Книги: "Dynamical temperature measurement"

1

Lawton, B. Transient temperature in engineering and science. Oxford: Oxford University Press, 1996.

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2

Stocks, Dana R. Further development of the dynamic gas temperature measurement system. West Palm Beach, FL: Pratt & Whitney, Government Products Division, 1986.

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3

Elmore, D. L. [Further development of the dynamic gas temperature measurement system. [West Palm Beach, FL: Pratt & Whitney, Government Products Division, 1987.

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4

American Society of Mechanical Engineers. Winter Meeting. Pressure and temperature measurements: Presented at the Winter Annual Meeting of the American Society of Mechanical Engineers, Anaheim, California, December 7-12, 1986. New York, N.Y. (345 E. 47th St., New York 10017): American Society of Mechanical Engineers, 1986.

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5

American Society of Mechanical Engineers. Winter Meeting. Pressure and temperature measurements: Presented at the Winter Annual Meeting of the American Society of Mechanical Engineers, Anaheim, California, December 7-12, 1986. New York, N.Y. (345 E. 47th St., New York 10017): American Society of Mechanical Engineers, 1986.

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6

Wark, Candace. Development of a temperature measurement system with application to a jet in a cross flow experiment. [Washington, D.C.]: National Aeronautics and Space Administration, 1985.

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7

Bernstein, R. L. Large-scale sea surface temperature variability from satellite and shipboard measurements. [s.l.]: National Aeronautics and Space Administration, 1985.

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8

Johnson, Charles B. Dynamic measurement of total temperature, pressure, and velocity in the Langley 0.3-meter transomic cryogenic tunnel. [Washington, D.C.]: National Aeronautics and Space Administration, Scientific and Technical Information Branch, 1986.

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9

Johnson, Charles B. Dynamic measurement of total temperature, pressure, and velocity in the Langley 0.3-Meter Transonic Cryogenic Tunnel. Hampton, Va: Langley Research Center, 1986.

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10

Davis, William D. An algorithm for estimating the plume centerline temperature and ceiling jet temperature in the presence of a hot upper layer. Gaithersburg, MD: U.S. Dept. of Commerce, Technology Administration, National Institute of Standards and Technology, 1998.

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11

Davis, William D. An algorithm for estimating the plume centerline temperature and ceiling jet temperature in the presence of a hot upper layer. Gaithersburg, MD: U.S. Dept. of Commerce, Technology Administration, National Institute of Standards and Technology, 1998.

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12

Wieserman, W. R. High frequency, high temperature specific core loss and dynamic B-H hysteresis loop characteristics of soft magnetic alloys. [Washington, D.C.]: NASA, 1990.

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13

Thermal and Flow Measurements. CRC, 2008.

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14

J, Panda, and NASA Glenn Research Center, eds. Rayleigh scattering diagnostic for dynamic measurement of velocity and temperature. [Cleveland, Ohio]: National Aeronautics and Space Administration, Glenn Research Center, 2001.

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15

V, Farrell Patrick, ed. Optical diagnostics for fluids, solids, and combustion II: 3-4 August, 2003, San Diego, California, USA. Bellingham, Wash: SPIE, 2003.

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16

Optical diagnostics for fluids, solids, and combustion II: 3-4 August 2003, San Diego, California, USA. Bellingham, WA: SPIE, 2004.

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17

National Institute of Standards and Technology (U.S.), ed. Comparison of algorithms to calculate plume centerline temperature and ceiling jet temperature with experiments. [Gaithersburg, Md.?]: U.S. Dept. of Commerce, Technology Administration, National Institute of Standards and Technology, 2000.

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18

F, Foss John, and Lewis Research Center, eds. Development of a temperature measurement system with application to a jet in a cross flow experiment. [Washington, D.C.]: National Aeronautics and Space Administration, 1985.

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19

Mercer, Carolyn. Optical Metrology for Fluids, Combustion and Solids. Springer, 2003.

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20

Brock, Fred V., and Scott J. Richardson. Meteorological Measurement Systems. Oxford University Press, 2001. http://dx.doi.org/10.1093/oso/9780195134513.001.0001.

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This book treats instrumentation used in meteorological surface systems, both on the synoptic scale and the mesoscale, and the instrumentation used in upper air soundings. The text includes material on first- and second-order differential equations as applied to instrument dynamic performance, and required solutions are developed. Sensor physics are emphasized in order to explain how sensors work and to explore the strengths and weaknesses of each design type. The book is organized according to sensor type and function (temperature, humidity, and wind sensors, for example), though several unifying themes are developed for each sensor. Functional diagrams are used to portray sensors as a set of logical functions, and static sensitivity is derived from a sensor's transfer equation, focusing attention on sensor physics and on ways in which particular designs might be improved. Sensor performance specifications are explored, helping to compare various instruments and to tell users what to expect as a reasonable level of performance. Finally, the text examines the critical area of environmental exposure of instruments. In a well-designed, properly installed, and well-maintained meteorological measurement system, exposure problems are usually the largest source of error, making this chapter one of the most useful sections of the book.

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21

A real time dynamic data acquisition and processing system for velocity, density, and total temperature fluctuation measurements. Hampton, Va: National Aeronautics and Space Administration, Langley Research Center, 1991.

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22

Center, Langley Research, ed. A real time dynamic data acquisition and processing system for velocity, density, and total temperature fluctuation measurements. Hampton, Va: National Aeronautics and Space Administration, Langley Research Center, 1991.

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23

R, Mercer Carolyn, Cha Soyoung S, and Shen Gongxin, eds. Optical diagnostics for fluids, solids, and combustion: July 31-2 August 2001, San Diego, USA. Bellingham, Wash., USA: SPIE, 2001.

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24

1952-, Chelton Dudley, and United States. National Aeronautics and Space Administration., eds. Large-scale sea surface temperature variability from satellite and shipboard measurements. [Washington, D.C: National Aeronautics and Space Administration, 1985.

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25

1952-, Chelton Dudley, and United States. National Aeronautics and Space Administration., eds. Large-scale sea surface temperature variability from satellite and shipboard measurements. [Washington, D.C: National Aeronautics and Space Administration, 1985.

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26

Mørup, Steen, Cathrine Frandsen, and Mikkel F. Hansen. Magnetic properties of nanoparticles. Edited by A. V. Narlikar and Y. Y. Fu. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780199533053.013.20.

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This article discusses the magnetic properties of nanoparticles. It first considers magnetic domains and the critical size for single-domain behavior of magnetic nanoparticles before providing an overview of magnetic anisotropy in nanoparticles. It then examines magnetic dynamics in nanoparticles, with particular emphasis on superparamagnetic relaxation and the use of Mössbauer spectroscopy, dc magnetization measurements, and ac susceptibility measurements for studies of superparamagnetic relaxation. It also describes magnetic dynamics below the blocking temperature, magnetic interactions between nanoparticles, and fluctuations of the magnetization directions. Finally, it analyzes the magnetic structure of nanoparticles, focusing on magnetic phase transitions and surface effects, non-collinear spin structures, and magnetic moments of antiferromagnetic nanoparticles.

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27

United States. National Aeronautics and Space Administration., ed. A final report on optical diagnostics of gas-dynamic flows using advanced laser measurement techniques. [Washington, DC: National Aeronautics and Space Administration, 1985.

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28

S, Cha Soyoung, Bryanston-Cross P, Mercer Carolyn R, Society of Photo-optical Instrumentation Engineers., Visualization Society of Japan, and Institution of Mechanical Engineers (Great Britain), eds. Optical diagnostics for fluids/heat/combustion and photomechanics for solids: 21-23 July 1999, Denver, Colorado. Bellingham, Wash., USA: SPIE, 1999.

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29

S, Cha Soyoung, Trolinger Jim, and Society of Photo-optical Instrumentation Engineers., eds. Optical diagnostics in fluid and thermal flow: 14-16 July 1993, San Diego, California. Bellingham, Wash., USA: SPIE, 1993.

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30

S, Cha Soyoung, Trolinger Jim, Kawahashi Masaaki, and Society of Photo-optical Instrumentation Engineers., eds. Optical technology in fluid, thermal, and combustion flow III: 28-31 July 1997, San Diego, California. Bellingham, Wash., USA: SPIE, 1997.

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31

A, Notarianni Kathy, Tapper Phillip Z, and National Institute of Standards and Technology (U.S.), eds. An algorithm for estimating the plume centerline temperature and ceiling jet temperature in the presence of a hot upper layer. Gaithersburg, MD: U.S. Dept. of Commerce, Technology Administration, National Institute of Standards and Technology, 1998.

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32

Structural Testing Technology at High Temperature. Society for Experimental, 1991.

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33

Eriksson, Olle, Anders Bergman, Lars Bergqvist, and Johan Hellsvik. Atomistic Spin Dynamics. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198788669.001.0001.

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The purpose of this book is to provide a theoretical foundation and an understanding of atomistic spin-dynamics, and to give examples of where the atomistic Landau-Lifshitz-Gilbert equation can and should be used. The contents involve a description of density functional theory both from a fundamental viewpoint as well as a practical one, with several examples of how this theory can be used for the evaluation of ground state properties like spin and orbital moments, magnetic form-factors, magnetic anisotropy, Heisenberg exchange parameters, and the Gilbert damping parameter. This book also outlines how interatomic exchange interactions are relevant for the effective field used in the temporal evolution of atomistic spins. The equation of motion for atomistic spin-dynamics is derived starting from the quantum mechanical equation of motion of the spin-operator. It is shown that this lead to the atomistic Landau-Lifshitz-Gilbert equation, provided a Born-Oppenheimer-like approximation is made, where the motion of atomic spins is considered slower than that of the electrons. It is also described how finite temperature effects may enter the theory of atomistic spin-dynamics, via Langevin dynamics. Details of the practical implementation of the resulting stochastic differential equation are provided, and several examples illustrating the accuracy and importance of this method are given. Examples are given of how atomistic spin-dynamics reproduce experimental data of magnon dispersion of bulk and thin-film systems, the damping parameter, the formation of skyrmionic states, all-thermal switching motion, and ultrafast magnetization measurements.

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34

Haan, Patrick Voss-de. Vortex Dynamics in the High-Temperature Superconductors YBa2Cu3O7 and Bi2Sr2CaCu2O8+[delta] in Low- and High-Dissipative Transport Measurement. ibidem-Verlag, 2000.

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35

S, Cha Soyoung, Trolinger Jim, and Society of Photo-optical Instrumentation Engineers., eds. Optical techniques in fluid, thermal, and combustion flow: 10-13 July 1995, San Diego, California. Bellingham, Wash., USA: SPIE, 1995.

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36

Society for Experimental Mechanics (U.S.), ed. Structural testing technology at high temperature: November 4-6, 1991, Stouffer Center Plaza Hotel, Dayton, Ohio. Bethel, CT: The Society for Experimental Mechanics, 1991.

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37

L, Butcher Robert, and United States. National Aeronautics and Space Administration., eds. Spacelab qualified infrared imager for microgravity science experiments. [Washington, D.C: National Aeronautics and Space Administration, 1990.

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38

Jet Propulsion Laboratory (U.S.) and Nova University, eds. Air-sea interaction with SSM/I and altimeter: Report of the NASA Ocean Energy Fluxes Science Working Group. Pasadena, Calif: Jet Propulsion Laboratory, California Institute of Technology, 1985.

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39

Jet Propulsion Laboratory (U.S.) and Nova University, eds. Air-sea interaction with SSM/I and altimeter: Report of the NASA Ocean Energy Fluxes Science Working Group. Pasadena, Calif: Jet Propulsion Laboratory, California Institute of Technology, 1985.

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40

Xue, Yongkang, Yaoming Ma, and Qian Li. Land–Climate Interaction Over the Tibetan Plateau. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.592.

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The Tibetan Plateau (TP) is the largest and highest plateau on Earth. Due to its elevation, it receives much more downward shortwave radiation than other areas, which results in very strong diurnal and seasonal changes of the surface energy components and other meteorological variables, such as surface temperature and the convective atmospheric boundary layer. With such unique land process conditions on a distinct geomorphic unit, the TP has been identified as having the strongest land/atmosphere interactions in the mid-latitudes.Three major TP land/atmosphere interaction issues are presented in this article: (1) Scientists have long been aware of the role of the TP in atmospheric circulation. The view that the TP’s thermal and dynamic forcing drives the Asian monsoon has been prevalent in the literature for decades. In addition to the TP’s topographic effect, diagnostic and modeling studies have shown that the TP provides a huge, elevated heat source to the middle troposphere, and that the sensible heat pump plays a major role in the regional climate and in the formation of the Asian monsoon. Recent modeling studies, however, suggest that the south and west slopes of the Himalayas produce a strong monsoon by insulating warm and moist tropical air from the cold and dry extratropics, so the TP heat source cannot be considered as a factor for driving the Indian monsoon. The climate models’ shortcomings have been speculated to cause the discrepancies/controversies in the modeling results in this aspect. (2) The TP snow cover and Asian monsoon relationship is considered as another hot topic in TP land/atmosphere interaction studies and was proposed as early as 1884. Using ground measurements and remote sensing data available since the 1970s, a number of studies have confirmed the empirical relationship between TP snow cover and the Asian monsoon, albeit sometimes with different signs. Sensitivity studies using numerical modeling have also demonstrated the effects of snow on the monsoon but were normally tested with specified extreme snow cover conditions. There are also controversies regarding the possible mechanisms through which snow affects the monsoon. Currently, snow is no longer a factor in the statistic prediction model for the Indian monsoon prediction in the Indian Meteorological Department. These controversial issues indicate the necessity of having measurements that are more comprehensive over the TP to better understand the nature of the TP land/atmosphere interactions and evaluate the model-produced results. (3) The TP is one of the major areas in China greatly affected by land degradation due to both natural processes and anthropogenic activities. Preliminary modeling studies have been conducted to assess its possible impact on climate and regional hydrology. Assessments using global and regional models with more realistic TP land degradation data are imperative.Due to high elevation and harsh climate conditions, measurements over the TP used to be sparse. Fortunately, since the 1990s, state-of-the-art observational long-term station networks in the TP and neighboring regions have been established. Four large field experiments since 1996, among many observational activities, are presented in this article. These experiments should greatly help further research on TP land/atmosphere interactions.

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41

Delgado Martín, Jordi, Andrea Muñoz-Ibáñez, and Ismael Himar Falcón-Suárez. 6th International Workshop on Rock Physics: A Coruña, Spain 13 -17 June 2022: Book of Abstracts. 2022nd ed. Servizo de Publicacións da UDC, 2022. http://dx.doi.org/10.17979/spudc.000005.

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[Abstract] The 6th International Workshop on Rock Physics (6IWRP) was held A Coruña, Spain, between 13th and 17th of June, 2022. This meeting follows the track of the five successful encounters held in Golden (USA, 2011), Southampton (UK, 2013), Perth (Australia, 2015), Trondheim (Norway, 2017) and Hong Kong (China, 2019). The aim of the workshop was to bring together experiences allowing to illustrate, discuss and exchange recent advances in the wide realm of rock physics, including theoretical developments, in situ and laboratory scale experiments as well as digital analysis. While rock physics is at the core of the oil & gas industry applications, it is also essential to enable the energy transition challenge (e.g. CO2 and H2 storage, geothermal), ensure a safe and adequate use of natural resources and develop efficient waste management strategies. The topics of 6IWRP covered a broad spectrum of rock physics-related research activities, including: • Experimental rock physics. New techniques, approaches and applications; Characterization of the static and dynamic properties of rocks and fluids; Multiphysics measurements (NMR, electrical resistivity…); Deep/crustal scale rock physics. • Modelling and multiscale applications: from the lab to the field. Numerical analysis and model development; Data science applications; Upscaling; Microseismicity and earthquakes; Subsurface stresses and tectonic deformations. • Coupled phenomena and rock properties: exploring interactions. Anisotropy; Flow and fractures; Temperature effects; Rock-fluid interaction; Fluid and pressure effects on geophysical signatures. • The energy transition challenge. Applications to energy storage (hydrogen storage in porous media), geothermal resources, energy production (gas hydrates), geological utilization and storage of CO2, nuclear waste disposal. • Rock physics templates: advances and applications. Quantitative assessment; Applications to reser voir characterization (role of seismic wave anisotropy and fracture networks). • Advanced rock physics tools. Machine learning; application of imaging (X-ray CT, X-ray μCT, FIB-SEM…) to obtain rock proper ties. This book compiles more than 50 abstracts, summarizing the works presented in the 6IWRP by rock physicists from all over the world, belonging to both academia and industry. This book means an updated overview of the rock physics research worldwide.

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