Heavy metal uptake and chemical changes in the rhizosphere of Thlaspi caerulescens and Thlaspi ochroleucum grown in contaminated soils

Thlaspi caerulescens (J. and C. Presl) and Thlaspi ochroleucum (Boiss. ex Heldr) were grown in three different soils containing moderate to high amounts of heavy metals in a pot experiment, using a rhizobag technique. ir: caerulescens accumulated significantly more Zn in the shoots than I: ochroleucum. The concentrations of Zn in the shoots of I: caerulescens ranged from 3100 to 8100 mg kg(-1) dry matter (DM), but only from 800 to 1600 mg kg(-1) DM in 2: ochroleucum. Total uptake of Zn in the shoots of I: caerulescens was about 5 times that of I: ochroleucum. In contrast, the differences between the two species in the uptake of Cd, Cr, Cu, Ni and Pb were generally small. Concentrations of mobile Zn (extractable with 1 IM NH4NO3) in the rhizosphere and non-rhizosphere soils decreased considerably after growth of both plants, but the decreases were greater with I: caerulescens than with I: ochroleucum. The decreases in the mobile fraction accounted for less than 10% of the total Zn uptake by I caerulescens indicating that this species was effective in mobilising Zn from less soluble fractions in the soils. The rhizosphere soils tended to have higher concentrations of mobile Zn than the non-rhizosphere soils, probably because of the lower pH in the rhizosphere. The pH in the rhizosphere soils was 0.2-0.4 units lower than that in the non-rhizosphere soils at the end of the experiment. However, there were no significant differences between the two species in the degree of rhizosphere acidification. The results suggest that I: caerulescens has potential for removing Zn from moderately to highly contaminated soils, but that this ability was not related to the pH changes in the rhizosphere.