Slowing nitrification with a nitrification inhibitor (NI) provides an enhan
ced NH4 supply (EAS), which has improved N uptake efficiency and crop yield
. A physiological response to EAS has been demon strated in container exper
iments with restricted rooting volumes and uniform N distribution, but less
is known about root responses to EAS when distributions of N forms are not
uniform. Greenhouse and 2-yr field experiments were conducted to determine
how the root system of wheat (Triticum aestivum L.) responds to EAS. Three
N sources: (i) calcium nitrate (NO3); (ii) urea with a nitrification inhib
itor, nitrapyrin (NH4+M); and (iii) 50% NO3 + 50% NH4 + NI were uniformly i
ncorporated in the field into the top 20 cm of a Shano silt loam soil (Coar
se-silty, mixed, superactive, mesic Xeric Haplocambid). Urea with a NI incr
eased NH4 in the top 30 cm of soil and increased root surface area densitie
s in this soil layer at the boot stage in both Sears. Rooting was either de
creased or not affected by NH4 + NI relative to NO3 in the 30- to 90-cm sub
soil. In a greenhouse experiment, NO3, NH4 + NI, or NH4 + NI + CaCl2 were u
niformly mixed into the top 20 cm of soil (diffused) or banded at the 20-cm
depth in rooting-boxes (5 by 17 by 70 cm), Nodal root density at boot stag
e increased in the fertilized zones with NH4+NI, mostly in the presence of
CaCl2, compared with NO3, while seminal roots in the fertilized zones were
only enhanced by banded NO3. Wheat root types responded differentially to N
forms and the associated differences in vertical distribution.