Fe-pUla ed clay mine al-based o mula ions o imazaquin o educed leaching in soil
T.
Undabey ia M.e. Galán-Jiménez ,
E.
Gómez-Pan oja ,
J.
Vázquez ' ,
B.
Casal ,
F.
Be gaya ,
E.
Mo illo
Slow elease o mula ions
oí"
he he bicide imazaquin (2-( 4-isop oPYI-4-me hyl-5-oxo-4,S-dihyd o-IH-
imidazol-2-yl)quinoline-3-ca boxylic acid) we e p epa ed by i s adso p ion
00
Fe-pilla ed
c1ay
mine als
(Fe
PILCs).
Fe
PILes
we e
syn hesized by he eac ion
o Na+
-mon mo illoni e (SWy-2)
wi h
base-hyd olyzed
50-
lu ions
o
Fe
and
AL
The
Fej(Fe
+
Al)
a ios used
we e
0, 0.05, 0.15
and
0.50.
Fe
PILes
showed
basal spacing
alues o 5.2 and 1.8
nm
which
we e
due
o ¡ on c1us e s
be ween
delamina ed
c1ay
laye s,
and
in e cala ed alu-
minum
polyoxoca ions, espec i ely.As ¡ on
con en
inc eased,
he
pilla ing p ocess yielded PILe
wi h
lowe
mi-
c opo osi y
and
la ge
me
sopo asi y.
Ihe
a ini y
o
imazaquin on
Fe
PIlCs
was
e y high ela i e
o
Al
PIlC, as
e
ealed in i s highe
he bidde
adso p ion alues
and
lowe
deso p ion pe cen s. Compe i i e adso p ion
o
an-
ions such as sul a e,
phospha e
and
chlo ide
p a ided
e idence
o
o ma ion
o
inne
sphe e
complexes
o
imazaquin
on
Fe
PIlCs. Slow elease o mula ions
we e
p epa ed
by
enhanced
adso p ion
o
he
he bicide
am imazaquin-cyc1odex in (CD) complexes in solu ion.
COs
we e
able
o
enhance
up
o 8.5- old
he
solubili y
o
imazaquin,
by
he
o ma ion
o
inc1usion complexes
whe e
he
quinolinic moie y
o
he he bicide
was
pa ially
apped
wi hin
he
CO
ca i y. Release
o he
he bidde
in
sandy
soil
was
abou
lj2- old
lowe
am
Fe
PIlC o mu-
la ions ela i e
o
he
comme cial o mula ion.
1.
In oduc ion
He bicides a e applied o impede he g ow h o weeds and im-
p o e he yield o c ops. Howe e , only a pa o he applied amoun
eaches i s a ge whe eas he es emains ei he a ached o he soil
colloids o unde goes deg ada ion and ans e p ocesses such
as
mi-
g a ion o he he bicide o su ace and g oundwa e , which has been
epo ed o be one o he main sou ces o pollu ed wa e s (Finizio e
aL,
2011; Me cal e e
aL,
2011
).
Io
minimize his e ec , esea ch has
ocused in he las decades
on
he de elopmen o slow elease o -
mula ions
(SRFs)
o he bicides ha pe mi o dec ease he losses o
he used amoun s bu o achie e good bioac i i y, hus p o iding
sa e en i onmen al o mula ions (Femández-U usono
e
aL,
2000;
Sopeña
e
al., 2005; Undabey ia
e
al., 2000, 2003, 2010
).
Clay
mine als ha e been s udied
as
good candida es
o
SRF
because
o hei good adso ben p ope ies in addi ion
o
hei abundance and
low-cos . Mos o he s udies we e pe o med on mon mo illoni e
(M ) whose su ace was modi ied p e iously om hyd ophilic o hy-
d ophobic
by
p e-adso bing o ga üc ca ions, which we e u he used
o
enhanced adso p ion o he ac i e ing edien . In gene al, high
adso p ion
is
usually co ela ed wi h slow elease p ope ies (Mishael
e
aL,
2003
).
Recen ly, hyd o alci es we e used based on he same
p inciple, bu using o ganic anions (Zhenlan
e
aL
, 2009
).
O he clay
mine al-based app oaches we e apping o he he bicide
by
coagula-
ion o delamina ed clay mine allaye s (Nennemann e
aL
, 2001a
),
ad-
so p ion a e p e ious he mal ea men (Bojemuelle e
al
,
2001
),
ben oni e polyme gels (
i
e
aL,
2009
),
and sepioli e gels (Maqueda
e
al., 2008, 2009
).
Pilla ed clay mine als
(PILCs)
we e p o ed e y e ec i e in he ad-
so p ion o he bicides and o ganic con aminan s due o geome ical
compa ibili y be ween he s uc u al po es and molecula dimensions
o he
chemicals, in addi ion o hei speci ic in e ac ions wi h he pil-
la s and laye s
o he
clay mine al (Cheknane
e
aL,
2010
).
Adso p ion
capaci y o
PILC
was used o he p epa a ion o
SRF
o he bicides
(Ge s l e
aL
, 1998; Nennemann
e
aL
, 2001b
).
Imazaquin
(IMZQ)
is
a selec i e imidazolinone he bicide used
o
b oad-spec um weed con ol in legume
aops
(Ab ens, 1994
).
IMZQ
has an acidic ca boxyl and a basic quinoline unc ional g oup wi h
pKa
alues o 3.8, and
2.0,
espec i ely (Regi ano e
aL,
2005
).
The e o e, i ex-
is s
as
an anion a ypical
soil
pH
alues, inc easing i s isk
o
leaching
down he
soil
p o ile. A
PILC
o nula ion was designed o educe i s
leaching
in
soil
(Polubeso a e
al.
, 2002
).
In
he cu en wo k,
SRFs
o
he he bicide imazaquin we e designed based on
PILC
p epa ed om hy-
d olyzed i on solu ions ins ead. Imidazolinone he bicides a e known
o
o n complexes wi h ansi ion me als (
E e
e
aL,
1998
).
Imazaquin
adso p ion on soils wi h di e en physicochemical p ope ies was g ea -
e on he
soil
con aining highe amo phous i on oxide con en
(Undabey ia e al., 2004). This poin ed o he o ma ion o s onge com-
plexes wi h i on o e o he elemen s as aluminum, and hence, enhanced
imazaquin adso p ion and s onge e en ion on Fe PILC. The alidi y o
his app oach o he p epa a ion o SRF was examined in he cu en
pape .
In gene al, he ac i e ing edien loading on clay-based o mula ions
is limi ed by he he bicide solubili y, which p e en s u he adso p ion.
Cyclodex ins (CDs) a e cyclic oligosaccha ides p oduced by he enzy-
ma ic b eakdown o s a ch by bac e ia. These molecules ha e a o oidal
shape, wi h a hyd ophobic in e io ca i y and hyd ophilic aces (Szej li,
1998). The abili y o hese molecules o o m inclusion complexes wi h
non-pola molecules has been exploi ed in he pha maceu ical indus y
as a solubili y enhancemen agen (Bikia is, 2011). En i onmen al ap-
plica ions o subsu ace soil emedia ion o o ganics ha e s a ed o
be desc ibed based on he e y poo CD adso p ion on soil colloids
(Feny esi e al., 2011; Villa e de e al., 2005). The e o e, he ac i e in-
g edien con en o he PILC o mula ions can be inc eased by
pe o ming adso p ion o he he bicide in solu ion om CD inclusion
complexes. The he bicide will be solubilized and adso bed on he clay
mine al whe eas he CD will emain mos ly in solu ion.
The objec i es o his wo k we e: (i) o p epa e Fe PILCs as adso -
ben s o he p epa a ion o SRF; (ii) o s udy he o ma ion o inclu-
sion complexes o IMZQ wi h CD; (iii) o p epa e slow elease
o mula ions om CD–IMZQ solu ions; and finally (i ) o es hese
o mula ions o slow elease.
2. Ma e ials and me hods
2.1. Ma e ials
Wyoming Na
+
–M (SWy-2) was ob ained om he Sou ce Clays Re-
posi o y o The Clay Mine als Socie y (Columbia, MO) (ca ion exchange
capaci y 0.8 mmol/g). Al (NO)
3
∙9H
2
O, FeCl
3
∙6H
2
O, NaCl, Na
2
SO
4
,
Na
3
PO
4
,H
3
PO
4
and NaOH we e pu chased om Sigma-Ald ich (Sigma
Chemical Co., S . Louis, MO). HPLC g ade-ace oni ile was ob ained
om Teknok omaS.A. (Ba celona, Spain). Imazaquin (IMZQ 97% pu i y)
was supplied by Sigma-Ald ich and i s comme cial o mula ion
(Scep e , 180 g a.i. L
−1
) by Agan Mak eshim (Lé ida, Spain). Cyclodex-
ins (CDs) we e pu chased om Cyclolab (Budapes , Hunga y). CDs
employed we e: α-CD, β-CD, hyd oxyp opyl-β-CD (HPβ), and andomly
me hyla ed-β-CD (RAMEβ). Fig. 1 shows he s uc u al o mulas o IMZQ
and CD.
The uppe pa (0–20 cm) o sandy soil classified as Typic
Xe opsammen was collec ed, and passed h ough a 2 mm sie e be o e
use. This soil has a pH o 8.9 and 0.79% o o ganic ma e (mo e de ailed
physicochemical p ope ies a e gi en in Undabey ia e al., 2012).
2.2. P epa a ion o pilla ed clay mine als
Aluminum ni a e and i on chlo ide solu ions in se e al Fe/(Al + Fe)
mola a ios (0, 0.05, 0.15, 0.5) we e hyd olyzed by i a ion wi h 0.4 M
NaOH unde ni ogen a mosphe e. The Al/OH mola a io was 2.0. These
pilla ing solu ions we e aged o 7 days. Then, 10 g o clay mine al was
dispe sed in 250 mL wa e , and he pilla ing solu ions in a a io o
10 mmol (Fe + Al)/g clay mine al we e added slowly wi h a pe is al ic
pump unde ni ogen a mosphe e. The final clay mine al con en was
1% (w:w). The dispe sions we e unde shaking o 24 h, ollowed by
cen i uging, emo al o chlo ide by dialysis, and d y- eezing. Finally,
he powde clay mine als we e hea ed o 3 h a 300 °C unde ni ogen
a mosphe e.
A nomencla u e was used o he PILCs whe e he fi s le e s, Al o Fe,
espec i ely indica ed he absence o p esence o i on in he pilla ing so-
lu ions, and he ollowing numbe s indica ed he used Fe/(Al + Fe) a io.
2.3. Cha ac e iza ion o PILC
The chemical composi ion o he PILC was de e mined by X- ay
fluo escence (PANaly ical Model Axios).
O
OR
RO OR
O
O
RO
OR
OR
O
O
RO OR
RO
O
O
OOR
OR
RO
O
OR
RO
RO
O
O
OR
RO
OR
O
n
α-CD, n = 1, R = H
β-CD, n = 2, R = H
HP-β, n = 2, R = H o CH2-CHOH-CH3
RAMEβ, n = 2, R = H o CH3
Fig. 1. S uc u al o mulas o he he bicide imazaquin and cyclodex ins.
383T. Undabey ia e al. / Applied Clay Science 80–81 (2013) 382–389
X- ay di ac ion o he clay mine al samples was pe o med on a
Philips X'Pe di ac ome e (model An on Paa HTK) wi h Cu Kα,
26 mA and 36 kV, coun ing ime o 10 s/s ep collec ed om 1 o 25° (2θ).
Su ace a ea alues we e de e mined by using he BET me hod.
The adso p ion o N
2
was measu ed wi h a mul i-s a ion high speed
gas so p ion analyze (Quan ach ome Ins umen s NOVA 4200). The
samples we e ou gassed by hea ing a 200 °C o 2 h.
Fou ie ans o m in a ed (FTIR) spec a o he Fe-0.5 PILC we e
eco ded in KB pelle s (2 w .% sample) using a JASCO spec ome e
(model FT/IR 6300) wi h a DTGS de ec o , in he ange o 4000–
700 cm
−1
. Resolu ion was o 2 cm
−1
. 300 scans we e accumula ed
o imp o ing he signal o noise a io in he spec a.
2.4. Adso p ion–deso p ion s udies
IMZQ adso p ion expe imen s we e pe o med in duplica e by
mixing 24 mg o he PILCs wi h 15 mL o he bicide solu ions anging
up o 160 μM. P elimina y kine ic s udies indica ed ha adso p ion
eached equilib ium a e 24 h; hus, he dispe sions we e shaken o
24 h a 20 °C. Subsequen ly, he dispe sions we e cen i uged and he
concen a ion o he bicide in he supe na an s was analyzed. Deso p-
ion expe imen s we e also pe o med o ce ain concen a ions (16,
64 and 160 μM) by eplacing he whole supe na an o he adso p ion
expe imen s wi h wa e , e-equilib a ing o 24 h, cen i uging and u -
he analyzing o he he bicide in he supe na an .
Adso p ion o IMZQ on PILCs was also s udied in he p esence o
NaCl, Na
2
SO
4
and Na
3
PO
4
elec oly es. The added amoun o bo h he -
bicide and elec oly e anion was 160 μeq/L. Clay mine al concen a-
ion was also 1.6 g/L.
IMZQ–CD complexes we e p epa ed om solu ions o 100 mM CD
con aining dissol ed amoun s o IMZQ as de e mined p e iously om
he solubili y diag ams (1.61 and 1.29 mM o HPβand RAMEβ, e-
spec i ely), by successi e dilu ions. Fe-0.5 PILC was ea ed wi h he
IMZQ–CD solu ions a 1.6 g/L, and he adso bed he bicide was de e -
mined as p e iously indica ed. The amoun o CD adso bed was de e -
mined by analysis o he supe na an as desc ibed in Takeuchi and
Miwa (1999).
FTIR spec a o he he bicide be o e and a e adso p ion on Fe-0.5
PILC we e also eco ded.
2.5. Imazaquin solubili y s udies in he aqueous phase in he p esence o
di e en CDs
Solubili y s udies we e ca ied ou acco ding o he me hod e-
po ed by Higuchi and Conno s (1965). IMZQ (10 mg) was added in
excess o i s solubili y a 25 °C (60 mg/L) o aqueous solu ions
(10 mL) con aining a ious concen a ions o one o he CDs. The
ange was om 0 o 16 mM o β-CD and om 0 o 100 mM o
α-CD, HPβand RAMEβ. The expe imen s we e ca ied ou in ipli-
ca e. Flasks con aining he dispe sions we e sealed and shaken o
1 week. This eac ion ime was chosen a e p elimina y kine ic s ud-
ies (da a no shown). Dispe sions we e hen fil e ed using a sy inge
h ough a 0.22-μm Millipo e cellulose glass fibe memb ane fil e ,
and he concen a ion o IMZQ in he fil a e was de e mined by
HPLC (Shimadzu Model 10A) equipped wi h a PDA de ec o as de-
sc ibed in Undabey ia e al. (2008).
The appa en s abili y cons an Kc was calcula ed om he
s aigh line ob ained in he phase solubili y diag am, ollowing he
equa ion p oposed by Higuchi and Conno s (1965):
Kc ¼Slope=S01−SlopeðÞ
whe e S
0
is he IMZQ equilib ium concen a ion in aqueous solu ion
in he absence o CD, and Slope is he slope o he phase solubili y di-
ag am. Solubili y e ficiency (Se) was also ob ained om he solubili y
diag ams, which is defined as he inc emen in he appa en solubili y
o IMZQ a a fixed CD concen a ion wi h espec o i s solubili y in
he absence o CD.
The inclusion complex o he he bicide wi h RAMEβwas cha ac-
e ized by
1
H-NMR. The expe imen s we e un a 25 °C using a B uke
AMX 500 spec ome e . The concen a ions employed we e 100 mM
o CD and 1.28 mM o IMZQ.
2.6. P epa a ion o imazaquin o mula ions
The o mula ions we e p epa ed by adso p ion o IMZQ–CD com-
plexes on Fe-0.5 PILC a 1.6 g/L. The used CDs we e HP-βand RAMEβ.
The used concen a ions we e 100 mM o bo h CDs, and he amoun
o IMZQ dissol ed in he CD solu ions was 1.61 mM o HPβand
1.29 mM o RAMEβ.
The dispe sions we e shaken o 24 h a 20 °C. Then, he he bicide
was analyzed in he emo ed supe na an , whe eas he pelle s we e
d y- ozen yielding he PILC o mula ions. They we e deno ed as
Fe-0.5 PILC-HPβand Fe-0.5 PILC-RAMEβ.
2.7. Release o he bicide
The elease o he he bicide om Fe-0.5PILC and comme cial o -
mula ion was conduc ed by using Büchne unnels. In his p ocedu e
98.9 g o he sandy soil was added o a Büchne unnel (9.5 cm in e -
nal diame e ) equipped wi h a pape fil e on he bo om. The soil
laye was homogenized o a 0.5 cm heigh . The soil su ace was uni-
o mly sp ayed wi h he di e en he bicide o mula ions a a a e o
140 kg o ac i e ing edien s pe ha. The soil laye in each unnel
was i iga ed 14 imes wi h 15 mL, each washing co esponding o
2.12 mm ain a 20 min in e als. The olume elu ed a e each i iga-
ion was collec ed, and he concen a ion o he bicide in he eluen
was de e mined.
3. Resul s and discussion
3.1. PILC cha ac e iza ion
Table 1 shows he clay mine al elemen al composi ion ob ained
om he aw clay and a e pilla ing wi h Al and Al–Fe oligome s. In-
e cala ion o hese oligome s was success ul as no ed in he inc ease
in Al con en ela i e o he ini ial clay mine al and also in he in-
c ease in Fe which pa alleled he Fe/(Al + Fe) a io used in he
pilla ing p ocess.
The e is also a dec ease in he oc ahed al Mg con en in he
pilla ed clay mine als due o he a ack o p o ons om he oligome ic
ca ions, which a e decomposed a e hea ing in oxide pilla s wi h he
subsequen p o on elease (B adley and Kydd, 1993). This Mg elease
yielded hyd oxyl acid si es. Howe e , hese acid si es a e no espon-
sible o he s ong B öns ed acidi y epo ed in hese ypes o ma e-
ials, which is a he a ibu ed o Al (o Al–Fe) pilla s (Zubko e
al., 1994) as a consequence o he g ea e dissocia ion o pilla s by hy-
d a ing wa e molecules (Schu z e al., 1987).
Table 1
Chemical analysis o he aw clay mine al and PILCs exp essed as oxide pe cen age.
SWy-2 Al-PILC Fe-0.05-PILC Fe-0.15-PILC Fe-0.5-PILC
SiO
2
60.08 56.94 47.95 45.49 34.36
Al
2
O
3
17.89 21.28 24.94 23.00 16.14
Fe
2
O
3
3.84 1.00 7.39 15.00 31.18
K
2
O 0.46 0.21 0.34 0.35 0.27
MgO 2.48 2.56 1.79 1.61 1.10
CaO 1.22 0.06 0.06 0.07 0.07
Na
2
O 1.39 0.14 0.19 0.18 0.12
384 T. Undabey ia e al. / Applied Clay Science 80–81 (2013) 382–389
3.2. X- ay di ac ion
The X- ay di ac og ams co esponding o he PILC by in e cala-
ion o Al and Fe oligome s a e shown in Fig. 2. The Al PILC showed
basal spacing a 1.8 nm, indica ing a 0.9 nm in e laye space in good
ag eemen wi h he size o he Keggin ca ion. In con as , Al–Fe PILC
showed an addi ional peak a 5.2 nm, which emained cons an
when inc easing Fe/(Fe + Al) a io. This peak a low angle was o
lowe in ensi y compa ed o ha a 1.8 nm o an Fe/(Al + Fe) a io
o 0.05. Howe e , he con a y endency was obse ed a la ge a ios,
a no iceable dec ease in he in ensi y o he peak a 1.8 nm which was
shi ed o highe angles o an Fe/(Al + Fe) a io o 0.5. This endency
was al eady obse ed by Mandalia e al. (1998). These au ho s
ob ained basal spacing alues as high as 7.2 nm o an Fe/(Al + Fe)
a io o 0.5. The di e en obse ed basal spacing alues a low angles
can be due o he di e en (Fe + Al)/OH a ios used in he o ma ion
o he Fe and Al oligome s, since he pilla ing p ocess is s ongly de-
penden on expe imen al condi ions such as empe a u e and pH,
and also dependen on he na u e o he exchangeable ca ion and es-
pecially on he me al/base a io used.
The high basal spacing ob ained in he cu en s udy di e ed wi h
he as majo i y o p e ious s udies pe o med wi h Fe-based PILCs
(Bandosz and Cheng, 1997; Cañiza es e al., 1999; Heylen and
Vansan , 1997) which showed he la ges basal spacing o abou
2.5 nm. This can be due o he ac ha he s a ing ma e ials we e
clay mine als wi h highe CEC han SWy-2. Al polyoxoca ions a e
mo e e ec i e in neu alizing nega i e cha ge because o hei mo e
plana shapes han hose o Fe ha ha e a mo e sphe ical shape
(Oades, 1984). Consequen ly, he lowe he clay mine al laye cha ge,
he lowe he Al-oligome compe i ion and he la ge he Fe
polyoxoca ion in e cala ion. Clina d e al. (2003) obse ed by ansmis-
sion elec on mic oscopy ha Al–Fe PILCs a e composed by pa icles
sepa a ed om each o he by egula mesopo es, which con ained com-
pac agg ega es o Fe oxide nodules. The sphe oid clus e s o med by
condensa ion o hese Fe nodules had an app oxima e diame e o
3.8 nm. This alue co ela ed qui e well wi h an in e laye space o ap-
p oxima ely 4.2 nm co esponding o he basal spacing o 5.2 nm, in he
cu en s udy.
The di ac ion obse ed a 1.8 nm was he only peak o samples
p epa ed in he absence o i on; he e o e, his peak was due o he o -
ma ion o Al pilla s as usually desc ibed in Al-PILC (Be gaya e al., 2006).
The in ensi y dec ease obse ed o his di ac ion peak o 1.4 nm in
Fe-0.5 PILC indica ed he p esence o smalle Al oligome s. The XRD
da a ag eed wi h p e ious Mössbaue esul s ha indica ed no Al sub-
s i u ion in he Fe pilla s and ha Al and Fe o med sepa a e pilla s o
phases in he in e laye space (Aouad e al., 2010).
3.3. Po osi y
The pilla ing p ocess inc eased conside ably he o al su ace a ea
(Table 2) compa ed o he S
BET
o he aw clay mine al (32 m
2
g
−1
).
The S
BET
dec eased sligh ly (abou 20% educ ion) wi h inc eased Fe
con en . Howe e , he mic opo e a ea dec eased by abou 80% om
Al PILC o Fe-0.5-PILC. The la ge dec ease o he mic opo e a ea s.
he o al su ace a ea indica ed ha mos o he new su ace a ea c e-
a ed in he pilla ing p ocess wi h Fe species co esponded o meso-
and mac opo es. In gene al, he ma e ials p oduced om in e cala-
ion o i on oxyhyd oxides c ea e smalle mic opo e olumes and
su ace a eas compa ed o Al PILC (Bakas e al., 1994; Mish a e al.,
1996; Pinna aia e al., 1983). This was usually a ibu ed o i on spe-
cies adso bed on he ex e nal su ace o he smec i e leading o spa ial
a angemen wi h po e o ma ion o di e en sizes in he mic o- and
mesopo e egion (Bandosz and Cheng, 1997; Ma co-B own e al.,
2012). The mesopo es esul ed om in e pa icle spaces gene a ed
by h ee-dimensional coagg ega ion o i on polyoxoca ions on he
clay mine al su ace o ming delamina ed s uc u es, whe eas mic o-
po es a ose om in e cala ion o smalle hyd olyzed i on oxides and
om mic opo ous in e s ices exis ing among he i on agg ega es and
clay mine al laye s (Yuan e al., 2008).
3.4. Adso p ion iso he ms
IMZQ did no adso b on he aw M (SWy-2) used in he pilla ing
p ocesses due o elec os a ic epulsion a he equilib ium pH be ween
he nega i ely cha ged molecules o he he bicide and he nega i ely
cha ged clay mine al laye s. Howe e , he he bicide adso bed on PILC,
wi h inc eased adso p ion as he i on con en inc eased (Fig. 3). This
ag eed wi h p e ious s udies ha epo ed enhanced IMZQ adso p ion
by Al and Fe oxyhyd oxides in soils wi h low o ganic ma e con en
(Genna i e al., 1998; Regi ano e al., 1997). Undabey ia e al. (2004)
s udied IMZQ adso p ion in soils wi h di e en physicochemical p op-
e ies, and obse ed ha he highes adso p ion occu ed on loam sil
soil due o i s high con en o amo phous i on oxides. This high a fini y
o he IMZQ he bicide o i on oxides would explain alues o maximal
adso p ion up o ou - old la ge han ha on Al PILC.
Adso p ion on Fe PILC was ela ed o he i on con en as well as o
he po osi y o he samples. IMZQ adso p ion inc eased as he meso-
and mac opo e su ace inc eased. The e o e, IMZQ in e ac ion wi h
he pilla s in he in e laye spaces is g ea ly acili a ed. Howe e ,
he g ea e IMZQ e en ion on Fe PILCs o e Al PILC was p obably e-
la ed o a s onge adso p ion mechanism. Al PILC showed highe ex-
e nal su ace a ea alue han Fe-0.05 PILC, bu i s IMZQ adso p ion
was lowe . Polubeso a e al. (2002) sugges ed ha IMZQ adso p ion
on Al PILC was occu ing h ough elec os a ic in e ac ions o he an-
ionic he bicide molecules wi h posi i ely cha ged si es o pilla s ha
a e a ibu ed o Lewis acidi y, in addi ion o hyd ogen bonding o
B öns ed acid si es wi h he ca boxyla e moie y, ni ogen and oxygen
a oms o IMZQ. Bo h mechanisms p o ide less igh binding han
inne -sphe e complexa ion, acili a ing IMZQ deso p ion. Deso p ion
o IMZQ was pe o med by eplacing he comple e supe na an by
dis illed wa e (Table 3). The deso p ion pe cen s we e ex emely
high wi h Al PILC and independen o he ini ial concen a ion, bu
we e la gely educed when using Fe PILC, he la ges he inc ease in
0 5 10 15 20 25
0
50
100
150
200
250
300
In ensi y
2θ
Al-PilC
Fe-0.05-PilC
Fe-0.15-PilC
Fe-0.5-PILC
5.2 nm
1.8 nm
1.4 nm
Fig. 2. X- ay di ac ion o PILCs.
Table 2
Su ace cha ac e iza ion o PILCs.
Sample S
BET
(m
2
g
−1
)
Ex e nal su ace
a ea (m
2
g
−1
)
Mic opo e a ea
(m
2
g
−1
)
Al PILC 213 34 179
Fe-0.05 PILC 190 19 170
Fe-0.15 PILC 195 101 94
Fe-0.5 PILC 172 135 38
385T. Undabey ia e al. / Applied Clay Science 80–81 (2013) 382–389
Fe con en he lowes he deso p ion pe cen s. This sugges s ha
o he adso p ion mechanisms may be ope a ing on Fe PILC. To find
ou he mechanisms in ol ed, IMZQ adso p ion was pe o med on
Al PILC and Fe-0.5PILC in he p esence o compe i i e anions, whose
adso p ion was occu ing h ough di e en mechanisms. The com-
pe i i e anions we e chlo ide, which was adso bed as ou e -sphe e
complex; phospha e, as inne -sphe e complex; and sul a e, which
was adso bed by bo h mechanisms (Polubeso a e al., 2000). The
amoun o adso bed IMZQ dec eased in he p esence o all he elec-
oly es (Table 4). Howe e , he e we e ema kable di e ences
depending on he PILC. The educ ion in he amoun adso bed in Al
PILC was lowe in he p esence o sul a e ela i e o chlo ide. This im-
plied a la ge so p ion o he he bicide on Al PILC by an elec os a ic
mechanism. On he con a y, he opposi e end was obse ed o Fe
PILC, whe e he educ ion in he adso bed amoun s was mo e p om-
inen in he p esence o sul a e s. chlo ide. In bo h clay mine als, he
la ge dec ease in he adso bed amoun s in he p esence o phospha e
was due o he inc ease in he nega i e su ace cha ge when phos-
pha e was adso bed; he e o e, he bicide adso p ion would dec ease
(Polubeso a e al., 2002).
Ca boxylic he bicide adso p ion on i on and aluminum oxides is
s ongly dependen on he he bicide s uc u e. Adso p ion o 2,4-D
occu ed h ough coulombic in e ac ions be ween he o ganic anion
and he posi i ely cha ged oxide su aces (Clausen and Fab icius,
2001; Wa son e al., 1973). Vasude an e al. (2002) obse ed a p e -
e en ial adso p ion o he he bicide quinme ac on i on oxides such
as hema i e and goe hi e o e Al oxides; howe e , he he bicide
2,4-D did no show any selec i i y. These au ho s sugges ed ha
o he addi ional mechanisms on quinme ac adso p ion we e ope a -
ing, and a ionalized he highe p e e ence o e Fe oxides on he con-
ibu ion be ween he he e ocyclic N and Fe (III) in he o ma ion o
co alen bond. The he bicides IMZQ and quinme ac ha e analogous
chemical s uc u es; bo h o hem a e quinoline-ca boxylic acids,
sugges ing simila adso p ion mechanisms. Ma co-B own e al.
(2012) obse ed simila coo dina ion o he py idinic ni ogen o
he he bicide piclo am wi h he su ace i on cen e s on Fe PILC.
The esul s o his s udy also poin ed ou o a p e e en ial adso p-
ion mechanism o IMZQ on Fe PILCs h ough o ma ion o inne -
sphe e complexes. Leone e al. (2001) a ibu ed o a ligand exchange
mechanism he adso p ion o imidazolinone he bicides on he i on
oxide e ihyd i e. Bo h mechanisms can be ope a ing on Fe PILC
which pe mi s o explain he high he bicide a fini y compa ed o Al
PILC as no iced in he high adso p ion alues and low deso p ion
pe cen s.
E idence o he mechanisms in ol ed in he adso p ion o he he -
bicide on he Fe PILC was pa ly suppo ed by IR spec oscopy (Fig. 4).
The spec a o he he bicide showed abso p ion bands a 1732 and
1694 cm
−1
due o ca bonyl s e ching ib a ions o he ca boxylic
and ke one moie ies, espec i ely; mul iple ing ib a ions a ising
mainly om he quinoline moie y be ween 1650 and 1300 cm
−1
(1643, 1563, 1487, 1450, 1402, 1365, 1315, 1290 cm
−1
); C H
in-plane bending ib a ions in he 1300–1050 cm
−1
ange (specifi-
cally, 1268, 1209 and 1123 cm
−1
), C H ou -o -plane bending ib a-
ions below 1000 cm
−1
(a 982, 858, 799 cm
−1
) and C H wagging
coupled wi h a ing ib a ion a 758 cm
−1
(Bajpai e al., 2000;
Kum u e al., 2012; Ozël e al., 2001). In he Fe PILC (Fig. 4b), he po-
si ion and assignmen o he main abso p ion bands we e (Qin e al.,
2010; Yuan e al., 2008): 1636 cm
−1
o OH bending o wa e ;
1013 cm
−1
o Si O s e ching ib a ion; 916 cm
−1
o Al Al OH
de o ma ion; and 882 and 796 cm
−1
o Si O ib a ions o some
qua z impu i ies o he aw mine al. The IR spec um a e adso p-
ion o he he bicide (Fig. 4c) showed some ea u es sugges ing he
in ol emen o N-dono ligand and o ma ion o inne -sphe e com-
plexes: i) Fe–N coo dina ion h ough he quinoline moie y we e e-
po ed by Özel e al. (2001) o yield upwa d shi s o mos o he
ing ib a ions be ween 4 and 22 cm
−1
as in Fig. 4c (1457, 1408,
1369, 1329, 1297 cm
−1
); and ii) he absence o he ing ib a ion
bands a 1643 and 1563 cm
−1
o he p is ine he bicide (Fig. 4a)
which a e associa ed o p o ona ed quinoline ni ogen (quinolinium
moie ies) (Pusino e al., 2003) and used as a finge p in o de e mi-
na ion o B öns ed acid si es in clay mine als (Co ma e al., 1993), also
sugges ed coo dina ion o he N a om o he quinoline ing o Fe cen-
e s. In addi ion, he new abso p ion bands a 1250 and 1188 cm
−1
we e due o C O s e ching ib a ions esul ing om he eac ion
o he ca boxylic moie y wi h Fe oxyhyd oxides, simila ly o es e s
o ino ganic alcohols. The lack o de ec ion o he C_O s e ching e-
quency in hese ypes o in e ac ions is due o he ac ha i can a y
wi hin e y wide limi s and he e o e, no ound a he ypical ca -
bonyl equencies o no mal sa u a ed es e s wi h o ganic alcohols
(1750–1730 cm
−1
)(Bellamy, 1975). These esul s also poin ou o -
ma ion o inne -sphe e complexes o he he bicide h ough i s ca -
boxylic moie y o Fe pilla s.
3.5. Solubili y diag ams o imazaquin in he p esence o cyclodex ins
Solubili y diag ams o IMZQ wi h ou CDs showed a linea in-
c ease in he he bicide solubili y when inc easing CD concen a ion
(Fig. 5). These cu es we e indica ing o ma ion in solu ion o com-
plexes wi hou a defined solubili y limi , which co esponded o A
L
ype acco ding o Higuchi and Conno s classifica ion (Higuchi and
Conno s, 1965). A
L
ype indica es o ma ion o 1:1 inclusion com-
plexes be ween CD and he gues molecule. The condi ional o ma ion
0 20 40 60 80 100 120 140
0
10
20
30
40
50
60
70
Imazaquín adso bed (µmol/g)
Equilib ium concen a ion (µM)
Al-PilC
Fe-0.05-PilC
Fe-0.15-PilC
Fe-0.5-PilC
Fig. 3. Adso p ion iso he ms o imazaquin on PILCs.
Table 3
Pe cen ages o imazaquin deso bed as a unc ion o he concen a ion used.
a
IMZQ added, μM Al PILC Fe-0.05 PILC Fe-0.15 PILC Fe-0.5 PILC
16 75.8 ± 6.1% 80.7 ± 5.4% 83.3 ± 9.0% 52.3 ± 1.0%
64 73.0 ± 5.7% 80.5 ± 3.2% 66.4 ± 2.1% 48.6 ± 0.1%
160 73.4 ± 3.6% 64.5 ± 2.3% 56.6 ± 1.8% 38.5 ± 0.2%
a
Clay mine al concen a ion was 1.6 g/L.
Table 4
Reduc ion pe cen s in imazaquin adso p ion on PILCs in he p esence o se e al elec-
oly es. Imazaquin o anion a io was 1:1.
a
NaCl Na
2
SO
4
Na
3
PO
4
Al PILC 11.01 ± 1.63 6.18 ± 0.57 86.72 ± 1.94
Fe-0.5 PILC 30.42 ± 1.84 74.51 ± 1.37 92.58 ± 3.5
a
The added amoun o he bicide was 160 μM.
386 T. Undabey ia e al. / Applied Clay Science 80–81 (2013) 382–389

cons an s o he complexes we e calcula ed as well as he maximal in-
c emen in he he bicide solubili y (Table 5).
The alues o he appa en s abili y cons an s (Kc) o β-CD and i s
de i a i es we e much la ge han ha o α-CD. The low alue o his
CD can be due o he mo e educed dimensions o i s ca i y, which
would hinde he en ance o he he bicide; he e o e he in e ac ion
mode will be di e en when using β-CD and de i a i es which
p esen a mo e op imal accommoda ion be ween he hyd ophobic
ca i y and he non-pola moie ies o he he bicide.
The highes complexa ion cons an as well as he maximal inc e-
men in IMZQ solubili y occu ed wi h HPβ(up o 8- old o 0.1 M
concen a ion). A simila alue o cons an was obse ed o β-CD
bu he enhanced solubili y o he he bicide was lowe due o i s
lowe solubili y. The enhanced solubili y o he he bicide was also e-
ma kable wi h RAMEβ, wi h solubili y inc emen s up o 6- old o a
0.1 M concen a ion and high complexa ion cons an .
3.6. S udy o imazaquin–cyclodex in inclusion complexes
1
H-NMR spec oscopy is a use ul and powe ul ool which pe mi s
he cha ac e iza ion o complexes in solu ion by moni o ing he
chemical shi s o CD-p o ons and hose o he gues molecule.
Table 6 shows he chemical shi s o he he bicide and o i s inclu-
sion complex wi h RAMEβ. The shi s o CD p o ons we e no possi-
ble o moni o due o he high ee CD concen a ion ela i e o he
ac ion o ming inclusion complexes. Consequen ly, he changes
we e only ollowed in he he bicide spec a whose peaks did no
o e lap wi h hose o he CD.
S udies on inclusion complexes o β-CD and de i a i es showed
shi s o low fields o he gues molecule p o ons which a e in e ac ing
wi hin he CD ca i y (Goyenechea e al., 2001; Lezcano e al., 2003;
Pé ez-Ma ínez e al., 2000). In Table 6, he highes shi was ob ained
o H-4. High shi s we e also obse ed o H-6 and H-7. These ea u es
indica ed in e ac ion o he he bicide ia he quinolinic ing wi h he
CD. Howe e , he shi s o hese a oma ic p o ons we e occu ing a
high field ins ead. Masson e al. (1998) obse ed a simila e ec on
chlo ambucil inclusion wi h β-CD, which was explained on he basis
o he opposi e e ec p oduced by s ong hyd ogen bonding in ol ing
N elec o pai wi h he CD. These da a poin ed ou ha he quinolinic
moie y o he he bicide is pa ially apped wi hin he CD ca i y, wi h
he quinolinic N a om ou side o he ca i y and o ming s ong
H-bonding wi h pola ized wa e molecules o hyd oxyl g oups o he
CD. The small chemical shi s o p o ons loca ed in he imidazolinone
ing and i s subs i uen g oups indica e ha his ing was s aying ou -
side he ca i y. This in e ac ion was ied o find ou which CD p o ons
we e in e ac ing wi h H-4 by pe o ming NOE expe imen s. Howe e ,
he esul s we e unsuccess ul due o he high amoun o non-
complexed CDs. Simila obse a ions we e ob ained o he o he CDs.
3.7. Adso p ion o imazaquin in he p esence o cyclodex ins
In Fig. 3, adso p ion o IMZQ was highes on Fe-0.5 PILC. I s ad-
so p ion was linea and limi ed by he solubili y o he he bicide;
he e o e, his PILC was selec ed o inc ease IMZQ adso p ion in he
1800 1600 1400 1200 1000 800
1297
753
858
916
1006
1081
1150
965
1188
1329
1250
1369
1408
1457
c)
Wa enumbe (cm-1)
1636
882
796
779
916
1013
1116
b)
1636
1290
1315
734
799758
982
1209
858
1268
1123
1365
1450
1487
1402
1044
1563
1643
1694
1732
a)
Fig. 4. FTIR spec a o (a) IMZQ, (b) Fe-0.5-PILC and (c) a e IMZQ so p ion on
Fe-0.5-PILC.
0 20 40 60 80 100
0,0
0,2
0,4
0,6
0,8
1,0
1,2
1,4
1,6
1,8
2,0
Imazaquin concen a ion (mM)
CD concen a ion (mM)
Fig. 5. Phase solubili y diag ams o imazaquin in aqueous solu ions in he p esence o
CD: ( )α-CD, (■)β-CD, ( ) RAMEβand ( )HPβ.
Table 5
Appa en s abili y cons an s (Kc), co ela ion ac o s (R
2
), and solubili y inc ease (Se,
using 0–0.016 M o β-CD and 0–0.1 M o he o he CDs) o he inclusion compounds
ob ained be ween imazaquin and he di e en CDs.
β-CD HPβRAMEβα-CD
K(M
−1
) 71.0 ± 4.7 85.4 ± 2.6 59.2 ± 2.6 11.5 ± 3.4
Se 2.0 8.5 6.3 2.0
R
2
0.960 0.990 0.981 0.966
Table 6
Chemical shi s o ee imazaquin and RAMEβ: IMZQ complexes om
1
H-NMR
measu emen s (500 MHz, DMSO).
P o on Signal δ(IMZQ) δ(RAMEβ–IMZQ) Δδ
H-4 Single 8.927 8.845 −0.082
H-6 Double double 8.227 8.187 −0.040
H-7 Mul iple 7.972 7.927 −0.045
H-8 Mul iple 7.803 7.772 −0.031
H-9 Double double 8.169 8.144 −0.025
CH
3
Single 1.275 1.254 −0.021
CH(CH
3
)
2
Double 1.021 1.015 −0.006
CH(CH
3
)
2
Double 0.863 0.865 +0.002
CH(CH
3
)
2
Mul iple 1.960 1.949 −0.011
387T. Undabey ia e al. / Applied Clay Science 80–81 (2013) 382–389
p esence o CD. Adso p ion o he he bicide om CD–IMZQ would
p omo e he amoun o adso bed he bicide by enhancemen o
IMZQ solubili y. The CD would be only ac ing as a solubilizing agen
o inc ease he ac i e ing edien con en in he PILC-based o mula-
ions. The CDs used we e only RAMEβand HPβbecause hei he bi-
cide solubili y inc emen s a e he la ges (Table 5).
Adso p ion o he he bicide om CD–IMZQ complexes inc eased
la gely he amoun o he bicide adso bed compa ed o i s adso p ion
in he absence o CD (Fig. 6). He bicide adso p ion inc eased by 42% in
he p esence o RAMEβ. Smalle inc emen s we e ob ained o HPβ,
which is in good ag eemen wi h i s highe complexa ion cons an .
The CD in solu ion is compe ing wi h he so p ion si es on he Fe
PILC o IMZQ, impeding a la ge adso p ion. Adso p ion o bo h CD
on Fe PILC was de e mined o be negligible.
3.8. Release s udies
Fig. 7 shows he elu ion cu es o he comme cial o mula ion
Scep e as well as hose o Fe-0.5 PILC p epa ed in he p esence o
CD. A e 14 i iga ions, he amoun eleased om he o al applied
was 87.8 ± 3.1% o he comme cial o mula ion. The high elu ion
ob ained in his sandy soil wi h he comme cial o mula ion ag ees
wi h he s udy by Undabey ia e al. (2004) who de e mined ha ad-
so p ion o he he bicide on his soil mainly occu ed h ough he o -
ganic ma e , om which deso bed easily. A e 14 i iga ions, he
o al amoun s eleased om he o al applied we e 40.2 ± 6.7 and
47.4 ± 4.8% o hose p epa ed, espec i ely, wi h RAMEβand HPβ,
amoun ing o a significan educ ion in elease o 54 and 46%, espec-
i ely, compa ed o he comme cial o mula ion.
4. Conclusions
Fe PILCs we e syn hesized o hedesign o slow elease o mula ions
o he he bicide IMZQ. The app oach used was he high a fini y o his
he bicide obse ed o i on oxide su aces; he e o e, an enhanced ad-
so p ion o he he bicide on i on-based clay mine als which pa alleled
a slow elease could be achie ed. Fe PILCs we e syn hesized and cha ac-
e ized. XRD and po osi y measu emen s we e in ag eemen wi h p e i-
ous s udies indica ing a mesopo ous s uc u e o med by coagg ega ion
o i on oxide clus e s wi h clay mine al delamina ed laye s. Unless igh
binding mechanisms a e ope a ing, a la ge po e will acili a e he in e -
ac ion o he he bicide wi h i on nodulesand also IMZQ deso p ion om
he Fe PILCs. Compe i i e adso p ion o anions showed ha IMZQ
was adso bed mainly by inne -sphe e complexa ion; howe e , o he
mechanisms may be ac ing. Inne -sphe e complexa ion was also sup-
po ed by IR spec oscopy.
The inc ease in he loading o he bicide on clay mine als o p epa-
a ion o o mula ions is usually hinde ed by he he bicide solubili y.
This is o e come by he use o solubilizing agen s, usually su ac an s.
Howe e , he use o CDs, which a e non- oxic, biodeg adable chemicals,
is a good al e na i e. IMZQ solubili y was g ea ly enhanced in he p es-
ence o CD, by he o ma ion o inclusion complexes. The use o hese
complexes inc eased he amoun o IMZQ adso bed on he clay mine al
up o 42%. Release o he he bicide in sandy soil om o mula ions p e-
pa ed om CD–IMZQ complexes was e a ded by 1/2- old compa ed o
he comme cial o mula ion Scep e .
Acknowledgmen s
This esea ch was suppo ed by he MEC P ojec CTM2009-07425
and he Jun a de Andalucía P ojec P09-RNM4581. Bo h p ojec s e-
cei ed unding by he Eu opean Social Fund. The au ho s acknowledge
he CITIUS se ice om he Uni e si y o Se ille o he NMR acili ies.
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0 200 400 600 800 1000 1200
0
10
20
30
40
50
60
70
80
90
100
110
120
130
Imazaquin adso bed (µmol/g)
Equilib ium concen a ion (µM)
Fig. 6. Adso p ion iso he ms o imazaquin on Fe-0.5-PILC in he absence (■) and
p esence o RAMEβ() and HPβ( ).
0 2 4 6 8 10121416
0
5
10
15
20
25
30
35
40
Imazaquin elu ed (% o he applied)
Numbe o i iga ions
Scep e
Fe-0.5-PilC-HP-ß-CD
Fe-0.5-PilC-RAMEB-CD
Fig. 7. He bicide elease om he comme cial and Fe PILC o mula ions.
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