ملخص
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.
| اللغة الأصلية | الإنجليزيّة |
|---|---|
| الصفحات (من إلى) | 2041-2046 |
| عدد الصفحات | 6 |
| دورية | Journal of the Chemical Society, Faraday Transactions I |
| مستوى الصوت | 68 |
| المعرِّفات الرقمية للأشياء | |
| حالة النشر | نُشِر - 1972 |
| منشور خارجيًا | نعم |
بصمة
أدرس بدقة موضوعات البحث “Physical properties of heavy-oxygen water. Absolute viscosity of H 218O between 15 and 35°C'. فهما يشكلان معًا بصمة فريدة.قم بذكر هذا
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