Impact of macropores and gravel outcrops on phosphorus leaching at the plot scale in silt loam soils

Authors

Derek M. Heeren, University of Nebraska-LincolnFollow
Garey A. Fox, North Carolina State UniversityFollow
Chad Penn, USDA Agricultural Research ServiceFollow
Todd Halihan, Oklahoma State University - Main CampusFollow
Daniel E. Storm, Oklahoma State University - Main CampusFollow
Brian Haggard, University of Arkansas, FayettevilleFollow

Date of this Version

6-2017

Citation

Heeren, D. M., G. A. Fox, C. J. Penn, T. Halihan, D. E. Storm, and B. E. Haggard. 2017. Impact of macropores and gravel outcrops on phosphorus leaching at the plot scale in silt loam soils. Transactions of the ASABE 60(3): 823-835, doi: 10.13031/trans.12015.

Comments

Copyright (c) 2017 D. M. Heeren, G. A. Fox, C. J. Penn, T. Halihan, D. E. Storm, & B. E. Haggard

Abstract

In response to increased nutrient loads in surface waters, scientists and engineers need to identify critical nutrient source areas and transport mechanisms within a catchment to protect beneficial uses of aquatic systems in a cost-effective manner. It was hypothesized that hydrologic heterogeneities (e.g., macropores and gravel outcrops) in the vadose zone play an integral role in affecting flow and solute transport between the soil surface and shallow alluvial aquifers. The objective of this research was to characterize phosphorus (P) leaching through silt loam soils to alluvial gravel aquifers in the floodplains of the Ozark ecoregion at the plot scale. Solute injection experiments used plots (1 m x 1 m, 3 m x 3 m, and 10 m x 10 m) that maintained a constant head for up to 52 h. Solutes in the injection water included P (highly sorptive), Rhodamine WT (slightly sorptive), and chloride (conservative). Electrical resistivity imaging identified zones of preferential flow. Fluid samples from observation wells indicated nonuniform subsurface flow and transport. The surface soil type, ranging from silt loam to clean gravel outcrops, had a significant impact on P leaching capacity, with gravel outcrops resulting in high infiltration rates and rapid solute detection in wells (e.g., 4 min). Even in silt loam soils without gravel outcrops, macropore flow resulted in rapid transport of P. Maximum transport velocity for soluble reactive P in one silt loam plot was 810 cm h-1, compared with a mean pore water velocity in the range of 25 to 130 cm h-1. Soluble reactive P concentrations in observation wells reached up to 0.54 mg L-1 in silt loam plots and 1.3 mg L-1 in gravel outcrop plots, demonstrating that a highly sorbing solute can be mobile.