Aerodynamic drag modeling of alpine skiers performing giant slalom turns.

PURPOSE: Aerodynamic drag plays an important role in performance for athletes practicing sports that involve high-velocity motions. In giant slalom, the skier is continuously changing his/her body posture, and this affects the energy dissipated in aerodynamic drag. It is therefore important to quantify this energy to understand the dynamic behavior of the skier. The aims of this study were to model the aerodynamic drag of alpine skiers in giant slalom simulated conditions and to apply these models in a field experiment to estimate energy dissipated through aerodynamic drag. METHODS: The aerodynamic characteristics of 15 recreational male and female skiers were measured in a wind tunnel while holding nine different skiing-specific postures. The drag and the frontal area were recorded simultaneously for each posture. Four generalized and two individualized models of the drag coefficient were built, using different sets of parameters. These models were subsequently applied in a field study designed to compare the aerodynamic energy losses between a dynamic and a compact skiing technique. RESULTS: The generalized models estimated aerodynamic drag with an accuracy of between 11.00% and 14.28%, and the individualized models estimated aerodynamic drag with an accuracy between 4.52% and 5.30%. The individualized model used for the field study showed that using a dynamic technique led to 10% more aerodynamic drag energy loss than using a compact technique. DISCUSSION: The individualized models were capable of discriminating different techniques performed by advanced skiers and seemed more accurate than the generalized models. The models presented here offer a simple yet accurate method to estimate the aerodynamic drag acting upon alpine skiers while rapidly moving through the range of positions typical to turning technique.

Measurement of absolute cell volume, osmotic membrane water permeability, and refractive index of transmembrane water and solute flux by digital holographic microscopy.

ABSTRACT. A dual-wavelength digital holographic microscope to measure absolute volume of living cells is proposed. The optical setup allows us to reconstruct two quantitative phase contrast images at two different wavelengths from a single hologram acquisition. When adding the absorbing dye fast green FCF as a dispersive agent to the extracellular medium, cellular thickness can be univocally determined in the full field of view. In addition to the absolute cell volume, the method can be applied to derive important biophysical parameters of living cells including osmotic membrane water permeability coefficient and the integral intracellular refractive index (RI). Further, the RI of transmembrane flux can be determined giving an indication about the nature of transported solutes. The proposed method is applied to cultured human embryonic kidney cells, Chinese hamster ovary cells, human red blood cells, mouse cortical astrocytes, and neurons.

Identification of opsA, a gene involved in solute stress mitigation and survival in soil, in the polycyclic aromatic hydrocarbon-degrading bacterium Novosphingobium sp. strain LH128.

The aim of this study was to identify genes involved in solute and matric stress mitigation in the polycyclic aromatic hydrocarbon (PAH)-degrading Novosphingobium sp. strain LH128. The genes were identified using plasposon mutagenesis and by selection of mutants that showed impaired growth in a medium containing 450 mM NaCl as a solute stress or 10% (wt/vol) polyethylene glycol (PEG) 6000 as a matric stress. Eleven and 14 mutants showed growth impairment when exposed to solute and matric stresses, respectively. The disrupted sequences were mapped on a draft genome sequence of strain LH128, and the corresponding gene functions were predicted. None of them were shared between solute and matric stress-impacted mutants. One NaCl-affected mutant (i.e., NA7E1) with a disruption in a gene encoding a putative outer membrane protein (OpsA) was susceptible to lower NaCl concentrations than the other mutants. The growth of NA7E1 was impacted by other ions and nonionic solutes and by sodium dodecyl sulfate (SDS), suggesting that opsA is involved in osmotic stress mitigation and/or outer membrane stability in strain LH128. NA7E1 was also the only mutant that showed reduced growth and less-efficient phenanthrene degradation in soil compared to the wild type. Moreover, the survival of NA7E1 in soil decreased significantly when the moisture content was decreased but was unaffected when soluble solutes from sandy soil were removed by washing. opsA appears to be important for the survival of strain LH128 in soil, especially in the case of reduced moisture content, probably by mitigating the effects of solute stress and retaining membrane stability.

Single-hole GPR reflection imaging of solute transport in a granitic aquifer

Identifying transport pathways in fractured rock is extremely challenging as flow is often organized in a few fractures that occupy a very small portion of the rock volume. We demonstrate that saline tracer experiments combined with single-hole ground penetrating radar (GPR) reflection imaging can be used to monitor saline tracer movement within mm-aperture fractures. A dipole tracer test was performed in a granitic aquifer by injecting a saline solution in a known fracture, while repeatedly acquiring single-hole GPR sections in the pumping borehole located 6 m away. The final depth-migrated difference sections make it possible to identify consistent temporal changes over a 30 m depth interval at locations corresponding to fractures previously imaged in GPR sections acquired under natural flow and tracer-free conditions. The experiment allows determining the dominant flow paths of the injected tracer and the velocity (0.4-0.7 m/min) of the tracer front. Citation: Dorn, C., N. Linde, T. Le Borgne, O. Bour, and L. Baron (2011), Single-hole GPR reflection imaging of solute transport in a granitic aquifer, Geophys. Res. Lett., 38, L08401, doi: 10.1029/2011GL047152.

Exposure to solute stress affects genome-wide expression but not the polycyclic aromatic hydrocarbon-degrading activity of Sphingomonas sp. strain LH128 in biofilms.

Members of the genus Sphingomonas are important catalysts for removal of polycyclic aromatic hydrocarbons (PAHs) in soil, but their activity can be affected by various stress factors. This study examines the physiological and genome-wide transcription response of the phenanthrene-degrading Sphingomonas sp. strain LH128 in biofilms to solute stress (invoked by 450 mM NaCl solution), either as an acute (4-h) or a chronic (3-day) exposure. The degree of membrane fatty acid saturation was increased as a response to chronic stress. Oxygen consumption in the biofilms and phenanthrene mineralization activities of biofilm cells were, however, not significantly affected after imposing either acute or chronic stress. This finding was in agreement with the transcriptomic data, since genes involved in PAH degradation were not differentially expressed in stressed conditions compared to nonstressed conditions. The transcriptomic data suggest that LH128 adapts to NaCl stress by (i) increasing the expression of genes coping with osmolytic and ionic stress such as biosynthesis of compatible solutes and regulation of ion homeostasis, (ii) increasing the expression of genes involved in general stress response, (iii) changing the expression of general and specific regulatory functions, and (iv) decreasing the expression of protein synthesis such as proteins involved in motility. Differences in gene expression between cells under acute and chronic stress suggest that LH128 goes through changes in genome-wide expression to fully adapt to NaCl stress, without significantly changing phenanthrene degrading activity.

Identification of genes potentially involved in solute stress response in Sphingomonas wittichii RW1 by transposon mutant recovery.

The term water stress refers to the effects of low water availability on microbial growth and physiology. Water availability has been proposed as a major constraint for the use of microorganisms in contaminated sites with the purpose of bioremediation. Sphingomonas wittichii RW1 is a bacterium capable of degrading the xenobiotic compounds dibenzofuran and dibenzo-p-dioxin, and has potential to be used for targeted bioremediation. The aim of the current work was to identify genes implicated in water stress in RW1 by means of transposon mutagenesis and mutant growth experiments. Conditions of low water potential were mimicked by adding NaCl to the growth media. Three different mutant selection or separation method were tested which, however recovered different mutants. Recovered transposon mutants with poorer growth under salt-induced water stress carried insertions in genes involved in proline and glutamate biosynthesis, and further in a gene putatively involved in aromatic compound catabolism. Transposon mutants growing poorer on medium with lowered water potential also included ones that had insertions in genes involved in more general functions such as transcriptional regulation, elongation factor, cell division protein, RNA polymerase β or an aconitase.

Dynamic drag modeling of submerged aquatic vegetation canopy flows

Vegetation has a profound effect on flow and sediment transport processes in natural rivers, by increasing both skin friction and form drag. The increase in drag introduces a drag discontinuity between the in-canopy flow and the flow above, which leads to the development of an inflection point in the velocity profile, resembling a free shear layer. Therefore, drag acts as the primary driver for the entire canopy system. Most current numerical hydraulic models which incorporate vegetation rely either on simple, static plant forms, or canopy-scaled drag terms. However, it is suggested that these are insufficient as vegetation canopies represent complex, dynamic, porous blockages within the flow, which are subject to spatially and temporally dynamic drag forces. Here we present a dynamic drag methodology within a CFD framework. Preliminary results for a benchmark cylinder case highlight the accuracy of the method, and suggest its applicability to more complex cases.

Atrial natriuretic peptides: reproducibility of renal effects and response of liver blood flow.

To assess the variability of the response to exogenous atrial natriuretic peptide (ANP), it was infused at the rate of 1 microgram/min for 2 h in 6 salt-loaded normal volunteers under controlled conditions on 2 occasions at an interval of 1 week. The effect on solute excretion and the haemodynamic and endocrine actions were highly reproducible. The constant ANP infusion caused a delayed and prolonged excretion of sodium, chloride and calcium, no change in potassium or phosphate excretion or in glomerular filtration rate but a marked decrease in renal plasma flow. Blood pressure, heart rate and the plasma levels of angiotensin II, aldosterone, arginine vasopressin and plasma renin activity were unaltered. The effect of a 2-h infusion of ANP 0.5 microgram/min or its vehicle on apparent hepatic blood flow (HBF) was also studied in 14 normal volunteers by measuring the indocyanine green clearance. A 21% decrease in HBF was observed in subjects who received the ANP infusion (p less than 0.01 vs vehicle). Thus, ANP infused at a dose that did not lower blood pressure decreased both renal and liver blood flow in normotensive volunteers. The renal and endocrine responses to ANP were reproducible over a 1-week interval.

Hydrogeophysical data integration at larger scales: Application of Bayesian sequential simulation for the characterization of heterogeneous alluvial aquifers

Knowledge of the spatial distribution of hydraulic conductivity (K) within an aquifer is critical for reliable predictions of solute transport and the development of effective groundwater management and/or remediation strategies. While core analyses and hydraulic logging can provide highly detailed information, such information is inherently localized around boreholes that tend to be sparsely distributed throughout the aquifer volume. Conversely, larger-scale hydraulic experiments like pumping and tracer tests provide relatively low-resolution estimates of K in the investigated subsurface region. As a result, traditional hydrogeological measurement techniques contain a gap in terms of spatial resolution and coverage, and they are often alone inadequate for characterizing heterogeneous aquifers. Geophysical methods have the potential to bridge this gap. The recent increased interest in the application of geophysical methods to hydrogeological problems is clearly evidenced by the formation and rapid growth of the domain of hydrogeophysics over the past decade (e.g., Rubin and Hubbard, 2005).

Capsule permeability via polymer and protein ingress/egress.

Static incubation tests, where microcapsules and beads are contacted with polymer and protein solutions, have been developed for the characterization of permselective materials applied for bioartificial organs and drug delivery. A combination of polymer ingress, detected by size-exclusion chromatography, and protein ingress/ egress, assessed by gel electrophoresis, provides information regarding the diffusion kinetics, molar mass cutoff(MMCO) and permeability. This represents an improvement over existing permeability measurements that are based on the diffusion of a single type of solute. Specifically, the permeability of capsules based on alginate, cellulose sulfate, polymethylene-co-guanidine were characterized as a function of membrane thickness. Solid alginate beads were also evaluated. The MMCO of these capsules was estimated to be between 80 and 90 kDa using polymers, and between 116-150 kDa with proteins. Apparently, the globular shape of the proteins (radius of gyration (Rg) of 4.2-4.6 nm) facilitates their passage through the membrane, comparatively to the polysaccharide coil conformation (Rg of 6.5-8.3 nm). An increase of the capsule membrane thickness reduced these values. The MMCO of the beads, which do not have a membrane limiting their permselective properties, was higher, between 110 and 200 kDa with dextrans, and between 150 and 220 kDa with proteins. Therefore, although the permeability estimated with biologically relevant molecules is generally higher due to their lower radius of gyration, both the MMCO of synthetic and natural watersoluble polymers correlate well, and can be used as in vitro metrics for the immune protection ability of microcapsules and microbeads. This article shows, to the authors' knowledge, the first reported concordance between permeability measures based on model natural and biological macromolecules.

High-resolution numerical modelling of flow-vegetation interactions

In this paper, we present and apply a new three-dimensional model for the prediction of canopy-flow and turbulence dynamics in open-channel flow. The approach uses a dynamic immersed boundary technique that is coupled in a sequentially staggered manner to a large eddy simulation. Two different biomechanical models are developed depending on whether the vegetation is dominated by bending or tensile forces. For bending plants, a model structured on the Euler-Bernoulli beam equation has been developed, whilst for tensile plants, an N-pendula model has been developed. Validation against flume data shows good agreement and demonstrates that for a given stem density, the models are able to simulate the extraction of energy from the mean flow at the stem-scale which leads to the drag discontinuity and associated mixing layer.

Dibenzofuran degradation by Sphingomonas wittichii RW1 under environmental stresses

Sphingomonas wittichii is a gram-negative Alpha-proteobacterium, capable of degrading xenobiotic compounds such as dibenzofuran (DBF), dibenzo-p-dioxin, carbazole, 2-hydroxybiphenyl or nitro diphenyl ether herbicides. The metabolism of strain RW1 has been the subject of previous studies and a number of genes involved in DBF degradation have been characterized. It is known that RW1 posseses a unique initial DBF dioxygenase (encoded by the dxnAl gene) that catalyzes the first step in the degradation pathway. None of the organisms known to be able to degrade DBF have a similar dioxygenase, the closest match being the DBF dioxygenase from Rhodococcus sp. with an overall amino acid similarity of 45%. Genes participating in the conversion of the metabolite salicylate via the ortho-cleavage pathway to TCA cycle intermediates were identified as well. Apart from this scarce information, however, there is a lack of global knowledge on the genes that are involved in DBF degradation by strain RW1 and the influence of environmental stresses on DBF-dependent global gene expression. A global analysis is necessary, because it may help to better understand the behaviour of the strain under field conditions and suggest improvements for the current bioaugmentation practice. Chapter 2 describes the results of whole-genome analysis to characterize the genes involved in DBF degradation by RW1. Micro-array analysis allowed us to detect differences in gene transcription when strain RW1 was exposed to DBF. This was complemented by ultra-high throughput sequencing of mutants no longer capable of growing on salicylate and DBF. Some of the genes of the ortho-cleavage pathway were induced 2 to 4 times in the presence of DBF, as well as the initial DBF dioxygenase. However two gene clusters, named 4925 and 5102 were induced up to 19 times in response to DBF induction. The cluster 4925 is putatively participating in a meta-cleavage pathway while the cluster 5102 might be part of a gentisate pathway. The three pathways, ortho-cleavage, meta-cleavage and gentisate pathway seem to be active in parallel when strain RW1 is exposed to DBF, presenting evidence for a redundancy of genes for DBF degradation in the genome of RW1. Chapter 3 focuses on exploiting genetic tools to construct bioreporters representative for DBF degradation in RW1. A set of basic tools for genetic manipulation in Sphingomonas wittichii RW1 was tested and optimized. Both plasmids and mini-transposons were evaluated for their ability to be maintained in RW1 with or without antibiotic selection pressure, and for their ability to lead to fluorescent protein expression in strain RW1 from a constitutive promoter. Putative promoter regions of three of the previously found DBF-induced genes (Swit_4925, Swit_5102 and Swit_4897-dxnAl) were then used to construct eg/^-bioreporters in RW1. Chapter 4 describes the use of the constructed RW1-based bioreporter strains for examining the expression of the DBF degradation pathway genes under microcosm conditions. The bioreporter strains were first exposed to different carbon sources in liquid culture to calibrate the egfp induction. Contrary to our expectations from micro-array analysis only the construct with the promoter from gene cluster 4925 responded to DBF, whereas the other two constructs did not show specific induction with DBF. The response from the bioreporters was subsequently tested for sensitivity to water stress, given that this could have an important impact in soils. Exposure to liquid cultures with decreasing water potential, achieved by NaCl or PEG addition to the growth media, showed that eGFP expression in RW1 from the promoter regions 4925 and 5102 was not directly influenced by water stress, but only through an overall reduction in growth rate. In contrast, expression of eGFP from the dxnAl or an uspA promoter was also directly dependent on the extent of water stress. The RW1 with the 4925 construct was subsequently used in soil microcosms to evaluate DBF bioavailability to the cells in presence or absence of native microbiota or other contaminated material. We found that RW1 could grow on DBF added to soil, but bioreporter expression suggested that competition with native microbiota for DBF intermediates may limit its ability to proliferate to a maximum. Chapter 5 describes the results from the experiments carried out to more specifically detect genes of RW1 that might be implicated in water stress resistance. Hereto we created transposon mutagenesis libraries in RW1, either with a classical mini-Tn5 or with a variant that would express egfp when the transposon would insert in a gene induced under water stress. Classical mutant libraries were screened by replica plating under high and low water stress conditions (achieved by adding NaCl to the agar medium). In addition, we screened for smaller microcolonies formed by mutants in agarose beads that could be analized with flow cytometry. A number of mutants impaired to grow on NaCl-supplemented media were recovered and the transposon insertion sites sequenced. In a second procedure we screened by flow cytometry for mutants with a higher eGFP production after exposure to growth medium with higher NaCl concentrations. Mutants from both libraries rarely overlapped. Discovered gene functions of the transposon insertions pointed to compatible solute synthesis (glutamate and proline), cell membrane synthesis and modification of cell membrane composition. The results obtained in the present study give us a more complete picture of the mechanisms of DBF degradation by S. wittichii RW1, how it reacts to different DBF availability and how the DBF catabolic activity may be affected by the conditions found in contaminated environments. - Sphingomonas wittichii est une alpha-protéobactérie gram-négative, capable de dégrader des composés xénobiotiques tels que le dibenzofurane (DBF), la dibenzo-p-dioxine, le carbazole, le 2-hydroxybiphényle ou les herbicides dérivés du nitro-diphényléther. Le métabolisme de la souche RW1 a fait l'objet d'études antérieures et un certain nombre de gènes impliqués dans la dégradation du DBF ont été caractérisés. Il est connu que RW1 possède une unique dioxygénase DBF initiale (codée par le gène dxnAl) qui catalyse la première étape de la voie de dégradation. Aucun des organismes connus pour être capables de dégrader le DBF n'a de dioxygénase similaire. L'enzyme la plus proche étant la DBF dioxygénase de Rhodococcus sp. avec 45% d'acides aminés conservés. Les gènes qui participent à la transformation du salicylate en métabolites intermédiaires du cycle de Krebs par la voie ort/io-cleavage ont aussi été identifiés. Outre ces informations lacunaires, il y a un manque de connaissances sur l'ensemble des gènes impliqués dans la dégradation du DBF par la souche RW1 ainsi que l'effet des stress environnementaux sur l'expression génétique globale, en présence du DBF. Une analyse globale est nécessaire, car elle peut aider à mieux comprendre le comportement de la souche dans les conditions de terrain et de proposer des améliorations pour l'utilisation de la bio-augmentation comme technique de bio-remédiation. Le chapitre 2 décrit les résultats de l'analyse du génome pour caractériser les gènes impliqués dans la dégradation du DBF par RW1. Une analyse de micro-arrays nous a permis de détecter des différences dans la transcription des gènes lorsque la souche RW1 a été exposée au DBF. L'analyse a été complétée par le criblage à ultra-haut débit de mutants qui n'étaient plus capables de croître avec le salicylate ou le DBF comme seule source de carbone. Certains des gènes de la voie ortho-cleavage, dont la DBF dioxygénase initiale, ont xî été induits 2 à 4 fois, en présence du DBF. Cependant, deux groupes de gènes, nommés 4925 et 5102 ont été induits jusqu'à 19 fois en réponse au DBF. Le cluster 4925 participe probablement dans une voie de meta-cleavage tandis que le cluster 5102 pourrait faire partie d'une voie du gentisate. Les trois voies, ortho-cleavage, meta-cleavage et la voie du gentisate semblent être activées en parallèle lorsque la souche RW1 est exposée au DBF, ce qui représente une redondance de voies pour la dégradation du DBF dans le génome de RW1. Le chapitre 3 se concentre sur l'exploitation des outils génétiques pour la construction de biorapporteurs de la dégradation du DBF par RW1. Un ensemble d'outils de base pour la manipulation génétique dans Sphingomonas wittichii RW1 a été testé et optimisé. Deux plasmides et mini-transposons ont été évalués pour leur capacité à être maintenu dans RW1 avec ou sans pression de sélection par des antibiotiques, et pour leur capacité à exprimer la protéine fluorescente verte (eGFP) dans la souche RW1. Les trois promoteurs des gènes Swit_4925, Swit_5102 et Swit_4897 (dxnAl), induits en réponse au DBF, ont ensuite été utilisés pour construire des biorapporteurs dans RW1. Le chapitre 4 décrit l'utilisation des souches biorapportrices construites pour l'analyse de l'expression des gènes de la voie de dégradation du DBF dans des microcosmes avec différents types de sols. Les souches biorapportrices ont d'abord été exposées à différentes sources de carbone en cultures liquides afin de calibrer l'induction de la eGFP. La construction avec le promoteur du gène 4925 a permis une réponse au DBF. Mais contrairement à nos attentes, basées sur les résultats de l'analyse des micro-arrays, les deux autres constructions n'ont pas montré d'induction spécifique au DBF. La réponse des biorapporteurs a ensuite été testée pour la sensibilité au stress hydrique, étant donné que cela pourrait avoir un impact important dans les microcosmes. La diminution du potentiel hydrique en culture liquide est obtenue par addition de NaCl ou de PEG au milieu de croissance. Nous avons montré que l'expression de la eGFP contrôlée par les promoteurs 4925 et 5102 n'était pas directement influencée par le stress hydrique, mais seulement par une réduction globale des taux de croissance. En revanche, l'expression de la eGFP dépendante des promoteurs dxnAl et uspA était aussi directement dépendante de l'ampleur du stress hydrique. La souche avec la construction 4925 a été utilisée par la suite dans des microcosmes avec différents types de sols pour évaluer la biodisponibilité du DBF en présence ou absence des microbes indigènes et d'autres composés contaminants. Nous avons constaté que RW1 pouvait se développer si le DBF a été ajouté au sol, mais l'expression de la eGFP par le biorapporteur suggère que la compétition avec la microbiota indigène pour les métabolites intermédiaires du DBF peut limiter sa capacité à proliférer de manière optimale. Le chapitre 5 décrit les résultats des expériences réalisées afin de détecter spécifiquement les gènes de RW1 qui pourraient être impliquées dans la résistance au stress hydrique. Ici on a crée des bibliothèques de mutants de RW1 par transposon, soit avec un mini-Tn5 classique ou avec une variante qui exprime la eGFP lorsque le transposon s'insère dans un gène induit par le stress hydrique. Les bibliothèques de mutants ont été criblées par la méthode classique de repiquage sur boîtes, dans des conditions de stress hydrique élevé (obtenu par l'addition de NaCl dans les boîtes). En outre, nous avons criblé des micro¬colonies dans des billes d'agarose qui ont pu être analysées par cytométrie de flux. Un certain nombre de mutants déficients à croître sur des milieux supplémentés avec du NaCl ont été isolés et les sites d'insertion du transposon séquencés. Dans une deuxième procédure nous avons criblé par cytométrie de flux des mutants avec une production de eGFP supérieure, après exposition à un milieu de croissance avec une concentration élevée de NaCl. Les mutants obtenus dans les deux bibliothèques n'étaient pas similaires. Les fonctions des gènes où se trouvent les insertions de transposons sont impliqués dans la synthèse de solutés compatibles (glutamate et de la proline), dans la synthèse de la membrane cellulaire et dans la modification de la composition de la membrane cellulaire. Les résultats obtenus dans la présente étude nous donnent une image plus complète des mécanismes de dégradation du DBF par S. wittichii RW1, comment cette souche réagit à la disponibilité du DBF et comment l'activité catabolique peut être affectée par les conditions rencontrées dans des environnements contaminés.

Regional-scale integration of multi-scale hydrological and geophysical data using a two-step Bayesian sequential simulation approach

Significant progress has been made with regard to the quantitative integration of geophysical and hydrological data at the local scale for the purpose of improving predictions of groundwater flow and solute transport. However, extending corresponding approaches to the regional scale still represents one of the major challenges in the domain of hydrogeophysics. To address this problem, we have developed a regional-scale data integration methodology based on a two-step Bayesian sequential simulation approach. Our objective is to generate high-resolution stochastic realizations of the regional-scale hydraulic conductivity field in the common case where there exist spatially exhaustive but poorly resolved measurements of a related geophysical parameter, as well as highly resolved but spatially sparse collocated measurements of this geophysical parameter and the hydraulic conductivity. To integrate this multi-scale, multi-parameter database, we first link the low- and high-resolution geophysical data via a stochastic downscaling procedure. This is followed by relating the downscaled geophysical data to the high-resolution hydraulic conductivity distribution. After outlining the general methodology of the approach, we demonstrate its application to a realistic synthetic example where we consider as data high-resolution measurements of the hydraulic and electrical conductivities at a small number of borehole locations, as well as spatially exhaustive, low-resolution estimates of the electrical conductivity obtained from surface-based electrical resistivity tomography. The different stochastic realizations of the hydraulic conductivity field obtained using our procedure are validated by comparing their solute transport behaviour with that of the underlying ?true? hydraulic conductivity field. We find that, even in the presence of strong subsurface heterogeneity, our proposed procedure allows for the generation of faithful representations of the regional-scale hydraulic conductivity structure and reliable predictions of solute transport over long, regional-scale distances.

Use of high-resolution geophysical data to characterize heterogeneous aquifers: influence of data integration method on hydrological predictions

The integration of geophysical data into the subsurface characterization problem has been shown in many cases to significantly improve hydrological knowledge by providing information at spatial scales and locations that is unattainable using conventional hydrological measurement techniques. The investigation of exactly how much benefit can be brought by geophysical data in terms of its effect on hydrological predictions, however, has received considerably less attention in the literature. Here, we examine the potential hydrological benefits brought by a recently introduced simulated annealing (SA) conditional stochastic simulation method designed for the assimilation of diverse hydrogeophysical data sets. We consider the specific case of integrating crosshole ground-penetrating radar (GPR) and borehole porosity log data to characterize the porosity distribution in saturated heterogeneous aquifers. In many cases, porosity is linked to hydraulic conductivity and thus to flow and transport behavior. To perform our evaluation, we first generate a number of synthetic porosity fields exhibiting varying degrees of spatial continuity and structural complexity. Next, we simulate the collection of crosshole GPR data between several boreholes in these fields, and the collection of porosity log data at the borehole locations. The inverted GPR data, together with the porosity logs, are then used to reconstruct the porosity field using the SA-based method, along with a number of other more elementary approaches. Assuming that the grid-cell-scale relationship between porosity and hydraulic conductivity is unique and known, the porosity realizations are then used in groundwater flow and contaminant transport simulations to assess the benefits and limitations of the different approaches.