HETEROGENEITY OF INFILTRATION RATES IN ALLUVIAL FLOODPLAINS AS MEASURED WITH A BERM INFILTRATION TECHNIQUE

Authors

Derek M. Heeren, University of Nebraska-LincolnFollow
Garey A. Fox, Oklahoma State UniversityFollow
Daniel E. Storm, Oklahoma State University

Date of this Version

4-2015

Citation

TRANSACTIONS OF THE ASABE, Vol. 58(3): 733-745, ISSN 2151-0032, DOI 10.13031/trans.58.11056

Comments

© 2015 American Society of Agricultural and Biological Engineers. Used by permission.

Abstract

Hydrologic heterogeneities (e.g., macropores and gravel outcrops) in floodplains are hypothesized to play an integral role in impacting flow and leaching between the soil surface and shallow alluvial aquifers, which are intricately connected to streams. Infiltration is often assumed to be uniform, but this neglects the spatial variability common in anisotropic, heterogeneous alluvial floodplain soils. The objective of this research was to quantify infiltration and hydraulic conductivity across a range of scales (point to 100 m²) using a berm infiltration technique. Plot-scale leaching experiments were performed across a range of soil types at each of three floodplain sites in northeastern Oklahoma and northwestern Arkansas. Plots maintained a constant head of 2 to 9 cm for up to 52 h. Effective saturated hydraulic conductivity (K_eff), based on plot-scale infiltration rates and a one-dimensional Darcy flow equation, ranged between 0.6 and 68 cm h^-1 and varied considerably even within a single floodplain. The K_eff was also calculated at the point scale using particle size distributions and Retention Curve (RETC). Point-scale estimates were significantly lower than plot-scale K_eff and also failed to capture the variability of K_eff. The estimated permeability of the limiting layer reported in soil surveys was consistent with point-scale estimates of K_eff but was lower than plot-scale K_eff at most sites. Tension infiltrometers showed that macropores accounted for approximately 84% to 99% of the total saturated hydraulic conductivity. The plot scale (1 to 100 m²) generally appears to be within the representative elementary volume (REV), but drift in K_eff occurs beyond the REV due to changing geomorphic formations. Plot-scale infiltration tests are recommended over point-scale estimates, although only small plots (1 m × 1 m) are necessary.