Relevant bibliographies by topics / Laboratory models

Academic literature on the topic 'Laboratory models'

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Published: 4 June 2021
Last updated: 6 February 2022

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Journal articles on the topic "Laboratory models"

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Semenov, D. A. "MODELS OF EXPERIMENTAL PLEURITE APPLICABLE ON LABORATORY ANIMALS." Amur Medical Journal, no. 3 (2017): 60–61. http://dx.doi.org/10.22448/amj.2017.3.60-61.

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Crider, Steven S., and Benjamin L. Sill. "Simple Groundwater Laboratory Models." Journal of Hydraulic Engineering 115, no. 6 (June 1989): 818–22. http://dx.doi.org/10.1061/(asce)0733-9429(1989)115:6(818).

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Ten Hagen, Timo L. M., and Alexander M. M. Eggermont. "Laboratory models of regional chemotherapy." International Journal of Hyperthermia 24, no. 3 (January 2008): 291–99. http://dx.doi.org/10.1080/02656730701883683.

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Weinberg, Mea A., and Michael Bral. "Laboratory animal models in periodontology." Journal of Clinical Periodontology 26, no. 6 (June 1999): 335–40. http://dx.doi.org/10.1034/j.1600-051x.1999.260601.x.

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Ciardi, A., S. V. Lebedev, C. Stehle, and T. Lery. "Laboratory models for astrophysical jets." Journal de Physique IV (Proceedings) 133 (June 2006): 1043–45. http://dx.doi.org/10.1051/jp4:2006133211.

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LEITCH, A. "Free convection in laboratory models." Earth-Science Reviews 29, no. 1-4 (October 1990): 369–83. http://dx.doi.org/10.1016/0012-8252(90)90049-2.

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Silva, Teane M. A., Erica A. Costa, Tatiane A. Paixão, Renée M. Tsolis, and Renato L. Santos. "Laboratory Animal Models for Brucellosis Research." Journal of Biomedicine and Biotechnology 2011 (2011): 1–9. http://dx.doi.org/10.1155/2011/518323.

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Brucellosis is a chronic infectious disease caused byBrucellaspp., a Gram-negative facultative intracellular pathogen that affects humans and animals, leading to significant impact on public health and animal industry. Human brucellosis is considered the most prevalent bacterial zoonosis in the world and is characterized by fever, weight loss, depression, hepato/splenomegaly, osteoarticular, and genital infections. Relevant aspects ofBrucellapathogenesis have been intensively investigated in culture cells and animal models. The mouse is the animal model more commonly used to study chronic infection caused byBrucella. This model is most frequently used to investigate specific pathogenic factors ofBrucellaspp., to characterize the host immune response, and to evaluate therapeutics and vaccines. Other animal species have been used as models for brucellosis including rats, guinea pigs, and monkeys. This paper discusses the murine and other laboratory animal models for human and animal brucellosis.
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Nair, Dhanya Venugopalan, and A. Gopala Reddy. "Laboratory animal models for esophageal cancer." Veterinary World 9, no. 11 (November 2016): 1229–32. http://dx.doi.org/10.14202/vetworld.2016.1229-1232.

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Gary, Michael Shayne, and Robert E. Wood. "Unpacking mental models through laboratory experiments." System Dynamics Review 32, no. 2 (April 2016): 101–29. http://dx.doi.org/10.1002/sdr.1560.

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Banzett, Robert B., Lewis Adams, Carl R. O'Donnell, Sean A. Gilman, Robert W. Lansing, and Richard M. Schwartzstein. "Using Laboratory Models to Test Treatment." American Journal of Respiratory and Critical Care Medicine 184, no. 8 (October 15, 2011): 920–27. http://dx.doi.org/10.1164/rccm.201101-0005oc.

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Dissertations / Theses on the topic "Laboratory models"

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Thomas, Ashwin Paul. "Simulated and laboratory models of aircraft sound transmission." Thesis, Georgia Institute of Technology, 2014. http://hdl.handle.net/1853/52319.

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With increased exposure to transportation noise, there have been continued efforts to help insulate homes from aircraft noise. Current aircraft noise guidelines are based primarily on outdoor sound levels. As people spend the majority of their time indoors, however, human perception is evidently more related to indoor sound levels. Investigations are being made to provide further insight into how typical residential constructions affect indoor response. A pilot study has built a single-room "test house", according to typical construction for mixed-humid climate regions, and has directly measured outdoor-to-indoor transmission of sound - with specific focus on continuous commercial aircraft signatures. The results of this study are being used to validate and improve modelling software that simulates a wide range of construction types and configurations for other US climate regions. The improved models will allow for increased flexibility in simulating the impacts of acoustic and energy retrofits. Overall, the project intends to improve the ability to predict acoustic performance for typical US construction types as well as for any possible design alterations for sound insulation.
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Mustow, R. E. "Aspects of dental plaque development in laboratory models." Thesis, University of Bristol, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.379543.

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Bosak, Tanja Kirschvink Joseph L. "Laboratory models of microbial biosignatures in carbonate rocks /." Diss., Pasadena, Calif. : California Institute of Technology, 2005. http://resolver.caltech.edu/CaltechETD:etd-12102004-144939.

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Occhiogrosso, A. "Development of astrochemical models based on laboratory data." Thesis, University College London (University of London), 2013. http://discovery.ucl.ac.uk/1415490/.

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The more we discover about the molecular composition of the interstellar medium (ISM) the more we realise how difficult it is to reproduce the mechanisms behind this complex chemistry. To date, over 175 different molecular species have been detected in the ISM. Many of them are formed in the gas phase, but there is a growing number of species that form more efficiently on grain surfaces during the collapse of star-forming cores. An important issue in mimicking the interstellar medium chemistry is that there are few observational clues about the synthesis of complex organic molecules on grains; experimental work coupled with chemical modelling is therefore essential in order to understand the chemical complexity of the ISM. UCL_CHEM is a computer model that takes into account the gas-grain interactions occurring during this collapse, with the aim of reproducing the observed abundances of molecules in various astronomical environments. The work in this thesis deals with the coupling of UCL_CHEM with the most recent experimental results on the formation in the solid state of various complex organic molecules including methyl formate (see Chapter 3) and ethylene oxide and acetaldehyde (whose chemistry is extensively discussed in Chapters 4 and 5), all which have been the subject of recent astronomical interest. Moreover, important revisions of some reactions occurring in the gas phase have also been made. Despite everything seeming straightforward concerning the interstellar chemistry in the gas phase, there is still a great deal to unearth in this regard. Oxygen, for instance, is an important player in the ISM because it is the most abundant element after hydrogen and helium. Although its chemistry seems well understood, we propose a revised scheme for its reactions with small unsaturated hydrocarbons (see Chapter 6) and we show how the new reaction network affects the molecular abundances of these linear carbon chains. In Chapter 6, we also emphasise the relevance in treating structural isomers as two different species when they show peculiar chemical behaviours. Another key issue in reproducing the interstellar molecular variety concerns the freezeout of species onto dust grain surfaces. In particular, we know little about the constituents of the icy mantles. In Chapter 7, we analyse the case of sulfur-bearing species because the most dominant ice component is still debated.
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Firoozfar, Ali Reza. "Rock scour in hydraulic laboratory analog scour models." Diss., University of Iowa, 2014. https://ir.uiowa.edu/etd/1456.

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Erosional processes of solid materials have been the focus of many researchers around the world. Erosion can commence within a wide range of material strengths depending on the amount of water-driven energy and material properties. Erosion could also occur due to Aeolian effects as well as chemical weathering but these forcings are not of the focus of this research. Instead, the focus here is on rock erosion in waterways and in particular downstream of dams. Rock erosion mostly takes place at the downstream of dams where the water conveys through the spillbays from upstream to the downstream during an extreme event. This phenomenon threatens both the structural soundness of the dam with implications to the public safety. It usually occurs when the applied hydrodynamic forces (average and fluctuating) exceed the strength of the rock mass formation. Rock scour at the downstream of dams due to high velocity impinging jet is a complex and highly dynamic process. So a deeper understanding of the process is crucial to determine the rock scour rate and extent. Hydraulic laboratory models have been employed to investigate hydraulic processes and proved to be reliable tools for testing soil/sediment erosion; however, the study of rock scour remains challenging. The prototype rock formation cannot be utilized in the laboratory models because the flowing water in the scaled model contains much less energy and exerts less forcing. On the other hand, the use of granular sediment (non-cohesive), as a standalone approach to mimic the rock formation is not a precise method, since it will most probably lead to inaccurate results. The idea of using a mixture of granular and cohesive sediment is investigated here to adequately simulate the rock erosion process in the laboratory scaled models. The granular sediment represents the rock blocks while the cohesive additive is a binder to keep the granular sediment together. The rock scour process can occur through four mechanisms; fracture failure, block removal, fatigue failure and abrasion. In this study, because the focus is on the hydrodynamic forcing effects on rock erosion, we assume that in the completely and intermittently jointed rock, erosion is mostly governed by fracture, block removal and fatigue failure. Abrasion is triggered by collisional effects and is not the focus here. So, we hypothesize that if the rock formation considered being pre-fractured, it can be simulated using a mixture of non-cohesive sediment with cohesive additive. This method was utilized to assess the rock scour process at the downstream of the Priest Rapids Dam. The Priest Rapids Dam project was part of a series of projects that was conducted at IIHR-Hydroscience & Engineering at The University of Iowa and sponsored by the Public Utility District No. 2 of Grant County, Ephrata, Washington (GCPUD) to investigate juvenile salmonid migration at the Wanapum/Priest Rapids Development. It is a hydroelectric, concrete gravity, and mid-elevation dam owned and operated by Public Utility District No. 2 of Grant County, Washington (the "District"). To aid the District in their evaluation of fish passage, IIHR-Hydroscience & Engineering constructed comprehensive three-dimensional physical models of the forebay and tailrace of Priest Rapids Dam and a third model of spillbays 19-22 and powerhouse Unit 1 (sectional model). As part of the last phase of the project, it was crucial to assess the effects of the newly designed fish bypass system on the downstream rock foundation scour. To investigate this process, the 1:64 Froude-based scale tailrace model of the dam was utilized. The mixture of gravel, bentonite clay, and water was employed to mimic the rock formation and simulate the bedrock scour process in the model. Series of preliminary experiments were conducted to find the optimum mixture of gravel, bentonite and water to accurately replicate an existing scour hole observed in the prototype tailrace. Two scenarios were considered. First, tests were conducted to estimate the scour potential downstream of the fish bypass, which is currently under construction. Second, the scour potential downstream of the dam was also assessed for the Probable Maximum Flood (PMF) with the fish bypass system running. Based on the model tests results and observations, the simulated bedrock (mixture of gravel and cohesive bentonite) was able to replicate the rock scour mechanisms, i.e. fracture process, block removal and fatigue observed in nature. During the fish bypass scour tests, it was observed that the erosion process occurs in the form of block removal and fatigue failure. During the PMF scour test, instead, it was observed that the mixture is eroded in chunks of substrate. This process can be representative of fracture failure in rock which occurs when the induced pressure fluctuation exceeds the fracture strength or equivalently toughness of the rock. In the preliminary phase of this work it was recognized that a prerequisite for replicating the processes in the laboratory is the proper preparation of the mixture. There is limited information available in the literature about how much cohesive additive is required to simulate the erosional strength of the prototype rock formation. For this reason, in this study the effort has been made to develop a method to simulate the rock formation for studying rock scour process in the laboratory analog scaled models. To simulate the bedrock formation, various combination of granular sediment (gravel), cohesive additive, and water were created and tested. Choosing an appropriate cohesive additive concentration is critical and nearly a balancing act. An appropriate cohesive additive concentration should be cohesive enough to bind the material and not too strong to be eroded by the flowing water in the scaled models. Moreover, its properties should not change over time. Various cohesive additives can be mentioned i.e. kaolin clay, bentonite clay, cement, grease, paraffin wax. Among all of them, bentonite clay was chosen as the appropriate cohesive additive due to its swelling characteristic. When bentonite is mixed with granular sediment, it is restricted by the non-cohesive sediment grains. The bentonite expands to fill the voids and forms a tough, leathery mineral mastic through which water cannot readily move. In order to assess the erodibility of the mixture the Jet Erosion Test (JET) apparatus was used. The JET apparatus is a vertical, submerged, circular, turbulent impinging jet which is widely accepted and utilized to assess cohesive soil erosion through flow impingement. There are devices such as flumes which could be effectively used for bank erosion where the flow shear action is prevalent. In this study, it was sought important that the forcing replicated in the experiments was of the same nature (normal impinging forcing instead of shear forcing) as observed in the downstream end of a dam. For this reason, JET was chosen as it provided a larger range of stresses (ranging between 100-1000 Pa) comparing to the flume device. The apparatus was designed based on the device developed by Hanson and Hunt (2007) and built at the IIHR-Hydroscience & Engineering. Various replicate samples were made with different combinations of gravel, sodium bentonite clay, and water. To determine the erosional strength of the samples (critical stress) they were tested using the JET apparatus. The critical stress was determined as the stress associated with zero eroded mass. The results revealed that the erosional strength of the simulated bedrock mixtures highly depends on the amount of adhesive component (bentonite clay). The mixtures with the higher percentage of bentonite clay are less susceptible to erosion. The erosion threshold plot - similar to Annandale's plot - for the simulated bedrock mixtures was developed. Using the erosional strength of the simulated bedrock mixtures, a step-by-step systematic method was developed to determine the optimum combination of weakly cohesive substrate in order to simulate the strength of the prototype bedrock. The method is based on the Annandale's erodibility index method and requires information about the prototype bedrock strength (erodibility index). The method is explained in conjunction with the Priest Rapids Dam project example. The old trial and error method to establish an optimum weakly cohesive substrate is costly and time consuming especially in the case of large scale laboratory models. Also, the applicability of the method would be questionable when there is not enough information or a past data set that can be used as a baseline (witness) test. The new method eliminates these problems and the optimum mixture can be established using the geological information of the prototype bedrock formation.
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TETTAMANZI, MICHELE. "EXPECTATIONS IN MACROECONOMICS: PERSPECTIVES, LABORATORY EXPERIMENTS AND AB MODELS." Doctoral thesis, Università Cattolica del Sacro Cuore, 2017. http://hdl.handle.net/10280/36156.

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La presente tesi studia le aspettative in macroeconomia contribuendo alla letteratura esistente sia indagando circa il meccanismo di formazione delle aspettative, sia analizzando come le aspettative a razionalità limitata influenzino la dinamica economica. Nel primo capitolo viene presentato un esperimento nel quale ai soggetti viene chiesto di predire il valore futuro dell'inflazione: a seconda del trattamento, i soggetti possono venire esposti ad un segnale, che mira a stabilizzare l'economia, che fungendo quindi da indicazione prospettica (Forward Guidance). I risultati vengono poi studiati sottolineando il meccanismo di formazione delle aspettative soprattutto in funzione della credibilità del segnale; inoltre viene studiata l'efficacia dello strumento di politica monetaria nella stabilizzazione del sistema economico: si evidenzia come un segnale informativo permetta una sensibile stabilizzazione dell'economia, prevenendo spirali deflazionistiche. Nel secondo capitolo viene sviluppato un modello ad agenti il quale incorpora un meccanismo di formazione delle aspettative a razionalità limitata, derivato da esperimenti precedenti. Inoltre, grazie ad un peculiare processo di aggregazione, viene derivato un modello analiticamente trattabile che permette di studiare il meccanismo di trasmissione di uno shock, isolando gli effetti dovuti all'eterogeneità fra gli agenti e alle aspettative: entrambi gli effetti sono considerevoli ed aiutano nello spiegare la dinamica economica.
The present dissertation analyses expectations in macroeconomics, contributing to the existing literature both studying the expectation formation process, and inquiring how economic dynamic is influenced by boundedly rational expectations. The first chapter presents a learn to forecast experiment in which subject are asked to form expectation regarding the future value of inflation: depending on the treatment, subjects might be exposed to a signal, which possibly aim at stabilizing economy, mimicking the non conventional monetary policy instrument called Delphic Forward Guidance. The collected data are studied trying to recover the underlying expectation formation process highlighting especially the role of credibility of the signal; moreover from the data emerges that informative Forward Guidance helps in stabilizing economy, drastically reducing the probability of deflationary spirals. The second chapter develops an agent-based model, encapsulating a boundedly rational expectation formation process, which had been extrapolated in previous experiments. Moreover benefiting from a specific aggregation procedure, we derive a model characterized by high analytical tractability, allowing hence to study the transmission mechanisms of a shock by insulating the effects due to the heterogeneity among agents and due to expectations: both the effects are sizable and help in understanding the dynamics of the economic system.
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Kiss, Andrew Elek. "Dynamics of laboratory models of the wind-driven ocean circulation." View thesis entry in Australian Digital Theses Program, 2000. http://thesis.anu.edu.au/public/adt-ANU20011018.115707/index.html.

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Kiss, Andrew Elek, and Andrew Kiss@anu edu au. "Dynamics of laboratory models of the wind-driven ocean circulation." The Australian National University. Research School of Earth Sciences, 2001. http://thesis.anu.edu.au./public/adt-ANU20011018.115707.

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This thesis presents a numerical exploration of the dynamics governing rotating flow driven by a surface stress in the " sliced cylinder " model of Pedlosky & Greenspan (1967) and Beardsley (1969), and its close relative, the " sliced cone " model introduced by Griffiths & Veronis (1997). The sliced cylinder model simulates the barotropic wind-driven circulation in a circular basin with vertical sidewalls, using a depth gradient to mimic the effects of a gradient in Coriolis parameter. In the sliced cone the vertical sidewalls are replaced by an azimuthally uniform slope around the perimeter of the basin to simulate a continental slope. Since these models can be implemented in the laboratory, their dynamics can be explored by a complementary interplay of analysis and numerical and laboratory experiments. ¶ In this thesis a derivation is presented of a generalised quasigeostrophic formulation which is valid for linear and moderately nonlinear barotropic flows over large-amplitude topography on an f-plane, yet retains the simplicity and conservation properties of the standard quasigeostrophic vorticity equation (which is valid only for small depth variations). This formulation is implemented in a numerical model based on a code developed by Page (1982) and Becker & Page (1990). ¶ The accuracy of the formulation and its implementation are confirmed by detailed comparisons with the laboratory sliced cylinder and sliced cone results of Griffiths (Griffiths & Kiss, 1999) and Griffiths & Veronis (1997), respectively. The numerical model is then used to provide insight into the dynamics responsible for the observed laboratory flows. In the linear limit the numerical model reveals shortcomings in the sliced cone analysis by Griffiths & Veronis (1998) in the region where the slope and interior join, and shows that the potential vorticity is dissipated in an extended region at the bottom of the slope rather than a localised region at the east as suggested by Griffiths & Veronis (1997, 1998). Welander's thermal analogy (Welander, 1968) is used to explain the linear circulation pattern, and demonstrates that the broadly distributed potential vorticity dissipation is due to the closure of geostrophic contours in this geometry. ¶ The numerical results also provide insight into features of the flow at finite Rossby number. It is demonstrated that separation of the western boundary current in the sliced cylinder is closely associated with a " crisis " due to excessive potential vorticity dissipation in the viscous sublayer, rather than insufficient dissipation in the outer western boundary current as suggested by Holland & Lin (1975) and Pedlosky (1987). The stability boundaries in both models are refined using the numerical results, clarifying in particular the way in which the western boundary current instability in the sliced cone disappears at large Rossby and/or Ekman number. A flow regime is also revealed in the sliced cylinder in which the boundary current separates without reversed flow, consistent with the potential vorticity " crisis " mechanism. In addition the location of the stability boundary is determined as a function of the aspect ratio of the sliced cylinder, which demonstrates that the flow is stabilised in narrow basins such as those used by Beardsley (1969, 1972, 1973) and Becker & Page (1990) relative to the much wider basin used by Griffiths & Kiss (1999). ¶ Laboratory studies of the sliced cone by Griffiths & Veronis (1997) showed that the flow became unstable only under anticyclonic forcing. It is shown in this thesis that the contrast between flow under cyclonic and anticyclonic forcing is due to the combined effects of the relative vorticity and topography in determining the shape of the potential vorticity contours. The vorticity at the bottom of the sidewall smooths out the potential vorticity contours under cyclonic forcing, but distorts them into highly contorted shapes under anticyclonic forcing. In addition, the flow is dominated by inertial boundary layers under cyclonic forcing and by standing Rossby waves under anticyclonic forcing due to the differing flow direction relative to the direction of Rossby wave phase propagation. The changes to the potential vorticity structure under strong cyclonic forcing reduce the potential vorticity changes experienced by fluid columns, and the flow approaches a steady free inertial circulation. In contrast, the complexity of the flow structure under anticyclonic forcing results in strong potential vorticity changes and also leads to barotropic instability under strong forcing. ¶ The numerical results indicate that the instabilities in both models arise through supercritical Hopf bifurcations. The two types of instability observed by Griffiths & Veronis (1997) in the sliced cone are shown to be related to the western boundary current instability and " interior instability " identified by Meacham & Berloff (1997). The western boundary current instability is trapped at the western side of the interior because its northward phase speed exceeds that of the fastest interior Rossby wave with the same meridional wavenumber, as discussed by Ierley & Young (1991). ¶ Numerical experiments with different lateral boundary conditions are also undertaken. These show that the flow in the sliced cylinder is dramatically altered when the free-slip boundary condition is used instead of the no-slip condition, as expected from the work of Blandford (1971). There is no separated jet, because the flow cannot experience a potential vorticity " crisis " with this boundary condition, so the western boundary current overshoots and enters the interior from the east. In contrast, the flow in the sliced cone is identical whether no-slip, free-slip or super-slip boundary conditions are applied to the horizontal flow at the top of the sloping sidewall, except in the immediate vicinity of this region. This insensitivity results from the extremely strong topographic steering near the edge of the basin due to the vanishing depth, which demands a balance between wind forcing and Ekman pumping on the upper slope, regardless of the lateral boundary condition. The sensitivity to the lateral boundary condition is related to the importance of lateral friction in the global vorticity balance. The integrated vorticity must vanish under the no-slip condition, so in the sliced cylinder the overall vorticity budget is dominated by lateral viscosity and Ekman friction is negligible. Under the free-slip condition the Ekman friction assumes a dominant role in the dissipation, leading to a dramatic change in the flow structure. In contrast, the much larger depth variation in the sliced cone leads to a global vorticity balance in which Ekman friction is always dominant, regardless of the boundary condition.
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Brown, Graham Alfred. "A study of bovine herpesvirus 1 pathogenesis using laboratory models." Thesis, University of Cambridge, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.304239.

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Siddall, Daniel Jonathan. "Patient specific spine models : the development of a laboratory validation spine." Thesis, University of Hull, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.396751.

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Books on the topic "Laboratory models"

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Liu, Dongyou, ed. Laboratory Models for Foodborne Infections. Boca Raton : CRC Press/Taylor & Francis, 2017. | Series: Food microbiology series: CRC Press, 2017. http://dx.doi.org/10.1201/9781315120089.

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Ancona, Deborah G. Groups in organizations: Extending laboratory models. Cambridge, Mass: Sloan School of Management, Massachusetts Institute of Technology, 1986.

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Debby, Van Dam, ed. Animal Models of Dementia. Totowa, NJ: Humana Press, 2011.

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Kortagere, Sandhya. In silico models for drug discovery. New York: Humana Press, 2013.

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Physical models and laboratory techniques in coastal engineering. Singapore: World Scientific, 1993.

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International Symposium on Retinal Degeneration (1992 Sardinia, Italy). Retinal degeneration: Clinical and laboratory applications. New York: Plenum Press, 1993.

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Manzella, David. Laboratory model 50 kW hall thruster. Cleveland, Ohio: National Aeronautics and Space Administration, Glenn Research Center, 2002.

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Hitzelberg, R. Laboratory manual for basic biomethodology of laboratory animals. Silver Spring, Md: MTM Associates, 1985.

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Wostmann, Bernard S. Germfree and gnotobiotic animal models: Background and applications. Boca Raton: CRC Press, 1996.

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Jensen, Ronald L. The business management laboratory. 4th ed. Homewood, Il: Irwin, 1992.

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Book chapters on the topic "Laboratory models"

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Agúndez, Marcelino. "Interstellar Chemical Models." In Laboratory Astrophysics, 219–32. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-90020-9_14.

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Agrawal, Mahesh Chandra. "Laboratory Models Developed." In Schistosomes and Schistosomiasis in South Asia, 285–309. India: Springer India, 2012. http://dx.doi.org/10.1007/978-81-322-0539-5_11.

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Prusinkiewicz, Przemyslaw, and Aristid Lindenmayer. "Models of plant organs." In The Virtual Laboratory, 119–31. New York, NY: Springer New York, 1990. http://dx.doi.org/10.1007/978-1-4613-8476-2_5.

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Church, Christopher R., and John T. Snow. "Laboratory models of tornadoes." In Geophysical Monograph Series, 277–95. Washington, D. C.: American Geophysical Union, 1993. http://dx.doi.org/10.1029/gm079p0277.

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Emilien, Gérard, Timothy Dinan, Ulla Marjatta Lepola, and Cécile Durlach. "Laboratory models of anxiety." In Anxiety Disorders, 249–86. Basel: Birkhäuser Basel, 2002. http://dx.doi.org/10.1007/978-3-0348-8157-9_9.

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Prusinkiewicz, Przemyslaw, and Deborah R. Fowler. "Shell models in three dimensions." In The Virtual Laboratory, 163–82. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-662-05291-4_10.

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Meinhardt, Hans. "Shell models in three dimensions." In The Virtual Laboratory, 166–85. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-540-92142-4_10.

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Prusinkiewicz, Przemyslaw, and Deborah R. Fowler. "Shell models in three dimensions." In The Virtual Laboratory, 163–82. Berlin, Heidelberg: Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-662-13135-0_10.

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Prusinkiewicz, Przemyslaw, and Deborah R. Fowler. "Shell models in three dimensions." In The Virtual Laboratory, 163–82. Berlin, Heidelberg: Springer Berlin Heidelberg, 1998. http://dx.doi.org/10.1007/978-3-662-03617-4_10.

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Prusinkiewicz, Przemyslaw, and Aristid Lindenmayer. "Developmental models of herbaceous plants." In The Virtual Laboratory, 63–97. New York, NY: Springer New York, 1990. http://dx.doi.org/10.1007/978-1-4613-8476-2_3.

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Conference papers on the topic "Laboratory models"

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Kowalski, M., and A. Sankowska. "Laboratory models of demultiplexer." In 2004. 1st International Conference on Electrical and Electronics Engineering (ICEEE). IEEE, 2004. http://dx.doi.org/10.1109/stysw.2004.1459929.

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Herbst, E. "Gas-Grain Models of Low-Mass Star Formation." In ASTROCHEMISTRY: From Laboratory Studies to Astronomical Observations. AIP, 2006. http://dx.doi.org/10.1063/1.2359564.

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Gailitis, Agris. "Laboratory astrophysics as exemplified by the Riga dynamo experiment." In MHD COUETTE FLOWS: Experiments and Models. AIP, 2004. http://dx.doi.org/10.1063/1.1832135.

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Brito, J. J., P. Toledo, and S. Alayon. "Virtual laboratory for automation combining inventor 3D models and Simulink control models: Virtual laboratory for automation." In 2018 IEEE Global Engineering Education Conference (EDUCON). IEEE, 2018. http://dx.doi.org/10.1109/educon.2018.8363279.

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Babic, F., and V. Gaspar. "Mobile technologies education based on smart laboratory models." In 2017 15th International Conference on Emerging eLearning Technologies and Applications (ICETA). IEEE, 2017. http://dx.doi.org/10.1109/iceta.2017.8102464.

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Meisingset, Knut Kristian, and Tao Yang. "Comparing Reservoir Fluid Models to PVT Laboratory Measurements." In SPE Bergen One Day Seminar. Society of Petroleum Engineers, 2017. http://dx.doi.org/10.2118/185903-ms.

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Nazarzehi, Valimohammad, and Alireza Fatehi. "Identification of Linear Models for a Laboratory Helicopter." In 2009 Second International Conference on Computer and Electrical Engineering. IEEE, 2009. http://dx.doi.org/10.1109/iccee.2009.44.

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Srpak, Dunja, Ivan Šumiga, Josip Srpak, and Emil Dumic. "DEVELOPING THE LABORATORY MODELS FOR WIRELESS ENERGY TRANSMISSION." In 12th International Conference on Education and New Learning Technologies. IATED, 2020. http://dx.doi.org/10.21125/edulearn.2020.0940.

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Mandrini, Cristina H. "Solar Coronal Loops and Coronal Heating Models." In MAGNETIC FIELDS IN THE UNIVERSE: From Laboratory and Stars to Primordial Structures. AIP, 2005. http://dx.doi.org/10.1063/1.2077175.

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Varri, A. L., G. Bertin, Giuseppe Bertin, Franca De Luca, Giuseppe Lodato, Roberto Pozzoli, and Massimiliano Romé. "Self-consistent models of quasi-relaxed rotating stellar systems." In PLASMAS IN THE LABORATORY AND THE UNIVERSE: Interactions, Patterns, and Turbulence. AIP, 2010. http://dx.doi.org/10.1063/1.3460118.

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Reports on the topic "Laboratory models"

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Whitehead, John A. Laboratory Models of Ocean Circulation. Fort Belvoir, VA: Defense Technical Information Center, June 1997. http://dx.doi.org/10.21236/ada326697.

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Boyer, Don L., Harindra J. Fernando, Andjelka N. Srdic, and Dale B. Haidvogel. Laboratory Benchmarks for the Development of Numerical Ocean Models. Fort Belvoir, VA: Defense Technical Information Center, September 2002. http://dx.doi.org/10.21236/ada628431.

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Haidvogel, Dale B., Don L. Boyer, Harindra J. Fernando, and Andjelka N. Srdic. Laboratory Benchmarks for the Development of Numerical Ocean Models. Fort Belvoir, VA: Defense Technical Information Center, September 2001. http://dx.doi.org/10.21236/ada625207.

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Blevins, John D., David F. Menicucci, Thomas, Jr Byrd, .), Sigifredo Gonzalez, Jerry W. Ginn, and Juan Ortiz-Moyet. Laboratory tests of IEC DER object models for grid applications. Office of Scientific and Technical Information (OSTI), February 2007. http://dx.doi.org/10.2172/903152.

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Covey, C., K. Caldeira, T. Guilderson, P. Cameron-Smith, B. Govindasamy, C. Swanston, M. Wickett, A. Mirin, and D. Bader. Global Biogeochemistry Models and Global Carbon Cycle Research at Lawrence Livermore National Laboratory. Office of Scientific and Technical Information (OSTI), May 2005. http://dx.doi.org/10.2172/15016353.

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Sobolik, S. R., and J. D. Miller. Preliminary validation of rock mass models by comparison to laboratory frictional sliding experiments. Office of Scientific and Technical Information (OSTI), September 1996. http://dx.doi.org/10.2172/582267.

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Kaetzel, Lawrence J., James R. Clifton, and Leslie J. Struble. Guidelines for the development of computer based models in a cementitious materials modeling laboratory. Gaithersburg, MD: National Institute of Standards and Technology, 1991. http://dx.doi.org/10.6028/nist.ir.4650.

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Duthinh, Dat. Finite-element models of the National Fire Research Laboratory (NFRL) and modular support structure. Gaithersburg, MD: National Institute of Standards and Technology, October 2012. http://dx.doi.org/10.6028/nist.ir.7886.

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Dushaw, Brian. North Pacific Acoustic Laboratory: Analysis of Shadow Zone Arrivals and Acoustic Propagation in Numerical Ocean Models. Fort Belvoir, VA: Defense Technical Information Center, February 2009. http://dx.doi.org/10.21236/ada494669.

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Dushaw, Brian. North Pacific Acoustic Laboratory: Analysis of Shadow Zone Arrivals and Acoustic Propagation in Numerical Ocean Models. Fort Belvoir, VA: Defense Technical Information Center, September 2007. http://dx.doi.org/10.21236/ada541751.

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