R. Siqueira et Ma. Pavan, COFFEE ROOT-GROWTH IN COMPACTED ACID SOIL LAYER WITH AND WITHOUT CHEMICAL RESTRICTIONS, Arquivos de biologia e tecnologia, 40(1), 1997, pp. 1-8
Coffea arabica L. Mundo Novo variety was grown for one year in PVC soi
l. columns, 60 cm high by 30 cm diameter, made up by superposing three
rings of 20 cm high each one. Samples of surface layer of an acid Oxi
sol were divided into two portions : limed to pH 6 and unlimed. The to
p (0-20 cm) and bottom (40-60 cm) rings had a soil bulk density of 0.8
g/cm(3), while the central ring (20-40 cm) was compacted to 0.8, 1.1.
and 1.4 g/cm(3). The rings were bounded by adhesive tape. Total dry w
eight of the plant tops and leaf nutrient concentrations were not affe
cted by compaction in limed soil, but decreased with increasing bulk d
ensity in unlimed soil. Compaction decreased root growth in both limed
and unlimed soil, but with greater reduction in unlimed soil. Compact
ion increased root growth in the overlying (0-20 cm) and underlying (4
0-60 cm) soil layers only if these soil volumes were limed, which was
associated with elevated Ca and reduced Al. The excess Al compounded b
y low Ca content in unlimed soil were the main causes which restricted
root growth even in well structured soil volume above and beneath the
compacted layer. These results demonstrated that Al toxicity and Ca n
utrition are the chief soil chemical constraints that determine the ab
ility of coffee plants to compensate when part of the root system is s
ubjected to physical impediment by enhancing root growth in volumes of
the soil where well structured conditions exist.