The influence of soil matric pressure on the acidity and cation composition of soil solutions extracted by different methods

Abstract

Abstract From the samples of gradually drying (beginning from the field moisture capacity, FMC) soddy-podzolic sandy loam soil (Albic Retisol (Loamic, Ochric)) contaminated with Zn were isolated the soil solutions (SS) by centrifugation, while from the other samples of the soil, moistened to FMC, various energy fractions of the SS were pressed using a hydraulic press. The acidity of the centrifuge solutions extracted from the soil of the experiment variant with the cultivation of plants (“barley”) was, on average, 1 pH higher than on “bare fallow”, and decreased with decreasing soil moisture content. The acidity of the solutions extracted from the soils of the “bare fallow” variant in the same range of soil moisture content practically did not change. It was also found that in more acidic solutions from the “bare fallow” variant the content of Ca, Mg, Mn, Zn and K was 2.4 – 6.9 times higher than the content of these metals in solutions from the “barley” variant. The positive correlation between pF and pH was clearly observed for the pressed solutions from the soils of both variants. Concentrations of Ca, Mg, Sr, Ba,Zn, K and Na in successively pressed fractions of SSs from more acidic soil of the “bare fallow” variant, on average, 3.0 – 8.4 times exceeded their concentrations in similar fractions of solutions of the “barley” variant and showed an inverse correlation with soil moisture (pF value).