14 research outputs found
A procedure to assess the importance of chemical kinetics in the humic-mediated transport of radionuclides in radiological performance assessment calculations
Previous work has shown that humic substances can bind metal ions in two
fractions: the exchangeable, where it is available instantaneously for reaction with
other sinks (such as mineral surfaces); and the non-exchangeable, from which it may
only dissociate slowly. In the absence of metal ion/humic/mineral surface ternary
complexes, if the dissociation rate is slow compared to the solution residence time in
the groundwater column, then metal in the non-exchangeable will have a
significantly higher mobility than that in the exchangeable. The critical factor is the
ratio of the non-exchangeable first order dissociation rate constant and the residence
time in the groundwater column, metal ion mobility increasing with decreasing rate
constant.
Sorption of humic/metal complexes at mineral surfaces may reduce mobility.
In addition to direct retardation, sorption also increases the residence time of the
non-exchangeable fraction, giving more time for dissociation and immobilisation.
The magnitude of the effect depends upon the concentrations of the mineral surface
humic binding sites and the humic in solution, along with the magnitudes of the
equilibrium constant and the forward and backward rate constants.
The non-exchangeable dissociation reaction and the sorption reaction may be
classified in terms of two Damkohler numbers, which can be used to determine the
importance of chemical kinetics during transport calculations. These numbers could
be used to determine when full chemical kinetic calculations are required for a
reliable prediction, and when equilibrium may be assumed, or when the reactions
are sufficiently slow that they may be ignored completely
The role of humic non-exchangeable binding in the promotion of metal ion
Metal ions form strong complexes with humic substances. When the metal ion is first complexed
by humic material, it is bound in an ‘exchangeable’ mode. The metal ion in this fraction is
strongly bound, however, if the metal–humic complex encounters a stronger binding site on a
surface, then the metal ion may dissociate from the humic substance and be immobilised.
However, over time, exchangeably-bound metal may transfer to a ‘non-exchangeable’ mode.
Transfer into this mode and dissociation from it are slow, regardless of the strength of the
competing sink, and so immobilisation may be hindered. A series of coupled chemical transport
calculations has been performed to investigate the likely effects of non-exchangeable binding upon
the transport of metal ions in the environment. The calculations show that metal in the nonexchangeable
mode will have a significantly higher mobility than that in the exchangeable mode.
The critical factor is the ratio of the non-exchangeable first-order dissociation rate constant and
the residence time in the groundwater column, metal ion mobility increasing with decreasing rate
constant. A second series of calculations has investigated the effect of the sorption to surfaces of
humic/metal complexes on the transport of the non-exchangeably bound metal. It was found that
such sorption may reduce mobility, depending upon the humic fraction to which the metal ion is
bound. For the more weakly sorbing humic fractions, under ambient conditions (humic
concentration etc.) the non-exchangeable fraction may still transport significantly. However, for
the more strongly sorbed fractions, the non-exchangeable fraction has little effect upon mobility.
In addition to direct retardation, sorption also increases the residence time of the nonexchangeable
fraction, giving more time for dissociation and immobilisation. The nonexchangeable
dissociation reaction, and the sorption reaction have been classified in terms of two
Damkohler numbers, which can be used to determine the importance of chemical kinetics during
transport calculations. These numbers have been used to develop a set of rules that determine
when full chemical kinetic calculations are required for a reliable prediction, and when
equilibrium may be assumed, or when the reactions are sufficiently slow that they may be ignored
completely
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Plutonium(IV) Sorption during Ferrihydrite Nanoparticle Formation
Understanding interactions between iron (oxyhydr)oxide nanoparticles and plutonium is essential to underpin technology to treat radioactive effluents, in cleanup of land contaminated with radionuclides, and to ensure the safe disposal of radioactive wastes. These interactions include a range of adsorption, precipitation, and incorporation processes. Here, we explore the mechanisms of plutonium sequestration during ferrihydrite precipitation from an acidic solution. The initial 1 M HNO3 solution with Fe(III)((aq)) and Pu-242(IV)((aq)) underwent controlled hydrolysis via the addition of NaOH to pH 9. The majority of Fe(III)((aq)) and Pu(IV)((aq)) was removed from solution between pH 2 and 3 during ferrihydrite formation. Analysis of Pu-ferrihydrite by extended X-ray absorption fine structure (EXAFS) spectroscopy showed that Pu(IV) formed an inner-sphere tetradentate complex on the ferrihydrite surface, with minor amounts of PuO2 present. Best fits to the EXAFS data collected from Pu-ferrihydrite samples aged for 2 and 6 months showed no statistically significant change in the Pu(IV)-Fe oxyhydroxide surface complex despite the ferrihydrite undergoing extensive recrystallization to hematite. This suggests the Pu remains strongly sorbed to the iron (oxyhydr)oxide surface and could be retained over extended time periods.Peer reviewe
Bovine cryptosporidiosis: impact, host-parasite interaction and control strategies
International audienceAbstractGastrointestinal disease caused by the apicomplexan parasite Cryptosporidium parvum is one of the most important diseases of young ruminant livestock, particularly neonatal calves. Infected animals may suffer from profuse watery diarrhoea, dehydration and in severe cases death can occur. At present, effective therapeutic and preventative measures are not available and a better understanding of the host–pathogen interactions is required. Cryptosporidium parvum is also an important zoonotic pathogen causing severe disease in people, with young children being particularly vulnerable. Our knowledge of the immune responses induced by Cryptosporidium parasites in clinically relevant hosts is very limited. This review discusses the impact of bovine cryptosporidiosis and describes how a thorough understanding of the host–pathogen interactions may help to identify novel prevention and control strategies
The effects of humic substances on the transport of radionuclides: Recent improvements in the prediction of behaviour and the understanding of mechanisms
Some recent developments made during the European Union 6th Framework Integrated Project FUNMIG in the understanding and prediction of behaviour in ternary systems of radionuclides, humic substances and mineral surfaces are described. These developments are placed in the context of the existing literature. The aim is to describe the current understanding of humic substance mediated radionuclide transport as it may be applied to calculations in support of Radiological Performance Assessment. Some improvements in experimental techniques that provide the raw data to calibrate metal ion binding models are explained. The various metal ion binding models that are available are described and contrasted, before the recent development of ternary system models, in particular the Ligand Charge Distribution model that can predict metal ion and humic substance behaviour in ternary systems. The kinetic effects in ternary systems are described along with the models that are used to describe them. Finally, the remaining challenges in making predictions of radionuclide transport for the Radiological Performance Assessment of radioactive waste repositories are discussed. © 2011 Elsevier Ltd. All rights reserve
Kinetic studies of the quartz/sand, Eu3+ and humic acid ternary system
The interactions of Eu3+ ions, humic acid and quartz in ternary system
experiments have been studied. The variations in the amount of humic acid and Eu3+
with time have been determined as a function of humic acid concentration. The
desorption of both humic acid and europium have also been measured. A simple
mathematical model has been developed that is able to predict the behaviour of both
metal ion and humic acid. There is multi-component behaviour in the experiments,
and the modelling suggests that for the sorption step at least, heterogeneity of the
surface binding sites dominates. However, there is hysteresis in the desoprtion
behaviour of the humic, which could be due to chemical and/or size fractionation on
the quartz surface