Does Spontaneous Secondary Succession Contribute to the Drying of the Topsoil?

• Published in: Forests Vol. 14; no. 2; p. 356
• Main Authors: Hewelke, Edyta, Zaniewski, Piotr T., Zaniewska, Ewa, Papierowska, Ewa, Gozdowski, Dariusz, Łachacz, Andrzej, Górska, Ewa Beata
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.02.2023
• Subjects: afforestation; Agricultural production; bio-hydro-physical soil properties; Carbon; Classification; Climate change; Comparative analysis; Coniferous forests; Contact angle; Drought; Drying; Ecological succession; Environmental aspects; Forests; Forests and forestry; Global warming; Hydrophobicity; Land use; Measurement; Moisture content; Moisture effects; Physiological aspects; Pine trees; Plant succession; Poland; Rain; Repellency; sandy soil; Sandy soils; Sessile drop method; soil hydrophobicity; Soil layers; Soil moisture; soil moisture content; Temperature; Topsoil; Vegetation; Water content; Water drops; Wetting; Wilting; Wilting point; Poland
• ISSN: 1999-4907; 1999-4907
• DOI: 10.3390/f14020356

The aim of the study was to analyse the moisture content (θ) and the persistence and strength of water repellency (SWR) on sandy soil excluded from cultivation and then undergoing spontaneous afforestation or weed infestation during an abnormally warm period. Three site plots in close proximity were selected, i.e., Scots pine forest—S1 (Dicrano-Pinion), birch forest—S3 (Molinio-Frangulion) 25 years old, and an abandoned field—S2 (Scleranthion annui) 1 year old, in Central Poland. The study covers the growing period in 2020 for the two upper soil layers. For the top layer, the average θ values for S1, S2, and S3 were 0.069, 0.101, and 0.123 cm3cm−3, respectively. In S1, the θ values were close to the permanent wilting point, and the actual SWR classes (water drop penetration time WDPT test) indicated the top layer as belonging to the extremely repellent class continuously for almost the whole study period. For other sites and soil layers, the wettable SWR classes were assessed. Whereas the severity of the potential SWR, based on measured values of the wetting contact angle (sessile drop method), also showed hydrophobicity for the top layer under the birch forest. The study provides new information regarding the risk of drying out the soil due to the SWR in sandy soils, depending on land use and climate warming.