Some aspects of the chemistry of lithium in soils

Summary

A method for the determination of exchangeable lithium using 0.5M NH₄Cl is described. The range of exchangeable Li in the fifty Papua New Guinea (PNG) soils analyzed was 0.002 to 0.409 μgg⁻¹ in contrast to five Australian soils which ranged from 0.032 to 0.830 μgg⁻¹. The PNG soils were divided into hill and alluvial soils with average exchangeable Li contents of 0.062 and 0.263 μgg⁻¹ respectively. No significant correlation between total and exchangeable Li was found in either group of soils althoughr=0.67 for the comined data and was significant at the 5% level. From the analysis of three profiles exchangeable Li was found to be at least twice as high (0.27 μgg⁻¹) in surface soils as in subsurface samples (0.10 μgg⁻¹). The average value of the deeper subsoil samples was 0.18 ppm.

R mode cluster analysis of the data for village garden soils collected on a sampling grid showed that exchangeable Li was more strongly assoicated with Ca and Mg than with pH, 0.05M EDTA soluble Zn, 0.5M NaHCO₃ soluble P or exchangeable Na and K. Computer constructed isographs using the analyses of grid samples from a garden illustrated the association between Li, Ca and Mg and the inverse association with Na.

The correlation coefficient between Ca and Li in the ash of three food plants (Gnetum gnemon, Hibiscus abelmoschus andStenochlaena plustris) while not significant on an individual basis, was significant when the data was combined suggesting that the association between these elements in the soil may reflect an association in the ash returned to the soil when the garden was cleared. The correlation coefficient between soil exchangeable Li and Li in plant ash was positive, but not significant.

Adsorption experiments over a five-day period demonstrated that Li was strongly adsorbed from solution. On average 63–75% of the adsorbed Li was fixed in a form which was not exchangeable with 0.5M NH₄Cl or soluble in 0.05M EDTA.