A. Bufogle et al., RICE PLANT-GROWTH AND NITROGEN ACCUMULATION IN DRILL-SEEDED AND WATER-SEEDED CULTURE, Soil Science Society of America journal, 61(3), 1997, pp. 832-839
Nitrogen fertilization strategies for flooded rice (Oryza sativa L.) d
epend on understanding plant N demand. Seasonal N accumulation researc
h in general is limited, and is nonexistent in water-seeded (WS) cultu
re. A field study was conducted for 3 yr in Louisiana and 1 yr in Arka
nsas to characterize plant growth and N accumulation by rite at differ
ent development stages, and to compare these factors in drill-seeded (
DS) and WS culture. 'Cypress' rice was grown on a Crowley silt loam (f
ine, montmorillonitic, thermic Typic Albaqualf). Straw, grain, roots,
and soil were collected at eight growth stages. Nitrogen-15-labeled ur
ea was applied to 75 by 75 cm microplots enclosed by stainless steel r
etainers. Total dry matter increased each season, and grain dry matter
was similar each year. In 1994 and 1995, both surface and subsurface
root growth increased linearly until 90% heading. Fertilizer N accumul
ation increased to the four-leaf plus 21-d or panicle differentiation
(PD) stages. Native soil N and remobilization of N from straw provided
N needed for maturing grain. From heading plus 21 d to maturity, fact
ors did not differ under either DS or WS each year. At early and late
stages of development, factors did not differ under DS and WS in Louis
iana. Differences in N accumulation and fertilizer N recovery were see
n in Arkansas. This suggests that, under Louisiana conditions, results
from experiments in DS and WS are interchangeable. Variation of the m
easured factors among years was significant, suggesting that even when
labeled N is used, results from multiple seasons are required for acc
urate interpretation.