Kinetics of halogen substituted aniline transformation in anaerobic estuarine sediment

The kinetics of halogen substituted anilines were examined in estuarine sediment collected from Tsurumi river, Japan. Aniline was substituted with F, Cl, Br and I groups at meta or para positions on the aromatic ring. The transformation of all the compounds followed a first-order reaction kinetics with rate constants for the disappearance ranging between 0.002 to 0.006 day−1 or half lives between 108 and 669 days. Results indicated that para substituted anilines transformed two to four times faster compared to meta substituted ones. The rate of transformation followed the order: I > Br > Cl > F. A quantitative structure-activity relationship was evaluated relating the first-order rate constant in sediment with several readily available molecular descriptors: carbon-halogen bond strength, Hammett sigma constants, Taft steric constant, and Lipophilic constant. In addition octanol/water partition coefficients and solubility were included in the correlation. The relationship obtained was only significant between the rate constant and lipophilic constant.

[1]  K. Timmis,et al.  Microbial mineralization of ring-substituted anilines through an ortho-cleavage pathway , 1985, Applied and environmental microbiology.

[2]  W. Peijnenburg,et al.  Development of a structure-reactivity relationship for the photohydrolysis of substituted aromatic halides , 1992 .

[3]  J. Struijś,et al.  Reductive dehalogenation of dichloroanilines by anaerobic microorganisms in fresh and dichlorophenol-acclimated pond sediment , 1989, Applied and environmental microbiology.

[4]  J. Suflita,et al.  Sequential reductive dehalogenation of chloroanilines by microorganisms from a methanogenic aquifer , 1989 .

[5]  Toxicities of Chloroanilines to Photobacterium Phosphoreum and their Correlations with Effects on Other Organisms and Structural Parameters , 1984 .

[6]  D. Kosson,et al.  Metabolism of aniline under different anaerobic electron‐accepting and nutritional conditions , 1994 .

[7]  J. Plimmer,et al.  Microbial oxidation of 4-chloroaniline. , 1973, Journal of agricultural and food chemistry.

[8]  K. Kaiser,et al.  TOXICITIES OF SELECTED CHLOROANILINES TO FOUR STRAINS OF YEAST , 1984 .

[9]  D. Meent,et al.  Reductive transformations of halogenated aromatic hydrocarbons in anaerobic water‐sediment systems: Kinetics, mechanisms and products , 1992 .

[10]  N. Wolfe,et al.  Kinetic studies of the reduction of aromatic AZO compounds in anaerobic sediment/water systems , 1987 .

[11]  F. Feeherry,et al.  Microbial transformation of 2,4,6-trinitrotoluene and other nitroaromatic compounds , 1976, Applied and environmental microbiology.

[12]  J. Suflita,et al.  Effect of Sulfate and Organic Carbon Supplements on Reductive Dehalogenation of Chloroanilines in Anaerobic Aquifer Slurries , 1990, Applied and environmental microbiology.

[13]  D. Meent,et al.  QSARs for predicting biotic and abiotic reductive transformation rate constants of halogenated hydrocarbons in anoxic sediment systems , 1991 .

[14]  Willie J.G.M. Peijnenburg,et al.  QSARs for predicting reductive transformation rate constants of halogenated aromatic hydrocarbons in anoxic sediment systems , 1992 .

[15]  J. Tiedje,et al.  Microbial reductive dehalogenation. , 1992, Microbiological reviews.