Μετάφραση και ανάλυση λέξεων από την τεχνητή νοημοσύνη ChatGPT
Σε αυτήν τη σελίδα μπορείτε να λάβετε μια λεπτομερή ανάλυση μιας λέξης ή μιας φράσης, η οποία δημιουργήθηκε χρησιμοποιώντας το ChatGPT, την καλύτερη τεχνολογία τεχνητής νοημοσύνης μέχρι σήμερα:
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- χρησιμοποιείται πιο συχνά στον προφορικό ή γραπτό λόγο
- επιλογές μετάφρασης λέξεων
- παραδείγματα χρήσης (πολλές φράσεις με μετάφραση)
- ετυμολογία
Τι (ποιος) είναι gaseous$30967$ - ορισμός
![Isothermal curves depicting the non-ideality of a ''real gas.'' The changes in volume (depicted by Z, [[compressibility factor]]) which occur as the pressure is varied.
The compressibility factor Z, is equal to the ratio Z = PV/nRT.
An ideal gas, with compressibility factor Z = 1, is described by the horizontal line where the y-axis is equal to 1. Non-ideality can be described as the deviation of a gas above or below Z = 1.](https://commons.wikimedia.org/wiki/Special:FilePath/Compressibility Factor of Air 75-200 K.png?width=200 "Isothermal curves depicting the non-ideality of a ''real gas.'' The changes in volume (depicted by Z, [[compressibility factor]]) which occur as the pressure is varied.
The compressibility factor Z, is equal to the ratio Z = PV/nRT.
An ideal gas, with compressibility factor Z = 1, is described by the horizontal line where the y-axis is equal to 1. Non-ideality can be described as the deviation of a gas above or below Z = 1.")
![Dalton]]'s notation.](https://commons.wikimedia.org/wiki/Special:FilePath/Daltons symbols.gif?width=200 "Dalton]]'s notation.")
![Random motion of gas particles results in [[diffusion]].](https://commons.wikimedia.org/wiki/Special:FilePath/Diffusion animation.gif?width=200 "Random motion of gas particles results in [[diffusion]].")
![21 April 1990 eruption of [[Mount Redoubt]], Alaska, illustrating real gases not in thermodynamic equilibrium.](https://commons.wikimedia.org/wiki/Special:FilePath/MountRedoubtEruption.jpg?width=200 "21 April 1990 eruption of [[Mount Redoubt]], Alaska, illustrating real gases not in thermodynamic equilibrium.")
![[[Delta wing]] in wind tunnel. The shadows form as the indices of refraction change within the gas as it compresses on the leading edge of this wing.](https://commons.wikimedia.org/wiki/Special:FilePath/Schlierenfoto Mach 17 Delta - NASA.jpg?width=200 "[[Delta wing]] in wind tunnel. The shadows form as the indices of refraction change within the gas as it compresses on the leading edge of this wing.")
![Robinson Crusoe Islands]] on 15 September 1999, shows a turbulent cloud pattern called a [[Kármán vortex street]]](https://commons.wikimedia.org/wiki/Special:FilePath/Vortex-street-1.jpg?width=200 "Robinson Crusoe Islands]] on 15 September 1999, shows a turbulent cloud pattern called a [[Kármán vortex street]]")
You're gas, wheezed Simon, laughing at his Pal's latest joke.
Βικιπαίδεια
Gaseous ionization detectors are radiation detection instruments used in particle physics to detect the presence of ionizing particles, and in radiation protection applications to measure ionizing radiation.
They use the ionising effect of radiation upon a gas-filled sensor. If a particle has enough energy to ionize a gas atom or molecule, the resulting electrons and ions cause a current flow which can be measured.
Gaseous ionisation detectors form an important group of instruments used for radiation detection and measurement. This article gives a quick overview of the principal types, and more detailed information can be found in the articles on each instrument. The accompanying plot shows the variation of ion pair generation with varying applied voltage for constant incident radiation. There are three main practical operating regions, one of which each type utilises.
