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Early pedogenesis of a Technosol developing on iron industry deposits

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HAL Id: hal-02746294

https://hal.inrae.fr/hal-02746294

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Early pedogenesis of a Technosol developing on iron

industry deposits

Hermine Huot, Marie-Odile Simonnot, Françoise Watteau, Philippe Marion,

Jacques Yvon, Pierre Faure, Philippe de Donato, Patrick Charbonnier,

Jean-Louis Morel

To cite this version:

Hermine Huot, Marie-Odile Simonnot, Françoise Watteau, Philippe Marion, Jacques Yvon, et al.. Early pedogenesis of a Technosol developing on iron industry deposits. 7. International Conference of the Working Group on Soils in Urban, Industrial, Traffic, Mining and Military Areas (SUITMA) of International Union of Soil Sciences, Sep 2013, Torun, Poland. 14 p. �hal-02746294�

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Early pedogenesis of a Technosol developing on iron industry

deposits

Hermine Huota,b,c,d, Marie-Odile Simonnotc,d, Françoise Watteaua,b, Philippe Marione,f, Jacques Yvone,f, Pierre Faureg,h, Philippe De Donatoe,f, Patrick

Charbonnieri, Jean-Louis Morela,b

a

Université de Lorraine, Laboratoire Sols et Environnement, UMR 1120, Vandoeuvre-lès-Nancy, F-54518, France

b

INRA, Laboratoire Sols et Environnement, UMR 1120, Vandoeuvre-lès-Nancy, F-54518, France

c

Université de Lorraine, Laboratoire Réactions et Génie des Procédés, UMR 7274, Nancy, F-54001, France

d

CNRS, Laboratoire Réactions et Génie des Procédés, UMR 7274, Nancy, F-54001, France

e

Université de Lorraine, GéoRessources, UMR 7359, Vandoeuvre-lès-Nancy, F-54518, France

f

CNRS, GéoRessources, UMR 7359, Vandoeuvre-lès-Nancy, F- 54518, France g

Université de Lorraine, Laboratoire Interdisciplinaire des Environnements Continentaux, UMR 7360, Vandoeuvre-lès-Nancy, F- 54506, France h

CNRS, Laboratoire Interdisciplinaire des Environnements Continentaux, UMR 7360, Vandoeuvre-lès-Nancy, F- 54506, France

i

ArcelorMittal Real Estate France, F-57700 Hayange, France

Keywords : Technosol, iron industry settling pond, pedogenesis, rhizosphere

As a result of increasing soil anthropisation, large surface areas covered by anthropogenic materials are submitted to environmental factors (e.g. climate, organisms). Pedogenesis of the developing Technosols is often characterized by an intense and rapid weathering (1, 2, 3). However, the nature, localization, and extent of the pedogenetic processes occurring in Technosols are still little known.

To assess the soil formation on purely anthropogenic parental materials, a former settling pond of iron industry sludge colonized by vegetation since ca. 50 years was chosen. The soil is composed of contrasted layers, and an organic layer has developed at the surface (4, 5, 6). Composition, mineral and organic components and structure of the soil were studied as tracers of the material origin and indicators of early pedogenetic processes. Also, historical records regarding the industrial operations were analyzed. Twelve layers were sampled in the first two meters of the profile. Mineralogy was determined with XRD, IR, Mössbauer spectroscopy, SEM and TEM-EDS. Spectroscopic and molecular analyses were carried out on solvent extractable organic matter. Thin sections were prepared for some layers.

Results showed a stratification of the soil profile resulting from successive sludge supplies. Composition, mineralogy, and structure of the layers of the Technosol were derived from the industrial raw materials and processes. Elemental composition reflected the enrichment in volatile elements, and organic analyses the dumping of oil and combustion by-products. Part of the mineral phases was inherited from raw materials, and others resulted from the industrial processes (e.g. high temperature

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phases). Pedogenetic processes were obvious with the development of an organo-mineral horizon. In the deeper layers, analysis of microstructure and organo-mineralogy revealed physical (cracks, solute movements) and chemical processes (dissolution, precipitation). These phenomena occurred primarily in cracks and at the interfaces between two layers. Also, roots, which have colonized the whole profile, and developed preferentially in these areas, have induced changes in their rhizosphere (modification of porosity and metal extractability). In conclusion, the Technosol results from successive steps of pedogenesis, driven firstly by drying-wetting cycles and changes of physico-chemical conditions induced by the climatic factor, and finally by biological processes in relation with root development.

(1) Zevenbergen, C. et al., 1999. Clay formation and metal fixation during weathering of coal fly ash. Environmental Science and Technology, 33, 3405‑3409.

(2) Rossiter, D.G. 2007. Classification of urban and industrial soils in the World Reference Base for Soil Resources. Journal of Soils and Sediments, 7, 96‑100.

(3) Séré, G., et al., 2010. Early pedogenic evolution of constructed Technosols.

Journal of Soils and Sediments, 10, 1246‑1254.

(4) Schwartz, C. et al., 2001. Le pédologue en milieux industriels et urbains. I. Sols d’une friche industrielle. Etude et Gestion des Sols, 8, 135‑148.

(5) Sauer, D. and Burghardt, W., 2006. The occurrence and distribution of various forms of silica and zeolites in soils developed from wastes of iron production.

Catena, 65, 247‑257

(6) Huot, H. et al., 2012. Characteristics and potential pedogenetic processes of a Technosol developing on iron industry deposits. Journal of Soils and Sediments, doi: 10.1007//s11368-012-0513-1

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