Climax / Ioannis Scholastici ab Ambrosio monacho Camaldulensi è graeco in latinum conuersus, et nunc primum editus.

Marca tip. en port. (Zappella, 226)

Mystico epithalamio : cantico nupcial armonioso ... en el desposorio sagrado ... con ... Christo ... siendo en el siglo Doña Josepha Duran, Rubio, Tallada y Salinas, en la religion la Mad.e Teresa Josepha de Jesus en el ... convento de Carmelitas Descalzas de San Joseph de ... Valencia

Texto fechado en 1753

Bibliotheque françoise ou Histoire de la litterature françoise : dans laquelle on montre l'utilité que l'on peut retirer des livres publiés en françois depuis l'origine de l'imprimerie ... /

Mode of access: Internet.

Patología interna /

Mode of access: Internet.

Water network dynamics at the critical moment of a peptide's ß-turn formation:a molecular dynamics study

All-atom molecular dynamics simulations for a single molecule of Leu-Enkephalin in aqueous solution have been used to study the role of the water network during the formation of ß-turns. We give a detailed account of the intramolecular hydrogen bonding, the water-peptide hydrogen bonding, and the orientation and residence times of water molecules focusing on the short critical periods of transition to the stable ß-turns. These studies suggest that, when intramolecular hydrogen bonding between the first and fourth residue of the ß-turn is not present, the disruption of the water network and the establishment of water bridges constitute decisive factors in the formation and stability of the ß-turn. Finally, we provide possible explanations and mechanisms for the formations of different kinds of ß-turns.

Grain size composition of ocean and sea bottom sediments

On the basis of a long term research of the authors a database model of grain size composition of unlithified marine and ocean bottom sediments has been created. An improved method of water-mechanical analysis has been offered. Grain size parameters of main types of bottom sediments have been measured and calculated. The genetic interpretation of results and regularities of sandy, aleuritic and pelitic material in basins of sedimentation are under discussion.