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Investigating the Fate and
Transport of PPCPs in the
Environment
Ashley Funk
Advisor: Monica Higgins
Environmental Studies
Wellesley College
Funded by Sophomore Early Research Program
Why fate and transport of PPCPs?
Important parameters
Experimental setup and results
Pharmaceuticals and personal care products (PPCPs) are
frequently detected in our rivers and streams
Kolpin, D., E. Furlong, et al. (2002). "Pharmaceuticals, hormones, and other organic wastewater contaminants in US streams,
1999-2000: A national reconnaissance.“
Nonprescription Drugs
Pharmaceuticals and personal care products (PPCPs) are
found in our rivers and streams in low concentrations
Understanding the fate and transport of PPCPs is important to
predicting their impact on ecosystems and human health
Nonprescription drugs
Kolpin, D., E. Furlong, et al. (2002). "Pharmaceuticals, hormones, and other organic wastewater contaminants in US streams,
1999-2000: A national reconnaissance.“
We chose caffeine as an example PPCP because it is
frequently found and is an indicator of other contamination
Currently, predicting PPCP movement in the environment
relies on the soil distribution coefficient, or Kd
start
Caffeine
Currently, predicting PPCP movement in the environment
relies on the soil distribution coefficient, or Kd
Caffeine
equilibrium
EquilibriumSoilConcentration[g/kg]
Equilibrium Aqueous Concentration [g/L]
Kd describes the relationship between the aqueous
concentration and soil concentration at equilibrium
Aqueous concentration
Soil concentration
slope =
soil distribution coefficient, Kd
In the subsurface PPCPs may not behave exactly as they do
in a laboratory flask, in part, because they are moving Drinking
Water
FLOW
Release to
Environment
Movement of substances in groundwater can be described
by the advection-dispersion equation
𝜕𝐶
𝜕𝑡
= 𝜆
𝜕2 𝐶
𝜕𝑥2
− 𝑣 𝑥
𝜕𝐶
𝜕𝑥
AdvectionDispersion
Concentration
Time
Dispersivity Velocity
If we know the velocity of water, we can use
concentration data from a conservative tracer
to determine the dispersivity.
Position
RelativeConcentration
Pore Volume
C/C0 = 1
C/C0 = 0
0 1 2
Influent
Ideal Effluent
In an ideal column, without soil, the entire effluent front
should appear at one pore volume
Dispersion is a function of substances traveling around and
through the soil particles
Faster
Slower
RelativeConcentration
Pore Volume
C/C0 = 1
C/C0 = 0
0 1 2
Ideal Effluent
Nonreactive
Tracer
Faster
Slower
Because of dispersion, the effluent front in the soil column
will center on one pore volume but have an “s” shape
RelativeConcentration
Pore Volume
C/C0 = 1
C/C0 = 0
0 1 2
Nonreactive
Tracer
Reactive
Chemical
The reactive chemical will have an “s” shaped front but will
be delays because of interactions with the soil particles
A reactive substance may move through the column more
slowly than the non-reactive tracer.
𝑅
𝜕𝐶
𝜕𝑡
= 𝜆
𝜕2 𝐶
𝜕𝑥2
− 𝑣 𝑥
𝜕𝐶
𝜕𝑥
Retardation Factor
When we know the velocity and the dispersivity of
the column, we can use concentration data from our
PPCP to determine the retardation factor.
In the prediction of fate and transport, it is assumed that
retardation factor is related to Kd
𝑅 = 1 +
𝜌 𝑏
𝜃
𝐾 𝑑
To answer this question we need to be able to measure or
calculate the velocity, dispersivity, and retardation factor.
Will the observations in flow-
through systems … … match what could be
predicted from the
observations in batch
system?
To simplify the environment, we used a one-dimensional
column system to measure caffeine movement Drinking
Water
FLOW
Release to
Environment
To simplify the environment, we used a one-dimensional
column system to measure caffeine movement
FLOW
To simplify the environment, we used a one-dimensional
column system to measure caffeine movement
Pump
Column
Effluent
Influent
We need to be able to measure or calculate the
velocity, dispersivity, and retardation factor.
We estimated the velocity by measuring volume of effluent
per unit time and dividing by the column area
Pump
Column
Effluent
Influent
Ultrapure
Water
flowrate ~ 5 mL/hr
velocity = 23 cm/day
We introduce artificial groundwater and measure the
chloride concentration as a conservative tracer
Pump
Column
Effluent
Influent
Artificial
Groundwater
We estimated the dispersivity by fitting experimental results
of chloride ion to the advection dispersion equation.
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
0.0 0.5 1.0 1.5 2.0 2.5 3.0 3.5 4.0 4.5
RelativeConcentration
Pore Volume
Chloride
We estimated the dispersivity by fitting experimental results
of chloride ion to the advection dispersion equation
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
0.0 0.5 1.0 1.5 2.0 2.5 3.0 3.5 4.0 4.5
RelativeConcentration
Pore Volume
Chloride ADE Prediction
 = 0.299 cm
R2 = 0.76
We spike the artificial groundwater and with caffeine to find
the retardation factor
Pump
Column
Effluent
Influent
Caffeine +
Artificial
Groundwater
Knowing the velocity and the dispersivity, we can determine
the retardation factor of caffeine in sand columns
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 8.0
RelativeConcentration
Pore Volume
Caffeine
Knowing the velocity and the dispersivity, we can determine
the retardation factor of caffeine in sand columns
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 8.0
RelativeConcentration
Pore Volume
Caffeine R = 1.0
R2 = 0.87
Knowing the velocity and the dispersivity, we can determine
the retardation factor of caffeine in sand columns
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 8.0
RelativeConcentration
Pore Volume
Caffeine R = 1.0 R = 1.5
R2 = 0.87
Knowing the velocity and the dispersivity, we can determine
the retardation factor of caffeine in sand columns
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 8.0
RelativeConcentration
Pore Volume
Caffeine R = 1.0 R = 2.0
R2 = 0.49
𝑅 = 1 +
𝜌 𝑏
𝜃
𝐾 𝑑
Future work will vary experimental conditions to replicate
expected environmental conditions
Solution Properties:
pH
Ionic strength
Soil Properties:
Organic carbon
Minerals
PPCP Properties:
Size
Charge
Caffeine
Understanding the fate and transport of
PPCPs is important to assess their impact on
ecosystems and human health
The soil distribution coefficient and
the retardation factor are important
parameters that will be dependent
on environmental conditions.
We were able to estimate
the retardation factor of
caffeine in sand columns.
Final_RuhlmanPresentation No Notes

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Final_RuhlmanPresentation No Notes

  • 1. Investigating the Fate and Transport of PPCPs in the Environment Ashley Funk Advisor: Monica Higgins Environmental Studies Wellesley College Funded by Sophomore Early Research Program
  • 2. Why fate and transport of PPCPs? Important parameters Experimental setup and results
  • 3. Pharmaceuticals and personal care products (PPCPs) are frequently detected in our rivers and streams Kolpin, D., E. Furlong, et al. (2002). "Pharmaceuticals, hormones, and other organic wastewater contaminants in US streams, 1999-2000: A national reconnaissance.“ Nonprescription Drugs
  • 4. Pharmaceuticals and personal care products (PPCPs) are found in our rivers and streams in low concentrations Understanding the fate and transport of PPCPs is important to predicting their impact on ecosystems and human health Nonprescription drugs Kolpin, D., E. Furlong, et al. (2002). "Pharmaceuticals, hormones, and other organic wastewater contaminants in US streams, 1999-2000: A national reconnaissance.“
  • 5. We chose caffeine as an example PPCP because it is frequently found and is an indicator of other contamination
  • 6. Currently, predicting PPCP movement in the environment relies on the soil distribution coefficient, or Kd start Caffeine
  • 7. Currently, predicting PPCP movement in the environment relies on the soil distribution coefficient, or Kd Caffeine equilibrium
  • 8. EquilibriumSoilConcentration[g/kg] Equilibrium Aqueous Concentration [g/L] Kd describes the relationship between the aqueous concentration and soil concentration at equilibrium Aqueous concentration Soil concentration slope = soil distribution coefficient, Kd
  • 9. In the subsurface PPCPs may not behave exactly as they do in a laboratory flask, in part, because they are moving Drinking Water FLOW Release to Environment
  • 10. Movement of substances in groundwater can be described by the advection-dispersion equation 𝜕𝐶 𝜕𝑡 = 𝜆 𝜕2 𝐶 𝜕𝑥2 − 𝑣 𝑥 𝜕𝐶 𝜕𝑥 AdvectionDispersion Concentration Time Dispersivity Velocity If we know the velocity of water, we can use concentration data from a conservative tracer to determine the dispersivity. Position
  • 11. RelativeConcentration Pore Volume C/C0 = 1 C/C0 = 0 0 1 2 Influent Ideal Effluent In an ideal column, without soil, the entire effluent front should appear at one pore volume
  • 12. Dispersion is a function of substances traveling around and through the soil particles Faster Slower
  • 13. RelativeConcentration Pore Volume C/C0 = 1 C/C0 = 0 0 1 2 Ideal Effluent Nonreactive Tracer Faster Slower Because of dispersion, the effluent front in the soil column will center on one pore volume but have an “s” shape
  • 14. RelativeConcentration Pore Volume C/C0 = 1 C/C0 = 0 0 1 2 Nonreactive Tracer Reactive Chemical The reactive chemical will have an “s” shaped front but will be delays because of interactions with the soil particles
  • 15. A reactive substance may move through the column more slowly than the non-reactive tracer. 𝑅 𝜕𝐶 𝜕𝑡 = 𝜆 𝜕2 𝐶 𝜕𝑥2 − 𝑣 𝑥 𝜕𝐶 𝜕𝑥 Retardation Factor When we know the velocity and the dispersivity of the column, we can use concentration data from our PPCP to determine the retardation factor.
  • 16. In the prediction of fate and transport, it is assumed that retardation factor is related to Kd 𝑅 = 1 + 𝜌 𝑏 𝜃 𝐾 𝑑 To answer this question we need to be able to measure or calculate the velocity, dispersivity, and retardation factor. Will the observations in flow- through systems … … match what could be predicted from the observations in batch system?
  • 17. To simplify the environment, we used a one-dimensional column system to measure caffeine movement Drinking Water FLOW Release to Environment
  • 18. To simplify the environment, we used a one-dimensional column system to measure caffeine movement FLOW
  • 19. To simplify the environment, we used a one-dimensional column system to measure caffeine movement Pump Column Effluent Influent We need to be able to measure or calculate the velocity, dispersivity, and retardation factor.
  • 20. We estimated the velocity by measuring volume of effluent per unit time and dividing by the column area Pump Column Effluent Influent Ultrapure Water flowrate ~ 5 mL/hr velocity = 23 cm/day
  • 21. We introduce artificial groundwater and measure the chloride concentration as a conservative tracer Pump Column Effluent Influent Artificial Groundwater
  • 22. We estimated the dispersivity by fitting experimental results of chloride ion to the advection dispersion equation. 0.0 0.2 0.4 0.6 0.8 1.0 1.2 1.4 0.0 0.5 1.0 1.5 2.0 2.5 3.0 3.5 4.0 4.5 RelativeConcentration Pore Volume Chloride
  • 23. We estimated the dispersivity by fitting experimental results of chloride ion to the advection dispersion equation 0.0 0.2 0.4 0.6 0.8 1.0 1.2 1.4 0.0 0.5 1.0 1.5 2.0 2.5 3.0 3.5 4.0 4.5 RelativeConcentration Pore Volume Chloride ADE Prediction  = 0.299 cm R2 = 0.76
  • 24. We spike the artificial groundwater and with caffeine to find the retardation factor Pump Column Effluent Influent Caffeine + Artificial Groundwater
  • 25. Knowing the velocity and the dispersivity, we can determine the retardation factor of caffeine in sand columns 0.0 0.2 0.4 0.6 0.8 1.0 1.2 1.4 0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 8.0 RelativeConcentration Pore Volume Caffeine
  • 26. Knowing the velocity and the dispersivity, we can determine the retardation factor of caffeine in sand columns 0.0 0.2 0.4 0.6 0.8 1.0 1.2 1.4 0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 8.0 RelativeConcentration Pore Volume Caffeine R = 1.0 R2 = 0.87
  • 27. Knowing the velocity and the dispersivity, we can determine the retardation factor of caffeine in sand columns 0.0 0.2 0.4 0.6 0.8 1.0 1.2 1.4 0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 8.0 RelativeConcentration Pore Volume Caffeine R = 1.0 R = 1.5 R2 = 0.87
  • 28. Knowing the velocity and the dispersivity, we can determine the retardation factor of caffeine in sand columns 0.0 0.2 0.4 0.6 0.8 1.0 1.2 1.4 0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 8.0 RelativeConcentration Pore Volume Caffeine R = 1.0 R = 2.0 R2 = 0.49 𝑅 = 1 + 𝜌 𝑏 𝜃 𝐾 𝑑
  • 29. Future work will vary experimental conditions to replicate expected environmental conditions Solution Properties: pH Ionic strength Soil Properties: Organic carbon Minerals PPCP Properties: Size Charge Caffeine
  • 30. Understanding the fate and transport of PPCPs is important to assess their impact on ecosystems and human health The soil distribution coefficient and the retardation factor are important parameters that will be dependent on environmental conditions. We were able to estimate the retardation factor of caffeine in sand columns.