Phenolic acid content of soils from wheat-no till, wheat-conventional till, and fallow-conventional till soybean cropping systems

Soil core (0-2.5 and/or 0.10 cm) samples were taken from wheat-no till, wheat-conventional till, and fallow-conventional till soybean cropping systems from July to October of 1989 and extracted with water in an autoclave. The soil extracts were analyzed for seven common phenolic acids (p-coumaric, v...

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Veröffentlicht in:Journal of chemical ecology 1991-06, Vol.17 (6), p.1045-1068
Hauptverfasser: Blum, U. (North Carolina State University, Raleigh, NC), Wentworth, T.R, Klein, K, Worsham, A.D, King, L.D, Gerig, T.M, Lyu, S.W
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Sprache:eng
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Zusammenfassung:Soil core (0-2.5 and/or 0.10 cm) samples were taken from wheat-no till, wheat-conventional till, and fallow-conventional till soybean cropping systems from July to October of 1989 and extracted with water in an autoclave. The soil extracts were analyzed for seven common phenolic acids (p-coumaric, vanillic, p-hydroxybenzoic, syringic, caffeic, ferulic, and sinapic; in order of importance) by high-performance liquid chromatography. The highest concentration observed was 4 micrograms/g soil for p-coumaric acid. Folin and Ciocalteu's phenol reagent was used to determine total phenolic acid content. Total phenolic acid content of 0- to 2.5-cm core samples was approximately 34% higher than that of the 0- to 10-cm core samples. Phenolic acid content of 0- to 2.5-cm core samples from wheat-no till systems was significantly higher than those from all other cropping systems. Individual phenolic acids and total phenolic acid content of soils were highly correlated. The last two observations were confirmed by principal component analysis. The concentrations were confirmed by principal component analysis of individual phenolic acids extracted from soil samples were related to soil pH, water content of soil samples, total soil carbon, and total soil nitrogen. Indirect evidence suggested that phenolic acids recovered by the water-autoclave procedure used came primarily from bound forms in the soil samples
ISSN:0098-0331
1573-1561
DOI:10.1007/BF01402933