Semiheavy water

Last updated
Semiheavy water
Spacefill model of water Semiheavy-water-3D-vdW.png
Spacefill model of water
Semiheavy water.svg
Names
IUPAC name
(2H1)Water
Other names
Deuterium hydrogen monoxide
Deuterium hydrogen oxide, Water-d1, Water-d
Identifiers
3D model (JSmol)
ChEBI
ChemSpider
115
PubChem CID
  • InChI=1S/H2O/h1H2/i/hD
    Key: XLYOFNOQVPJJNP-DYCDLGHISA-N
  • [2H]O
Properties
H2HO or HDO
Molar mass 19.0214 g mol−1
Appearance Very pale blue, transparent liquid, very similar to regular water
Density 1.054 g cm−3
Melting point 3.81 °C (38.86 °F; 276.96 K)
Boiling point 100.74 °C (213.33 °F; 373.89 K)
miscible
log P −0.65
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
X mark.svgN  verify  (what is  Yes check.svgYX mark.svgN ?)

Semiheavy water (HDO) is a naturally occurring chemical variant of water. Other variants include heavy water (D2O), and H2O. It shares most of its properties with common water (1H2O), with its distinguishing feature being a single hydrogen atom per water molecule being of the heavier isotope deuterium (2H or D), as opposed to the far more common protium (1H). This difference of one more neutron in one of the hydrogen atoms does not notably change its chemical properties, as these are mostly dictated by the number of valence electrons an atom has. The only notable difference to common water is a larger mass, as a result of the extra neutron per atom. Thus, when the same volume of HDO and H2O are weighed, the HDO will be heavier, lending it its name.

In an amount of water, about 1 molecule in 3,200 is HDO (one hydrogen in 6,400 is 2H). By comparison, heavy water [1] occurs at a proportion of about 1 molecule in 41 million (i.e., 1 in 6,4002). This makes semiheavy water far more common than heavy water (D2O).

Contents

The freezing point of semiheavy water is close to the freezing point of heavy water at 3.81°C, with the freezing point of heavy water being 3.82°C.

Production

On Earth, semiheavy water occurs naturally in normal water at a proportion of about 1 molecule in 3,200; because 1 in 6,400 hydrogen atoms in water is deuterium, which is 1 part in 3,200 by weight. HDO may be separated from normal water by distillation or electrolysis, or by various chemical exchange processes, all of which exploit a kinetic isotope effect. Partial enrichment also occurs in natural bodies of water under certain evaporation conditions. [2] (For more information about the distribution of deuterium in water, see Vienna Standard Mean Ocean Water and Hydrogen isotope biogeochemistry.)

See also

References

  1. "Heavy water | chemical compound". Encyclopedia Britannica. Retrieved 2019-04-24.
  2. Craig, H.; Gordon, L. I.; Horibe, Y. (1963). "Isotopic exchange effects in the evaporation of water: 1. Low-temperature experimental results". Journal of Geophysical Research. 68 (17): 5079–5087. Bibcode:1963JGR....68.5079C. doi:10.1029/JZ068i017p05079.

Further reading