A SIMPLE KINETIC APPROACH TO DERIVE THE ECOLOGICAL DOSE VALUE, ED(50), FOR THE ASSESSMENT OF CR(VI) TOXICITY TO SOIL BIOLOGICAL PROPERTIES

Citation
Tw. Speir et al., A SIMPLE KINETIC APPROACH TO DERIVE THE ECOLOGICAL DOSE VALUE, ED(50), FOR THE ASSESSMENT OF CR(VI) TOXICITY TO SOIL BIOLOGICAL PROPERTIES, Soil biology & biochemistry, 27(6), 1995, pp. 801-810
Citations number
31
Categorie Soggetti
Agriculture Soil Science
Journal title
ISSN journal
00380717
Volume
27
Issue
6
Year of publication
1995
Pages
801 - 810
Database
ISI
SICI code
0038-0717(1995)27:6<801:ASKATD>2.0.ZU;2-P
Abstract
Three New Zealand soils of contrasting texture, organic matter content and cation exchange capacity (CEC) were amended with K2Cr2O7 solution s, spanning two concentration ranges, 0-5 mu mol Cr(VI) g(-1) soil and 0-50 mu mol Cr(VI) g(-1) soil. Samples were assayed for phosphatase, sulphatase and urease enzyme activities, and for basal respiration, mi crobial biomass C, dimethyl sulphoxide(DMSO)-reducing activity and den itrification, 3 and 60 d after amendment. Extractability of Cr(VI) fro m similarly amended samples was measured from 0 to 100 d. Cr(VI) prove d to be strongly inhibiting of most of the biological properties and i n most instances inhibition was explained by one or both of two simple Michaelis-Menten kinetic models. The first of these (Model 1) simulat ed fully competitive kinetics and the second (Model 2) simulated parti ally competitive kinetics. A single inhibition constant, similar to ED (50) as conceptualized in previous studies, could usually be calculate d for each property in each soil. The properties could be ranked in th e following order of decreasing sensitivity to Cr(VI): denitrification > DMSO-reduction > sulphatase activity approximate to biomass C > pho sphatase activity > urease activity > respiration. For the most sensit ive property, denitrification, ED(50) values range from 63 to 730 nmol Cr g(-1) soil. Soil mineral surface area, organic matter content and CEC influenced the sensitivity of properties between soils. Although t he extent of inhibition often diminished with time, the differences we re generally much smaller than the observed decline in extractability of Cr(VI), indicating that a persistent, long-term inhibition, outlast ing the Cr(VI) itself, had occurred.