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We discuss the theoretical development of the measurement of the T2* component from a surface nuclear magnetic resonance (SNMR) experiment using superconducting quantum interference devices (SQUIDS) as a point B-field receiver.
We discuss the differences between point receivers compared to traditional coincident-loop receivers, and demonstrate the first measurements of T2* with a SQUID sensor at the hydrogeophysical test site in Schillerslage, Germany.
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