isomass

English

Etymology

iso- +‎ mass

Noun

isomass

(physics) A condition of having the same mass.
- 2004, Klaus G. Heumann, Handbook of Elemental Speciation: Techniques and Methodology, →ISBN:
  If a packet of isomass ions is accelerated through the same potential difference, the ions will achieve an equal velocity and arrive at the detector with a time spread corresponding to their initial spatial distribution in the direction of the flight tube.
- 2010, H. V. Klapdor-Kleingrothaus, Seventy Years of Double Beta Decay, →ISBN:
  In Fig. 4 the isomass lines of equal m_ee in the oscillation parameter space are shown, together with various bounds from existing and future reactor and accelerator oscillation experiments.
- 2013, Sarah A. Fagents, ‎Tracy K. P. Gregg, & ‎Rosaly M. C. Lopes, Modeling Volcanic Processes: The Physics and Mathematics of Volcanism, →ISBN:
  Values of square root of area and mass/area of isomass lines for the Etna 1998 tephra deposit.
(cyrstallography) The mechanism by which crystal formation tends toward spherical formations which minimize the surface to volume ratio.

单词	isomass
释义	isomass English Etymology iso- +‎ mass Noun isomass (physics) A condition of having the same mass. 2004, Klaus G. Heumann, Handbook of Elemental Speciation: Techniques and Methodology, →ISBN: If a packet of isomass ions is accelerated through the same potential difference, the ions will achieve an equal velocity and arrive at the detector with a time spread corresponding to their initial spatial distribution in the direction of the flight tube. 2010, H. V. Klapdor-Kleingrothaus, Seventy Years of Double Beta Decay, →ISBN: In Fig. 4 the isomass lines of equal m_ee in the oscillation parameter space are shown, together with various bounds from existing and future reactor and accelerator oscillation experiments. 2013, Sarah A. Fagents, ‎Tracy K. P. Gregg, & ‎Rosaly M. C. Lopes, Modeling Volcanic Processes: The Physics and Mathematics of Volcanism, →ISBN: Values of square root of area and mass/area of isomass lines for the Etna 1998 tephra deposit. (cyrstallography) The mechanism by which crystal formation tends toward spherical formations which minimize the surface to volume ratio.
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