COMPARISON OF CHEMICAL-COMPOSITION OF SOIL SOLUTIONS COLLECTED BY ZERO-TENSION PLATE LYSIMETERS WITH THOSE FROM CERAMIC-CUP LYSIMETERS IN AFOREST SOIL

We analysed the chemistry of solutions collected from soil by zero-ten sion plate lysimeters and cup lysimeters connected to a constant sucti on (600 hPa) under Douglas fir in the Beaujolais mountains (France). T he chemistry of zero-tension lysimeters' (ZTL) and tension lysimeters' (TL) solutions differed enormously: TL solutions were most concentrat ed in Si, NH4+-N, NO3-N, Cl-, Mg2+ and Al3+ and TOC, whereas Ca2+ and K+ concentrations were greater in ZTL solutions. Organic matter (OM) g reatly influenced the solution chemistry in both ZTL and TL. The chemi stry of ZTL solutions was affected mainly by OM mineralization in the forest floor and upper soil horizon, and that of TL solution seemed to be related to destabilization of humified compounds under the new veg etation. Nitrification was important: residual nitrification led to ex cess protons neutralized in weathering or ion exchange reactions, mobi lized cations, mainly Al3+. Selectivity coefficients calculated both f or ZTL and TL solutions formalized the differences between the two typ es of solutions. Nevertheless, these coefficients remained most often within the same order of magnitude indicating relations between them. Solutions from the two devices provided different information and shou ld not be used for the same objectives. Solutions from ZTL are suited for ecosystem input-output budgets, whereas TL solutions are more usef ul when equilibrium between the solution and solid phase or when plant nutrition are considered.