Task 1-4 : Petrophysical characterization [GM, ISTerre, IC2MP]

Objectives :
Measure petrophysical properties of the samples in Nojima and Soultz characterized in tasks T1.1-T1.3, to derive a petrophysical proxy of alteration. The main target property will be electrical resistivity, also measured by borehole geophysics [T1.5]

Description of planned work :
(1) A first part of this work will extend the preliminary work undertaken by Ph. Pezard on electrical resistivity, to target more specifically the main fault zone. Complex resistivity measurements [GM] provides also induced polarization of the samples on a broad frequency range. Resistivity is depending (i) on surface conductivity, which could be related to Cation Exchange Capacity [IC2MP] and mineralogy [T1.1] and (ii) on the porous network and its tortuosity (X-Ray CT scan [T1.2], 14C-PMMA [IC2MP]). Hence, resistivity is both dependent on alteration and on damage.
(2) On the other end, sonic velocities [ISTerre] are expected to be primarily dependent on damage.
(3) By comparing both datasets, we plan to derive a calibration of resistivity and sonic velocities as petrophysical proxies of alteration

AnalysisPurposeInstitute in chargeNojimaSoultz
Complex resistivity Measurement of complex resistivity at several frequencies, for samples imbibed with fluids of increasing electrical conductivity
→ Geophysical proxy of alteration & damage
GM (Gibert + Pezard++ PhD) Selected samples Selected samples
Sonic velocities P- and S- wave velocities under ambient pressure.
→ Geophysical proxy of damage
ISTerre Grenoble (Doan) Systematic Selected samples
CEC Cation Exchange Capacity (method NF X31-130)
→ rough proportion of swellable clays, zeolites
→ Surface conductivity
IC2MP Poitiers (Patrier, Baron) Systematic Selected samples
14C-PMMA Radiography of samples impregnated by 14C-PMMA
→ fine imaging of fracture network (down to 50 Å)
IC2MP Poitiers (Sardini + Billon + M2 Poitiers #2) Selected samples

Updated on 1er avril 2024