The inversion of surface-NMR T₁ data for improved aquifer characterization

verfasst von

Mike Müller-Petke, Jan O. Walbrecker, Rosemary Knight

Abstract

A crucial component in sustainable freshwater management is the reliable and cost-effective characterization of groundwater aquifers. A technique that allows noninvasive characterization of shallow (<100 m) aquifers is surface nuclear magnetic resonance (surface NMR). The measured parameter longitudinal relaxation time T₁ provides a link to pore-scale properties and can be used to estimate the hydraulic conductivity of the sampled region. The recent development of an optimized acquisition scheme, phase-cycled pseudosaturation recovery (pcPSR), has significantly advanced our ability to acquire surface-NMR T₁ data. Building on these findings, we developed an inversion scheme that can reconstruct the depth-distribution of T₁ from pcPSR data. To stabilize the inversion, we took a staggered approach:We first determined the distribution of water content and effective transverse relaxation time T*₂, and then we resolved the T₁ structure. We tested the capability of the inversion in a synthetic study using models containing an unconfined and confined aquifer under conditions of low and high levels of ambient electromagnetic noise. The results allowed us to optimize the design of pcPSR experiments, finding that acquiring pcPSR data at three interpulse delay times is the best choice when acquiring surface-NMR data in an area with no prior information. We have verified our inversion approach in a field study in Nebraska, USA, where we had access to borehole lithologic information and logging-NMR T₁ measurements. Although the structural details (<1 m) detected in logging NMR were not resolved in surface NMR - highlighting the general resolution limitation of surface NMR - the two methods consistently revealed a zone of elevated T₁ corresponding to a sand and gravel unit, overlying a zone of lower T₁ corresponding to a sand/sandstone unit. Our developed inversion scheme is an important step toward the reliable interpretation of surface-NMR T₁ data for aquifer characterization.

Externe Organisation(en)

Leibniz-Institut für Angewandte Geophysik (LIAG)
Stanford University

Typ

Artikel

Journal

GEOPHYSICS

Band

78

Seiten

EN83-EN94

ISSN

0016-8033

Publikationsdatum

2013

Publikationsstatus

Veröffentlicht

Peer-reviewed

Ja

ASJC Scopus Sachgebiete

Geochemie und Petrologie

Ziele für nachhaltige Entwicklung

SDG 6 – Sauberes Wasser und sanitäre Einrichtungen

Elektronische Version(en)

https://doi.org/10.1190/GEO2013-0035.1 (Zugang: Unbekannt)