Download presentation

Presentation is loading. Please wait.

Published byRachel O'Leary Modified over 3 years ago

1
**Darcy’s law in heterogeneous medium - Introduction Averages**

Susanne Rudolph

2
**Heterogeneity of porous media**

Homogenous: A medium is homogenous with respect to a property if the property is independent of position within the medium. Isotropic: A medium is isotropic with respect to a property if the property is independent of the direction within the medium. Anisotropic: If at one point in the medium a property such as permeability varies with the direction.

3
**Anisotropy Reservoirs are commonly anisotropic with respect to the**

permeability. Anisotropy of permeability is due to evolution of formations; e.g. in carbonate rocks formation of channels within the formation rock due to dissolution of carbonates in water. Sedimentary porous media (e.g. sandstone) have layered structure. Permeability parallel to layers is mostly greater than perpendicular.

4
**Anisotropy Stratified formation are defined as anisotropic**

homogeneous medium when the thickness of the individual layer is smaller than the length of interest. In such cases the permeability cannot be determined from core samples because it would not display the real permeability. So far, only isotropic media have been considered wherein the permeability as constant factor (scalar) in Darcy’s law. Due to anisotropy is the direction of the pressure gradient vector different than the direction of the Darcy velocity vector at a point in the medium.

5
**Anisotropy Assume a porous medium with an arbitrary orientation with**

respect to the coordinate system and the pressure gradient points in the x-direction. Due to anisotropy the flow rates in the different directions are not the same. Darcy’s law for anisotropic media is (Ferrandon 1948):

6
**Anisotropy Herein kij are the elements of the permeability tensor with**

Permeability values depend on the orientation of the medium with respect to the coordinate system: With this, Darcy’s law can be written in vector notation as:

7
Anisotropy If it is assumed that the anisotropic medium is ‘orthotropic’ (they have 3 mutually orthogonal principal axes) and if the coordinate axes are aligned with the principal axes of the medium permeability tensor is diagonal An orthotropic material has two or three mutually orthogonal two-fold axes of rotational symmetry so that its mechanical properties are, in general, different along the directions of each of the axes. Orthotropic materials are thus anisotropic; their properties depend on the direction in which they are measured. An isotropic material, in contrast, has the same properties in every direction. One common example of an orthotropic material with two axes of symmetry would be a polymer reinforced by parallel glass or graphite fibers. The strength and stiffness of such a composite material will usually be greater in a direction parallel to the fibers than in the transverse direction. Another example would be a biological membrane, in which the properties in the plane of the membrane will be different from those in the perpendicular direction. Such materials are sometimes called transverse isotropic.

8
Heterogeneous Media Reservoirs are commonly heterogeneous. A reservoir consists of ‘patches’ with different properties. Often reservoir simulations are performed applying a cylindrical homogeneous structure. Main interest of reservoir engineers is the flow through porous medium and its understanding. Only in recent years heterogeneity is taken into account in order to analyze reservoir behavior. Geological or geostatistical models provide are detailed description of the heterogeneity of the reservoir.

9
Heterogeneous Media Details can often not be incorporated in reservoir simulation models. Permeability values have to be averaged. Averaging procedure has to be conducted with care to avoid erroneous averaged values. Mathematics provides computation of means such as arithmetic, harmonic and geometric mean.

10
Arithmetic mean - Sum of all the values of which the arithmetic mean has to be determined divided by the number of summed values. - For a set of data X = (x1, x2, x3,…,xn) the arithmetic mean is: Note: - If the arithmetic mean is determined of values varying strongly in value/order of magnitude, it might give an erroneous high average value. - Arithmetic mean can only be taken from values with the same reference.

11
Harmonic mean - The number of values divided by the sum of the reciprocal values of the property. For a set of data X = (x1, x2, x3,…, xn) the harmonic mean is: Derived from electrotechnique computing the avarage resistance of a electrical circuit with two resistors in parallel

12
Geometric mean Indicates the central tendency or a typical value of a set of parameters. For a set of data X = (x1, x2, x3,…, xn) the geometric mean is: Can only applied to possitive values. Is smaller or equal to the arithmetic mean of the same data set Is closely related to arithmetic mean

13
**Relation between arithmetic and geometric mean**

For a set of data X = (x1, x2, x3,…,xn) the geometric mean can be written as an arithmetic mean by taking the natural logarithm: For positive values of xi: Hn(x) ≤ Gn(x) ≤ An(x)

14
**Average permeability for heterogeneous media**

After recalling the meaning of the different ways to take mean values, the averaging of the permeability is considered for heterogeneous reservoirs Use of average permeability only for simple flow cases. Rock system composed of distinct layers with different properties. Only flow of a homgeneous fluid (, = constant); therefore use of hydraulic conductivity analogous to use of permeability.

15
**Average permeability for heterogeneous media**

Two situations are considered: Flow is parallel to layers Flow is normal/perpenticular to layers ki: permeability; bi: thickness of layer i; Qi: flow rate through layer I; W: width of the layers; same for all layers μ: viscosity of fluid; assumed to be equal for all systems and constant Φ: fluid potential A: cross-sectional area

16
**Flow parallel to layers 1-D & linear flow**

17
**Flow parallel to layers 1-D & linear flow**

Driving force described by difference of fluid potentials (piezometric head) 1 and 2.

18
**Flow parallel to layers 1-D & linear flow**

Flow rate of each layer expressed by Darcy’s law: Total flow rate Q: sum of the flow rates through each layer: With the cross-sectional area:

19
**Flow parallel to layers 1-D & linear flow**

Transmissitivity: product of the thickness and the permeability over the visocsity This gives then: Combining this result with the same flow rate Q through a porous medium of the thickness b described in terms of the equivalent permeability kparallel or transmittivity Tparallel:

20
**Flow parallel to layers 1-D & linear flow**

Gives:

21
**Flow parallel to layers 1-D & linear flow**

Rewriting the effective or equivalent permeability for the horizontal flow parallel to the layers gives: Which is the arithmetic average of the permeability.

22
**Flow parallel to layers 1-D &radial flow**

hT

23
**Flow parallel to layers 1-D &radial flow**

Driving force described by difference of fluid potentials (piezometric head) 1 and 2. hT

24
**Flow parallel to layers 1-D & radial flow**

Flow rate of each layer expressed by Darcy’s law: Total flow rate Q: sum of the flow rates through each layer:

25
**Flow parallel to layers 1-D & radial flow**

Transmissitivity: product of the thickness and the permeability over the visocsity This gives then: Combining this result with the same flow rate Q through a porous medium of the thickness hT described in terms of the equivalent permeability kparallel or transmittivity Tparallel:

26
**Flow parallel to layers 1-D & radial flow**

Gives:

27
**Flow normal to layers 1D & linear flow**

Datum level

28
**Flow normal to layers 1D & linear flow**

Horizontal flow normal or perpendicular to layers: Total flow rate per unit width is unchanged. The total drop of the head Δ is now the sum of the drop of heads for each layer Δi Datum level Rock Fluid Interactions – Part 1 AES1310

29
**Flow normal to layers 1D & linear flow**

The drop of the piezometric head of each section of the layer is described by Darcy’s law: The total piezometric head is then:

30
**Flow normal to layers 1D & linear flow**

Combining the equation again with the result obtained regarding the porous medium described by an equivalent or effective permeability knormal for the flow with the same flow rate Q through a porous medium of the length L: Gives:

31
**Flow normal to layers 1D & linear flow**

Rewriting the permeability for the horizontal flow normal to the layers gives: Which is the harmonic average of the permeability.

32
**Flow normal to layers 1D & radial flow**

33
**Flow normal to layers 1D & radial flow**

Now we consider the horizontal flow normal or perpendicular to layers occurs. For this case the total flow rate per unit width is unchanged. The total drop of the head Δ is now the sum of the drop of heads for each layer Δi. Horizontal flow is considered, thus change of fluid potential is equal to pressure drop.

34
**Flow normal to layers 1D & radial flow**

The drop of the piezometric head of each section of the layer is described by Darcy’s law: The total piezometric head is then: And the flow rate:

35
**Flow normal to layers 1D & radial flow**

Combining the equation again with the result obtained regarding the porous medium described by an equivalent or effective permeability knormal for the flow with the same flow rate Q through a radial porous medium with an outer radius re and a inner radius rw: Gives:

36
**Averaging of permeability**

From the equations to describe the flow parallel and normal to layers follows that the equivalent permeabilities of parallel flow are larger than of the normal flow: This can be prooved by considering frist two layers and then increasing the number of layers while computing the knormal and kparallel.

37
**Averaging of permeability**

Note: The geometric mean is commonly used for the description of the average permeability in a chessboard reservoir (= area is subdivided in blocks of equal size) Cardwell and Parsons showed for chessboard arrangement that the equivalent permeability lays between the one of parallel flow and the one of normal flow. This is in agreement what we saw before: Hn(x) ≤ Gn(x) ≤ An(x)

38
**Averaging of permeability**

Determine the average permeability of the situation described in the tables for linear flow and radial flow. What are the ratios of the separate flows in these beds? What are the ratios of the separate piezometric heads in these beds? Perpendicular flow Parallel flow Bed Length or radius L or R [ft] Perm [mD] 1 250 25 2 50 3 500 100 4 1000 200 Bed Thickness H [ft] Perm [mD] 1 20 100 2 15 200 3 10 300 4 5 400

Similar presentations

Presentation is loading. Please wait....

OK

Chapter 1 The Study of Body Function Image PowerPoint

Chapter 1 The Study of Body Function Image PowerPoint

© 2017 SlidePlayer.com Inc.

All rights reserved.

Ads by Google

Ppt on duty roster template Ppt on porter's five forces model pdf Free ppt on mind power Ppt on preservation of public property search Ppt on carburetor diagram Ppt on 60 years of indian parliament Ppt on mammals and egg laying animals Ppt on airbags in cars Ppt on social networking security Ppt on metro cash and carry