Nanoscale detection of metastable states in porous and granular media

TL;DR

This study demonstrates nanoscale detection of metastable states in porous sandstone using superconducting thin films, revealing how external cooling triggers microfractures linked to microseismicity in geologic reservoirs.

Contribution

It introduces a novel nanoscale sensing method using superconducting Al films to detect metastable states and microfractures in sandstone, advancing understanding of microseismic triggers.

Findings

Sharp resistance jumps indicate microfractures in sandstone.

Microwave-induced Shapiro steps confirm superconducting network of nanobridges.

Detection of metastable states correlates with microseismic activity potential.

Abstract

Microseismicity in subsurface geologic environments, such as sandstone gas reservoirs, is expected in the presence of liquid or gas injection. Although difficult to predict, the potential for microseismic events is important to field-scale projects, such as geologic storage of CO2 whereby the gas is injected into natural sandstone formations. We conjecture that a primary factor causing microseismicity is the existence of metastable states in granular porous medium and provide experimental evidence for its validity. External perturbation trigger abrupt relaxation events, which, with a certain probability, can grow into macroscopic microseismic events. Here the triggering perturbation is produced by cooling to a cryogenic temperature. As the "sensor" for the abrupt relaxation events we use thin Al films deposited on the sandstone surface. We show that as the temperature is varied, the films' resistance exhibits sharp jumps, which we attribute to mechanical restructuring or microfractures in the fabric of the sandstone. We checked the superconducting characteristics of the Al thin films on the sandstone and found microwave-induced Shapiro steps on the voltage-current diagrams. Such quantized steps provide indicates that the film is made of a network of nanobridges, which makes it ever more sensitive to abrupt relaxation events occurring in the substrate, i.e., in the underlying sandstone.