T iron - ορισμός. Τι είναι το T iron
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Τι (ποιος) είναι T iron - ορισμός

NUCLIDES WITH ATOMIC NUMBER OF 26, BUT WITH DIFFERING MASS NUMBERS
Iron-60; Iron-57; Iron-58; Iron-54; Iron isotopes; Iron-52; Iron-53; Iron-59; Iron-45; Iron-46; Iron-47; Iron-48; Iron-49; Iron-50; Iron-51; Iron-61; Iron-62; Iron-63; Iron-64; Iron-65; Iron-66; Iron-67; Iron-68; Iron-69; Iron-70; Iron-71; Iron-72; Iron-52m; Iron-53m; Iron-54m; Iron-61m; Iron-65m; Iron-67m; Iron 60; Iron isotope

T iron      
·- ·see under T.
sad iron         
  • Flat iron stove
  • Iron collection
  • [[Josephine Baker]] ironing (1956)
  • Box iron ([[Minalin, Pampanga]], [[Philippines]] Museum).
  • A 1950s [[Morphy Richards]] electric iron with original box
  • Pereslavl]]
TOOL OR APPLIANCE FOR SMOOTHING CLOTH USING HEAT AND PRESSURE
Sad iron; Steam iron; Electric iron; Tailor's goose; Iron (appliance); Clothes pressing iron; Flatiron (appliance); Goffering iron; Laundry iron; Clothing iron; Sadiron; Steam generator iron
¦ noun historical a flat iron.
Origin
from sad, in the obs. sense 'weighty'.
steam iron         
  • Flat iron stove
  • Iron collection
  • [[Josephine Baker]] ironing (1956)
  • Box iron ([[Minalin, Pampanga]], [[Philippines]] Museum).
  • A 1950s [[Morphy Richards]] electric iron with original box
  • Pereslavl]]
TOOL OR APPLIANCE FOR SMOOTHING CLOTH USING HEAT AND PRESSURE
Sad iron; Steam iron; Electric iron; Tailor's goose; Iron (appliance); Clothes pressing iron; Flatiron (appliance); Goffering iron; Laundry iron; Clothing iron; Sadiron; Steam generator iron
¦ noun an electric iron that emits steam from holes in its flat surface.

Βικιπαίδεια

Isotopes of iron

Naturally occurring iron (26Fe) consists of four stable isotopes: 5.845% of 54Fe (possibly radioactive with a half-life over 4.4×1020 years), 91.754% of 56Fe, 2.119% of 57Fe and 0.286% of 58Fe. There are 24 known radioactive isotopes, the most stable of which are 60Fe (half-life 2.6 million years) and 55Fe (half-life 2.7 years).

Much of the past work on measuring the isotopic composition of Fe has centered on determining 60Fe variations due to processes accompanying nucleosynthesis (i.e., meteorite studies) and ore formation. In the last decade however, advances in mass spectrometry technology have allowed the detection and quantification of minute, naturally occurring variations in the ratios of the stable isotopes of iron. Much of this work has been driven by the Earth and planetary science communities, although applications to biological and industrial systems are beginning to emerge.