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Books on the topic 'Total pressure and total temperature measurement'

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Author: Grafiati
Published: 10 March 2023

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1

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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2

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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3

Total pressure measurements in vacuum technology. Orlando: Academic Press, 1985.

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4

Leck, J. H. Total and partial pressure measurement in vacuum systems. Glasgow: Blackie, 1989.

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5

Leck, J. H. Total and Partial Pressure Measurement in Vacuum Systems. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4613-0877-5.

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6

Outlaw, R. A. Introduction to total, and partial, pressure measurements in vacuum systems. Washington, D.C: National Aeronautics and Space Administration, Office of Management, Scientific and Technical Information Division, 1989.

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7

Outlaw, R. A. Introduction to total- and partial-pressure measurements in vacuum systems. Washington D.C: National Aeronautics and Space Administration, 1989.

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8

Howard, Dave. Wind River Watershed temperature total maximum daily load: Detailed implementation plan. Olympia, WA: Washington State Dept. of Ecology, 2004.

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9

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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10

Angell, J. K. Annual and seasonal global variation in total ozone and layer-mean ozone, 1958-1985. Oak Ridge, Tenn: Oak Ridge National Laboratory, 1987.

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11

Tanner, Dwight Q. Total dissolved gas, barometric pressure, and water temperature data, lower Columbia River, Oregon and Washington, 1996. Portland, Or: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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12

E, Harrison Howard, McKenzie Stuart W, United States. Army. Corps of Engineers, and Geological Survey (U.S.), eds. Total dissolved gas, barometric pressure, and water temperature data, lower Columbia River, Oregon and Washington, 1996. Portland, Or: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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13

Berman, A. Total Pressure Measurements in Vacuum Technology. Elsevier Science & Technology Books, 2014.

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14

Total and Partial Pressure Measurement in Vacuum Systems. Springer, 2011.

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15

Leck, John Henry. Total and Partial Pressure Measurement in Vacuum Systems. Springer, 2012.

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16

Leck, John Henry. Total and Partial Pressure Measurement in Vacuum Systems. Springer London, Limited, 2012.

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17

Impact Pressure and Total Temperature Interpretation at Hypersonic Mach Number. Creative Media Partners, LLC, 2021.

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18

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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19

Comparison of total peripheral resistance and blood velocity as obtained from Doppler ultrasound waveforms during rest, exercise and recovery. 1991.

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20

Comparison of total peripheral resistance and blood velocity as obtained from Doppler ultrasound waveforms during rest, exercise and recovery. 1991.

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21

Comparison of total peripheral resistance and blood velocity as obtained from Doppler ultrasound waveforms during rest, exercise and recovery. 1992.

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22

Clarke, Andrew. Energy and heat. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199551668.003.0002.

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Energy is the capacity to do work and heat is the spontaneous flow of energy from one body or system to another through the random movement of atoms or molecules. The entropy of a system determines how much of its internal energy is unavailable for work under isothermal conditions, and the Gibbs energy is the energy available for work under isothermal conditions and constant pressure. The Second Law of Thermodynamics states that for any reaction to proceed spontaneously the total entropy (system plus surroundings) must increase, which is why metabolic processes release heat. All organisms are thermodynamically open systems, exchanging both energy and matter with their surroundings. They can decrease their entropy in growth and development by ensuring a greater increase in the entropy of the environment. For an ideal gas in thermal equilibrium the distribution of energy across the component atoms or molecules is described by the Maxwell-Boltzmann equation. This distribution is fixed by the temperature of the system.
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23

Sherwood, Dennis, and Paul Dalby. Thermodynamics and mathematics. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198782957.003.0004.

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Most school mathematics is about how one variable, y, varies with respect to one other variable, x, according to an equation such as y = 3x2. Equations like this underpin the student’s knowledge of algebra, and differential and integral calculus. Thermodynamics, however, is necessarily about how a variable, such as the pressure P, varies with respect not to one but to three variables simultaneously – for example, the mole number n, the volume V, and the temperature T. This makes the algebra of thermodynamics more complex, and also implies that mutual changes between pairs of variables is described not in terms of total derivatives of the form dy/dx, but rather by partial derivatives of the form (∂P/∂T)V. Many students find the leap from dy/dx to (∂P/∂T)V very difficult - the purpose of this chapter is therefore to build the reader’s confidence in understanding, and manipulating, functions of two and three variables.
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24

Baloh, Robert W. Hallpike’s Caloric Test. Oxford University Press, 2016. http://dx.doi.org/10.1093/med/9780190600129.003.0015.

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Charles Hallpike decided that greater precision could be obtained with the caloric test by measurement of one or more attributes of the responses to some suitably graded stimulus. He chose to measure the duration of induced nystagmus. Hallpike chose water at 30°C and 44°C (7°C below and above body temperature, respectively) and allowed it to flow for 40 seconds. These temperatures were generally well tolerated, and the comparatively large quantity of water and rapid flow minimized errors due to misdirecting the stream within the ear canal. A simple chart was used to summarize the results of the bithermal caloric test. The chart consisted of two continuous lines, each representing a total of a 3-minute period, subdivided into 10-second intervals. Hallpike conducted a series of experiments on the phenomenon of directional preponderance with caloric testing and emphasized the importance of vestibular tonus originating from the inner ear receptors.
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