Anthranilic acid oxidase system of Tecomastans—III.: Studies on the conversion of o-aminophenol to catechol

The terminal step in the oxidation of anthranilic acid to catechol by anthranilic acid oxidase system from Tecoma stans, which converts o-aminophenol to catechol has been studied in detail. The reaction catalyses the conversion of one molecule of o-aminophenol to one molecule each of ammonia and catechol. The partially purified enzyme has a pH optimum of 6·2 in citrate-phosphate buffer and a temperature optimum of 45°. The metal ions, Mg2+, Co2+ and Fe3+ were inhibitory to the reaction. Metal chelating agents like 8-hydroxyquinoline, o-phenanthroline, and diethyldithiocarbamate, caused a high degree of inhibition. A sulfhydryl requirement for the reaction was inferred from the inhibition of the reaction by p-chloromercuribenzoate and its reversal with GSH. Atebrin inhibition was reversed by addition of FAD to the reaction mixture.

Conversion of isophenoxazine to catechol in Tecoma stans

Isophenoxazine, formed by the condensation of two molecules of o-aminophenol, is reduced by an enzyme system from Tecoma stans leaves to two molecules of catechol. The reaction proceeds well under anaerobic conditions; a 1–2 mole stoichiometry between the substrate disappeared and the product formed was maintained. The enzyme showed maximum activity at pH 5. The substrate at high concentrations caused a diminution in the activity and the optimum concentration of substrate was at 6 × 10−4 Image . The enzyme preparation was able to convert cinnabarinic acid and diphenylene dioxide 2,3-quinone into the corresponding catechol substances. The diphenylene dioxide 2,3-quinone at the same concentration was three times more susceptible to enzymic cleavage than isophenoxazine. Cinnabarinic acid inhibited the enzymic cleavage of isophenoxazine competitively. None of the known electron donors was found to activate the reaction. Inhibition studies suggested that intact sulfhydryl groups are necessary for enzyme activity. Heavy metal ions like Hg++, Ag+, Co++, Fe++, Ni++, and Fe3++ inhibited the reaction. Metal chelating agents did not have any effect on the enzyme.

The conversion of 3-hydroxyanthranilic acid to cinnabarinic acid by the nuclear fraction of rat liver

Although several authors have implicated 3-hydroxyanthranilic acid (3-OHA) as an intermediate in tryptophaniacin pathway in animals (Kaplan, 1961), alternative pathways of metabolism of this compound have not been fully explored. Madhusudanan Nair obtained an enzyme from spinach leaves which could convert 3-OHA to cinnabarinic acid (private communication). Viollier and Süllmann (1950) reported the conversion of 3-OHA to an unidentified red compound by rat liver homogenates. The present investigation describes the identification of this product as cinnabarinic acid (2-amino-3-H-isophenoxazine-3-one-1,9-dicarboxylic acid). Cinnabarinic acid is known to occur in nature along with cinnabarin is olated from the fungus Polystictus sanguineus (Gripenberg et al., 1957; Gripenberg, 1958).

Enzymatic conversion of anthranilic acid to catechol by chloroplast from the leaves of Tecoma stans

An enzyme system which converts anthranilic acid to catechol was detected in the leaves of Tecoma stans, and its properties studied. The system is present exclusively in the chloroplast fraction of the leaves. The optimum pH of the reaction is 5·2 and maximum activity was obtained with citrate-phosphate buffer. There was good stoichiometry between the amounts of anthranilic acid disappeared and the amounts of catechol and ammonia formed. The enzyme system showed an absolute requirement for oxygen and evidence was obtained for the probable participation of NADPH and FAD in the hydroxylation step. The optimum concentration of anthranilic acid was 10−4 M; at higher concentrations the reaction was inhibited to a considerable extent. Cyanide, pyrophosphate, and EDTA also caused inhibition indicating a requirement for metal ions.

Conversion of an equilenane to the estrane: Synthesis of dl-3-methoxy-17β-carboxy-1,3,5(10)-estratriene

dl-3-Methoxy-11-oxo-17β-carboxy-1,3,5(10),6,8-estrapentaene has been converted to dl-3-methoxy-17β-carboxy-1,3,5(10)-estratriene in fairly good yield.

A new chiral oxazoline derived from camphor and its conversion to (R)-2-methylalkanoic acids

1S,5R,7R)-(-)-10, 10-Dimethyl-3-ethyl-4-oxa--atricyclo[5.2.1.0(1,5)]dec-2-ene 2 was prepared in 95% yield from (1S)-1-amino-2-exo-hydroxyapocamphane 1. The chiral oxazoline could be alkylated (Lhttp://eprints.iisc.ernet.in/cgi/users/home?screen=EPrint::Edit&eprintid=31175&stage=core#tDA/THF/-78 degrees C/RX, RX = ethyl, n-propyl, n-butyl iodides or benzyl bromide) to 3 in 95% yield and > 95% diastereoselectivity, and the products hydrolysed to (R)-2-methylalkanoic acids 4 (43-47% yield, 93-98% e.e.). (C) 2000 Elsevier Science Ltd. All rights reserved.

Preparation and characterization of rubidium-beta-alumina by the gel-to-crystallite conversion method

Preparation of Rb-beta -alumina was realized by the gel-to-crystallite conversion method. Reaction of hydrated aluminum hydroxide gel with RbOH in ethanol medium gave rise to the Rb+-inserted pseudoboehmite precursor under wet chemical conditions. The thermal decomposition of the precursor yielded Rb-beta -alumina. The Rb2O:Al2O3 ratio of monophasic Rb-beta -alumina ranged from 1:10 to 1:22. The extended stability in the compositional range is due to the fact that the conduction planes containing Rb+ and O2- ions can have lower occupancy of Rb+ ions for larger sized alkali ions, permitting the steric separation of the adjoining spinel blocks. High-resolution electron microscopy revealed that the decreasing occupancy of alkali ions in the conduction plane is balanced by changing widths of spinel blocks arising from the shift of tetrahedral Al3+ ions to octahedral sites and an accompanying increase in stacking defects. (C) 2000 Elsevier Science Ltd. All rights reserved.

How the development of condensation particle counters is reforming our view on atmospheric nucleation

Aerosol particles deteriorate air quality, atmospheric visibility and our health. They affect the Earth s climate by absorbing and scattering sunlight, forming clouds, and also via several feed-back mechanisms. The net effect on the radiative balance is negative, i.e. cooling, which means that particles counteract the effect of greenhouse gases. However, particles are one of the poorly known pieces in the climate puzzle. Some of the airborne particles are natural, some anthropogenic; some enter the atmosphere in particle form, while others form by gas-to-particle conversion. Unless the sources and dynamical processes shaping the particle population are quantified, they cannot be incorporated into climate models. The molecular level understanding of new particle formation is still inadequate, mainly due to the lack of suitable measurement techniques to detect the smallest particles and their precursors. This thesis has contributed to our ability to measure newly formed particles. Three new condensation particle counter applications for measuring the concentration of nano-particles were developed. The suitability of the methods for detecting both charged and electrically neutral particles and molecular clusters as small as 1 nm in diameter was thoroughly tested both in laboratory and field conditions. It was shown that condensation particle counting has reached the size scale of individual molecules, and besides measuring the concentration they can be used for getting size information. In addition to atmospheric research, the particle counters could have various applications in other fields, especially in nanotechnology. Using the new instruments, the first continuous time series of neutral sub-3 nm particle concentrations were measured at two field sites, which represent two different kinds of environments: the boreal forest and the Atlantic coastline, both of which are known to be hot-spots for new particle formation. The contribution of ions to the total concentrations in this size range was estimated, and it could be concluded that the fraction of ions was usually minor, especially in boreal forest conditions. Since the ionization rate is connected to the amount of cosmic rays entering the atmosphere, the relative contribution of neutral to charged nucleation mechanisms extends beyond academic interest, and links the research directly to current climate debate.