𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Quantitative determination of the mordenite content of natural zeolite rocks by infrared spectroscopy

✍ Scribed by J. Hlavay; I. Vassányi; J. Inczédy


Publisher
Elsevier Science
Year
1985
Tongue
English
Weight
177 KB
Volume
41
Category
Article
ISSN
1386-1425

No coin nor oath required. For personal study only.


📜 SIMILAR VOLUMES


The quantitative determination of glass
✍ A.R.N. Eberendu; K.E. Daugherty 📂 Article 📅 1984 🏛 Elsevier Science 🌐 English ⚖ 447 KB

Determinations of the glass content of synthetic and blast furnace slags by infrared absorption spectroscopy are described. A linear relationship e×ists between the calculated infrared absorption R-values and the percentage glass determined by optical microscopy count. The use of an internal standar

Determination of the base pairing conten
✍ George J. Thomas Jr. 📂 Article 📅 1969 🏛 Wiley (John Wiley & Sons) 🌐 English ⚖ 544 KB

A method is described for determiniig the fractions of adenineuracil and guaninecytosine base pain of partly double-helical ribonucleic acids in aqueous solution. The method is based upon the ability to distinguish between paired and unpaired bases by means of infrared spectroscopy of their deuteriu

Quantitative determination of polymer an
✍ N. Dupuy; C. Ruckebusch; L. Duponchel; P. Beurdeley-Saudou; B. Amram; J.P. Huven 📂 Article 📅 1996 🏛 Elsevier Science 🌐 English ⚖ 595 KB

The quality of a printed image on coated papers, to a great extent, depends on the coating surface properties (nature of the components, relative abundance and so on). The potential of infrared spectroscopy as a rapid analytical technique for the quantitative analysis of the coating is demonstrated.

Determination of the base-pairing conten
✍ U. Schernau; Th. Ackermann 📂 Article 📅 1977 🏛 Wiley (John Wiley & Sons) 🌐 English ⚖ 448 KB 👁 1 views

## Abstract Infrared spectroscopy was used for the determination of the base‐pairing content of four specific tRNAs in deuterium oxide solution. Infrared spectra were obtained in the 1750–1550 cm^−1^ region at various temperatures ranging from about 15 to 90°C. Melting curves were constructed by pl