FIELD-EVALUATION IN ACID SOILS OF STRAINS OF RHIZOBIUM-LEGUMINOSARUM BV TRIFOLII SELECTED FOR THEIR TOLERANCE OR SENSITIVITY TO ACID SOIL FACTORS IN AGAR MEDIUM
Lg. Gemell et Rj. Roughley, FIELD-EVALUATION IN ACID SOILS OF STRAINS OF RHIZOBIUM-LEGUMINOSARUM BV TRIFOLII SELECTED FOR THEIR TOLERANCE OR SENSITIVITY TO ACID SOIL FACTORS IN AGAR MEDIUM, Soil biology & biochemistry, 25(10), 1993, pp. 1447-1452
We report field experiments which tested the performance of ten strain
s of Rhizobium leguminosarum by. trifolii in acid soils. The strains h
ad been classified as either tolerant or sensitive to mineral imbalanc
es associated with acid soils and to low pH, on an agar medium. The so
ils of the two sites were pH 4.0 and 4.2 (10 mm CaCl2) and all strains
with one exception originated from acid soils at or near these sites.
All strains colonized the rhizospheres of subterranean clover equally
well but were more successful at the site where the naturalized popul
ation of rhizobia was smaller. Nodulation by the inoculant strains in
the first year was poor; they formed only 8 and 2.9% of the nodules at
Sites 1 and 2 respectively. The two strains originating from Site 1 f
ormed a mean of only 2% of the 173 nodules tested from plots where it
had been introduced at Site 1. The naturalized strains formed a dispro
portionate number of nodules relative to their number in the rhizosphe
re. Higher rates of inoculation in the second year, although not marke
dly affecting rhizosphere numbers, increased nodule initiation by the
inoculant strains but not in proportion to their numbers. Unexpectedly
, the most successful strains in each year were those classified as ac
id-sensitive; they formed a higher proportion of the nodules than thos
e classified as acid-tolerant. The results suggest that in soil, facto
rs other than pH and inorganic nutrients are important or that a strai
n's genetic background is of such importance that it can mask the impr
oved nodulation in an acid soil expected from selecting for tolerance
on an agar medium.