Aquifer Variation Characteristics of Overlying Strata in Coal Mining Based on Time-Lapse Apparent Resistivity Monitoring

W. Du; S. Peng; G. Zhu; X. Zhang

doi:10.3997/2214-4609.201802745

Aquifer Variation Characteristics of Overlying Strata in Coal Mining Based on Time-Lapse Apparent Resistivity Monitoring
Authors W. Du¹, S. Peng¹, G. Zhu¹, X. Zhang¹
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Affiliations: ¹ China University of Mining & Technology
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 2nd Conference on Geophysics for Mineral Exploration and Mining, Sep 2018, Volume 2018, p.1 - 5
DOI: https://doi.org/10.3997/2214-4609.201802745

Abstract

Summary

Time-lapse apparent resistivity monitoring carries out multiple observations for the same stratum at certain time intervals to study the temporal-spatial variations of aquifer characteristics of overlying strata, which can be repeated multiple 2D observation. Time-lapse apparent resistivity monitoring involves aspects such as data acquisition, processing and interpretation and inversion.

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2018-09-09

2024-04-19

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References

W. F.Du, S. P.Peng, G. W.Zhu,
2014, Time-lapse geophysical technology-based study on overburden strata changes induced by modern coal mining. International Journal of Coal Science & Technology, 1(2):184–191.
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Aquifer Variation Characteristics of Overlying Strata in Coal Mining Based on Time-Lapse Apparent Resistivity Monitoring

Conference Proceedings 2018, 1 (2018); https://doi.org/10.3997/2214-4609.201802745

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Aquifer Variation Characteristics of Overlying Strata in Coal Mining Based on Time-Lapse Apparent Resistivity Monitoring

Abstract

From This Site

Most Read This Month

Most Cited This Month Most Cited RSS feed

The natural combination of full and image‐based waveform inversion

Poststack diffraction imaging using reverse‐time migration

Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks

Fracture detection by Gaussian beam imaging of seismic data and image spectrum analysis

Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture