Relevant bibliographies by topics / Laboratory modelling

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Laboratory modelling'

Author: Grafiati
Published: 4 June 2021
Last updated: 14 March 2023

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Journal articles on the topic "Laboratory modelling"

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Bright, Frank. "Laboratory modelling of fluorescein interactions." Contact Lens and Anterior Eye 35 (December 2012): e49. http://dx.doi.org/10.1016/j.clae.2012.10.061.

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Kopysov, S. P., A. K. Novikov, V. N. Rychkov, Yu A. Sagdeeva, and L. E. Tonkov. "Virtual laboratory for finite element modelling." Vestnik Udmurtskogo Universiteta. Matematika. Mekhanika. Komp'yuternye Nauki, no. 4 (December 2010): 131–45. http://dx.doi.org/10.20537/vm100415.

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Rodin, E. Y., and N. J. Taber. "Yeast growth modelling in a laboratory." Mathematical and Computer Modelling 10, no. 1 (1988): 67–73. http://dx.doi.org/10.1016/0895-7177(88)90123-9.

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Sommeria, J., and H. Didelle. "Laboratory modelling of atmospheric dynamical processes." European Physical Journal Conferences 1 (2009): 101–11. http://dx.doi.org/10.1140/epjconf/e2009-00913-0.

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Glukhova, Marina V. "MODELLING OF EXPERIMENTAL TRICHINOSIS OF LABORATORY RODENTS." Vestnik of Ulyanovsk State Agricultural Academy, no. 4(36) (December 4, 2016): 83–85. http://dx.doi.org/10.18286/1816-4501-2016-4-83-85.

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Kutsenko, Volodymyr, Gennadiy Ivanov, and Oleksandr Prodan. "Modelling of spondylolisthesis in small laboratory animals." ORTHOPAEDICS, TRAUMATOLOGY and PROSTHETICS, no. 4 (March 26, 2011): 63. http://dx.doi.org/10.15674/0030-59872011463-68.

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Yam, Ke, William D. McCaffrey, Derek B. Ingham, and Alan D. Burns. "CFD modelling of selected laboratory turbidity currents." Journal of Hydraulic Research 49, no. 5 (2011): 657–66. http://dx.doi.org/10.1080/00221686.2011.607303.

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Saxena, Priyam, Kyle Hoegh, Lev Khazanovich, and Alex Gotlif. "Laboratory and analytical modelling of misaligned dowel." International Journal of Pavement Engineering 13, no. 3 (2012): 209–15. http://dx.doi.org/10.1080/10298436.2011.596936.

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Zhang, Rong, Marcel Zijlema, and Marcel J. F. Stive. "Laboratory validation of SWASH longshore current modelling." Coastal Engineering 142 (December 2018): 95–105. http://dx.doi.org/10.1016/j.coastaleng.2018.10.005.

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Ashmore, Peter E. "Laboratory modelling of gravel braided stream morphology." Earth Surface Processes and Landforms 7, no. 3 (2007): 201–25. http://dx.doi.org/10.1002/esp.3290070301.

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Dissertations / Theses on the topic "Laboratory modelling"

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Okwedadi, A. C. "Laboratory modelling of soil collapsibility." Thesis, Coventry University, 2015. http://curve.coventry.ac.uk/open/items/7a09337f-ac03-494f-bf57-fc320f7c0e7b/1.

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Collapsible soils covers naturally over 10% of the earth’s surface. This makes it a global problem and it is essential that engineers identify and control collapsibility prior to construction. Hence in this thesis, a study on identification, evaluation and control of soil collapsibility is undertaken. Four geologically different soils have been tested at five compactive variables from optimum moisture content (OMC). The soils tested include: Brown inorganic silty clay of low plasticity (A); White inorganic silt with slight plasticity (B); Red inorganic clay of intermediate plasticity (C); and Brown sand-clay mixtures with inorganic clay of low plasticity (D). The soils were each compacted at moisture variations 60% - 80%, 80% - 95%, 95% - 105%, 110% - 125% and 125% - 150% respectively representing ‘Low Dry OMC’, ‘High Dry OMC’, ‘At OMC’, ‘Low Wet OMC’ and ‘High Wet OMC’. The major causes of collapsibility of soil and the geomorphological processes that gives the pedogenesis of collapsible soils, is highlighted and great emphasis is placed on the adverse effect of collapsible soils. The experimental results from particle size distribution, Atterberg, compaction, triaxial and double oedometer tests showed that the soil’s percentage fine with the fines material (silt or clay), coefficient of uniformity, optimum moisture content, Atterberg limits, and stress-strain properties affect the metastability of the soils and they can be compared to the soil’s collapse potential when pressures and moisture content are applied on the soils. Results obtained showed that the soil’s collapse potential is directly proportional to 1) percentage fines, 2) the difference between the silt and clay percentage, 3) the Atterberg limits (liquid limit, plastic limit and plasticity index), and 4) internal friction angle; and inversely proportional to 1) coefficient of uniformity, 2) initial moisture content, 3) cohesion and finally 4) peak deviator stress. Each soil’s geological property proved to have an adverse effect on the metastability of the soils especially the dry of optimum moisture content. The most interesting results were obtained from the oedometer test. Results of the critical pressure varied with each soil and their compactive variable; Most of the soils at their ‘dry OMC’ had the highest collapse potential. In general, the lower the critical pressure the higher the collapse potential of the soil. The experimental data obtained herein were checked with the past research collapse indexes and found the results agreeing with just two research work out of eighteen examinations. Finally models for identifying soil collapsibility are generated with relationship between parameters from sieve, Atterberg, proctor compaction and triaxial. Laboratory data and data from twelve research work were used to verify the models and they show that the models work. After the verification of these formulas with past research data collected, the best models were three compactive variable models. The models give a collapsibility index in terms of percentage fines, initial moisture content, initial degree of saturation and initial dry density.
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Sandbach, Steven D. "Mathematical and laboratory modelling of ventilation." Thesis, University of Manchester, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.506639.

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Kelley, Douglas H. "Rotating, hydromagnetic laboratory experiment modelling planetary cores." College Park, Md.: University of Maryland, 2009. http://hdl.handle.net/1903/9100.

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Thesis (Ph.D.) -- University of Maryland, College Park, 2009.<br>Thesis research directed by: Dept. of Physics. Title from t.p. of PDF. Includes bibliographical references. Published by UMI Dissertation Services, Ann Arbor, Mich. Also available in paper.
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Franklin, James. "Laboratory modelling of breaking internal solitary waves." Thesis, University of Dundee, 2014. https://discovery.dundee.ac.uk/en/studentTheses/bf2741dd-7183-4aa5-817e-f5d533269c95.

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Bentley, Mark Stephen. "Space weathering on mercury : laboratory studies and modelling." Thesis, Open University, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.413806.

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Revet, Guilhem. "Modelling magnetized accretion columns of young stars in the laboratory." Thesis, Université Paris-Saclay (ComUE), 2018. http://www.theses.fr/2018SACLX046/document.

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Le travail présenté dans cette thèse s’inscrit dans le domaine de l'astrophysique de laboratoire, qui consiste à étudier en laboratoire des processus physiques qui se produisent dans des objets astrophysiques. Les principaux avantages ici sont que les processus peuvent être étudiés de manière contrôlée et que leur dynamique complète peut être étudiée. Présentement, nous avons profité des installations laser à haute intensité pour effectuer nos études.Pour cela, dans ce manuscrit, seront traitées les questions liées à l'astrophysique de laboratoire qui impliquent l'interaction d’un plasma en détente dans le vide en présence d’un champ magnétique ambiant. La présence d'un champ magnétique dans une variété de phénomènes astrophysiques rend l’introduction de cette composante magnétique dans le laboratoire nécessaire afin que ces études soient pertinentes. Pour ce faire, en collaboration avec Laboratoire National des Champs Magnétiques Intenses -LNCMI, une bobine Helmholtz, spécialement conçue pour travailler dans un environnement laser a été développée, permettant d'atteindre une force de champ magnétique jusqu'à 30 T.Les objets astrophysiques sur lesquels cette étude est centrée sont les étoiles jeunes ou « Young Stellar Objects » (YSOs). Plusieurs étapes du processus de formation de ces étoiles seront ici étudiées : (i) la génération de jets collimatés à très grande échelle, (ii) la dynamique d'accrétion impliquant, dans la représentation standard, des flux de matière tombant sur la surface de l’étoile sous forme de colonnes magnétiquement confinées, et (iii) des canaux d'accrétion plus exotiques, comme l'accrétion équatoriale qui implique la propagation du plasma perpendiculairement aux lignes de champ magnétique.Plus précisément, dans un premier chapitre, la dynamique de formation des jets sera discutée. Une première partie est dédiée au mécanisme de formation de jet dans un champ magnétique poloïdal (aligné par rapport à l'axe principal d’expansion du plasma). Une seconde partie traite de la distorsion d'une telle formation de jet par l'interaction du même plasma en expansion avec un champ magnétique désaligné (c'est-à-dire présentant un angle par rapport à l'axe d’expansion du plasma). Enfin, une troisième partie détaille la propagation du plasma dans un champ magnétique perpendiculaire. Cette dernière partie nous permet d'étudier des canaux exotiques d'accumulation de matière sur les étoiles, consistant en une accrétion du disque d’accrétion directement vers l'étoile, c’est-à-dire sur le plan équatorial, impliquant une propagation orthogonale aux lignes de champ magnétiques. Le deuxième chapitre aborde le thème de la dynamique d'accrétion par l'intermédiaire de colonnes de matière magnétiquement confinées, tombant sur la surface stellaire. En utilisant la même configuration expérimentale que dans le premier chapitre, le jet formé (dans le cas du champ magnétique parfaitement aligné) est utilisé pour imiter la colonne d'accrétion et est lancé sur une cible secondaire qui agit comme la surface stellaire. La dynamique de choc à l'emplacement de l'obstacle est soigneusement étudiée et des liens avec les observations de phénomènes d’accrétion astrophysique sont construits. Un cocon de plasma, formé autour de la région d'impact via l'interaction avec le champ magnétique, est observé être similaire à celui trouvé dans les simulations astrophysiques. Ce cocon est un élément important en tant que milieu potentiel d'absorption des émissions X. Ce milieu permettrait en effet d'expliquer les écarts observés entre les émissions UV / optiques et les émissions X provenant des étoiles lors des phases d’accrétion<br>The work that is presented here has been performed in the frame of laboratory astrophysics, which consists in studying in the laboratory physical processes occurring in astrophysical objects. The main advantages in doing so are that the processes can be studied in a controlled way and that their full dynamics can be investigated. Here, we have been taking advantage of high-intensity laser facilities to perform our studies.In this manuscript, will be treated issues that include the interaction of a plasma expanding into vacuum with an ambient magnetic field. The presence of a magnetic field in a variety of astrophysical phenomena makes the inclusion of this component in the laboratory of great interest. We have used for our study a split Helmholtz coil, specifically designed in order to work in a laser environment, that allows for reaching a magnetic field strength up to 30 T.The astrophysical objects on which this study is focused are Young Stellar Objects (YSOs). Several steps of the star formation process are here investigated: (i) the generation of very long range, bright jets, (ii) the accretion dynamic involving, in the standard representation, matter falling down on the star in the shape of magnetically confined columns, and (iii) more exotic accretion channels, as the equatorial accretion that implies propagation of plasma perpendicularly to magnetic field lines.More precisely, in a first chapter, the jet formation dynamic will be discussed. A first part is dedicated to the jet formation mechanism in a poloidal magnetic field (aligned with respect to the main plasma expansion axis). A second part is dealing with the distortion of such jet formation via the interaction of the same expanding plasma with a misaligned magnetic field (i.e. presenting an angle with respect to the plasma expansion axis). Finally, a third part details the propagation of the plasma within a perpendicular magnetic field. This last part allows us to investigate exotic channels of matter accretion onto the stars, consisting of equatorial accretion from the disk to the star, through orthogonal magnetic field lines. The second chapter addresses the topic of the standard accretion dynamic via magnetically confined columns of matter, falling down onto the stellar surface. Using the same experimental setup as in the first chapter, the formed jet (in the case of the perfectly aligned magnetic field) is used to mimic the accretion column, and is launched onto a secondary target that acts as the stellar surface. The shock dynamic at the obstacle location is carefully studied and links with astrophysical accretion observations are built. A plasma cocoon, shaped around the impact region via the interaction with the magnetic field, is found to be similar to the one found in astrophysical simulations. This cocoon is an important element as a potential X-ray absorptive medium in order to explain observed discrepancies, between observed UV/Optical and X-ray emissions emitted from accreting stars
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Harrison, Mark. "Laboratory and modelling studies of phenols relevant to the atmosphere." Thesis, University of Edinburgh, 2003. http://hdl.handle.net/1842/14010.

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In order to investigate the kinetics and selectivity of the liquid phase nitration of phenol, reliable procedures for the production of the nitrating agents N<sub>2</sub>O<sub>5</sub> and CINO<sub>2</sub> were established. Production of N<sub>2</sub>O<sub>5</sub> was achieved <i>via</i> on-line mixing of NO<sub>2</sub> (1%) with O<sub>3</sub>(~5%) in the 2:1 ratio in a darkened reaction vessel. CINO<sub>2</sub> was produced by conversion of N<sub>2</sub>O<sub>5</sub> using NaCI solution (4 M). The concentration of nitrating agents was determined by bubbling the gas stream through water to yield nitrate which was analysed using Ion Chromatography and also by off-line reduction to nitrite followed by analysis using the sulphanilamide/UV method. A method for quantitative solid phase extraction with phenol in the aqueous phase. Nitration experiments were conducted under both acidic and basic conditions over a temperature range relevant to environmental processes. Results indicate the formation of 4-nitrosophenol (additionally characterised using GC-MS) as well as 2- and 4-nitrophenol (additionally characterised using GC-MS) as well as 2- and 4-nitrophenol. The product ratio of the products species has been shown to be dependent upon both the nitrating agent on pH. Finally, a chemical kinetic model has been developed to quantify the relative nitration pathways of aromatics in the troposphere. A box model, coded using FACSIMILE software, has been used to partitioning of benzene and phenol into the liquid phase and to assess the relative importance of the gas and liquid phases. The model includes the phase partitioning of 21 species and focuses on the conversion of benzene to phenol and finally nitrophenol in both the gas and liquid phase. Results indicate that the liquid phase contributes significantly to the production of nitrophenols in the troposphere. The system was shown to be sensitive to the assumed liquid water content over the range 3x10<sup>-9</sup> to 3x10<sup>-6</sup> as well as the droplet diameter and temperature. The accuracy of the liquid phase rate coefficients for the phenol + OH and phenol + NO<sub>3</sub> reactions were also shown to be very significant although altering the liquid phase benzene rate coefficient had little impact on the system as a whole. The model was also extending to include the partitioning of the nitrophenol products. This allowed an estimation to be made regarding the fate of the product species. At the benchmark <i>Lc</i> value of 3x10<sup>-7</sup>, used to describe tropospheric cloud conditions, some 58% of the nitrophenols are produced by liquid phase processes whereas less than 2% of the nitrophenols remains in the liquid. This suggests that a great deal of the nitrophenol that may be observed in the gas phase is actually produced through liquid phase pathways.
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Finotello, Alvise. "Tidal Channel Patterns: Field Investigations, Numerical Modelling and Laboratory Experiments." Doctoral thesis, Università degli studi di Padova, 2017. http://hdl.handle.net/11577/3425863.

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Tidal meandering channels are ubiquitous features of tidal landscapes and play a fundamental role on the eco-morphodynamic evolution of these environments. However, only a handful of papers provide details on tidal meander planimetric shape, morphometric characteristics and morphodynamic evolution, and the internal achitecture of tidal meanders has not been explored in detail. Moreover, the morphodynamic evolution of tidal meanders and the related sedimentary products have often been interpreted on the basis of the well developed models and theories existing for their fluvial counterparts, despite a number of differences were a priori identifiable. Toward the goal of improving current understanding of the morphodynamic evolution of tidal meanders, five main issues have been investigated in the present work: i) rates of migration and evolutionary dynamics of tidal meanders; ii) assessment and quantification of differences and analogies existing between the planform features of tidal and fluvial meanders; iii) variations of tidal meander hydrodynamics in response to different tidal phases, and the role that these variations exert on tidal meander sedimentary products; iv) role played by bidirectional flows, tidal asymmetries and lateral tributaries; v) assessment of influence of tide amplitude, basin slope and initial shoreline configuration on tidal channel network ontogeny and evolution via laboratory experiment. A multidisciplinary approach has been adopted, with different methodologies encompassing remote sensing techniques, field observations, numerical modelling and physical-laboratory experiments. Activities have been carried out in parallel with sedimentological studies, in order to provide a comprehensive framework. The main results from this work highlighted that: I) once conveniently scaled with channel width, tidal meander migration rates are very similar to those displayed by fluvial meanders, thus challenging the paradigm of tidal meanders as a stable landscape features; II) differences and analogies between tidal and fluvial meander planforms can be addressed in a quantitative way, and different metrics exist thta allow one to successfully quantify these differences; III) strong asymmetries exist between different tidal phases, exerting a crucial role on the depositional patterns of tidal meanders; IV) under certain conditions, lateral tributaries can strongly influence the evolution of bends modifying local mechanisms of flow and sediment distribution; V) tidal channel network features evolve differently in response to different tidal ranges, basin slopes and relative sea level changes, whereas the number of breaches along the initial shoreline seems to have little effect on the evolution of the network itself.<br>Le reti di canali meandriformi costituiscono una delle principali componenti dei sistemi mareali, e giocano un ruolo di fondamentale importanza nell’evoluzione eco-morfodinamica di questi ambienti. Tuttavia, solo un numero limitato di studi scientifici ne ha analizzato le configurazioni planimetriche, le caratteristiche morfometriche e l’evoluzione morfodinamica. Inoltre, l’evoluzione morfodinamica e i prodotti sedimentari dei meandri a marea sono spesso stati interpretati sulla base di teorie e modelli sviluppati per i loro omologhi fluviali, nonostante numerose differenze tra le due tipologie siano identificabili a priori. Nell’intento di comprendere più approfonditamente l’evoluzione morfodinamica dei meandri a marea, nel presente lavoro sono stati studiati 5 differenti argomenti: i) tassi di migrazione e dinamiche evolutiove dei meandri a marea; ii) stima e quantificazione delle differenze planimetriche esistenti tra meandri fluviali e tidali; iii) variazioni dell’idrodinamica dei meandri a marea in risposta all’alternanza delle fasi mareali, e influenza di queste variazioni sui prodotti sedimentari propri dei meandri a marea; iv) ruolo della bidirezionalità del flusso, delle asimmetrie mareali e dei tributari laterali; v) stima dell’influenza dell’ampiezza di marea, delle pendenze topografiche del bacino tidale e della configurazione iniziale della linea di costa sulla nascita ed evoluzione morfologica delle reti di canali a marea. Nelle suddette analisi é stato utilizzato un approccio di tipo multidisciplinare, combinando metodologie quali remote-sensing, osservazioni in situ, modellazione numerica ed esperimenti su modelli fisici. Le attività sono state condotte in parallelo con studi sedimentologici, così da fornire un quadro che fosse il più esaustivo possibile. I principali risultati ottenuti evidenziano che: I) se convenientemente normnalizzati con la larghezza del canale, i tassi di migrazione dei meandri a marea sono molto simili a quelli dei loro corrispettivi fluviali, inficiando così il paradigma che vede i meandri tidali come un’entità morfologica essenzialmente stabile; II) le differenze tra meandri tidali e fluvali non sono solo qualitative, e diverse sono le metriche che possono essere utilizzate per quantificare queste differenze; III) le asimmetrie tra le diverse fasi di marea sono significative, e influenzano i patterns deposizionali in modo determinante; IV) gli affluenti laterali possono influenzare fortemente l’evoluzione dei meandri, modificando i meccanismi locali di distrubuzione dei flussi e dei sedimenti; V) le reti di canali a marea evolvono in modo diverso in risposta a differenti ampiezze di marea, pendenze del bacino tidale e cambiamenti del livello relativo del medio mare, mentre la configurazione iniziale della linea di costa non sembra avere effetti significativi sull’evoluzione della rete stessa.
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Migdalska, Anna Marta. "Modelling human genetic disorders in mice." Thesis, University of Cambridge, 2012. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.610341.

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Narasimhan, Balaji. "Electrokinetic barriers to contaminant transport, numerical modelling and laboratory-scale experimentation." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0003/MQ45103.pdf.

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Books on the topic "Laboratory modelling"

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Birgelis, Vitas. Mathematical modelling of a laboratory ball mill. Laurentian University, School of Engineering, 1986.

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1938-, Rattray C., and Clark Robert G. 1944-, eds. The Unified computation laboratory: Modelling, specifications, and tools. Clarendon Press, 1992.

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1943-, Eberwein Wolf-Dieter, ed. Transformation processes in Eastern Europe: Perspectives from the modelling laboratory. P. Lang, 1992.

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Ferrari, Alessio, and Lyesse Laloui, eds. Advances in Laboratory Testing and Modelling of Soils and Shales (ATMSS). Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-52773-4.

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Hope, Christopher Keith. Biological removal of manganese from groundwater: Laboratory modelling using Leptothrix discophora. University of Birmingham, 1998.

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Richter, O. Environmental fate modelling of pesticides: From the laboratory to the field scale. VCH, 1996.

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Schetzen, Martin. Discrete systems laboratory using MATLAB. Brooks/Cole, 2000.

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Nordic Workshop on Integrated Energy and Environmental Modelling (1990 Forsøgsanlıg Risø). Nordic Workshop on Integrated Energy and Environmental Modelling, held at Risø National Laboratory, 15-16 February 1990. Nordisk Ministeråd, 1990.

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Workshop on Mesoscale Modelling, Turbulence and Diffusion (1987 Risø National Laboratory). Proceedings of Workshop on Mesoscale Modelling, Turbulence, and Diffusion at Risø National Laboratory, Denmark, 12-15 May 1987. Edited by Pearce R. P. 1924- and Atmospheric Sciences Laboratory (U.S.). Risø National Laboratory, 1987.

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G, Seybold Paul, and Cheng Chao-Kun, eds. Cellular automata modeling of chemical systems: A textbook and laboratory manual. Springer, 2005.

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Book chapters on the topic "Laboratory modelling"

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Sazhok, Mykola. "Speech Modelling Virtual Laboratory." In Speech Processing, Recognition and Artificial Neural Networks. Springer London, 1999. http://dx.doi.org/10.1007/978-1-4471-0845-0_12.

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Banning, Edward B. "Probability, Modelling, and Statistical Inference." In The Archaeologist's Laboratory. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-47992-3_8.

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Pallavicini, R. "Stellar Flares: Observations and Modelling." In The Sun: A Laboratory for Astrophysics. Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-2765-3_26.

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Shen, Baotang, Xizhen Sun, and Baoliang Zhang. "Laboratory Studies of 2D and 3D Rock Fracture Propagation." In Modelling Rock Fracturing Processes. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-35525-8_3.

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Zhuang, Li, Sunggyu Jung, Melvin Diaz, and Kwang Yeom Kim. "Laboratory Investigations on the Hydraulic Fracturing of Granite Cores." In Modelling Rock Fracturing Processes. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-35525-8_4.

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Yin, Zhen-Yu, Pierre-Yves Hicher, and Yin-Fu Jin. "Introduction of Laboratory Tests for Soils." In Practice of Constitutive Modelling for Saturated Soils. Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-15-6307-2_3.

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Lane-Serff, G. F., P. F. Linden, D. J. Parker, and D. A. Smeed. "Laboratory Modelling of Natural Ventilation Via Chimneys." In Architecture and Urban Space. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-017-0778-7_75.

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Galland, Olivier, Eoghan Holohan, Benjamin van Wyk de Vries, and Steffi Burchardt. "Laboratory Modelling of Volcano Plumbing Systems: A Review." In Physical Geology of Shallow Magmatic Systems. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-14084-1_9.

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Chernov, Vladimir, and Alexander Ezersky. "Laboratory Modelling and Acoustic Diagnostics of Hydrodynamical Processes." In Nonlinear Waves and Pattern Dynamics. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-78193-8_13.

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Galland, Olivier, Eoghan Holohan, Benjamin van Wyk de Vries, and Steffi Burchardt. "Laboratory Modelling of Volcano Plumbing Systems: A Review." In Physical Geology of Shallow Magmatic Systems. Springer International Publishing, 2015. http://dx.doi.org/10.1007/11157_2015_9.

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Conference papers on the topic "Laboratory modelling"

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Honc, Daniel, and Frantisek Dusek. "Novel Multivariable Laboratory Plant." In 26th Conference on Modelling and Simulation. ECMS, 2012. http://dx.doi.org/10.7148/2012-0468-0473.

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Ren, Shuo, and Frederic D. McKenzie. "Collaborative Virtual Environment For Engineering Laboratory." In 29th Conference on Modelling and Simulation. ECMS, 2015. http://dx.doi.org/10.7148/2015-0157.

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Jayaratne, Ravindra, Edgar Mendoza, Rodolfo Silva, and Francisco Gutiérrez. "Laboratory Modelling of Scour on Seawalls." In Coastal Structures and Solutions to Coastal Disasters Joint Conference 2015. American Society of Civil Engineers, 2017. http://dx.doi.org/10.1061/9780784480304.084.

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Chalupa, Petr, Martin Maly, and Jakub Novak. "Nonlinear Simulink Model Of Magnetic Levitation Laboratory Plant." In 30th Conference on Modelling and Simulation. ECMS, 2016. http://dx.doi.org/10.7148/2016-0293.

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"Characterising mineral slurry dewatering through laboratory centrifugation." In 20th International Congress on Modelling and Simulation (MODSIM2013). Modelling and Simulation Society of Australia and New Zealand, 2013. http://dx.doi.org/10.36334/modsim.2013.a11.berres.

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Chalupa, Petr, Jakub Novak, and Martin Maly. "Modelling And Model Predictive Control Of Magnetic Levitation Laboratory Plant." In 31st Conference on Modelling and Simulation. ECMS, 2017. http://dx.doi.org/10.7148/2017-0367.

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"Applying Conformance Checking on Virtual Laboratory Experiments." In the 21st International Conference on Modelling and Applied Simulation. CAL-TEK srl, 2022. http://dx.doi.org/10.46354/i3m.2022.mas.002.

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"Combined ERT and GPR for Laboratory Modelling Experiment." In The Second Eurasian RISK-2020 Conference and Symposium. AIJR Publisher, 2020. http://dx.doi.org/10.21467/abstracts.93.66.

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Upadhyay, Vineet K., Yogang Singh, and V. G. Idichandy. "Modelling and control of an underwater laboratory glider." In 2015 IEEE Underwater Technology (UT). IEEE, 2015. http://dx.doi.org/10.1109/ut.2015.7108311.

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Bedrikovetsky, P. G., R. P. Lopes, F. F. Rosario, M. C. Bezerra, and E. A. Lima. "Oilfield Scaling - Part I: Mathematical and Laboratory Modelling." In SPE Latin American and Caribbean Petroleum Engineering Conference. Society of Petroleum Engineers, 2003. http://dx.doi.org/10.2118/81127-ms.

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Reports on the topic "Laboratory modelling"

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Munhuweyi, Ngonidzashe Portia, Zita Ekeocha, Stephen Robert Byrn, and Kari L. Clase. Resource Modelling for the QC Laboratory at XYZ Pharmaceuticals in Southern Africa. Purdue University, 2021. http://dx.doi.org/10.5703/1288284317431.

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Quality control (QC) laboratories are critical components in drug manufacturing and running them efficiently contributes to better, consistent supply of cost-effective quality products, while also and preventing deaths due to untimely delivery or unavailability of medicines. Having a resource modelling tool to estimate resources needed to handle a particular demand in a given system is essential for efficient running of QC laboratory. This study was done to establish such a model at XYZ Pharmaceuticals. The list of all products manufactured by XYZ Pharmaceuticals Southern Africa was reviewed; and product families for all products were identified. Analysts’ hands on time (HOT) to process one sample of each of the product families was estimated. The number of analysts required to support the workload at XYZ Pharmaceuticals was calculated using the HOTs for the different product families and the Maslaton’s Calculation Model. A baseline resource model was established.
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Comolli, A. G., E. S. Johanson, L. K. Lee, G. A. Popper, and T. O. Smith. Catalytic Two-Stage Liquefaction (CTSL{trademark}) process: Laboratory scale studies modelling and technical assessment. Final report, [October 1, 1988--June 30, 1993]. Office of Scientific and Technical Information (OSTI), 1993. http://dx.doi.org/10.2172/10132028.

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Shamonia, Volodymyr H., Olena V. Semenikhina, Volodymyr V. Proshkin, Olha V. Lebid, Serhii Ya Kharchenko, and Oksana S. Lytvyn. Using the Proteus virtual environment to train future IT professionals. [б. в.], 2020. http://dx.doi.org/10.31812/123456789/3760.

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Based on literature review it was established that the use of augmented reality as an innovative technology of student training occurs in following directions: 3D image rendering; recognition and marking of real objects; interaction of a virtual object with a person in real time. The main advantages of using AR and VR in the educational process are highlighted: clarity, ability to simulate processes and phenomena, integration of educational disciplines, building an open education system, increasing motivation for learning, etc. It has been found that in the field of physical process modelling the Proteus Physics Laboratory is a popular example of augmented reality. Using the Proteus environment allows to visualize the functioning of the functional nodes of the computing system at the micro level. This is especially important for programming systems with limited resources, such as microcontrollers in the process of training future IT professionals. Experiment took place at Borys Grinchenko Kyiv University and Sumy State Pedagogical University named after A. S. Makarenko with students majoring in Computer Science (field of knowledge is Secondary Education (Informatics)). It was found that computer modelling has a positive effect on mastering the basics of microelectronics. The ways of further scientific researches for grounding, development and experimental verification of forms, methods and augmented reality, and can be used in the professional training of future IT specialists are outlined in the article.
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Waganet, R. J., John Duxbury, Uri Mingelgrin, John Hutson, and Zev Gerstl. Consequences of Nonequilibrium Pesticide Fate Processes on Probability of Leaching from Agricultural Lands. United States Department of Agriculture, 1994. http://dx.doi.org/10.32747/1994.7568769.bard.

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Pesticide leaching in heterogeneous field soils is relatively unstudied and is the focus of this project. A wide variety of heterogeneous soils exist, characterized by processes that result from the presence of structural cracks, worm holes, and other preferred pathways within which the majority of transport can occur (called physical non-equilibrium processes), along with the presence of sorption processes that are both equilibrium and kinetic (chemical non-equilibrium processes). Previous studies of pesticide leaching have focused primarily on relatively homogeneous soils, which are less widely distributed in nature, but more studied due to the relative ease with which quantitative theory can be applied to interpret experimental results. The objectives of the proposed project were: first, to gain greater insight into the basic physical and chemical processes that characterize non-equilibrium systems, second, to improve our ability to predict pesticide leaching in heterogeneous field soils, and third, to estimate the consequences of non-equilibrium processes at the field scale by conducting an analysis of the probability of pesticide leaching when non-equilibrium processes prevail. The laboratory, theoretical and modelling aspects of the project were successful; the field aspects less so. We gained greater insight into basic processes in heterogeneous field soils, and we improved and tested tools (simulation models) and the methodology of using such tools for assessing the probability of pesticide leaching as a contribution to broader risk analysis efforts.
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Spencer, Khalil J., Jung Ho Rim, Donivan R. Porterfield, Robert Clifford Roback, Hakim Boukhalfa, and Floyd E. Stanley. High-Precision Plutonium Isotopic Compositions Measured on Los Alamos National Laboratory’s General’s Tanks Samples: Bearing on Model Ages, Reactor Modelling, and Sources of Material. Further Discussion of Chronometry. Office of Scientific and Technical Information (OSTI), 2015. http://dx.doi.org/10.2172/1188192.

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