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Magnetic Resonance in the Subsurface – 5th International ... - LIAG

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10.00 - 10.50 Coffee Break & Poster Session<br />

10.50 - 11.10 Hybrid and multi-objective genetic algorithm<br />

applications <strong>in</strong> MRS data <strong>in</strong>version<br />

Advances <strong>in</strong> hydrological parameterization 1<br />

11.10 - 11.30 Recent advancements <strong>in</strong> NMR for characteriz<strong>in</strong>g<br />

<strong>the</strong> vadose zone<br />

11.30 - 11.50 Direct <strong>in</strong>version for water retention parameters<br />

from MRS measurements <strong>in</strong> <strong>the</strong><br />

saturated/unsaturated zone <strong>–</strong> a sensitivity study<br />

11.50 - 12.10 MRS subsurface parametrization for coupled<br />

hydrological Marmites model<br />

12.10 - 12.30 An efficient full coupled <strong>in</strong>version of aquifer<br />

test, MRS and TEM data<br />

12.30 - 14.00 Lunch<br />

14.00 - 17.20 Advances <strong>in</strong> hydrological parameterization 2<br />

14.00 - 14.20 The <strong>in</strong>tegration of logg<strong>in</strong>g and surface NMR for<br />

mapp<strong>in</strong>g spatial variation <strong>in</strong> hydraulic<br />

conductivity<br />

14.20 - 14.40 Hard rock hydrogeophysics applied to<br />

hydrological model parameterization - Sardón<br />

catchment case study (Salamanca, Spa<strong>in</strong>)<br />

14.40 - 15.00 A laboratory study to determ<strong>in</strong>e <strong>the</strong> effect of<br />

surface roughness and gra<strong>in</strong> diameter on NMR<br />

relaxation rates of glass bead packs.<br />

15.00 - 15.20 A numerical study of <strong>the</strong> relationship between<br />

NMR relaxation and permeability <strong>in</strong> materials<br />

with large pores<br />

15.20 - 15.40 Coffee Break<br />

Case Studies 2<br />

15.40 - 16.00 NMR Logg<strong>in</strong>g: A tool for quantify<strong>in</strong>g effective<br />

porosity and hydraulic conductivity with<strong>in</strong> <strong>the</strong><br />

Murray Darl<strong>in</strong>g Bas<strong>in</strong> of Australia<br />

16.00 - 16.20 Feasibility study of <strong>the</strong> MRS monitor<strong>in</strong>g <strong>in</strong> a 3D<br />

hydrogeological structure: aquifer recharge<br />

from a pond <strong>in</strong> <strong>the</strong> Sahel (Niger)<br />

16.20 - 16.40 Investigat<strong>in</strong>g hydraulic properties of a glacial<br />

sand deposit <strong>in</strong> <strong>the</strong> north of Sweden<br />

16.40 - 17.00 Estmat<strong>in</strong>g regional groundwater reserve <strong>in</strong> a<br />

clayey sandstone aquifer of Cambodia<br />

17.00 - 17.20 The Applications of MRS for detection of<br />

Groundwater-<strong>in</strong>duced disasters , <strong>in</strong> Ch<strong>in</strong>a<br />

<strong>Magnetic</strong> <strong>Resonance</strong> <strong>in</strong> <strong>the</strong> <strong>Subsurface</strong> <strong>–</strong> 5 th <strong>International</strong> Workshop on <strong>Magnetic</strong> <strong>Resonance</strong><br />

Hannover, Germany, 25 <strong>–</strong> 27 September 2012<br />

Akca<br />

Walsh<br />

Costabel<br />

Baronc<strong>in</strong>i-<br />

Turricchia<br />

Vilhelmsen<br />

Knight<br />

Francés<br />

Keat<strong>in</strong>g<br />

Dlubac<br />

Abraham<br />

Boucher<br />

Pertuu<br />

Vouillamoz<br />

Jun<br />

10

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