Abstract

AbstractSoil wettability is important for understanding a wide range of earth system processes, from agricultural productivity to debris flows and sediment fan formation. However, there is limited research considering how soil–water interactions, where the soil grains are naturally hydrophobic, might change in the presence of oil from natural hydrocarbon leakage or oil spills. Here we show how slippery liquid‐infused porous surfaces (SLIPS) apply to hydrophobic soils, by physical modelling of surfaces of different grain sizes and examining their interactions with water before and after impregnation with silicone oil. Using contact and sliding angle measurements and laser scanning fluorescence confocal microscopy, we demonstrate that soil SLIPS can be created with thick oil layers and thin conformal oil layers on median grain sizes of 231 μm and 32 μm, respectively. Until now, SLIPS have only been observed in human‐made materials and biological surfaces. The mechanisms reported here demonstrate that SLIPS can occur in natural granular materials, providing a new mechanism for water‐shedding in soil and sediment systems. Furthermore, the water‐shedding properties may be long lasting as conformal oil layers are stabilized by capillary forces. These results have important implications for understanding soil physics and mechanics where oil is present in a soil, and for agricultural hydrophobicity on shallow slopes.Highlights We model oil contamination on a hydrophobic model soil as a mechanism for creating SLIPS. Soil SLIPS have implications for water‐shedding, oil spill remediation and earth processes. Our model soils exhibit extreme water‐shedding, illustrated by low water droplet sliding angles. This is the first physical modelling observation of SLIPS arising from hydrophobic soil.

Highlights

  • Wettability is a measure of a soils affinity for water

  • The overall trend shows apparent decreasing of the contact angle and Contact angle hysteresis (CAH) increasing with increasing grain size

  • The low sliding angle at the smallest grain size and the retention of the droplet on the near-vertical surface at the highest grain size dramatically illustrate the concepts of “slippy” and “sticky” surfaces we introduced in the Concepts of Water Repellence section

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Summary

Introduction

Wettability is a measure of a soils affinity for water. Water-repellent, or hydrophobic, soil has a low affinity for water and low rates of infiltration, with hydrological and geomorphological consequences (Jordán, Zavala, Mataix-Solera, & Doerr, 2013). Water repellence leads to poor agricultural productivity due to the formation of preferential flow paths and finger flow, which affects the transport of water and solutes (Shakesby, Doerr, & Walsh, 2000; van Ommen, Dekker, Dijksma, Hulshof, & van der Molen, 1988; Wang et al, 2018). In some circumstances, this can lead to groundwater contamination through leaching of pesticides and other substances (Blackwell, 2000; Van Dam et al, 1990). This stability can lead to reduced evaporation of water from deep within the soil profile (Hallett, 2007); a similar process increases carbon sequestration, through reduced biodegradation of organic matter or increased aggregate stability (Bachmann et al, 2008; Piccolo, Spaccini, Haberhauer, & Gerzabek, 1999; Spaccini, Piccolo, Conte, Haberhauer, & Gerzabek, 2002)

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