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Benzylamine, also known as phenylmethylamine, is an organic chemical compound with the condensed structural formula C 6 H 5 CH 2 NH 2 (sometimes abbreviated as PhCH 2 NH 2 or BnNH 2). It consists of a benzyl group, C 6 H 5 CH 2, attached to an amine functional group , NH 2 .
Dibenzylamine is an organic compound with the formula (C 6 H 5 CH 2) 2 NH.It is classified as a secondary amine, being the middle member of the series that includes the primary amine benzylamine (C 6 H 5 CH 2 NH 2) and the tertiary amine tribenzylamine ((C 6 H 5 CH 2) 3 N).
Solubility in water. 1.2 g/100mL Hazards GHS labelling: Pictograms. ... N,N-Dimethylbenzylamine can be synthesized by the Eschweiler–Clarke reaction of benzylamine ...
Pargyline is an derivative of benzylamine and is also known as N-methyl-N-propargylbenzylamine. [13] [49] It is used pharmaceutically as the hydrochloride salt. [4] [5] [13] Pargyline is a lipophilic compound, with a predicted log P of about 2.1. [49] [26]
This page contains tables of azeotrope data for various binary and ternary mixtures of solvents. The data include the composition of a mixture by weight (in binary azeotropes, when only one fraction is given, it is the fraction of the second component), the boiling point (b.p.) of a component, the boiling point of a mixture, and the specific gravity of the mixture.
N-isopropylbenzylamine is a compound that has appeared in chemical literature often playing an intermediary role in applications of experimental synthesis and novel organic transformations.
1-Phenylethylamine may be prepared by the reductive amination of acetophenone: [1]. C 6 H 5 C(O)CH 3 + NH 3 + H 2 → C 6 H 5 CH(NH 2)CH 3 + H 2 O. The Leuckart reaction, using ammonium formate, is another method for this transformation.
A solubility equilibrium exists when a chemical compound in the solid state is in chemical equilibrium with a solution containing the compound. This type of equilibrium is an example of dynamic equilibrium in that some individual molecules migrate between the solid and solution phases such that the rates of dissolution and precipitation are equal to one another.