Transactions of the ASAE · 1983 · 110 citations · 0 references
Precision AgricultureEngineeringBotanyEffective DispersionAgricultural EconomicsRoot-soil InteractionSoil PropertyPlant-soil InteractionRoot SystemSoil ScienceCrop Water RelationPlant RootsSediment TransportSolute ModelingSoilless FarmingEnvironmental EngineeringPhysiologyRoot MorphologyPlant Physiology
Solute transport modeling in agricultural soils must account for crop roots and root channels, prompting investigation of their impact on soil solute movement. The study performed two‑year chloride breakthrough experiments in uniformly packed sandy loam and loamy sand columns, cycling from bare soil to wheat‑planted columns and back to bare soil after crop death. Loamy sand exhibited higher dispersion than sandy loam in precrop runs, but dispersion decreased with active roots and peaked post‑crop due to residual root channels, while immobile water fractions rose from negligible in precrop to 11–39 % in cropped and post‑crop experiments, indicating significant pore bypass.
ABSTRACT SINCE many of the practical applications of solute modeling are to situations where crop roots are present, it is necessary to investigate the effect of roots and void root channels on the transport of solutes through soils. In an attempt to do this chloride breakthrough experiments were conducted over a two year period in soil columns packed uniformly with sandy loam or loamy sand. A series of experiments were conducted in bare soil, followed by repeated experiments with wheat plants in the columns, and finally in bare soil again after the wheat crop had died. The loamy sand columns showed significantly higher dispersion than the sandy loam columns in the precrop experiments, but the effective dispersion decreased when the experiments were repeated with plant roots present. The post crop experiment showed the highest dispersion of any of the studies possibly due to the presence of old root channels in the soil. Very little immobile water was present in the precrop experiments, but both the cropped experiments and the post crop experiments exhibited significant pore bypass; immobile water fractions ranged from 11 percent to 39 percent of the total water content.