Researcher: Coupling of holocene self-compaction models and compaction due to overexploitation of confined aquifers with application to the Mekong river delta via EURAXESS

Università degli Studi di Padova

Padova, Italy 🇮🇹

Offer Description

Delta subsidence is the result of a complex interplay of natural and human-induced (anthropogenic) drivers and processes in the subsurface. Subsidence processes strongly depend on local geology, hydrology, and water management and especially human-induced subsidence can be highly variable in both time and space. In most deltas current subsidence is predominantly caused by two processes acting at different depths: a) compaction of shallow sediments, driven by physical loading by the sediments themselves or drainage, and b) aquifer-system compaction, driven by groundwater extraction. Process interactions between different depth domains may have significant impact on the total amount and the spatial-temporal distribution of subsidence in a delta. The research is aimed to develop a novel dual-model approach of two complementary, state-of-the-art numerical model codes: NATSUB3D simulating autocompaction and iMOD-SUBCR simulating aquifer system compaction due to groundwater pumping.

Where to apply

Website: https://protocollo.unipd.it/albo/viewer

Requirements

Additional Information

Eligibility criteria

Eligible destination country/ies for fellows:

  • Italy

Eligibility of fellows: country/ies of residence:

  • OTHER

Eligibility of fellows: nationality/ies:

  • OTHER

Additional comments

  • Annual budget: 24320
  • Frequency of calls: 12 mesi
  • International mobility required: no

Website for additional job details: https://protocollo.unipd.it/albo/viewer


POSITION TYPE

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