The conventional 1 M NH4OAc-exchangeable potassium (K+) soil test is inadeq
uate in soils where nonexchangeable K+ contributes significantly to crop nu
trition. Studies were conducted (i) to compare the abilities of the I M NH4
OAc method with a modified NaBPh4 method to estimate critical soil K+ level
s, (ii) to estimate the contribution of nonexchangeable K+ to plant-availab
le Iii, (iii) to compare the abilities of the 1 M NH4OAc method and the mod
ified NaBPh4 method to estimate plant dry matter yield and plant-available
K+, and (iv) to compare the abilities of both methods to measure soil K+ ba
lance. Winter wheat (Triticum aestivum L. 'Abe') was grown in eleven Midwes
tern soils in a greenhouse using consecutive 28-d defoliation and regrowth
cycles. Soils also were incubated for 6 mo with five K+ rates (0-809 mg Kkg(-1)). Ammonium acetate- and NaBPh4-extractable K+ (5-min extraction peri
od) were determined in soil samples taken after every three defoliation cyc
les and after incubation, Critical soil K+ levels could not be determined b
y either method alone but could be predicted by including cation-exchange c
apacity (CEC) and illitic K+ content in regression models. Nonexchangeable
K+ represented a significant portion of plant-available K+. Plant-available
K+ and dry matter (DM) yield were well related to NH4OAc-extractable KI on
ly in soils with low nonexchangeable K+ contribution (r(2) = 0.889 and 0.91
5, respectively), but they were well related to NaBPh4-extractable KI in al
l soils (r(2) = 0.984 and 0.874, respectively). Slopes for NH4OAc-extractab
le K+ vs, soil K+ balance varied widely among soils (0.16-0.68) depending o
n NH4OAc-extractable K+, illitic K+. and clay content, but for NaBPh4-extra
ctable K+ slopes were near unity, These studies suggest that the modified N
aBPh4 method may be a superior Kt soil test compared to the NH4OAc method.
Illite content and CEC data may help in developing better soil Kt managemen
t guidelines.