MIGRATEv10 Example 10: Contaminant Transport in Fractured Media with Sorption

Contaminant transport through fractured till and clay liner showing sorption and plume migration into aquifer
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Introduction

MIGRATEv10 Example 10 introduces a more advanced and realistic scenario by incorporating:

  • Fractured media flow
  • Sorption of contaminants

This example builds on earlier cases by modeling contaminant migration through a landfill barrier system that includes both compacted clay and a fractured till layer, while accounting for retardation due to sorption.

It also serves as the 2-D extension of a similar case presented in POLLUTEv6 (Example 6), providing greater spatial detail and realism.


Conceptual Model Overview

The modeled system consists of:

  • A landfill source
  • A 1 m compacted clay liner
  • A 3 m fractured till layer
  • An underlying 1 m aquifer

Key Modeling Objective

This example aims to:

  • Simulate contaminant transport through fractured porous media
  • Evaluate the effect of sorption on contaminant migration
  • Demonstrate how fracture flow influences plume behavior

Barrier System Description

1. Compacted Clay Layer

PropertyValue
Thickness1 m
FunctionPrimary barrier
Sorption (Kd)1.5 mL/g

2. Fractured Till Layer

PropertyValue
Thickness3 m
FunctionSecondary transport layer
Sorption (Kd)1.5 mL/g

👉 The fractured structure allows faster transport pathways, while sorption slows contaminant movement.


Source Characteristics

ParameterValue
Waste Thickness6.25 m
Density600 kg/m³
Contaminant Fraction0.2%
Peak Concentration1000 mg/L
Landfill Width200 m

The contaminant is assumed to reach peak concentration early and then migrate downward.


Flow and Leachate Generation

Leachate Collection Rate

Qc = qo – va = 0.3 – 0.02 = 0.28 m/a

Where:

  • ( qo ) = infiltration through cover = 0.3 m/a
  • ( va ) = downward Darcy velocity = 0.02 m/a

Aquifer Properties

ParameterValue
Thickness1 m
Porosity0.35
Inflow Velocity4 m/a

Base Outflow Velocity

vb = 4 + (200 \times 0.02) = 8 0 m/a

This reflects the combined effect of:

  • Natural groundwater flow
  • Additional inflow from the landfill

Modeling Approach in MIGRATEv10

Step 1: Define Layered System

  • Clay liner (1 m)
  • Fractured till (3 m)
  • Aquifer (1 m)

Step 2: Assign Sorption Properties

  • Set distribution coefficient (Kd = 1.5 mL/g) for both layers

Step 3: Define Source Conditions

  • Peak concentration: 1000 mg/L
  • Finite mass source

Step 4: Apply Flow Conditions

  • Darcy velocity through deposit
  • Infiltration rate
  • Base outflow velocity

Step 5: Run Simulation

  • Evaluate plume migration
  • Analyze concentration profiles

Graphical Output: Concentration vs Distance

PDF Report

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Interpretation of Results

1. Effect of Fractured Media

  • Fractures provide preferential pathways
  • Faster contaminant movement compared to homogeneous media

2. Role of Sorption

  • Sorption slows contaminant migration
  • Reduces peak concentrations
  • Increases travel time

3. Combined Effect

  • Fractures accelerate transport
  • Sorption retards transport

👉 The resulting plume reflects a balance between these competing processes


4. Aquifer Impact

  • Increased base velocity enhances dilution
  • Contaminant concentrations depend on:
    • Flow rate
    • Sorption
    • Fracture connectivity

Key Insights

  • Fractured media significantly alters contaminant pathways
  • Sorption is critical for predicting realistic transport rates
  • Ignoring either process can lead to misleading results
  • MIGRATEv10 can simulate complex coupled processes effectively

Key Takeaways

  • Fractures increase transport speed
  • Sorption decreases contaminant mobility
  • Combined processes produce realistic plume behavior
  • Accurate modeling requires:
    • Proper parameter selection
    • Understanding of subsurface conditions

Final Thoughts

MIGRATEv10 Example 10 demonstrates how real-world complexity can be incorporated into contaminant transport modeling. By including both fractured flow and sorption, this example provides a more accurate representation of subsurface conditions commonly encountered in landfill environments.

This example is especially relevant for:

  • Fractured tills and bedrock systems
  • Long-term contaminant migration studies
  • Environmental risk assessments

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