Cm. Su et al., EXTRACTABLE SOIL BORON AND ALFALFA UPTAKE - CALCIUM-CARBONATE EFFECTSON ACID SOIL, Soil Science Society of America journal, 58(5), 1994, pp. 1445-1450
Since soil tests for B in fine-textured soils give inconsistent predic
tions and the amendment of acidic soils with CaCO3 is a common practic
e, the suitability of extractants for plant-available B in a CaCO3-ame
nded clayey soil was studied. This research investigated the pH effect
on B adsorption, the changes in the amounts of hot-water-extractable
B (HW-B), mannitol-extractable B (MANN-B), and soil solution B (SOLN-B
) as a result of B and CaCO3 addition to a silty clay soil (a clayey,
mixed, mesic Typic Humaquept) with an initial pH of 4.2. The relations
hip between the amounts of extractable B and B uptake by alfalfa (Medi
cago sativa L.) was also studied. Amounts of extractable B in soil wer
e in the order HW-B > MANN-B > SOLN-B, decreasing with increasing pH a
nd after growth of alfalfa. Addition of 2.5 and 5.0 g CaCO3 kg(-1) inc
reased alfalfa dry matter yield; whereas addition of 0.5 and 1,5 mK B
kg(-1) had no effect. In the absence of added B, the B concentration i
n alfalfa shoots decreased with increasing pH. Linear correlations bet
ween B concentration in alfalfa shoots and extractable B in soil were
significant for all three cuts and for all three extractants. Total up
take of B was significantly correlated with all forms of extractable B
except HW-B for the third cut only. Inclusion of pH improved the rela
tionship for the other cuts. The dilution of B in plant shoots by CaCO
3-stimulated growth may result in B deficiency.