C. Tang et Q. Yu, Impact of chemical composition of legume residues and initial soil pH on pH change of a soil after residue incorporation, PLANT SOIL, 215(1), 1999, pp. 29-38
Reports on the effect of organic matter addition on soil pH have been contr
adictory. This study examined the effect of applying legume residues differ
ing in concentrations of N (4.3-45.5 mg g(-1)) and excess cations/organic a
nions (0.22-1.56 mmol g(-1)) on pH change of five soils differing in initia
l pH (3.60-5.58 in 0.01 M CaCl2) under sterile and non-sterile conditions.
Addition of the legume residues at a level of 1% soil weight increased the
pH of all soils by up to 2 units after incubation for 35 and 100 d under no
n-sterile conditions. Exceptions were the Lancelin (initial pH 5.06) and Ke
llerberin (pH 5.58) soils with addition of clover roots (excess cations 22
cmol/kg) for 100 d where soil pH decreased by 0.13-0.15 units as compared t
o the control. The amounts of alkalinity produced in soil correlated positi
vely with concentrations of excess cations and total nitrogen of the added
legume residues, and negatively with the initial pH of the soil. When soil
was fumigated with chloroform during incubation, similar trends of soil pH
changes and alkalinity production, due to legume residues addition, were di
splayed but the effects of the residue on alkalinity production in the Wodj
il and Lancelin soils were much less than under non-sterile conditions. Dir
ect shaking of soil with the residues under sterile conditions increased th
e amount of alkalinity in the soils with initial pH of 3.60-4.54, but not i
n the soils with initial pH of 5.06 and 5.58. The maximal alkalinity produc
tion was less than one third of that produced in the soil after 100 d of in
cubation under non-sterile conditions. The results suggest that the directi
on and the magnitude of pH change depend largely on the concentration of or
ganic anions in the residues, initial soil pH and the degree of residue dec
omposition. The incorporation of crop residues, especially those with high
concentrations of excess cations, is recommended in minimizing soil acidifi
cation in farming systems.