Parameters influencing run-off on vegetated urban soils: A case study in Marseilles, France

• Published in: Geoderma 2020-10, Vol.376, p.114455-11, Article 114455
• Main Authors: Díaz-Sanz, Jesús, Robert, Samuel, Keller, Catherine
• Format: Article
• Language: English
• Subjects: Compaction; Environmental Sciences; Geography; Humanities and Social Sciences; Infiltration; Run-off; Technosols; Tile industry; Urban soils
• ISSN: 0016-7061; 1872-6259
• DOI: 10.1016/j.geoderma.2020.114455

•The field saturated hydraulic conductivity (Kfs) can assess run-off on urban soils.•Organic matter content can affect Kfs in recent vegetated urban soils.•The older the age of the current land-use, the larger Kfs.•Vegetated urban soils can mitigate run-off in areas with extreme precipitations.•Spatial planning should consider Kfs of vegetated urban soils. In urban areas, episodes of extreme precipitation may generate run-off floods, but urban soils are seldom considered in spatial planning documents. Our aim was to assess the infiltration of vegetated urban soils and to identify the soil parameters affecting infiltration in order to explore the potential of these soils for run-off mitigation under a Mediterranean climate with extreme precipitation episodes. We compared vegetated soils in the “urban” zone of the Marseilles’ 16th district (France) either lying on former clay quarries or tile factories (T) or not (NT) and with different land-uses. We used a simplified method to measure field saturated hydraulic conductivity (Kfs), measured penetration resistance in the first 0.15 m (Qd) and analysed physico-chemical properties in the first horizon. Levels of run-off production were estimated according to Kfs and an adaptation of USDA Hydrologic Soil Groups. All soils were Technosols or Anthrosols regardless of their prior history. We found that land-use history influenced Kfs, with T soils and soils with current vegetated land-use younger than 13 years having lower Kfs than NT soils and soils with land-use older than 13 years. Soil organic matter content influenced Kfs positively when soils were young, while vegetation cover and penetration resistance (most of the soils had Qd > 2 MPa) had not a clear effect on Kfs. Overall, combining Kfs and soil depth, 14.3% of the T soils and 84.6% of the NT soils had low levels of run-off production. It is therefore recommended that 1) Technosols or Anthrosols should be characterised for their unique physico-chemical and physical properties but also for their land-use history, and 2) the infiltration of these soils should be considered in spatial planning documents.