Periodic pumping tests were conducted using a double-packer probe placed at four different depth levels in borehole GDP-1 at Grimselpass, Central Swiss Alps, penetrating a hydrothermally active fault. The tests had the general objective to explore the potential of periodic testing for hydraulic characterization of faults, representing inherently complex heterogeneous hydraulic features that pose problems for conventional approaches. Site selection reflects the specific question regarding the value of this test type for quality control of hydraulic stimulations of potential geothermal reservoirs. The performed evaluation of amplitude ratio and phase shift between pressure and flow rate in the pumping interval employed analytical solutions for various flow regimes. In addition to the previously presented 1-D and radial-flow models, we extended the one for radial flow in a system of concentric shells with varying hydraulic properties and newly developed one for bilinear flow. In addition to these injectivity analyses, we pursued a vertical-interference analysis resting on observed amplitude ratio and phase shift between the periodic pressure signals above or below packers and in the interval by numerical modeling of the non-radial-flow situation. When relying on the same model the order of magnitude of transmissivity values derived from the analyses of periodic tests agrees with that gained from conventional hydraulic tests. The field campaign confirmed several advantages of the periodic testing, for example, reduced constraints on testing time relative to conventional tests since a periodic signal can easily be separated from changing background pressure by detrending and Fourier transformation. The discrepancies between aspects of the results from the periodic tests and the predictions of the considered simplified models indicate a hydraulically complex subsurface at the drill site that exhibits also hydromechanical features in accord with structural information gained from logging. The exploratory modeling of vertical injectivity shows its potential for analysing hydraulic anisotropy. Yet, more comprehensive modeling will be required to take full advantage of all the pressure records typically acquired when using a double-packer probe for periodic tests.
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Univ Ghent, Dept Geol, Lab Appl Geol & Hydrogeol, Krijgslaan 281,S8, B-9000 Ghent, BelgiumBahir Dar Univ, Blue Nile Water Inst, Sch Earth Sci, POB 79, Bahir Dar, Ethiopia
Yenehun, Alemu
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Belay, Ashebir Sewale
Asmamaw, Desale Kidane
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Bahir Dar Univ, Blue Nile Water Inst, Dept Nat Resource Management, POB 79, Bahir Dar, EthiopiaBahir Dar Univ, Blue Nile Water Inst, Sch Earth Sci, POB 79, Bahir Dar, Ethiopia
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Univ Rouen, CNRS, UMR 6143, M2C,Morphodynam Continentale & Cotiere, Mont St Aignan, FranceUniv Rouen, CNRS, UMR 6143, M2C,Morphodynam Continentale & Cotiere, Mont St Aignan, France
Ahmed, A. Soueid
Jardani, A.
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Univ Rouen, CNRS, UMR 6143, M2C,Morphodynam Continentale & Cotiere, Mont St Aignan, FranceUniv Rouen, CNRS, UMR 6143, M2C,Morphodynam Continentale & Cotiere, Mont St Aignan, France
Jardani, A.
Revil, A.
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Univ Savoie Mt Blanc, CNRS, ISTerre, UMR 5275,Equipe Geophys Volcans, F-73376 Le Bourget Du Lac, FranceUniv Rouen, CNRS, UMR 6143, M2C,Morphodynam Continentale & Cotiere, Mont St Aignan, France
Revil, A.
Dupont, J. P.
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Univ Rouen, CNRS, UMR 6143, M2C,Morphodynam Continentale & Cotiere, Mont St Aignan, FranceUniv Rouen, CNRS, UMR 6143, M2C,Morphodynam Continentale & Cotiere, Mont St Aignan, France