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A New Approach to Hydraulic Flow
Unit Determination and its Application
in Prediction of Petrophysical
Properties of Hydrocarbon Reservoirs
By:
Mohammad Izadi
Supervisor: Dr Ali Ghalambor
Contents:
1) Quick Review
2) Experimental Work
3) Future Work
Quick Review:
- Reservoir Characterization
- Rock Typing
- Hydraulic Flow Unit
Quick Review (Cont.):
- Mathematical models:
1 1
(1 ) (1 ). gr
w s V
k
S F S
φ
φ φτ
× = ×
− −
3
2
2 2 2
1
(1 )
(1 )gr
w
s V
k S
F S
φ
τ φ
= × × −
−
Porosity-permeability relationship:
Approach 1:
Approach 2:
(1 )1
(1 ). gr
w
s V
Sk
F S
φ
φ φτ
−
= ×
−
Experimental Work:
Routine and Special
Core Analysis
Berea Sandstone
- exposures near Berea, Cuyahoga County, Ohio
-Traditionally, Mississippian age but recently, Late Devonian age.
-The Berea formed when sand was carried by streams into the
Ohio sea from the Canadian Shield to the north and from the
Catskill Delta to the east.
-Small grain and composed of quartz sand
held together by silica.
Wampakoneta Courthouse, www.ohiohistorycentral.org
1) Selection of Sandstone
Blocks in the lab
2) Cutting plugs
with 1 inch x 1 inch
3) Drying 4) Weighting and labeling
Experimental Work (Cont.):
5) Measuring porosity
Boyles Law: 1 1 2 2PV PV=
Porosity Distribution
0.00
5.00
10.00
15.00
20.00
25.00
30.00
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17
Samples
Porosity,%
6) Measuring permeability (liquid)
14700 QL
k
A P
µ
=
∆
Permeability Distribution
0
50
100
150
200
250
300
350
400
450
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17
Samples
Permeability,md
7) Measuring capillary pressure
2 cos
c non wetting wettingP P P
r
σ θ
−= − =
Capillary Pressure Distribution
0
5
10
15
20
25
0 10 20 30 40 50 60 70 80 90 100
Sw, %
Pc,psi
8) XRD Test
Core Laboratories. Inc
Samples are divided into:
- No lamination,
-Two layers lamination,
- Shale
Samples Quartz, % Clay, % Others, %
sample 1 86.00 8.00 6.00
sample 2 87.00 8.00 5.00
sample 3 41.00 37.00 22.00
sample 4 97.00 3.00 0.00
sample 5 96.00 3.00 1.00
sample 6 95.00 4.00 1.00
sample 7 59.00 6.00
35
(calcit
e)
Future Work
1) Interpreting experimental data
2) Comparison of the two models
3) Field data evaluation
Thank you!
Questions??????

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Overview of Experimental works conducted in this work

  • 1. A New Approach to Hydraulic Flow Unit Determination and its Application in Prediction of Petrophysical Properties of Hydrocarbon Reservoirs By: Mohammad Izadi Supervisor: Dr Ali Ghalambor
  • 2. Contents: 1) Quick Review 2) Experimental Work 3) Future Work
  • 3. Quick Review: - Reservoir Characterization - Rock Typing - Hydraulic Flow Unit
  • 4. Quick Review (Cont.): - Mathematical models: 1 1 (1 ) (1 ). gr w s V k S F S φ φ φτ × = × − − 3 2 2 2 2 1 (1 ) (1 )gr w s V k S F S φ τ φ = × × − − Porosity-permeability relationship: Approach 1: Approach 2: (1 )1 (1 ). gr w s V Sk F S φ φ φτ − = × −
  • 5. Experimental Work: Routine and Special Core Analysis Berea Sandstone - exposures near Berea, Cuyahoga County, Ohio -Traditionally, Mississippian age but recently, Late Devonian age. -The Berea formed when sand was carried by streams into the Ohio sea from the Canadian Shield to the north and from the Catskill Delta to the east. -Small grain and composed of quartz sand held together by silica. Wampakoneta Courthouse, www.ohiohistorycentral.org
  • 6. 1) Selection of Sandstone Blocks in the lab 2) Cutting plugs with 1 inch x 1 inch 3) Drying 4) Weighting and labeling Experimental Work (Cont.):
  • 7. 5) Measuring porosity Boyles Law: 1 1 2 2PV PV= Porosity Distribution 0.00 5.00 10.00 15.00 20.00 25.00 30.00 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 Samples Porosity,%
  • 8. 6) Measuring permeability (liquid) 14700 QL k A P µ = ∆ Permeability Distribution 0 50 100 150 200 250 300 350 400 450 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 Samples Permeability,md
  • 9. 7) Measuring capillary pressure 2 cos c non wetting wettingP P P r σ θ −= − = Capillary Pressure Distribution 0 5 10 15 20 25 0 10 20 30 40 50 60 70 80 90 100 Sw, % Pc,psi
  • 10. 8) XRD Test Core Laboratories. Inc Samples are divided into: - No lamination, -Two layers lamination, - Shale Samples Quartz, % Clay, % Others, % sample 1 86.00 8.00 6.00 sample 2 87.00 8.00 5.00 sample 3 41.00 37.00 22.00 sample 4 97.00 3.00 0.00 sample 5 96.00 3.00 1.00 sample 6 95.00 4.00 1.00 sample 7 59.00 6.00 35 (calcit e)
  • 11. Future Work 1) Interpreting experimental data 2) Comparison of the two models 3) Field data evaluation

Notes de l'éditeur

  1. Definition of Res. Charac. Rock Typing. Hydraulic Flow Unit