review of hydraulic stimulation technology
play

Review of Hydraulic Stimulation Technology R. Jung, F. Rummel - PowerPoint PPT Presentation

Review of Hydraulic Stimulation Technology R. Jung, F. Rummel ENGINE Workshop 3 Ittingen 29./30.06.2006 Mechanical properties of fractures 2 a pressure volume Mechanical properties of fractures 2 a 2a dw/dp dV/dp [m] [mm/bar]


  1. Review of Hydraulic Stimulation Technology R. Jung, F. Rummel ENGINE Workshop 3 Ittingen 29./30.06.2006

  2. Mechanical properties of fractures 2 a pressure volume

  3. Mechanical properties of fractures 2 a 2a dw/dp dV/dp [m] [mm/bar] [m³/bar] 1 0.003 3 · 10 -6 10 0.03 0.003 100 0.3 3 1000 3 3000 in contact 0.001-0.01 E = 50 GPa

  4. Mechanical properties of fractures 2 a 2 a + 2 ∆ a pressure volume

  5. Fracture propagation 2 a 2 a + 2 ∆ a Griffith (1921) ∆ W pressure ∆ W ≥ 2 ∆ a· γ γ : surface energy volume γ = 10 – 100 J/m²

  6. Fracture propagation 2 a σ θ ∝ K I / √ r r K I = p · √ π a Irvin (1958) K IC : fracture toughness K I = K IC K IC = 1 MPa·m 1/2

  7. fluid flow in fractures w q = (w 3 /12)/µ·dp/dx = T/µ·dp/dx T : fracture transmissibility µ : viscosity

  8. fluid flow in fractures w q = (w 3 /12)/µ·dp/dx = T/µ·dp/dx w T T [mm] [m³] [D·m] 10 -16 10 -4 0.01 0.1 10 -13 0,1 10 -10 1 100 10 -7 10 5 10 Porous aquifer 10 -11 10

  9. fluid flow in fractures w dp/dx = q·µ/T w q dp/dx [mm] [l/(s · m)] [bar/m] 10 5 0.01 1 0.1 1 100 1 1 0.1 10 -4 10 1

  10. fluid flow in fractures 2 a High gradients at the fracture tip

  11. Hydrodynamic fracture models x << x >> h h f f f f Khristianovich, Zheltov, Geertsma, de Klerk (KGD) Perkins, Kern, and Nordgren (PKN) Model Geometry Model Geometry

  12. Hydrodynamic fracture models KGD fracture model (1955, 1969) 1 / 4   ⋅ µ ⋅ − ν ⋅ 2 q ( 1 ) x π   i f = ⋅   w 2 , 27   ⋅ G h  4      f x << h E f f = G = elastic shear modulus, Pa G ⋅ + ν 2 ( 1 ) q i = injection rate, m³/s µ = apparent viscosity, Pa·s E = Young‘s modulus, Pa ν = Poisson’s ratio x f = fracture half length, m h f = Fracture height, m

  13. Hydrodynamic fracture models PKN fracture model 1 / 4 ⋅ µ ⋅ − ν ⋅   q ( 1 ) x π   = ⋅ i f ⋅ γ   w 2 , 31   G 4     x >> h f f E = G G = elastic shear modulus, ⋅ + ν 2 ( 1 ) q i = injection rate µ = apparent viscosity q i = injection rate, bpm (10 7 - 2x10 5 psi) E = Young‘s modulus µ = apparent viscosity, cp ν = Poisson’s ratio (0,15 - 0,4) G = elastic shear modulus, psi x f = fracture half length x f = fracture half length, ft γ = geometry factor app. 0,75

  14. Hydrodynamic fracture models Comparision with static fracture models 2a Griffith KDG [m] w c , [mm] w c , [mm] 1 0.025 0.4 10 0.075 1.2 100 0.25 4 1000 0.75 12 q = 1 l/(s·m) water

  15. Fluid losses C L = fluid loss coefficient A = element of fracture area t = time measured from pump start τ = time measured from creation of A ⋅ ⋅ 2 C A = q L L − τ t

  16. Fluid losses V olume injected = created fracture volume + fluid leak off q i = injection rate = + t i = injection time V V V i f L A f = fracture area w = average fracture width ⋅ = ⋅ + ⋅ ⋅ ⋅ ⋅ ⋅ q t A w K C ( 2 A ) r t i i f L L f p i C L = leakoff coefficient r p = ratio of net to fracture height 1  8  ⋅ η + π ⋅ − η (Nolte) ( 1 ) K L =   2  3  V f η = fluid efficiency = V i V pad = pad volume not carrying proppants

  17. post frac tests T D = T/k·x f x f Q = 0.1 l/(s·m) T T D = 0.1 k,s

  18. post frac tests Test 08h 30000000 25000000 20000000 Pa 15000000 10000000 5000000 0 1 10 100 1000 10000 100000 s T D = 0.1

  19. post frac tests T D = T/k·x f x f Q = 0.1 l/(s·m) T T D = 1 k,s

  20. post frac tests Test 08c 16000000 14000000 12000000 10000000 Pa 8000000 6000000 4000000 2000000 0 0,00 2,00 4,00 6,00 8,00 10,00 12,00 14,00 16,00 18,00 s^(1/4) T D = 1

  21. post frac tests T D = T/k·x f x f Q = 0.1 l/(s·m) T T D = 10 k,s

  22. post frac tests Test 08 g 12000000 10000000 8000000 Pa 6000000 4000000 2000000 0 0,00 2,00 4,00 6,00 8,00 10,00 12,00 14,00 16,00 18,00 s^(1/4) T D = 10

Download Presentation
Download Policy: The content available on the website is offered to you 'AS IS' for your personal information and use only. It cannot be commercialized, licensed, or distributed on other websites without prior consent from the author. To download a presentation, simply click this link. If you encounter any difficulties during the download process, it's possible that the publisher has removed the file from their server.

Recommend


More recommend