Saturated hydraulic conductivity (
Ksat) is fundamental to shallow groundwater processes. There is an ongoing need for observed and model validated
Ksat values. A study was initiated in a representative catchment of the Chesapeake Bay Watershed in the Northeast USA,
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Saturated hydraulic conductivity (
Ksat) is fundamental to shallow groundwater processes. There is an ongoing need for observed and model validated
Ksat values. A study was initiated in a representative catchment of the Chesapeake Bay Watershed in the Northeast USA, to collect observed
Ksat and validate five
Ksat pedotransfer functions. Soil physical characteristics were quantified for dry bulk density (
bdry), porosity, and soil texture, while
Ksat was quantified using piezometric slug tests. Average
bdry and porosity ranged from 1.03 to 1.30 g/cm
3 and 0.51 to 0.61, respectively. Surface soil (0–5 cm)
bdry and porosity were significantly (
p < 0.05) lower and higher, respectively, than deeper soils (i.e., 25–30 cm; 45–50 cm).
bdry and porosity were significantly different with location (
p < 0.05). Average soil composition was 92% sand. Average
Ksat ranged from 0.29 to 4.76 m/day and significantly differed (
p < 0.05) by location. Four models showed that spatial variability in farm-scale
Ksat estimates was small (CV < 0.5) and one model performed better when
Ksat was 1.5 to 2.5 m/day. The two-parameter model that relied on silt/clay fractions performed best (ME = 0.78 m/day; SSE = 20.68 m
2/day
2; RMSE = 1.36 m/day). Results validate the use of simple, soil-property-based models to predict
Ksat, thereby increasing model applicability and transferability.
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