Green roof ageing or Isolatic Technosol’s pedogenesis?

Autor: Geoffroy Séré, Ryad Bouzouidja, Violaine Galzin, Gustave Rousseau, David Lacroix, Rémy Claverie
Přispěvatelé: Centre d'Etudes et d'Expertise sur les Risques, l'Environnement, la Mobilité et l'Aménagement - Direction Est (Cerema Direction Est), Centre d'Etudes et d'Expertise sur les Risques, l'Environnement, la Mobilité et l'Aménagement (Cerema), Laboratoire Sols et Environnement (LSE), Institut National de la Recherche Agronomique (INRA)-Université de Lorraine (UL), Centre d'Etudes et d'Expertise sur les Risques, l'Environnement, la Mobilité et l'Aménagement - Equipe-projet TEAM (Cerema Equipe-projet TEAM), Laboratoire d'Energétique et de Mécanique Théorique Appliquée (LEMTA ), Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS), Laboratoire Énergies et Mécanique Théorique et Appliquée (LEMTA )
Jazyk: angličtina
Rok vydání: 2018
Předmět:
Zdroj: Journal of Soils and Sediments
Journal of Soils and Sediments, Springer Verlag, 2018, 18 (2), pp.418-425. ⟨10.1007/s11368-016-1513-3⟩
ISSN: 1439-0108
1614-7480
DOI: 10.1007/s11368-016-1513-3⟩
Popis: International audience; Purpose Green roofs (GR) offer a way to improve several ecosystem services in cities. However, the performances of GR are basically considered as steady over time whereas they are living media subject to ageing that are rarely managed by their owners. This study transposes a pedological approach to evaluate changes in GR physical structure and chemical composition over time.Materials and methods A full-scale experimental plot with various vegetation cover was studied. A dedicated sampling strategy was implemented to monitor substrate’s evolution over 4 years. Then, physical and chemical characterisation (carbon and nitrogen contents, particle size distribution, porosity, soil water retention) was conducted and compared to results on the original substrate.Results and discussion The upper layer of the substrate (0 to 5 cm depth) contained a large amount of fine and short roots whereas the root density was much smaller in the lower layer of the substrate (5 to 10 cm depth). There was a global drop of the organic carbon content from 5 % in the initial substrate to 2 % in the 4-year-old substrate. On the contrary, the nitrogen concentration has increased by 0.4 % during the same period. Themesoporosity decreased drastically from 0.11 to 0.02 cm3 cm−3.On the whole substrate, the
Databáze: OpenAIRE