Hh. Schomberg et al., DECOMPOSITION AND NITROGEN DYNAMICS OF CROP RESIDUES - RESIDUE QUALITY AND WATER EFFECTS, Soil Science Society of America journal, 58(2), 1994, pp. 372-381
Understanding environmental and residue influences on decomposition an
d nutrient dynamics under diverse conditions is critical for efficient
resource management. Our objective was to evaluate the influence of w
ater on decomposition and N dynamics for surface and buried residues.
Decomposition of alfalfa (Medicago sativa L.), grain sorghum (Sorghum
bicolor [L.] Moench), and winter wheat (Triticum aestivum L. emend. Th
ell.) residues in fiberglass bags on the surface or buried at 120 mm i
n Pullman soil (fine, mixed, thermic Torrertic Paleustoll) at Bushland
, TX, was measured from May 1990 to May 1991. A line-source sprinkler
provided five water regimes (336, 287, 166, 60, and 5 mm) while precip
itation provided 305 mm water. Decomposition coefficients (k) were gre
ater for alfalfa than for wheat or grain sorghum and were greater for
buried than for surface residues. Rate coefficients increased linearly
with water applied. The increase was greater for alfalfa than for sor
ghum and wheat. Net N mineralization occurred from alfalfa residues th
roughout the study. Net N immobilization was longer than 1 yr for surf
ace wheat and sorghum and about 0.33 yr for buried residues. Both N(ma
x) (grams N immobilized per kilogram of original biomass) and N(eqv) (
grams N immobilized per kilogram of biomass loss) were influenced by c
rop and placement but not water regime. The N(max) value was similar f
or surface wheat and sorghum residues but was 50% lower for buried whe
at than for sorghum. The N(eqv) indicated the N requirement of microor
ganisms was less for buried than for surface residues. Water and resid
ue quality interactions affecting decomposition and N dynamics should
be considered in residue management strategies for soil protection and
nutrient cycling.