Modeling Subsurface Drainage in Compacted Cultivated Histosols

Abstract

Reclaiming histosols in Montéregie region, Québec, Canada, increases peat decomposition and compaction rate and decreases the effectiveness of subsurface drainage. The objective of this paper was to use HYDRUS-2D to model the behavior of subsurface drainage systems, in order to evaluate the compaction effect on drain depth and spacing, and to determine the compact layer thickness and saturated hydraulic conductivities (Ksat) resulting in an improvement of subsurface drainage]. The drainage model was calibrated [Nash-Sutcliffe efficiency coefficient (NSE) = 0.958, percent bias (PBIAS) = −0.57%] using Ksat, meteorological data, and matric potential (h) data measured on the project site from June 10 to July 19, 2017. The calibrated and validated model was used to analyze the variation of h values (Δh in cm d−1) as a function of drain spacing (2–7 m) and drain depth (1 and 1.2 m) and to identify the response surface of Δh to various compact layer thickness and Ksat combinations. The results showed that Δh was on average 58% greater below the compact layer than above it and that reducing drain spacing or increasing drain depth does not improve the drainage rate. The analysis of the compact layer thickness and Ksat effect on Δh showed that for a Δh of 40 cm d−1, Ksat actual values in the two uppermost layers should be multiplied by 50 for compact layer thickness varying from 12 to 35 cm. Water percolation in the soil is reduced by the compact layer. Soil management methods for improving Ksat should therefore be better than deepening the drains or and reducing the spacing.

Delineating soil moisture dynamics within an evapotranspiration surface barrier using spatial‐temporal analysis

“…The flow equation incorporates a sink term to account for water uptake by plant roots (Šimůnek et al., 2012). HYDRUS has been used for modeling flow in the vegetated surface covers (e.g., Berger, 2017, 2018; Guedessou et al., 2021; Ogorzalek et al., 2008; Wongkaew et al., 2018; Yasser et al., 2012). However, numerical convergence of water balance may occur for relatively coarse soils under long‐term realistic hydrologic conditions (Sage et al., 2000).…”