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On possible fluid detection in equivalent transversely isotropic mediaNormal access

Author: F.P. Adamus
Journal name: Geophysical Prospecting
Issue: Vol 67, No 9, November 2019 pp. 2319 - 2331
DOI: 10.1111/1365-2478.12862
Organisations: Wiley
Language: English
Info: Article, PDF ( 932.27Kb )

Summary:
We consider a transversely isotropic medium that is long-wave equivalent to a stack of thin, parallel, isotropic layers and is obtained using the Backus average. In such media, we analyse the relations among anisotropy parameters; Thomsen parameters, and δ, and a new parameter ϕ. We discuss the last parameter and show its essential properties; it equals 0 in the case of isotropy of equivalent medium and/or constant Lam´e coefficient λ in layers. The second property occurs to make ϕ sensitive to variations of λ in thin-bedded sequences. According to Gassmann, in isotropic media the variation of fluid content affects only the Lam´e coefficient λ, not μ; thus, the sensitivity to changes of λ is an essential property in the context of possible detection of fluids. We show algebraically and numerically that ϕ is more sensitive to these variations than or δ. Nevertheless, each of these parameters is dependent on the changes of μ; to understand this influence, we exhibit comprehensive tables that illustrate the behaviour of anisotropy parameters with respect to specific variations of λ and μ. The changes of μ in layers can be presented by the Thomsen parameter γ that depends on them solely. Hence, knowing the values of elasticity coefficients of equivalent transversely isotropic medium, we may compute ϕ and γ , and based on the aforementioned tables, we predict the expected variation of λ; in this way, we propose a new method of possible fluid detection. Also, we show that the prior approach of possible detection of fluids, proposed by Berryman et al., may be unreliable in specific cases. To establish our results, we use the Monte Carlo method; for the range and chosen variations of Lam´e coefficients λ and μ – relevant to sandstones – we generate these coefficients in thin layers and, after the averaging process, we obtain an equivalent transversely isotropic medium. We repeat that process numerous times to get many equivalent transversely isotropic media, and – for each of them – we compute their anisotropy parameters. We illustrate ϕ, and δ in the form of crossplots that are relevant to the chosen variations of λ and μ. Additionally, we present a table with the computed ranges of anisotropy parameters that correspond to different variations of Lam´e coefficients.

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