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Theorem ofOrthogonal Non-Linear Flow in Porous Media
By QI Chengwei
ABSTRACT: Substituting the Orthogonal Power- QuotientEquation into the continuity equation of incompressible fluid steadily flowingin porous media, to achieve the governing equation of orthogonal non- linearflow in porous media at low velocities. This governing equation is a secondorder non-linear partial differential equation, thus except straight streamlinefields, it’s extremely hard to be solved symbolically. Coordinating fieldtheory with differential geometry, to qualitatively analyze geometriccharacteristics of the flow fields, and gain the‘theorem of orthogonalnon-linear flow in porous media: Supposing that iso-intensity surfaces ofpressure and streamlines of non- linear flow in porous media are orthogonal to eachother, if the flow fields are curved streamline fields, then the streamlines ofcompressible or incompressible single- phase fluid non-linearly flowing inporous media and the streamlines of incompressible single-phase fluid linearlyflowing in porous media are in different shapes under the same condition. Underthe orthogonality hypothesis, the shapes of iso-intensity surfaces of pressureare also different.’Drawing an analogy with Stokes flow, to point out the possibilityof non- orthogonality between iso- intensity surfaces of pressure andstreamlines of the fluid non-linearly flowing in porous media.
Key words: mechanics of fluids in porous media,geometric characteristics of flow fields, Orthogonal Power- Quotient ContinuityEquation, curved streamline field, lemma, StreamlineCurvature Vector Formula, Complex Curvature Formula, Shattering Fracturing
正交非线性渗流定理表明:无限大等厚均质各向同性水平地层内具有无限导流能力且铅垂贯穿地层的有限长无宽直裂缝激发的正交非线性渗流场的流线不是以裂缝端线等高点为焦点的双曲线,等压面也不是以裂缝端线为焦线的椭圆柱面。拟共形?
非线性渗流的等压面与流线是否正交,可通过测试具有非线性渗流特征的等厚均质各向同性水平岩板内二维曲流场的等压面与板缘壁面是否正交来判定。若不正交,谁能极之?不管是否正交,为理论非线性渗流力学奠基仅需一个曲流压强场显函数。
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