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Multiphase Field- Multiphase Field- scale Modeling: Brine scale Modeling: Brine Transport Transport Ann Cook Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Brice Loose Keegan Roberts Keegan Roberts Amber Sallerson Amber Sallerson Katy Schulte Katy Schulte Martina Vlckova Martina Vlckova Thomas Willingham Thomas Willingham

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Page 1: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Multiphase Field-scale Multiphase Field-scale Modeling: Brine TransportModeling: Brine Transport

Ann CookAnn CookPerPer Hatlevik

Jonathan LevineBrice LooseBrice Loose

Keegan Roberts Keegan Roberts Amber Sallerson Amber Sallerson

Katy SchulteKaty SchulteMartina VlckovaMartina Vlckova

Thomas WillinghamThomas Willingham

Page 2: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Introduction to DNAPLs

• Types• Sources• Behavior

PCE, TCE, DCE, VC, CT, CF, DCM,

TCA

gh

an

anc )(

Page 3: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Introduction to DNAPLs

• Long lived • Difficult to remove• Health Hazards

– Liver problems– Increased risk of cancer– Nervous system, or circulatory problems1

Density of Water (rw)

Density of DNAPL (rn)

~1 g/mL ~1.45-1.62 g/mL

Page 4: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Brine Treatment Technology

• How does it work?– Mobilization of the NAPL

• Increase Gravimetric Forces• Decrease Capillary Trapping Forces

Page 5: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

glr an

an )(

Brine Treatment Technology

• sn-a = NAPL-aqueous interfacial tension• r = effective pore size• rn = NAPL density• ra = aqueous phase density• g = gravitational acceleration• l = characteristic length of NAPL

pool in vertical direction

Page 6: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Brine Treatment Technology

• How does it work?– Closed system on 5 sides

Area of Remediation Sheet-piles

Plan ViewImpermeable Layer (e.g., clay)

Profile View

Page 7: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Brine Treatment Technology

• How does it work?

No Flow Boundary

No Flow Boundary

Page 8: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Brine Treatment Technology

• How does it work?

Pump in Pump in Brine LayerBrine Layer

Page 9: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Brine Treatment Technology

• How does it work?

Lower Lower Water TableWater Table

Page 10: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Brine Treatment Technology

• Gravimetric Forces

Removal Removal of of DNAPLDNAPL

Page 11: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Brine Treatment Technology

• How does it work?

Page 12: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Brine Treatment Technology

• How does it work?

Removal Removal of of DNAPLDNAPL

Page 13: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Brine Treatment Technology

• How does it work?

Page 14: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Brine Treatment Technology

• How does it work?

Remove Remove BrineBrine <1% Original

DNAPL Mass

Page 15: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Brine Treatment Technology

• How does it work?

<1% Original = MeetDNAPL Mass Standards

Page 16: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Brine Treatment Technology

• Why is it novel?– $$ Cheaper $$– Higher rates of removal than current

technologies

Pump and Treat Natural Attenuation

Page 17: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Possible Instabilities in the System

• Physical– Density (changes and/or differences)– Excessive Surfactant Concentration bypass– Pore Clogging

• Model– Fingering – Gravity - Rayleigh

Page 18: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Rayleigh-Taylor Instability

• Initial density stratified domain

• Unstable system (small perturbations)

• Occur in model and physical system

Brine

Ground

Water

Page 19: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Rayleigh Number

• Dimensionless Number

• Ratio

dispersiondiffusion

ngravitatiobuoyancy

Ra

Page 20: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Modified Rayleigh Number

T

c

D

HURa

Lamb

Lamb

VD

VPe

0

*

1250*1

*

Pe

RaRa

Page 21: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

SUTRA

• Code written by USGS• Simulates single phase fluid flow and

transport in the subsurface• Uses a combination of finite-element

and finite difference methods to solve a series of equations

Page 22: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Conservation Equations

• Species Balance Equation

• Species-Summed Flow Equation

Page 23: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

SUTRA Transport

Math Magic

Page 24: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

SUTRA Fluid FlowSpecies Summed

Flow Equation

Darcy’s Law

Math Magic

Page 25: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Requirements for SUTRA

DL < 4aL

Pe < 2

• DL = local distance between sides of an element measured in the direction parallel to local flow

• aL = longitudinal dispersivity

Page 26: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

SUTRA Goal

• To model a freshwater system where we inject brine– 3D model– Relatively small in the y-direction

• Visualize system instabilities

• Removal of brine from system

Page 27: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Simulations Ran

1. Brine slumping model

2. Fully saturated fresh water system with brine injection

3. Unsaturated brine injection

4. Multiple well configurations

Page 28: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Example Problem: Slumping brine interface

which admits an analytic solution in the case that the vertical scale is much less that the horizontal (H << R), and a constant hydraulic conductivity (Kc)

High frequency spatial hydraulic conductivity

Page 29: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Homogenization permits approximation of K(x,z,t) as a constantthat captures the variability

Homogenized equations compare well with the accepted numerical solution. High frequency variations are absent.

Page 30: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Evaluate Instabilities

Extraction Well

Injection Wells

Page 31: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Fingering

waterbrine qq

Fingering due to viscous instability

waterbrine

dl

dhkq

Page 32: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

SUTRA MODELINGBCs

Page 33: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

SUTRA MODELINGInitial Injection

Page 34: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

SUTRA MODELINGBrine Injection

Page 35: Multiphase Field-scale Modeling: Brine Transport Ann Cook Per Per Hatlevik Jonathan Levine Brice Loose Keegan Roberts Amber Sallerson Katy Schulte Martina

Transport and Flow EquationsAKA “The Magic”