The objective of this study was to evaluate the B adsorption capacity in fo
ur lowland soils from Lavras, MG, Brazil, through Langmuir and Freundlich i
sotherm parameters. This study was conducted throughout October and Novembe
r, 1998. Samples of Alluvial Soil, Low-Humic Gley Humic Gley and artificial
ly drained Bog Soil were collected in 0-20 cm of profundity and sieved to 2
mm. Samples with or without liming application were incubated during 30 da
ys. Duplicates of 4.0 g soil samples, conditioned in polyethylene tubes, re
ceived eight doses of B (0, 2, 4, 8, 12, 16, 24 and 32 mug mL(-1)) prepared
with 20 ml, CaCl2.2H(2)O 0.01 mot L-1 solution, using boric acid. The amou
nt of B in the balance solution was measured through the Azomethine-H metho
d. The high organic matter content in Humic Gley soil provided higher B ads
orption capacity. The adsorption was highly correlated with organic matter,
specific surface area, kaolinite, and exchangeable aluminum. Lime applicat
ion provided decrease in B adsorption capacity for all soils.