Predictability of the Evolution of the Soil Structure using Water Flow Modeling for a Constructed Technosol
Résumé
This paper focuses on the rela on between the structure of a constructed Technosol and its hydraulic characteris cs during its early pedogenesis. The method is based on a 3-yr comparison of, on one hand, experimental measurements from an in situ gravita on lysimeter and, on the other hand, a modeling approach with HYDRUS-1D. The change of water fl ow pa erns with me was described. It was consistent with previous results for constructed Technosol aggrega on. Apart from seasonal varia ons, the specifi city of the hydraulic func oning of the constructed Technosol was shown to be due to the nature of its technogenic parent materials. The in situ evolu on of the hydrodynamics has been established and partly linked to external factors (climate, vegeta on). The direct modeling and the op miza on of the parameters over fi rst a 3-yr period and then three 9-mo periods accurately represented global water fl ow trends at the pedon scale. However it failed to simulate precisely the main events, such as massive leachate ou low. An evolu on with me of some of the hydraulic proper es was shown, expressing the structuring of the soil. The existence of two dis nct me-scales (slow and steady/fast and cyclic) of the evolu on of hydraulic parameters was then formulated as a new hypothesis. Abbrevia ons: Hz, horizon; TDR, me domain refl ectometry.
Domaines
Science des sols
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