Effects of pH on chemical stability and de-esterification of fenoxaprop-ethyl by purified enzymes, bacterial extracts, and soils

Citation
Rm. Zablotowicz et al., Effects of pH on chemical stability and de-esterification of fenoxaprop-ethyl by purified enzymes, bacterial extracts, and soils, J AGR FOOD, 48(10), 2000, pp. 4711-4716
Citations number
31
Categorie Soggetti
Agricultural Chemistry","Chemistry & Analysis
Journal title
JOURNAL OF AGRICULTURAL AND FOOD CHEMISTRY
ISSN journal
00218561 → ACNP
Volume
48
Issue
10
Year of publication
2000
Pages
4711 - 4716
Database
ISI
SICI code
0021-8561(200010)48:10<4711:EOPOCS>2.0.ZU;2-H
Abstract
De-esterification is an initial step in the metabolism of certain herbicide s, for example, fenoxapropethyl [(+/-)-ethyl 2-[4-[(6-chloro-2-benzoxaolyl) oxy]phenox]propanoate] (FE). The ethyl-ester bond cleavage of FE to fenoxap rop acid (FA) by purified enzymes, crude bacterial enzyme preparations, and soils was investigated. In similar experiments fluorescein diacetate (FDA) was used as an alternative substrate. FE stability was pH sensitive in aci dic buffered solutions; that is, below pH 4.6, rapid nonenzymatic hydrolysi s of the benzoxazolyl-oxy-phenoxy ether linkage occurred, forming 6-chloro- 2,3-dihydro-bcnzoxazol-2-one (CDHB) and ethyl 4-hydroxyphenoxypropanoate or 4-hydroxyphenoxypropanoate. With porcine esterase and cell-free Pseudomona s fluorescens extracts, activity on FE and FDA was most rapid at pH 7.6-8.6 but decreased 80-90% at pH 5.6. Yeast (Candida cylindrica) lipase-mediated de-esterification of FE and FDA was not as sensitive to pH; that is, activ ity at pH 4.6 was 70% of that at pH 7.6. Short-term incubations (20 h) were conducted in eight soils (pH 4.5-6.9) treated with C-14-chlorophenyl ring- labeled FE (2 mg kg(-1)). In the most acidic soils (pH 4.4-4.5) 25% of the C-14 was recovered as FA, versus 30-40% in moderately acid soils (pH 5.0-5. 6) and 55% in neutral soils (pH 6.8-6.9). There was a similar correlation b etween soil pH and FDA de-esterification. CDHB was formed in all acidic soi ls with levels 4-fold greater in pH 4.4-4.5 soils than in pH 5.0-5.6 soils. CDHB was not formed in neutral soils. Results demonstrate some chemical hy drolysis (benzoxazolyl-oxy-phenoxy ether linkage) of FE in acid soils, the sensitivity of enzymatic de-esterification of FE to pH, and the potential o f FDA as a colorimetric indicator for esterase hydrolysis of FE.