Soil Science Society of America Journal · 1970 · 32 citations · 0 references
AgricultureAgronomySoil SciencesResource RecoverySoil FertilitySoil Organic MatterLitter DecompositionNitrogen RecoveryNitrogen RemovalNutrient RetentionPlant Residue DecompositionResidue DecompositionAmmoniation Of Crop ResiduesDecomposition In Forest SoilsForest Residue BurningOrganic Residue DecompositionSoil SterilizationUrea HydrolysisUrease ActivityWoody Litter Decomposition
Abstract Gaseous loss of NH 3 from prilled urea, surface applied at 100 kg N/ha to undisturbed dry organic residue over moist soil under slash pine ( Pinus elliottii Engelm. var. elliottii ), averaged 4% in 7 days as compared with 2% for an area that was control‐burned 5 weeks previous, and 5% for one from which loose debris had been removed. This was approximately equivalent to removal by burning. Residual urea recovery of 41% for the burned area as compared with 16 and 12% for the undisturbed and cleaned areas, indicated urease inactivation and partial soil sterilization by burning. Where urea had been applied to moist undisturbed organic residue, hydrolysis approached completion in 3 days and was accompanied by 9% N loss as NH 3 . Various types and orientations of needle‐bearing portions of branches of slash pine were submitted to a 75–100 cm drop of prilled urea at 100 kg N/ha. From 0.32–0.87 g of pellets were retained per meter of branch. Aspiration tests under typical alternating night and day humidities and native urease activity showed only 3% loss of this retained urea‐N as NH 3 in 4 days. At 8 days an average of 52% of the initially retained N was still dilute‐acid soluble from macerated bark plus needle stubs, with a ratio of seven parts urea N to three parts NH 4 + ‐N. The remainder, except for the small gaseous loss, probably was assimilated.