Ground displacement data around the city of Ravenna do not support uplifting Venice by water injection

The proposed injection of seawater in a brackish, sandy aquifer lying 600–800 m under the lagoon of Venice to lift Venice itself uniformly up to 30 cm in 10 years raises many problems. We discuss here whether a smooth uplift can be obtained as claimed by the proponents. We first underline the simila...

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Bibliographic Details
Published inTerra nova (Oxford, England) Vol. 21; no. 2; pp. 144 - 150
Main Authors Schrefler, B. A., Ricceri, G., Achilli, V., Menin, A., Salomoni, V. A.
Format Journal Article
LanguageEnglish
Published Oxford, UK Blackwell Publishing Ltd 01.04.2009
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Summary:The proposed injection of seawater in a brackish, sandy aquifer lying 600–800 m under the lagoon of Venice to lift Venice itself uniformly up to 30 cm in 10 years raises many problems. We discuss here whether a smooth uplift can be obtained as claimed by the proponents. We first underline the similarities between the Ravenna and Venice case. We then examine the subsidence around Ravenna because of fluid extraction and the measured surface displacements for the period when there is pressure recovery both in the depleted gas reservoir close to Ravenna and in the upper aquifer system. Uniform surface settlements are nowhere observed and strong influence of local heterogeneities cannot be ruled out. The whole picture suggests great caution and the need for much more investigation before undertaking such an injection.
Bibliography:istex:A681778EEB210B53B44F261B378613828DD3C1C5
ark:/67375/WNG-S26PS4DL-V
ArticleID:TER867
ISSN:0954-4879
1365-3121
DOI:10.1111/j.1365-3121.2009.00867.x