Vacuum drying water-repellent sandy soil: Anoxic conditions retain original soil water repellency under variable soil drying temperature and air pressure

•Soil water repellency (SWR) best measured by vacuum drying under anoxic conditions.•Similar soil water contents occurred for 20 °C vacuum and 105 °C oven-dried soil.•No difference in SWR between samples vacuum-dried anoxically at 20 °C or 105 °C.•Drying at 105 °C decreased SWR compared to 20 °C und...

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Veröffentlicht in:Geoderma 2020-08, Vol.372, p.114385, Article 114385
Hauptverfasser: Wong, Enoch V.S., Ward, Philip R., Murphy, Daniel V., Leopold, Matthias, Barton, Louise
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Sprache:eng
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Zusammenfassung:•Soil water repellency (SWR) best measured by vacuum drying under anoxic conditions.•Similar soil water contents occurred for 20 °C vacuum and 105 °C oven-dried soil.•No difference in SWR between samples vacuum-dried anoxically at 20 °C or 105 °C.•Drying at 105 °C decreased SWR compared to 20 °C under oxic conditions at 101 kPa. Monitoring land degradation due to soil water repellency (SWR) through space and time is often complicated by different soil drying temperatures and drying times that generate artefacts causing inconsistent SWR results. This study aimed to develop a reproducible soil drying method at room temperature for the severity of potential SWR determination. We compared conventional 105 °C oven drying under oxic conditions (101.3 kPa) and vacuum drying under anoxic conditions (20 °C and low air pressure 1.3 kPa)—both drying methods removed the same amount of water from soil. We then investigated the effect of aeration condition (anoxic or oxic), temperature (20 °C or 105 °C) and air pressure (1.3 kPa or 101.3 kPa) on SWR and residual soil water content after drying using a complete factorial design. We hypothesised that 1) SWR will decrease with low air pressure under both oxic and anoxic conditions, 2) SWR will remain unchanged with temperature under anoxic conditions, and 3) conventional air drying treatments will have the highest residual soil water content. We used sieved, air-dried soil (
ISSN:0016-7061
1872-6259
DOI:10.1016/j.geoderma.2020.114385