DAMN 发表于 2025-3-23 13:22:38
Analysis of Formation Water Sampled from Core,ity logs, and its variation within a field indicates extent of reservoir or zone connectivity in aquifer beneath a field. Water is not always produced, or is not produced long enough to ensure absence of contamination with drilling mud filtrate. Use of tritium tracer in mud allows correction for conReclaim 发表于 2025-3-23 16:27:59
Establishment of a Geological Fracture Model for Dual Porosity Simulations on the Ekofisk Field,and both lithological and fracture data were assembled. Fracture density distribution in the reservoir was mapped on the basis of estimated tectonic matrix block dimensions in the cored walls. Observed relationships between fracture density, lithology and structural positions formed the basis for stanalogous 发表于 2025-3-23 18:40:10
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http://reply.papertrans.cn/67/6682/668168/668168_16.pngPAEAN 发表于 2025-3-24 12:43:06
G. Nerbyor fields. Linearization at this point yields a bilinear system in ℝ.; hence the linearized system is a special case of the general model considered in the preceding chapter. However, here we use an additional structure: The systems group is a Lie group and the usual Lie algebra rank condition for l琐碎 发表于 2025-3-24 18:52:55
http://reply.papertrans.cn/67/6682/668168/668168_18.png占线 发表于 2025-3-24 19:47:38
L. Sundal,C. A. Kossack,J. Kleppelization of time-invariant linear differential equations; roughly, they may be viewed as linear differential equations, where the coefficients are determined by a dynamical system on a metric base space .. Section 5.1 describes some examples for these systems (in particular, linearized control systeglisten 发表于 2025-3-25 00:05:19
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