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Stoneley guided waves : What is missing in Biot's theory? / Korneev, V. A.; Ponomarenko, A. V.; Kashtan, B. M.

Poromechanics IV - 4th Biot Conference on Poromechanics. ред. / Hoe I. Ling; Andrew Smyth; Raimondo Betti. DEStech Publications Inc, 2009. стр. 706-711 (Poromechanics IV - 4th Biot Conference on Poromechanics).

Результаты исследований: Публикации в книгах, отчётах, сборниках, трудах конференций › статья в сборнике материалов конференции › Рецензирование

Harvard

Korneev, VA, Ponomarenko, AV & Kashtan, BM 2009, Stoneley guided waves: What is missing in Biot's theory? в HI Ling, A Smyth & R Betti (ред.), Poromechanics IV - 4th Biot Conference on Poromechanics. Poromechanics IV - 4th Biot Conference on Poromechanics, DEStech Publications Inc, стр. 706-711, 4th Biot Conference on Poromechanics, New York, Соединенные Штаты Америки, 8/06/09.

APA

Korneev, V. A., Ponomarenko, A. V., & Kashtan, B. M. (2009). Stoneley guided waves: What is missing in Biot's theory? в H. I. Ling, A. Smyth, & R. Betti (Ред.), Poromechanics IV - 4th Biot Conference on Poromechanics (стр. 706-711). (Poromechanics IV - 4th Biot Conference on Poromechanics). DEStech Publications Inc.

Vancouver

Korneev VA, Ponomarenko AV, Kashtan BM. Stoneley guided waves: What is missing in Biot's theory? в Ling HI, Smyth A, Betti R, Редакторы, Poromechanics IV - 4th Biot Conference on Poromechanics. DEStech Publications Inc. 2009. стр. 706-711. (Poromechanics IV - 4th Biot Conference on Poromechanics).

Author

Korneev, V. A. ; Ponomarenko, A. V. ; Kashtan, B. M. / Stoneley guided waves : What is missing in Biot's theory?. Poromechanics IV - 4th Biot Conference on Poromechanics. Редактор / Hoe I. Ling ; Andrew Smyth ; Raimondo Betti. DEStech Publications Inc, 2009. стр. 706-711 (Poromechanics IV - 4th Biot Conference on Poromechanics).

BibTeX

@inproceedings{febbb90bdcbe4bbca46293ccaee43607,
title = "Stoneley guided waves: What is missing in Biot's theory?",
abstract = "Permeability values consistently demonstrate that measurements at field scale (hundreds of meters to kilometers) show an increase of several orders of magnitude compared to values obtained at laboratory scales. This behavior suggests that in reservoirs fluids flow primarily in fractures rather than in pores. Fluid-filled fractures are capable to carry two types of dispersive slow waves: Biot wave and Stoneley guided wave, which is not described by Biot's theory. Results of numerical modeling suggest that Stoneley guided wave has overwhelmingly large amplitude compared to all other waves excited by a source in a fracture. It is likely that Stoneley guided wave is a key phenomenon which might explain observed frequency-dependence and nonlinear behavior of fluid reservoirs.",
author = "Korneev, {V. A.} and Ponomarenko, {A. V.} and Kashtan, {B. M.}",
note = "Copyright: Copyright 2015 Elsevier B.V., All rights reserved.; 4th Biot Conference on Poromechanics ; Conference date: 08-06-2009 Through 10-06-2009",
year = "2009",
language = "English",
series = "Poromechanics IV - 4th Biot Conference on Poromechanics",
publisher = "DEStech Publications Inc",
pages = "706--711",
editor = "Ling, {Hoe I.} and Andrew Smyth and Raimondo Betti",
booktitle = "Poromechanics IV - 4th Biot Conference on Poromechanics",
address = "United States",

}

RIS

TY - GEN

T1 - Stoneley guided waves

T2 - 4th Biot Conference on Poromechanics

AU - Korneev, V. A.

AU - Ponomarenko, A. V.

AU - Kashtan, B. M.

N1 - Copyright: Copyright 2015 Elsevier B.V., All rights reserved.

PY - 2009

Y1 - 2009

N2 - Permeability values consistently demonstrate that measurements at field scale (hundreds of meters to kilometers) show an increase of several orders of magnitude compared to values obtained at laboratory scales. This behavior suggests that in reservoirs fluids flow primarily in fractures rather than in pores. Fluid-filled fractures are capable to carry two types of dispersive slow waves: Biot wave and Stoneley guided wave, which is not described by Biot's theory. Results of numerical modeling suggest that Stoneley guided wave has overwhelmingly large amplitude compared to all other waves excited by a source in a fracture. It is likely that Stoneley guided wave is a key phenomenon which might explain observed frequency-dependence and nonlinear behavior of fluid reservoirs.

AB - Permeability values consistently demonstrate that measurements at field scale (hundreds of meters to kilometers) show an increase of several orders of magnitude compared to values obtained at laboratory scales. This behavior suggests that in reservoirs fluids flow primarily in fractures rather than in pores. Fluid-filled fractures are capable to carry two types of dispersive slow waves: Biot wave and Stoneley guided wave, which is not described by Biot's theory. Results of numerical modeling suggest that Stoneley guided wave has overwhelmingly large amplitude compared to all other waves excited by a source in a fracture. It is likely that Stoneley guided wave is a key phenomenon which might explain observed frequency-dependence and nonlinear behavior of fluid reservoirs.

UR - http://www.scopus.com/inward/record.url?scp=84887369689&partnerID=8YFLogxK

M3 - Conference contribution

AN - SCOPUS:84887369689

T3 - Poromechanics IV - 4th Biot Conference on Poromechanics

SP - 706

EP - 711

BT - Poromechanics IV - 4th Biot Conference on Poromechanics

A2 - Ling, Hoe I.

A2 - Smyth, Andrew

A2 - Betti, Raimondo

PB - DEStech Publications Inc

Y2 - 8 June 2009 through 10 June 2009

ER -

ID: 73411770