0045-6535/78/0401--0365~02o00/0
Chemosphere No. 4, PP 365 - 370, 1978. © P e r g a m o n Press Ltd. l ~ i n f e d in Orea'~ Brifain.
ADSORPTION
OF SEVERAL
HERBICIDES AND
BY
ILLITE
Martine TERCE, Station de Science du Sol - I. N . R . A . (Received in France 20 ~ r c h T h e r e are m a n y cult to p r o p o s e s o m e
1978;
MONTMORILLONITE,
KAOLINITE
CLAYS
R.
-Route
CALVET de St Cyr, Versailles - F R A N C E
received in UK for public~%ion 6 April
1978)
publications on clay-herbicide interactions but it is nevertheless diffi-
general rules to describe adsorption o w i n g to the great variability of the \
published data (except for c h a r g e d molecules,
such as paraquat).
Bibliographic studies s h o w
that m o n t m o r i l l o n i t e s have b e e n extensively
studied relative to other clays for w h i c h the follo-
w i n g publications are noteworthy : H A M A K E R
et al (1966) I, W E B E R
NAMARA
and TOTH
and W E E D
(1970) 3 . This lack of k n o w l e d g e leaves u n a n s w e r e d
(1968) z and M a c
several questions con-
cerning the part played by different clays in the soil. It is, therefore, desirable to p r o p o s e s o m e general conclusions on the adsorption of herbicides by clay adsorbants. T h e p u r p o s e of this p a p e r is to present e x p e r i m e n t a l results on the adsorption of several herbicides by an illite, a m o n t m o r i l l o n i t e and a kaolinite and to p r o p o s e s o m e solutions to the p r o b l e m s I - MATERIALS A
AND
e n c o u n t e r e d in this field of research.
METHODS
- Herbicides.
Nine herbicides are studied : Atrazine :2-chloro-4- e t h y l a m i n o triazine,
tentative
Terbutryne
: Z-Methylthio-4-Ethylamino-6-tert.-butylamino-
benzthiazuron : N - ( Z - b e n z o t h i a z o l y l ) - N - M e t h y l - N ' - m e t h y l u r e a , methoxyphenyl)-N,
N-dimethylurea,
-6-isopropylamino-l,?~ 5 i, 3, 5 triazine, M e t h a -
Metoxuron
: N'-(3-chloro-4-
Chlortoluron : N ' - ( 3 - c h l o r o - 4 - m e t h y l p h e n y l )
thylurea, Isoproturon : N'-(4-isopropylphenyl) 3, 5, 6-trichloropicolinic acid, P y r a z o n
- N, N - d i m e t h y l u r e a ,
Pieloram
- N, N - d i m e -
: 4 - amino
: l-phenyl-4-amino-5-chloro-pyridazone,
Napropamide:
N, N -diethyl-Z- (I -naphtalenyloxy)-napr o p a n a m i d e .
Products were
supplied by C I B A G E I G Y , PR OCIDA.
BASF,
BAYER,
RP
Phytosanitaire,
SANDOZ,
This w o r k w a s s p o n s o r e d by Ministate de la Culture et de l']~nvironnement ( F R A N C E ) .
365
-
366
Jo. 4
B - Clays. The clays used are a kaolinite calcium perties
from
Provins
saturated of t h e s e
a montmorillonite
and an illite from
fraction
less
clays are
from
Greece
(TERCE,
CALVET,
Le Puy in Velay (TESSIER,
1974) 4
1 9 7 5 ) 5 . T h e C1- f r e e ,
t h a n Z ~ of e a c h c l a y i s u s e d t h r o u g h o u t
this study.
Some pro-
g i v e n i n t a b l e I. Table I
Montmorillonite
Total s ~r fa_~e Area m g
813
Internal surface Z -1 Area m g
766
External surface 2 -1 Area m g C.E.C. meq/100
g
Chemical composition of b a s a l s u r f a c e
C - Adsorptxon
suspensions adjusted were case,
were were
made always
were
ranging
less
5 to 25
The suspensions centrifuged
at Z0°C.
228 nm (chlortohron),
63
130
104
18
Z7
hydroxyls
w i t h 25 m l of a q u e o u s
oxygene
to g e t v a l u e s
herbicide
and chlortoluron
of m i n e r a l .
than the herbicide
500 m g
for which adsorption
The maximum
solubilities.
solution.
concentrations
in the
T h e p H of t h e s u s p e n s i o n s
of 3, 4. 5, 6. 5 a n d 8. A d s o r p t i o n
(pH 3) a n d f i v e i n i t i a l c o n c e n t r a t i o n s
were
are
isotherms
used in each
~g/cm 3_
were
stirred
The supernatant
at : ZZZ-3 n m ( a t r a z ine),
mixed
with one gramme
in an acid medium
from
58
i n t h e c a s e of n a p r o p a m i d e
with exther HCI or NaOH
determined
130
measurements.
used except
measurement
II!ite
63
oxygene
25 m l o f c l a y s u s p e n s i o n of clay w e r e
Kaolinite
a t 20 ° C i n a t h e r m o s t a t e d solutions
ZZ5 n m ( t e r b u t r y n ) , 241 n m ( i s o p r o t u r o n ) ,
were
analyzed
agitator
f o r 24 h o u r s
by UV s p e c t r o m e t r y
Z44 n m ( m e t o x u r o n ) , ZZ4 n m ( p i c l o r a m ) ,
and then
absorption,
ZZ6 n m ( m e t h a b e n z t h i a z u r o n ~ 228 nm (pyrazon),
Z16 n m
No. 4
367
(napropamide). II - E X P E R I M E N T A L
RESULTS
T h e a m o u n t s of a d s o r b e d h e r b i c i d e at t h r e e pH v a l u e s a r e g i v e n in t a b l e II. Three substituted ureas
(chlortoluron,
isoproturon,
w h a t e v e r the pH o r the c l a y . F o r the o t h e r h e r b i c i d e s - Montmorillonite~ picloram
the a d s o r p t i o n d e c r e a s e s
Illite
with terbutryn,
in the o r d e r :
napropamide,
and p y r a z o n
- Montmorillonite> - lllit~
Kaolinite>
m e t o x u r o n ) a r e not a d s o r b e d
I11ite~ Kaolinite
Montmorillonite>
Kaolinite
with atrazine with methabenzthiazuron.
The r e s u l t s a l s o s h o w t h a t a d s o r p t i o n i n c r e a s e s
w i t h the m e d i u m a c i d i t y .
T a b l e II A m o u n t s of h e r b i c i d e
a d s o r b e d at d i f f e r e n t pH ( ~ m o l e g - I )
Montmorillonite Herbicides pH pH (initial concentration in the suspension) 2~ 8 - 3 6,5 Atrazine (0, 093 p m / c m 3) Z,8 0
pH 8
Kaolinite pH pH Z, 8 - 3 6,5
0
Terbutryn ( 0 , 0 4 5 ] ~ m / c m 3)
4,3
0,7
Methabenzthia zuron (0, 113 } ~ m / c m 3 )
3,3
0
0
Napr opamide _ (0, 091 p m / c m 5)
1,0
0,4
0,4
Pyrazon (0, 11Z } ~ m / c m 3)
0,8
Picloram (0, 112 } ~ m / c m 3) Phenyl ureas
0
0
Illite pH ~m 8
- 3
pH 6, 5
0,7
3,30
2,2
2,9
5,1
Z,5 0
0
0
Adsorption isotherms in acid conditions (pH.~3) m a y be described by a Freundlich type relation : Q = K C e I/n w h e r e
Q = Amount
adsorbed/unit m a s s of adsorbant
C e = Equilibrium concentration K and I/n = constants.
The v a l u e s of K and I / n a r e g i v e n in t a b l e III.
368,
Igo. 4
T a b l e III Characteristics
of a d s o r p t i o n i s o t h e r m ~ i n a c i d m e d i a . V a l u e s of Q i n u M / c m ~ a n d C e i n ~ M / c m 3.
Terbutryn
87 000
calculated
i
K
1/n
12 000
1/n O, 345
K 1,6
-
1,61
for values
Illite
Kaolinite
Montmorillonite 1/n K 0,78 2-0
Atrazine
of K w e r e
1,60
480
1, 16
L
Methabenzthiazuron
138
Napropamide
1, 10
56
Pyrazon
9
N D
1, 7
-
1,35
-
Picloram
L N D
of t e r b u t r y n
is very
great
N D
20
Adsorption
N D
compared
1
-
to the adsorption
of o t h e r h e r b i c i d e s .
Ill - DISCUSSION A - The main
parameters
The experimental the molecular the medium
properties
have allowed the three
of h e r b i c i d e s ,
properties
The molecular the dipolar
following parameters
the physico-chemical
properties
to b e v a r i e d :
of t h e a d s o r b a n t s
and
Among
( p K a = 4, 3),
or less
atrazine
c u l t to p r e d i c t
involved in adsorption
and polarizability
ionized
at pH values
of h e r b i c i d e
surface
properties
are
different
organic
molecules
may be variable.
crystal
essentially either
the ionizacoordination
bonds.
t h a n 3.
These
from
which allow are terbutryn
this point,
it i s d i f f i -
on clay s u r f a c e s .
structures
and chemical
as a consequence,
W h i l e it i s e a s y to p r e d i c t
very difficult to forecast
constants
of c l a y s u r f a c e s
( s e e t a b l e I) a n d ,
bonds and hydrogen
have ionization
( p K a = 3, 5). A p a r t
molecules
properties
clays have different
three
e q u a l to o r g r e a t e r
( p K a = 1, 67) a n d p i c l o r a m
the behaviour
The three
as coordination
are
a s w e l l a s t h e a b i l i t y to f o r m
used in this study,
b - The physico-chemical
on the contrary,
phenomena
bonds.
the molecules
to be m o r e
of h e r b i c i d e s
properties
character
bonds or hydrogen
them
conditions
acidity.
a - Molecular
bility,
of a d s o r p t i o n _
the characteristics
composition.
their
Their
a b i l i t y to a d s o r b
ion exchange
behaviours,
of o t h e r k i n d s of i n t e r a c t i o n s
it i s , such
369
~lo. 4
c - Medium
acidity.
Two phenomena is increased
:
t a k e p l a c e w h e n t h e a c i d i t y of a n h e r b i c i d e - c l a y
- ionization
of the herbicide
- aluminization variations
of the s u r f a c e
account
(TERGE,
system
molecules
of t h e c l a y ( M I L L E R ,
1965) 6 , J A C K S O N
(1960) 7 ) which produces
properties.
Since aluminum herbicides
suspension
and aluminum
CALVET,
hydroxides
1977 ; C A L V E T .
play an important TERCE,
p a r t in the a d s o r p t i o n
1977) 8 ' 9 i t
is necessary
of
to t a k e i n t o
the e f f e c t of the acidity on the clay adsorb a nt. B - Clay-herbicide
interactions.
a - Ionic bonds. These
are likely
all the molecules For
are anionic
the two triazines
of a tra z i n e
to b e p r e s e n t
a t pH v a l u e s
the adsorption
molecules
with picloram,
is closely
is also maximum
related
by several
ted adsorption
an ion exchange
sating
to
- either
molecules
are
authors
organic
w o u l d be e x p e c t e d .
Thus,
1966 , BAILEY,
protonated
the f o r m e r ,
A t p H v a l u e of Z, 9,
of i o n i z e d m o l e c u l e s .
(WEBBER,
between
protonated_
For
6~
it c a n b e s e e n i n This conclusion
1 9 6 8 ) 10' 12 w h o a t t r i b u -
molecules
and compa-
cations, - or a protonation
surfaces
(MORTLAND, b - Other Polar
description organic
in acid conditions.
to t h e n u m b e r
has been given previously
and terbutryn.
o f 6, 5 a n d 8 s o t h a t n o a d s o r p t i o n
a n d 96 ~ of t e r b u t r y n
t a b l e II t h a t a d s o r p t i o n
atrazine
water
1 9 7 5 ) 1Z'
d u e to t h e h y d r a t i o n
water
on clay
13
may exist but the experimental
Due to aluminization,
through
coordination
the surface
aluminum
bonds as has been supposed TERCE,
results cations
do not a l l o w any can interact
for the adsorption
with
of m e t h a -
1 9 7 7 ) 9 . T h i s k i n d of b o n d i s a l s o p o s s i b l e
and pyrazon.
Hydrogen
(CALVET,
forces
b y A1 a n d F e c l a y s ( C A L V E T ,
with napropamide
-
TERCE,
molecules
bonds.
and non-polar
molecules
benzthiazuron
1968 ; C A L V E T ,
possible
to b e g i v e n .
of the organic
bonds are equally molecules
TERCE,
possible
on clay surface.
1 9 7 5 ) 13 .
with : This was described
for atrazine
adsorbed
onAl-clay
No. 4
370
-
surface h y d r o x y l groups of kaolinite as have b e e n p r o p o s e d for the adsorption of
picloram (CHEUNG,
1973) 14 .
IV - C O N C L U S I O N M o n t m o r i l l o n i t e has, generally, a greater adsorption capacity than kaolinite and illite, but adsorption is a l w a y s very small in neutral m e d i u m .
T h r o u g h aluminization,
lies the clay properties and has a very great effect on adsorption_ played by the ionization of molecules, picloram,
O w i n g to the d o m i n a n t part
it is possible to a p p r o x i m a t e l y describe the adsorption of
atrazine and terbutryn in acid m e d i a _
one is limited to hypothesis
the acidity m o d i
F o r other conditions, and for other herbicides,
pertinent to the adsorption m e c h a n i s m s
f r o m a q u e o u s solutions.
Finally, no clear relations b e t w e e n adsorption and clay properties (surface area, C . E . C . . . ) can be proposed. T h e nature of the present results and the great variability of published results strongly indicate that adsorption is probably m a i n l y due to surface impurities such as A 1 or F e oxy-hydrc> xides. A s a consequence,
it a p p e a r s that the description of herbicide adsorption by clays depends
on the possibility of characterizing these impurities_
Further,
it m a y
be postulated that the clay
content of a soil, b a s e d on a g r a n u l o m e t r i c analysis, is nearly a l w a y s of no use in the study and description of adsorption. REFERENCES I. H A M A K E R
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