Mechanical Compliance of Individual Fractures in a Heterogeneous Rock Mass From Production-Type Full-Waveform Sonic Data

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Mechanical Compliance of Individual Fractures in a Heterogeneous Rock Mass From Production-Type Full-Waveform Sonic Data. / Zhou, Zhenya; Caspari, Eva; Barbosa, Nicolas Daniel et al.
In: Journal of geophysical research, Vol. 127.2022, No. 8, e2022JB024302, 03.08.2022.

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@article{044f44786c644e69a55590c0c1d51f5e,
title = "Mechanical Compliance of Individual Fractures in a Heterogeneous Rock Mass From Production-Type Full-Waveform Sonic Data",
abstract = "The mechanical fracture compliance is of interest in a number of geoscientific applications. Seismic borehole methods, especially full-waveform sonic (FWS) data, have indicated their potential to infer the compliance of macroscopic fractures under in situ conditions. These approaches rely on the assumption of a homogeneous background embedding the fractures and, as of yet, compliance estimates for individual fractures are limited to static FWS measurements. In this work, we assess the potential of inferring the compliance of individual fractures from standard, production-type FWS data in the presence of background heterogeneity. We first perform a comparative test on synthetic data to evaluate three approaches known as the transmission, phase, and group time delay methods. The results indicate that the former two produce adequate compliance estimates for scenarios with a strongly heterogeneous background or a damage zone around the fracture. These two methods are then applied to two FWS data sets acquired before and after a hydraulic stimulation campaign in a crystalline rock, which allows to test them on natural and man-made fractures. The transmission method turned out to be unsuitable for the considered data due to its reliance on amplitudes. Conversely, the travel time behavior remained stable and the phase time delay method produced robust and consistent estimates. The results for a newly created hydro-fracture imply the capability of resolving remarkably small compliance values of the order of 10 −14 m/Pa. This estimate is one order-of-magnitude smaller than that for the natural fracture, which may help to distinguish between these two fracture types.",
author = "Zhenya Zhou and Eva Caspari and Barbosa, {Nicolas Daniel} and Andrew Greenwood and Klaus Holliger",
note = "Publisher Copyright: {\textcopyright} 2022. The Authors.",
year = "2022",
month = aug,
day = "3",
doi = "10.1029/2022JB024302",
language = "English",
volume = "127.2022",
journal = "Journal of geophysical research",
issn = "2169-9313",
publisher = "American Geophysical Union",
number = "8",

}

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TY - JOUR

T1 - Mechanical Compliance of Individual Fractures in a Heterogeneous Rock Mass From Production-Type Full-Waveform Sonic Data

AU - Zhou, Zhenya

AU - Caspari, Eva

AU - Barbosa, Nicolas Daniel

AU - Greenwood, Andrew

AU - Holliger, Klaus

N1 - Publisher Copyright: © 2022. The Authors.

PY - 2022/8/3

Y1 - 2022/8/3

N2 - The mechanical fracture compliance is of interest in a number of geoscientific applications. Seismic borehole methods, especially full-waveform sonic (FWS) data, have indicated their potential to infer the compliance of macroscopic fractures under in situ conditions. These approaches rely on the assumption of a homogeneous background embedding the fractures and, as of yet, compliance estimates for individual fractures are limited to static FWS measurements. In this work, we assess the potential of inferring the compliance of individual fractures from standard, production-type FWS data in the presence of background heterogeneity. We first perform a comparative test on synthetic data to evaluate three approaches known as the transmission, phase, and group time delay methods. The results indicate that the former two produce adequate compliance estimates for scenarios with a strongly heterogeneous background or a damage zone around the fracture. These two methods are then applied to two FWS data sets acquired before and after a hydraulic stimulation campaign in a crystalline rock, which allows to test them on natural and man-made fractures. The transmission method turned out to be unsuitable for the considered data due to its reliance on amplitudes. Conversely, the travel time behavior remained stable and the phase time delay method produced robust and consistent estimates. The results for a newly created hydro-fracture imply the capability of resolving remarkably small compliance values of the order of 10 −14 m/Pa. This estimate is one order-of-magnitude smaller than that for the natural fracture, which may help to distinguish between these two fracture types.

AB - The mechanical fracture compliance is of interest in a number of geoscientific applications. Seismic borehole methods, especially full-waveform sonic (FWS) data, have indicated their potential to infer the compliance of macroscopic fractures under in situ conditions. These approaches rely on the assumption of a homogeneous background embedding the fractures and, as of yet, compliance estimates for individual fractures are limited to static FWS measurements. In this work, we assess the potential of inferring the compliance of individual fractures from standard, production-type FWS data in the presence of background heterogeneity. We first perform a comparative test on synthetic data to evaluate three approaches known as the transmission, phase, and group time delay methods. The results indicate that the former two produce adequate compliance estimates for scenarios with a strongly heterogeneous background or a damage zone around the fracture. These two methods are then applied to two FWS data sets acquired before and after a hydraulic stimulation campaign in a crystalline rock, which allows to test them on natural and man-made fractures. The transmission method turned out to be unsuitable for the considered data due to its reliance on amplitudes. Conversely, the travel time behavior remained stable and the phase time delay method produced robust and consistent estimates. The results for a newly created hydro-fracture imply the capability of resolving remarkably small compliance values of the order of 10 −14 m/Pa. This estimate is one order-of-magnitude smaller than that for the natural fracture, which may help to distinguish between these two fracture types.

UR - http://www.scopus.com/inward/record.url?scp=85136856617&partnerID=8YFLogxK

U2 - 10.1029/2022JB024302

DO - 10.1029/2022JB024302

M3 - Article

VL - 127.2022

JO - Journal of geophysical research

JF - Journal of geophysical research

SN - 2169-9313

IS - 8

M1 - e2022JB024302

ER -