142770-42-1 Purity
97%
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Isotope substitution has a great influence on the dielectric relaxation dynamics of hydrogen-bonded liquid water. This work studies the dielectric relaxation of light water (H216O), heavy water (D216O) and heavy oxygen water (H218O) in the temperature range of 278 to 338 K. Important conclusions include:
· Upon H/D exchange, it was observed a 20-35% increase in the corresponding relaxation time, while the substitution of 16O with 18O leads to a significantly smaller slow-down in dynamics, approximately 4-5%. When analyzing the thermal activation of relaxation using the extended Eyring theory, it can be found that the activation parameters for H216O and H218O are nearly identical.
· The increase in the relaxation time for H218O compared to H216O appears to be independent of temperature, indicating that the isotope effect is primarily influenced by classical mass effects that do not rely on temperature. The enhancement observed with 16O/18O substitution can be accurately described by the translational mass factor, even though the dipolar relaxation of water is inherently rotational, which would typically suggest that moments of inertia should dictate the relaxation time. The rise in relaxation time correlates with an increase in viscosity, implying that the deceleration of relaxation dynamics in H218O is driven by greater viscous friction.
· In contrast, the increase in relaxation time due to H/D exchange is significantly more pronounced and displays a strong dependence on temperature. Nonetheless, when scaling the relaxation times of D216O with the translational mass factor and adjusting for nuclear quantum effects with a corresponding temperature shift, these values align with those of H216O.
This work studied the effects of deuterated water (2H2O) and heavy-oxygen water (H218O) on the sliding speed of microtubules on kinesin-1 coated surfaces. It was found that an increase in the fraction of isotopic water used in the motility solution led to a decrease in the sliding speed of microtubules. These findings suggest that water isotopes appear to be an effective experimental knob for studying the effects of water on kinesin activity.
For each data point, several hundred microtubules were monitored at a stable temperature of 33.1 ± 0.1 °C. In the heavy-hydrogen water experiment, the calculated speed with 100% light water was 1016 ± 11 nm/s, whereas in the heavy-oxygen water experiment, it was recorded at 1007 ± 4 nm/s. An increase in either the heavy-hydrogen water buffer or the heavy-oxygen water buffer in the motility solution led to a linear decline in the estimated speed measurements.
At the highest concentration of the heavy-hydrogen water buffer tested, the estimated gliding speed dropped to 799 ± 8 nm/s, whereas the heavy-oxygen water buffer yielded a speed of 954 ± 16 nm/s. When compared to the light water buffer, the speed reduction for the heavy-hydrogen water was around 21%, and for the heavy-oxygen water, it was approximately 5%. This analysis also incorporates data from the deuterium-depleted light water buffer, which recorded a most probable speed of 1015 ± 4 nm/s.
The molecular formula of heavy-oxygen water is H2O.
Some synonyms of heavy-oxygen water are Water-18O, Oxygen-18, Water O-18.
The molecular weight of heavy-oxygen water is 20.015 g/mol.
Heavy-oxygen water was created on August 8, 2005.
The IUPAC name of heavy-oxygen water is oxidane.
The InChI of heavy-oxygen water is InChI=1S/H2O/h1H2/i1+2.
The InChIKey of heavy-oxygen water is XLYOFNOQVPJJNP-NJFSPNSNSA-N.
The CAS number of heavy-oxygen water is 14314-42-2.
The UNII of heavy-oxygen water is 7QV8F8BYNJ.
The molecular weight of heavy-oxygen water is 20.015 g/mol (computed by PubChem 2.1).