The alkali fluoride and carbonate bead test for uranium /

"April 1956."

De alkali volatilis usu tam interno quam externo [Manuscrito]/

Mode of access: Internet.

Expériences propres a faire connoitre que l'alkali volatil fluor est le remede le plus efficace dans les asphysies : avec des Remarques sur les Effets avantageux qu'il produit dans la morsure de la vipère, dasn la Rage, la Brulure, l'Apoplexie & c /

Mode of access: Internet.

Observations nouvelles sur les propriétés de l'alkali fluor ammoniacal : : d'après quelques Expériences faites par M.B***, du Collège royal & Académie de Chirurgie de Paris.

Mode of access: Internet.

Expériences propres à faire connoitre que l'alkali volatil fluor est le remède le plus efficace dans les axphyxies : avec les remarques sur les effets aventageux qu'il produit dans lamorsure de la vipère, dans la rage, la brulure, l'apoplexie, etc. /

Anteport.

A Theoretical and practical treatise on the manufacture of sulphuric acid and alkali : with the collateral branches /

Vol. 2-3 have title: The manufacture of sulphuric acid and alkali, with the collateral branches; a theoretical and practical treatise.

Crops used in the reclamation of alkali lands in Egypt /

Mode of access: Internet.

Reclamation of alkali soils /

Mode of access: Internet.

Disertación sobre el alkali volátil, leida en las oposiciones públicas para las plazas vacantes de la Real Botica,

Mode of access: Internet.

Reclamation of the Fresno type of black-alkali soil /

Mode of access: Internet.

A theoretical and practical treatise on the manufacture of sulphuric acid and alkali, with the collateral branches.

Mode of access: Internet.

Ueber das einwirkungsprodukt von alkali auf substituierte hydra...

Thesis (doctoral)--

Uber das verhalten einiger diketopiperazine gegen alkali.

Thesis (doctoral)--

Controlled trial of hyperbaric oxygen treatment for alkali corneal burn in the rabbit

Purpose: To evaluate the efficacy of hyperbaric oxygen therapy in the treatment of alkali-induced corneal burns in an animal model. Methods: Twenty-four rabbits were randomized into a control group (n = 12) and hyperbaric oxygen treatment group (n = 12). After induction of anaesthesia, the alkali burn model was established by application of 1 N sodium hydroxide to one eye of each rabbit. The hyperbaric oxygen treatment group was treated each day for 21 days with hyperbaric oxygen at 2.4 Atmospheres Absolute (ATA) for 1 h. The eyes of the animals were examined daily for 2 weeks and then weekly until the end of the trial. The principal endpoint was that of perforation of the cornea at which time the animals were killed with a lethal dose of either intravenous or intraperitoneal barbiturate and the eyes immediately enucleated and fixed in 10% neutral buffered formalin. All animals in which complete healing took placed were also killed, the eyes removed, fixed and examined histologically. Photographs were taken of the rabbit's eyes at weekly intervals and the area of vascularization and epithelial defects in the hyperbaric and control groups were compared. Results: Equal numbers (seven) of the control and hyperbaric oxygen treated groups had perforated corneas and there was no statistical difference in the mean time to perforation (control 30.1 days; treated 30 days). There was also no statistical difference between the two groups with respect to epithelial defect size. Conclusion: Treatment with hyperbaric oxygen for 1 h daily for 21 days had no beneficial effect on alkali-induced corneal burns.

The igneous charnockite—high-K alkali-calcic I-type granite—incipient charnockite association in Trivandrum Block, southern India

The Pan-African (640 Ma) Chengannoor granite intrudes the NW margin of the Neoproterozoic high-grade metamorphic terrain of the Trivandrum Block (TB), southern India, and is spatially associated with the Cardamom hills igneous charnockite massif (CM). Geochemical features characterize the Chengannoor granite as high-K alkali-calcic I-type granite. Within the constraints imposed by the high temperature, anhydrous, K-rich nature of the magmas, comparison with recent experimental studies on various granitold source compositions, and trace- and rare-earth-element modelling, the distinctive features of the Chengannoor granite reflect a source rock of igneous charnockitic nature. A petrogenetic model is proposed whereby there was a period of basaltic underplating; the partial melting of this basaltic lower crust formed the CM charnockites. The Chengannoor granite was produced by the partial melting of the charnoenderbites from the CM, with subsequent fractionation dominated by feldspars. In a regional context, the Chengannoor I-type granite is considered as a possible heat source for the near-UHT nature of metamorphism in the northern part of the TB. This is different from previous studies, which favoured CM charnockite as the major heat source. The Occurrence of incipient charnockites (both large scale as well as small scale) adjacent to the granite as well as pegmatites (which contain CO2, CO2-H2O, F and other volatiles), suggests that the fluids expelled from the alkaline magma upon solidification generated incipient charnockites through fluid-induced lowering of water activity. Thus the granite and associated alkaline pegmatites acted as conduits for the transfer of heat and volatiles in the Achankovil Shear Zone area, causing pervasive as well as patchy charnockite formation. The transport Of CO2 by felsic melts through the southern Indian middle crust is suggested to be part of a crustal-scale fluid system that linked mantle heat and CO2 input with upward migration of crustally derived felsic melts and incipient charnockite formation, resulting in an igneous charnockite - I-type granite - incipient charnockite association.