Table of Contents Table of Contents
Previous Page  48 / 743 Next Page
Information
Show Menu
Previous Page 48 / 743 Next Page
Page Background

Dynamic Data Analysis – v5.12.01 - © KAPPA 1988-2017

Chapte

r 2 – T heory

- p48/743

2.H.4

Conclusions

2.H.4.a

on this series of designs

Beyond the arbitrary split between input and output parameters set in the methodology of

Pressure Transient Analysis, we see that several groups of parameters govern the response of

the well / reservoir system.

Pure wellbore storage: The absolute position of the early time unit slope is only a function

of the wellbore storage C.

Transition from pure wellbore storage to IARF: The shape of the hump, which originally

was set to C

D

e

2.Skin

when dealing with type curves, is actually a function of C and r

w

e

-Skin

,

and is also slightly affected by

and c

t

. The whole curve is translated along the unit slope

as a function of k,

and h, the governing group being kh/

.

IARF: The governing group is kh/

defining the semilog slope, hence the level of the

derivative stabilization when IARF is reached.

There is a residual effect of rw, skin,

and c

t

that defines the constant term of the IARF

straight line. Generally the Skin factor is calculated from this constant term.

At late time the parameters that govern the position of the PSS unit slope are r

e

,

, c

t

and

h. The governing group is

.c

t

.h.r

e

². You may actually prefer the group 2

.r

e

².h.

.c

t

, and

you get V

pore

.c

t

, where V

pore

is the reservoir pore volume. What we arrived at here is

nothing more than material balance.

There is a residual effect of all factors that affected the transient diffusion before PSS was

reached, and which constitute the constant term of the PSS straight line.

2.H.4.b

on the equations

If we consider the IARF equation given in previous section:

 

 

 



 

Skin

rc

k

t

kh

qB

p tp

wt

i

.

8686 .0 228 .3

log

log

6. 162

2

…and if we re-shuffle it a bit, we get:

 

 

  



 

Skin

w

t

er

ch

kh

t

kh

qB

tp

log2 228 .3

log

log

log

6. 162

One can see that the slope is a function of kh/

, and that there is a constant term that shows,

among other things, the residual effect of r

w

e

-Skin

,



and c

t

.

If we consider the PSS equation given previously:

 





 

Skin

rC

A

kh

qB

t

hAc

qB

p tp

wA

t

i

4045 .0

ln

2

1

2. 141

234 .0

2