Geophysical Monitoring for Geologic Carbon Storage. Группа авторов. Читать онлайн. Newlib. NEWLIB.NET

Автор: Группа авторов
Издательство: John Wiley & Sons Limited
Серия:
Жанр произведения: География
Год издания: 0
isbn: 9781119156840
Скачать книгу
of compressional waves in fluid‐filled porous rocks with partial gas saturation (White Model): Part II, Results. Geophysics, 44, 1806–1812.

      8 Gassmann, F. (1951). Über die elastizität poröser medien. Vierteljahrsschrift der Naturforschenden Gesellschaft in Zürich, 96, 1–23. English translation is available from http://sepwww.stanford.edu/sep/berryman/PS/gassmann.pdf (Date last viewed 09/23/2021).

      9 Gurevich, B., Zyrianov, V. B., & Lopatnikov, S. L. (1997). Seismic attenuation in finely layered porous rocks: Effects of fluid flow and scattering. Geophysics, 62(1), 319–324.

      10 Head, K. H. (1982). Manual of soil laboratory testing, Vol. 2. Pentech Press.

      11 Ketcham, R. A., Slottke, D. T., & Sharp, J. (2010). Three‐dimensional measurement of fractures in heterogeneous materials using high‐resolution X‐ray computed tomography. Geosphere, 6(5), 499–514. https://doi.org/10.1130/GES00552.1

      12 Kolsky, H. (1949). An investigation of the mechanical properties of materials at very high rates of loading. Proceedings of the Physical Society of London B, 62, 676–700.

      13 Mavko, G., Mukerji, T., & Dvorkin, J. (1998). The rock physics handbook. Cambridge University Press.

      14 McCool, B., & Tripp, C. P. (2005). Inaccessible hydroxyl groups on silica are accessible in supercritical CO2. Journal of Physical Chemistry B, 109 (18), 8914–8919.

      15 Nakagawa, S. (2011). Split Hopkinson resonant bar test for sonic‐frequency acoustic velocity and attenuation measurements of small, isotropic geological samples. Review of Scientific Instruments, 82, 044901. https://doi.org/10.1063/1.3579501

      16 Nakagawa, S., & Schoenberg, M. A. (2007). Poroelastic modeling of seismic boundary conditions across a fracture. Journal of the Acoustical Society of America, 122(2), 831–847.

      17 Nakagawa, S., Kneafsey, T. J., Daley, T. M., Freifeld, B. M., & Rees, E. V. (2013). Laboratory seismic monitoring of supercritical CO2 flooding in sandstone cores using the Split Hopkinson Resonant Bar technique with concurrent X‐ray computed tomography imaging. Geophysical Prospecting, 61(2), 254–269. https://doi.org/10.1111/1365‐2478.12027

      18 Norris, A. N. (1993). Low‐frequency dispersion and attenuation in partially saturated rocks. Journal of the Acoustical Society of America, 94, 359–370.

      19 Pride, S. R. (2003). Relationships between seismic and hydrological properties. In Y. Rubin & S. Hubbard (Eds.), Hydrogeophysics (pp. 1–31). New York: Kluwer.

      20 Seol, Y., & Kneafsey, T. J. (2011). Methane hydrate induced permeability modification for multiphase flow in unsaturated porous media. Journal of Geophysical Research, 116(B8), B08102. https://doi.org/10.1029/2010JB008040

      21 Shi, J.‐Q., Xue, Z., & Durucan, S. (2007). Seismic monitoring of supercritical CO2 injection into a water‐saturated sandstone: Interpretation of P‐wave velocity data. International Journal of Greenhouse Gas Control, 1, 473–480. https://doi.org/10.1016/S1750‐5836(07)00013‐8

      22 Siggins, A. F. (2006). Velocity‐effective stress response of CO2‐saturated sandstones. Exploration Geophysics, 37, 60–66.

      23 Tittmann, B. R. (1977). Internal friction measurements and their implications in seismic Q structure models of the crust. In J. G. Heacock (Ed.), The Earth's crust (pp. 197–213). AGU Monograph, 20. Washington, D.C.: American Geophysical Union.

      24 Wang, Z., & Nur, A. (1989). Effects of CO2 flooding on wave velocities in rocks with hydrocarbons. SPE Reservoir Engineering, 4, 429–439.

      25 White, J. E., Mikhaylova, N. G., & Lyakhovistsky, F. M. (1975). Low‐frequency seismic waves in fluid‐saturated layered rocks. Izvestija Academy of Sciences, USSR. Physics of the Solid Earth, 11, 654–659.

      26 Xue, Z., Ohsumi, T., & Koide, H. (2005). An experimental study on seismic monitoring of a CO2 flooding in two sandstones. Energy, 30, 2352–2359. https://doi.org/10.1016/j.energy.2004.07.022

      Конец ознакомительного фрагмента.

      Текст предоставлен ООО «ЛитРес».

      Прочитайте эту книгу целиком, купив полную легальную версию на ЛитРес.

      Безопасно оплатить книгу можно банковской картой Visa, MasterCard, Maestro, со счета мобильного телефона, с платежного терминала, в салоне МТС или Связной, через PayPal, WebMoney, Яндекс.Деньги, QIWI Кошелек, бонусными картами или другим удобным Вам способом.

/9j/4AAQSkZJRgABAQEBLAEsAAD/7SHYUGhvdG9zaG9wIDMuMAA4QklNBAQAAAAAAAccAgAAAgAA ADhCSU0EJQAAAAAAEOjxXPMvwRihontnrcVk1bo4QklNBDoAAAAAAPcAAAAQAAAAAQAAAAAAC3By aW50T3V0cHV0AAAABQAAAABQc3RTYm9vbAEAAAAASW50ZWVudW0AAAAASW50ZQAAAABDbHJtAAAA D3ByaW50U2l4dGVlbkJpdGJvb2wAAAAAC3ByaW50ZXJOYW1lVEVYVAAAAAoAQQBkAG8AYgBlACAA UABEAEYAAAAAAA9wcmludFByb29mU2V0dXBPYmpjAAAADABQAHIAbwBvAGYAIABTAGUAdAB1AHAA AAAAAApwcm9vZlNldHVwAAAAAQAAAABCbHRuZW51bQAAAAxidWlsdGluUHJvb2YAAAAJcHJvb2ZD TVlLADhCSU0EOwAAAAACLQAAABAAAAABAAAAAAAScHJpbnRPdXRwdXRPcHRpb25zAAAAFwAAAABD cHRuYm9vbAAAAAAAQ2xicmJvb2wAAAAAAFJnc01ib29sAAAAAABDcm5DYm9vbAAAAAAAQ250Q2Jv b2wAAAAAAExibHNib29sAAAAAABOZ3R2Ym9vbAAAAAAARW1sRGJvb2wAAAAAAEludHJib29sAAAA AABCY2tnT2JqYwAAAAEAAAAAAABSR0JDAAAAAwAAAABSZCAgZG91YkBv4AAAAAAAAAAAAEdybiBk b3ViQG/gAAAAAAAAAAAAQmwgIGRvdWJAb+AAAAAAAAAAAABCcmRUVW50RiNSbHQAAAAAAAAAAAAA AABCbGQgVW50RiNSbHQAAAAAAAAAAAAAAABSc2x0VW50RiNQeGxAcsAAAAAAAAAAAAp2ZWN0b3JE YXRhYm9vbAEAAAAAUGdQc2VudW0AAAAAUGdQcwAAAABQZ1BDAAAAAExlZnRVbnRGI1JsdAAAAAAA AAAAAAAAAFRvcCBVbnRGI1JsdAAAAAAAAAAAAAAAAFNjbCBVbnRGI1ByY0BZAAAAAAAAAAAAEGNy b3BXaGVuUHJpbnRpbmdib29sAAAAAA5jcm9wUmVjdEJvdHRvbWxvbmcAAAAAAAAADGNyb3BSZWN0 TGVmdGxvbmcAAAAAAAAADWNyb3BSZWN0UmlnaHRsb25nAAAAAAAAAAtjcm9wUmVjdFRvcGxvbmcA AAAAADhCSU0D7QAAAAAAEAEsAAAAAQACASwAAAABAAI4QklNBCYAAAAAAA4AAAAAAAAAAAAAP4AA ADhCSU0EDQAAAAAABAAAAFo4QklNBBkAAAAAAAQAAAAeOEJJTQPzAAAAAAAJAAAAAAAAAAABADhC SU0nEAAAAAAACgABAAAAAAAAAAI4QklNA/UAAAAAAEgAL2ZmAAEAbGZmAAYAAAAAAAEAL2ZmAAEA oZmaAAYAAAAAAAEAMgAAAAEAWgAAAAYAAAAAAAEANQAAAAEALQAAAAYAAAAAAAE4QklNA/gAAAAA AHAAAP////////////////////////////8D6AAAAAD/////////////////////////////A+gA AAAA/////////////////////////////wPoAAAAAP////////////////////////////8D6AAA OEJJTQQIAAAAAAAQAAAAAQAAAkAAAAJAAAAAADhCSU0EHgAAAAAABAAAAAA4QklNBBoAAAAAA08A AAAGAAAAAAAAAAAAAA0KAAAKQQAAAA0AOQA3ADgAMQAxADEAOQAxADUANgA4ADMAMwAAAAEAAAAA AAAAAAAAAAAAAAAAAAAAAQAAAAAAAAAAAAAKQQAADQoAAAAAAAAAAAAAAAAAAAAAAQAAAAAAAAAA AAAAAAAAAAAAAAAQAAAAAQAAAAAAAG51bGwAAAACAAAABmJvdW5kc09iamMAAAABAAAAAAAAUmN0 MQAAAAQAAAAAVG9wIGxvbmcAAAAAAAAAAExlZnRsb25nAAAAAAAAAABCdG9tbG9uZwAADQoAAAAA UmdodGxvbmcAAApBAAAABnNsaWNlc1ZsTHMAAAABT2JqYwAAAAEAAAAAAAVzbGljZQAAABIAAAAH c2xpY2VJRGxvbmcAAAAAAAAAB2dyb3VwSURsb25nAAAAAAAAAAZvcmlnaW5lbnVtAAAADEVTbGlj ZU9yaWdpbgAAAA1hdXRvR2VuZXJhdGVkAAAAAFR5cGVlbnVtAAAACkVTbGljZVR5cGUAAAAASW1n IAAAAAZib3VuZHNPYmpjAAAAAQAAAAAAAFJjdDEAAAAEAAAAAFRvcCBsb25nAAAAAAAAAABMZWZ0 bG9uZwAAAAAAAAAAQnRvbWxvbmcAAA0KAAAAAFJnaHRsb25nAAAKQQAAAAN1cmxURVhUAAAAAQAA AAAAAG51bGxURVhUAAAAAQAAAAAAAE1zZ2VURVhUAAAAAQAAAAAABmFsdFRhZ1RFWFQAAAABAAAA AAAOY2VsbFRleHRJc0hUTUxib29sAQAAAAhjZWxsVGV4dFRFWFQAAAABAAAAAAAJaG9yekFsaWdu ZW51bQAAAA9FU2xpY2VIb3J6QWxpZ24AAAAHZGVmYXVsdAAAAAl2ZXJ0QWxpZ25lbnVtAAAAD0VT bGljZVZlcnRBbGlnbgAAAAdkZWZhdWx0AAAAC2JnQ29sb3JUeXBlZW51bQAAABFFU2xpY2VCR0Nv bG9yVHlwZQAAAABOb25lAAAACXRvcE91dHNldGxvbmcAAAAAAAAACmxlZnRPdXRzZXRsb25nAAAA AAAAAAxib3R0b21PdXRzZXRsb25nAAAAAAAAAAtyaWdodE91dHNldGxvbmcAAAAAADhCSU0EKAAA AAAADAAAAAI/8AAAAAAAADhCSU0EFAAAAAAABAAAAAI4QklNBAwAAAAAGNMAAAABAAAAfgAAAKAA AAF8AADtgAAAGLcAGAAB/9j/7QAMQWRvYmVfQ00AAf/uAA5BZG9iZQBkgAAAAAH/2