o hyd ogen p oduc ion by glyce ol s eam e o ming. Coke o ma ion
was no obse ed in he monoli h ca alys hanks o he s ong in e ac ion be ween he
ca alys pa icles and he alumina laye in he monoli h. The u iliza ion o me allic
monoli h ca alys s in p ac ical applica ions is e y impo an o con ol he hea and
mass anspo p ope ies since he majo i y o ca aly ic eac ions depend on hea
ans e , luid dynamics, and su ace eac ion kine ics. In addi ion o his, me allic
monoli hs a e excellen models o he ini ial s udies o mic ochannel eac o s in which
coupled endo- and exo he mic eac ions a e used o con olling he p ocess selec i i y
[23].
Conce ning he eac o modeling, se e al s udies on he kine ics and he eac ion
mechanism o glyce ol s eam e o ming ha e been ca ied ou in he las en yea s [14,
24-27]. Howe e , mos o he epo ed kine ics a e based on powe -law models and
e e o powde ed ca alys s. To he bes o ou knowledge, he e a e only wo wo ks
published e y ecen ly ha desc ibe a kine ic model o glyce ol s eam e o ming using
a wall-coa ed ca aly ic mic ochannel [28] and a kine ic s udy o au o he mal e o ming
o glyce ol in a dual laye monoli h ca alys [29], espec i ely. Liu e al. ound ha he
eac ion a e o glyce ol e o ming was no limi ed by mass ans e wi hin he ca alys
washcoa ed laye and he su ace eac ion was he a e con olling s ep Langmui -
Hinshelwood kine ics conside ing non-dissocia i e adso p ion o glyce ol and
dissocia i e adso p ion o s eam we e p oposed o desc ibe he au o he mal e o ming o
glyce ol in his dual laye monoli h ca alys [29].
This wo k in ol es a de ailed s udy wi h he aim o unde s anding he kine ic
beha io o he well-pe o ming Ni-based monoli h ca alys unde a wide ange o
condi ions (pa ial p essu e, esidence ime, empe a u e and ime-on-s eam), looking
ou o po en ial upscaling. We an icipa e ha unusual e ec s we e ound in his s udy,
which we a emp ed o a ionalize based on he da a a hand and p io knowledge. These
esul s may well dese e addi ional wo k, as hey hold p omise o imp o ed economics
a comme cial scale.
2. Expe imen al
2.1. Syn hesis o NiSn/CeO2-MgO/Al2O3 ca alys
NiSn/CeO2-MgO/Al2O3 ca alys was p epa ed by he imp egna ion me hod using a
syn hesis p ocedu e p e iously epo ed [19, 22]. Sphe ical pelle s o γ-Al2O3
(Sphe ali e SCS505) wi h 2.5 mm diame e we e milled in a high-ene gy ball mill in
o de o ob ain γ-Al2O3 wi h a pa icle size o 7–8 μm, which was used as suppo o
p epa e he ca alys used in his s udy. All he p ecu so s we e imp egna ed
simul aneously on he alumina suppo wi h an aqueous solu ion con aining app op ia e
quan i ies o Mg(NO3)2·6H2O (Sigma-Ald ich), Ce(NO3)3·6H2O (Fluka),
Ni(NO3)2·6H2O (Pan eac) and SnCl2 anhyd ous (Fluka), ollowed by d ying o e nigh
a 120°C and inal calcina ion in ai a 700°C o 12 h. The nominal me al loading was
26 w .% wi h a Ni- o-Sn a omic a io equal o 6.
2.2. Me allic monoli h manu ac u e
Me allic shee s o AluCh om YH ® wi h 50 μm hickness (Good ellow) we e used as
subs a es o p epa a ion o he me allic monoli h. Cylind ical monoli hs we e p epa ed
by olling la and co uga ed oils al e na i ely a ound a spindle (L = 30 mm, d = 16
mm, V = 6 cm3, cell densi y 170 cells/cm2), ollowing he s eps p esen ed in Fig. 1. This
geome y was op imized p e iously o ensu e a mo e e icien hea and mass ans e
[30-32], as will be discussed below. The me allic monoli h was he mally p e ea ed in
ai a 900 ºC o 22 h in o de o gene a e an adhe en α-Al2O3 laye [33]. This ea men
ensu es a good adhe ence o he ca alys o he me allic subs a e.
2.3.Washcoa ing p ocess
The i s equi emen o an e ec i e washcoa ing p ocess is ob aining s able slu ies.
In o de o achie e a uni o m coa ing o he me allic subs a e i is necessa y o p epa e
he slu y con olling he pa ame e s a ec ing i s s abili y, such as pa icle size o he
ma e ial o be dispe sed, solid con en o he suspension, pH and iscosi y. Fu he mo e,
he use o addi i es in he slu y o mula ion a emp s o imp o e he ca alys adhe ence
and he washcoa d ying p ocess. Fo ins ance, he addi ion o colloidal alumina
(Nyacol, 20 w % Al2O3), ha p esen s a na ow pa icle size dis ibu ion, enhances
ema kably he ca alys adhe ence owing o he smalle pa icles in e locking wi h he
la ge ones [34]. A e se e al ials o slu y o mula ion o washcoa ing, we achie ed
a s able aqueous slu y o he ca alys p e iously p epa ed as desc ibed in sec ion 2.1.
The ca alys was milled in an aga e mo a achie ing an a e age pa icle size o 12.7
μm. Since he isoelec ic poin (IEP) o he ca alys is equal o 7.8, he pH was ixed a

3.5 using ace ic acid o ensu e high alues o ze a po en ial, which ansla es in o high
epulsions be ween he pa icles and imp o ed s abili y o he slu ies. The ollowing
p opo ions o ca alys and colloidal alumina we e selec ed: 61 w % ca alys con en and
39 w % colloidal alumina, being he o al solid con en o he aqueous suspension ca. 24
w %. The me allic monoli h subs a e was dipped in o he slu y o 60 s, wi hd awn a a
cons an speed o 3 cm min-1 and hen he excess o suspension in he mic ochannels
was emo ed by cen i uga ion a 500 pm o 5 min. This p ocedu e was epea ed
se e al imes wi h in e media e d ying s eps a 120 C o 30 min be ween coa ings un il
ca. 200 mg o he ca alys was deposi ed. Finally, he coa ed s uc u ed suppo was
calcined a 700°C o 12 h. This p ocedu e esul ed in a ca alys loading on he monoli h
o 0.56 mg cm−2 a e ou washcoa ing s eps. The adhe ence o he ca aly ic laye was
e alua ed wi h he ul asound es [35] achie ing a alue be e han 97%
2.4. Ca aly ic pe o mance: s abili y es
The ca aly ic measu emen s we e ca ied ou in a compu e ized comme cial
Mic oac i i y Re e ence ca aly ic eac o (PID Eng&Tech), employing a Has elloy C-
276 ubula eac o (Au ocla e Enginee s) wi h 17 mm in e nal diame e , which
con ained he monoli h loaded wi h 200 mg o ca alys . P io o eac ion, he ca alys
was educed in si u a 750°C o 1 h wi h 100 mL min−1 o H2 (50%, / in ine ). The
expe imen al uns we e conduc ed a 750 °C and a mosphe ic p essu e wi h a s eam- o-
ca bon a io o 4 (ps eam ≈ 0.32 a m; pG ≈ 0.027 a m) and 100 NL g−1 h−1 con ac ime in
o de o ensu e an op imal ca aly ic ac i i y [19]. A he eac o ou le a Pel ie gas–
liquid sepa a o was i ed allowing he analysis o gas and liquid phase p oduc s
sepa a ely. Gas p oduc s we e analyzed on line using a mic oGC (Va ian 4900)
equipped wi h Po apak Q and MS-5A columns. Liquid p oduc s we e analyzed by
HPLC (Va ian 356-LC) equipped wi h a e ac i e index de ec o and a Hi-Plex H
column wi h deionized wa e as eluen .
2.5. Kine ic measu emen s
Kine ic da a o he glyce ol s eam e o ming eac ion we e collec ed a a mosphe ic
p essu e and a eac ion empe a u e o 600 ºC in o de o achie e in e media e
con e sions. Glyce ol-wa e mix u es wi h composi ions anging om 30 w .% o 45
w .% (co esponding o s eam- o-ca bon a ios o 1.7 o 4) we e ed o ensu e a
s oichiome ic excess o s eam. This s eam was dilu ed in o lowing N2 o yield s eam
pa ial p essu es in he ange ps eam = 0.11-0.32 a m. The esul ing con ac imes
employed in he expe imen al uns a e hus be ween 100 and 230 NL g-1 h-1. Thanks o
he high cell densi y o he monoli h designed, hese ansla e in o gas hou ly space
eloci y (GHSV) alues o 3500-7500 h-1. High GHSV igu es a e in e es ing om an
indus ial poin o iew, as hey would allow p ocess in ensi ica ion (PI) wi h mo e
compac eac o designs. Resul s p esen ed in his wo k co espond o a ime-on-s eam
o 7 min, al hough he ends we e ound consis en wi h esul s a e 1 h, and e en
much longe . A he indus ial scale a highe empe a u e would be used o ensu e a
maximal con e sion and ca aly ic s abili y such as 750 ºC (sec ion 2.4).
2.6. Model simula ion
As will be explained below, models used o help us in a ionalizing he da a comp ise
coupled di e en ial and algeb aic equa ions, namely p ope y balances along wi h a e
equa ions, which need o be sol ed simul aneously. To his end, models we e
implemen ed on Ma lab 7.11.0 as cus om made sc ip s. To sol e hem, we used he
buil -in sol e ode15s. I is a a iable-o de sol e based on nume ical di e en ia ion
o mulas. I was chosen because o i s abili y o deal wi h s i p oblems, which we
an icipa ed ha migh a ise i some o he pa hways in he p oposed eac ion scheme
lose ele ance as op imiza ion p oceeds. On op o ha , o pa ame e op imiza ion, a
high-le el mul is a p ocedu e was used, epea ing he op imiza ion algo i hm s a ing
om di e en combina ions o seed pa ame e alues esul ing om a loga i hmic-
ac o ial di ision o he pa ame e space. As o he op imiza ion algo i hm i sel , we
op ed o he minsea ch ou ine in Ma lab, which is a inely coded e sion o he
classical Nelde -Mead algo i hm. The objec i e unc ion (O.F.) in such a minimiza ion
was designed o be:
𝑂.𝐹.=∑[(𝐹𝐶𝑂
𝑒𝑥𝑝 −𝐹𝐶𝑂
𝑐𝑎𝑙𝑐)2+(𝐹𝐻2
𝑒𝑥𝑝 −𝐹𝐻2
𝑐𝑎𝑙𝑐)2] (Eq. 1)
whe e he summa ion ex ends o all expe imen s pe o med. This was chosen on he
basis ha : 1) he es o main p oduc s, namely H2O and CO2 we e ound o be
s oichiome ically ela ed o CO and H2 based on he wo main eac ions p esen ed
below, and 2) bo h H2 and CO a e majo p oduc s de ec ed by he same GC de ec o ,
hus maximizing epea abili y o measu emen s.
3. Resul s and discussion
3.1. Ca aly ic pe o mance
In o de o in es iga e he pe o mance o he monoli h ca alys o glyce ol s eam
e o ming, an ini ial expe imen was pe o med a 750 °C employing a s eam- o-ca bon
a io o 4 and a space eloci y o 100 NL g−1 h−1. Fig. 2 shows ha he monoli hic
ca alys exhibi ed good ac i i y and s abili y in e ms o hyd ogen yield o e 55 hou s o
ime-on-s eam. Only non-condensable p oduc s such as H2, CO2, CH4 and CO we e
o med by glyce ol s eam e o ming (Reac ion (1)), glyce ol decomposi ion (Reac ion
(2)) and WGS (Reac ion (3)). Fo ma ion o CH4 esul s om me hana ion eac ions
(Reac ions (4) and (5)) by coupling o H2 and CO o CO2 o med om glyce ol
decomposi ion.
C3H8O3 + 3H2O → 3CO2 + 7H2 (1)
C3H8O3 → 3CO + 4H2 (2)
CO + H2O ↔ CO2 + H2 (3)
CO + 3H2 ↔ CH4 + H2O (4)
CO2 + 4H2 ↔ CH4 + 2H2O (5)
2CO ↔ CO2 + C (6)
As can be seen in Fig. 2, he CO- o-CO2 mola a io emains p ac ically unal e ed.
This ag ees wi h he absence o ca bon deposi s ha could eac wi h he CO2 o med
acco ding o he Boudoua d eac ion (Reac ion (6)) and al e he CO- o-CO2 mola a io
as he eac ion p oceeds. In a p e ious epo [22], we ha e in es iga ed
comp ehensi ely he phenomena o deac i a ion by ca bon deposi ion as a unc ion o
he ca alys shape o glyce ol s eam e o ming eac ion and we demons a ed ha he
o ma ion o coke on he monoli hic ca alys is minimized. These cha ac e is ics make
his monoli hic ca alys app op ia e o an addi ional s udy o eac ion kine ics.
3.2. Reac ion kine ic model
Fig. 3 ep esen s ini ial glyce ol con e sion o non-condensable p oduc s as a unc ion
o space ime in he monoli hic ca alys . Space ime in his igu e has been e e ed o
he eac ion empe a u e (600 °C) o be mo e sugges i e o he sho esidence imes
ac ually used. Da a poin s a e labelled wi h pa ial p essu es o he eac an s in he eed
whe e Kp is he equilib ium cons an in eac ion (3), which can be es ima ed by
Callaghan’s equa ion [38] neglec ing he ugaci y coe icien s o being close o uni y:
𝑙𝑜𝑔10𝐾𝑃= −2.4198+0.0003855 𝑇+ 2180.6 𝑇−1 (Eq. 18)
In Fig. 7, he app oach o equilib ium o all da a poin s in Fig. 1 3 is ep esen ed as a
unc ion o glyce ol con e sion o e o ming p oduc s. No ice ha as glyce ol is ini ially
e o med on he ca alys i does no yield a p oduc mix u e in equilib ium. Howe e , in
Fig. 7 a clea ly e ol ing end can be disce ned, which would be in acco dance wi h
some in ol emen o he ca alys in he WGS eac ion.
3.3. Hea and mass ans e limi a ions
Rega ding Fig. 3b, one may hink o o he explana ions o hese ends, such as he
possibili y o a he mal unaway occu ing a longe space imes. In his case, as he
con e sion exceeds some h eshold alue, he hea eleased by he eac ion may no be
eadily exchanged h ough he monoli h walls, hus leading o hea ing and sel -
accele a ion o he eac ion. In spi e o he mode a e eac ion en halpy (-265 kJ mol-1),
gi en he high dilu ion o he eac an , good he mal conduc i i y (18 W m-1 K-1) and
high cell densi y (170 cells cm-2) o he me allic monoli h suppo , an unno iced ho spo
is unlikely o be a p oblem. Mo eo e , ansien esul s du ing eac o s a up do no
show an inc ease o con e sion wi h TOS o any change o he u nace empe a u e o
i s wa age.
Ne e heless, con en ional a e equa ions do no su ice o explain he obse ed
beha io , as was seen in Fig. 5. Ano he possibili y is ha he eac an mix u e does no
en e he monoli h su icien ly ho , and hus pa o he monoli h beha es as a hea

exchange , ope a ing a a limi ed eac ion a e. Only owa ds i s end he gas mix u e
would each he ac ual monoli h empe a u e, po en ially leading o a double
imp o emen as con ac ime is inc eased. To inspec his possibili y we de eloped an
al e na i e model in which hea ans e will be assumed p opo ional o he empe a u e
di e ence be ween he monoli h and he luid:
𝑑𝑇𝑓𝑙𝑢𝑖𝑑
𝑑𝑉 =𝜅·( 𝑇𝑚𝑜𝑛𝑜𝑙𝑖𝑡ℎ − 𝑇) (Eq. 19)
No ice ha in his case he p opo ionali y cons an would depend no ably on he
low, al hough i can be aken as a cons an o simula e an app oxima ed p o ile unde
gi en expe imen al condi ions. In his line, o educe he numbe o pa ame e s
depending on empe a u e, glyce ol consump ion a e was simpli ied down o a i s
o de eac ion, whose kine ic cons an depends exponen ially on empe a u e:
𝑑𝐹𝐺
𝑑𝑉 = −𝑘𝑑𝐺,873 ·𝑒𝑥𝑝(−𝐸𝑎𝑑𝐺
𝑅(1
𝑇− 1
873.15))·𝑝𝐺 (Eq. 20)
Fo his simula ion we assumed a ela i ely high ac i a ion ene gy o 110 kJ mol-1 as
a wo s -case scena io. Addi ionally, he equilib ium cons an o he WGS is also highly
empe a u e dependen (Eq. 18). One can obse e ha hese kine ics lead o a ela i ely
so e olu ion o he empe a u e and concen a ion p o iles (Fig. 8) and, consequen ly,
hey alone canno explain he ab up ends obse ed in Fig. 3b. In e es ingly, by
compa ing he CO- o-CO2 a io in Figs. 5 and 8 one can no ice, howe e , ha he e a e
di e ences: i is e en possible o obse e a maximum in he CO yield along he ca alys
in he la e igu e due o he e e sibili y o he WGS eac ion, hus emphasizing he
impo ance o empe a u e con ol i hyd ogen yields a e o be maximized, mo e so in
comme cial scale ope a ions whe e such he mal e ec s a e easie o occu
inad e en ly.
Ano he e ec ha dese es conside a ion is he hyd odynamic beha io o he
sys em. So a , we ha e based ou discussion on pseudohomogeneous kine ics, i.e. by
analogy o eac ions in homogeneous media. Howe e , he ca alys is he e ogeneous,
and he e o e i s ac i i y is limi ed o he su ace o i s channels. In pa icula , eac an s
ha e o di use o he monoli h su ace, and p oduc s need o coun e di use back o he
bulk gas phase (Fig. 9). The ease o his anspo is a ec ed by he bulk eloci y o he
luid s eam, a ec ing he e ec i e hickness o he bounda y laye nex o he ca alys .
On a mo e mac oscopic scale, Reynolds numbe , impinging on axial and adial
dispe sion, will also a ec he gas eloci y p o ile o some ex en . Howe e , hese
anspo coe icien s a e ela ed o he luid eloci y wi h powe -laws, whose exponen s
usually ake alues lowe han 1 [39]. In addi ion, no ice ha he ange o lows s udied
is a sho e han an o de o magni ude and s ill ma ked di e ences ha e been
obse ed. Gi en ha empe a u e di e ences, which (app oxima ely) ollow a law o
di ec p opo ionali y (i.e. a powe o he uni y, Eq. 19) and which a ec exponen ially
he eac ion a e cons an s canno explain some o he ab up changes obse ed, i is
unlikely ha mass anspo limi a ions could p o ide mo e ma ked dependencies.
As has been discussed, in spi e o he ela i ely limi ed pa ame ic space swep in his
s udy, a non-mono onic end has al eady been obse ed. This makes da a ha d o
in e p e e en when physical e ec s a e accoun ed o (di usion, dispe sion,
empe a u e). A combina ion o e ec s migh ce ainly o e an explana ion, al hough
would equi e mo e ex ensi e s udies o a oid o e i ing. Al e na i ely, i may well be
ha an addi ional, unaccoun ed e ec is in luencing he esul s. In ei he case, hese
ends a e ce ainly wo h u he s udy since, as illus a ed in Fig. 3b, could enable
d ama ic imp o emen s in e ms o ca alys ac i i y, allowing in e es ing op ions o
p ocess in ensi ica ion. I is expec ed ha pos -mo em cha ac e iza ion a e each
eac ion cycle along wi h ope ando s udies o he ca alys su ace will allow iden i ying
he pa icula ly ac i e ca aly ic cen e o he glyce ol s eam e o ming eac ion and
unde s anding he in insic eac ion mechanism, ye main aining he ema kable
selec i i y and s abili y o he p esen monoli h, os e ing in his way he indus ial
ealiza ion o his impo an p ocess.
4. Conclusions
We ha e de eloped models o in e p e he beha io o a Ni-based monoli hic ca alys
in he glyce ol s eam e o ming eac ion. A he e ogeneous kine ic model based on a
sequen ial eac ion scheme p esen ed easonable adhe ence o he expe imen al esul s.
Howe e , an unexpec ed beha io was encoun e ed o ce ain pa ame e alues, which
canno be explained by con en ional kine ic pa asi ic e ec s such as ca alys su ace
sa u a ion o he mal unaway. This beha io dese es u he in es iga ion as i may
un a el be e -pe o ming ca alys s o glyce ol s eam e o ming, a p ocess holding
g ea indus ial in e es .
NOMENCLATURE AND ABBREVIATIONS
Va iables, pa ame e s and cons an s
d Monoli h ex e nal diame e / cm
Ea Ac i a ion ene gy / kJ mol-1
F Mola low / mol s-1
GHSV Gas hou ly space eloci y ( o al low, 0 °C, 1 a m) / h-1
k Kine ic cons an / mol s-1 m-3 a m-1 o mol s-1 m-3 a m-2
KP Equilib ium cons an / -
L Monoli h leng h / cm
p Pa ial p essu e / a m
P To al p essu e / a m
Reac ion a e / mol s-1 m-3
R Uni e sal gases cons an / J mol-1 K-1
T Tempe a u e / °C
κ Modi ied global hea ans e coe icien / cm-3
V Monoli h olume / cm3
Γ App oach o equilib ium / -
τ Space ime / s
Subsc ip s
j j h componen
0 Ini ial
A Lump A
B Lump B
d The mal decomposi ion
G Glyce ol
S eam e o ming
WGS Wa e gas shi
ACKNOWLEDGMENTS
The au ho s g a e ully acknowledge he inancial assis ance om he Spanish
Minis e io de Economía y Compe i i idad – MINECO (ENE2013-47880-C3-2-R and
ENE2015-66975-C3-2-R) co- inanced by FEDER unds om he Eu opean Union. L.
F. Bobadilla hanks he “Jun a de Andalucía” o his ellowship wi h he p ojec POG-
TEP01965. V. Blay hanks he suppo om he Valencian Minis y o Educa ion.
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LIST OF FIGURES
Figu e 1. Manu ac u e and p epa a ion o cylind ical me allic monoli h
Figu e 7. App oach o equilib ium in he WGS eac ion as a unc ion o he ex en o
glyce ol s eam e o ming.

Figu e 8. E ec o limi ed p ehea ing on pseudohomogeneous i s -o de kine ics
wi h espec o glyce ol: (a) empe a u e p o ile, (b) main p oduc dis ibu ion (kdG
(873.15 K) = 200 mol s-1 m-3 a m-1, EadG 110 kJ mol-1, kWGS = 432 mol s-1 m-3 a m-2, pG0
= 0.034 a m, κ = 1 cm-3, T0 = 500 °C)
Figu e 9. Di usion and coun e di usion o and om he monoli h su ace