TY - JOUR
T1 - Physical properties of heavy-oxygen water. Absolute viscosity of H 2 18 O between 15 and 35° C
AU - Kudish, AI
AU - Wolf, D
AU - Steckel, F
PY - 1972
Y1 - 1972
N2 - The absolute viscosity of highly enriched heavy-oxygen water, H 218O, has been measured at 5°C intervals between 15 and 35°C, using a semi-automatic closed viscometer of the suspended-level type. A linear extrapolation was performed to determine the viscosity of 100% heavy-oxygen water, based upon the measured viscosity of natural water and that of a highly enriched heavy-oxygen water sample. The effect of isotope substitution on the viscosity of natural water has been analyzed for both H 218O and D216O. The viscosity ratio at 25°C for H218O/H216O is 1.0536, whereas that for D216O/H216O is 1.2316.
AB - The absolute viscosity of highly enriched heavy-oxygen water, H 218O, has been measured at 5°C intervals between 15 and 35°C, using a semi-automatic closed viscometer of the suspended-level type. A linear extrapolation was performed to determine the viscosity of 100% heavy-oxygen water, based upon the measured viscosity of natural water and that of a highly enriched heavy-oxygen water sample. The effect of isotope substitution on the viscosity of natural water has been analyzed for both H 218O and D216O. The viscosity ratio at 25°C for H218O/H216O is 1.0536, whereas that for D216O/H216O is 1.2316.
UR - http://www.scopus.com/inward/record.url?scp=0042311074&partnerID=8YFLogxK
U2 - 10.1039/F19726802041
DO - 10.1039/F19726802041
M3 - Article
AN - SCOPUS:0042311074
SN - 2050-5663
VL - 68
SP - 2041
EP - 2046
JO - Journal of the Chemical Society, Faraday Transactions 1: Physical Chemistry in Condensed Phases
JF - Journal of the Chemical Society, Faraday Transactions 1: Physical Chemistry in Condensed Phases
ER -