Journal of Molecular Catalysis A: Chemical 401 (2015) 13–17
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Journal of Molecular Catalysis A: Chemical
jou rn al hom epage: www.elsevier.com/locate/molcata
Heterogeneous catalysis
Alkaline hydrolysis of vinclozolin: Effect of humic acids
aggregates in water
J. Morales
a,∗
, A. Cid
b
, J.C. Mejuto
a
a
Department of Physical Chemistry, Faculty of Sciences, University of Vigo, 32004 Ourense, Spain
b
Chemistry Department, REQUIMTE-CQFB, Faculty of Science and Technology, New University of Lisbon, 2829-51-6 Monte da Caparica, Portugal
a r t i c l e i n f o
Article history:
Received 25 September 2014
Received in revised form 15 February 2015
Accepted 16 February 2015
Available online 19 February 2015
Keywords:
Vinclozolin
Humate aggregates
Colloids
Humic substances
Hydrolysis
a b s t r a c t
The influence of natural organic substances as humate colloidal aggregates in water solutions upon
the chemical stability of vinclozolin has been investigated in basic media. A large inhibition (9 times-
fold) has been observed and it has been rationalized in terms of a micellar pseudophase model. The
observed behaviour could increase significantly the half-life of this fungicide. Moreover, these experi-
mental results have been compared with the corresponding ones of other substances in these natural
colloidal aggregates.
© 2015 Elsevier B.V. All rights reserved.
1. Introduction
Vinclozolin (V) is a dicarboxamide non-systemic pesticide
(Scheme 1) used to control fungal diseases, blights, rots and
moulds in vineyards (grapes), fruits (strawberries, raspberries
and kiwi), vegetables (snap beans, lettuce and onions) or dif-
ferent types of ornamentals [1–5]. It may also be used on turf
grass for golf courses [6]. Being highly effective against common
fungi caused by Botrytis spp., Sclerotinia spp. or Monilinia spp.
[7–9]. It is well known that this fungicide is moderately per-
sistent in soil [10] and it is only partially broken down by soil
microorganisms [11–13]. Vinclozolin may degrade [14] to 3
′
,5
′
-
dichloro-2-hydroxy-2-methylbut-3-enanilide (see Scheme 1A) or
2-[(3,5-dichlorophenyl)-carbamoyl]oxy-2-methyl-3-butenoic acid
(see Scheme 1B). Both reactions will continue to degrade to a third
degradation product, 3,5-dichloroaniline (see Scheme 1C). In water,
it can be degraded by photolysis and/or hydrolysis processes, which
are favoured under neutral or basic conditions [15]. The acute
median lethal dose (LD
50
) for V is greater than 15,000 mg kg
−1
in
rats [10].
Humic substances, and more specifically humate colloidal
aggregates (HCAs), represent a large portion of organic matter
∗
Corresponding author. Tel.: +34 988 387031; fax: +34 988 387001.
E-mail addresses: morales@uvigo.es (J. Morales), acids@uvigo.es (A. Cid),
xmejuto@uvigo.es (J.C. Mejuto).
in natural environments and soils [16,17]. In fact, these organic
colloids include highly decomposed organic matter generally more
known as humus. Their nature as colloids and their behaviour in
solution is quite similar to the micellar aggregates [18–20]. Their
ability to absorb or adsorb different types of pollutants, both organic
and inorganic, made reconsider the use of these substances from a
chemical point of view, since traditionally they were considered
carriers. The adsorption properties and the respective compart-
mentalization of different substrates by humic substances cause
changes in the chemical reactivity when a reaction occurs in the
presence of these kind of colloidal aggregates [21]. Therefore, to
understand the role that humate aggregates currently have in envi-
ronmental processes, it requires the knowledge of their role from
a chemical kinetic view [22] because they can act as solvents, and
toxic reagents scavengers or natural catalysers. Furthermore, it has
been considered that the primary route of elimination of organic
xenobiotics such as polychlorinated biphenyls (PCBs), polycyclic
aromatic hydrocarbons (PAHs), pesticides or other substances is
related to the microorganism activity found in soil, neglecting the
essential importance of humus. However, the properties of these
humate aggregates and their catalytic capacity can be assumed the
need to consider other means of disposal [23–29].
New insights in the V reactivity, which is widely used in agricul-
ture, on the basis of a pseudophase model, were carried out because
the major composition of the organic matter in soils is HCAs [30]
and, moreover these compounds are also present in some condi-
tions in the natural waters [31]. Thus, the aim of the present work
http://dx.doi.org/10.1016/j.molcata.2015.02.017
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