Using the High-Resolution Piezocone to Determine Hydraulic Parameters and Mass Flux Distribution
5. Newell Mass Flux - MSECA equation) don’t rely on ... Estimating Mass Flux Using Integral Pump...
Transcript of 5. Newell Mass Flux - MSECA equation) don’t rely on ... Estimating Mass Flux Using Integral Pump...
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Measurement and Use of Mass Flux and Mass Discharge Cleanup 2013 Melbourne, Australia
Charles Newell, Ph.D., P.E., GSI Environmental Inc.
“Mag 7 Plume”
2 Two Views of the World: Concentration versus Mass Discharge
Site A: Very wide source
Very fast groundwater
Site B: Tiny source
Almost stagnant groundwater
But same maximum groundwater
Concentration…
3 Two Views of the World: Concentration versus Mass Discharge
u Concentration-based approach may not account for important site characteristics
But same maximum groundwater
Concentration…
Mega Site
Piss-Ant Site
Mass Flux / Mass Discharge Combine flow, size, concentration
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Mass flux, J Mass per area
per time
Mass discharge, Md
Mass per time ”
Integrate
Definitions
Sir Isaac Newton:
“Method of Fluxions”
“This plume has a mass discharge of 1.5 grams per day.”
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Five Methods for Mass Discharge
u Method 1: Transect Method
u Method 2: Well Capture/Pumping Methods
u Method 3: Passive Flux Meters
u Method 4: Using Existing Data (Isocontours)
u Method 5: Solute Transport Models
Source Strength
Plume Strength
Source
All methods are “ready to go”
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Method 1: Transect Method
Md = Mass discharge Cn = concentration in polygon n A n = Area of segment n
Step-by-step approach assuming uniform groundwater velocity
1. Draw transect: with polygons (“window panes”) for each well
2. Determine area (W • b = A)
3. Multiply and sum together:
Md = Σ (Cn• An•q)
Nichols and Roth, 2004
CROSS-SECTION W4 W3 W2 W1
< 0.5 ug/L
45 ug/L
74 ug/L
b Polygon
2
Width
Polygon 1
< 0.5 ug/L
Width
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q = K • i q = Groundwater Darcy velocity i = Hydraulic gradient K = Hydraulic conductivity*
Calculating Mass Discharge: Groundwater Darcy Velocity Term (q)
Variability in groundwater velocity - most applications of the transect method to date have assumed a uniform groundwater. Darcy velocity for the entire transect. However, different values for q may be used for different polygons if sufficient data are available.
Calculation of Darcy Velocity
• Hydraulic conductivity can be determined by pumping test, slug test, or estimated based on soil type
• Don’t use porosity – hydraulic calculations for groundwater (such as Theis equation) don’t rely on porosity
Md = Σ (Cn•An•qn)
9 Darcy Velocity (q) or Seepage Velocity (Vs)?
Md = Σ (Cn•An•qn)
Calculation Using Darcy Velocity
Calculation Using Seepage Velocity
Description Darcy velocity is averaged over entire transect area
Seepage velocity is velocity in open pore space
Diagram
Area Used for any Flow Calculation
Use entire transect area: Area = W • H
Use only open porosity area: Area = W • H • n
Flow Calculation
W
H
W
H n=porosity
Flow = K • i • W • H Flow = K • i • W • H • n
K * i =Darcy Velocity (q) K • i = Seepage Velocity (Vs) n
n
Flow = K • i • W • H Flow = K • i • W • H • n n
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Calculate Mass Discharge
by Hand t
N U M B E R 1
Calculator Exercise
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Building Transects: General Rules
u Can be permanent or temporary installations u No special well or sampling points needed u Can be based on longer single screen wells or
multilevel observations u Transect must be perpendicular or close to
perpendicular to groundwater flow
Source Strength
Plume Strength
Source
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Nichols and Roth, 2004
Transect Method: Using High Resolution Data
u Multi-level sampling means multiple level polygons
u Sum up all cells to get Mass Discharge (Md) in units of • Grams per day (g/dy) • or • Kilograms per year (kg/yr)
In this case • Md = 488 g/dy • or • Md = 178 kg/yr
w1 w2 w3 w4 w5
b1 b2
b3
b4
b5
b6
Transect GW Flow Direction
Transect
Figure 4-1
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Source: Guilbeault et al., 2005
(a) E
leva
tion
(m)
Ground New Hampshire PCE Site
Water Table
High Resolution Mass Flux Transect
Md: 56 grams per day (Mag 6 Plume)
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Tools for Transect Method: Calculator
Lead author: Shahla Farhat, Ph.D. free at www.gsi-net.com Microsoft Excel-based
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Key Features of Mass Flux Toolkit • Streamlines the data input process
• You pick interpolation method
• It does the calculations
• Uncertainty/sensitivity analysis • Graphical output
• How to use mass discharge data
• Overall resource for mass flux
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17 Method 2: Well Capture Mass Discharge Calculation
Nichols and Roth, 2004
Md = Mass discharge (grams per day)
Cwell = concentration in recovery well effluent (grams per liter)
Q = Well pumping rate (liters per day)
Md = Q x Cwell
Measure Q, Cwell from well Contaminant Source Groundwater
Flow Line Dissolved
Contaminant Plume
PumpingWell
Capture Zone
gram liter
liters day
= grams day
x
Figure 4-8
18 Well Capture Mass Discharge Calculation
Calculate mass discharge based on total capture of plume by pumping system
Nichols and Roth, 2004
Md = Mass discharge (grams per day)
Cwell = concentration in recovery well effluent (grams per liter)
Q = Well pumping rate (liters per day)
Md = Q x Cwell
Measure Q, Cwell from well Contaminant Source Groundwater
Flow Line Dissolved
Contaminant Plume
Supply Well
Capture Zone
gram liter
liters day
= grams day
x
Figure 4-8
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More Sophisticated Version Method 2
u Integral Pump Tests (IPT) • Steady state flow conditions, but handles changing
heterogeneous concentrations in plume
Figure 4-9. Estimating Mass Flux Using Integral Pump Test Series Data
Pumping tests with concentration time series measurements
Concentration vs. time during pumping tests (compound specific)
Total contaminant mass flux and average concentration
Transient inversion algorithm (analytical solution)
Groundwater Flow
Contaminated site
Source
of Pollutant
Well 1
Well 2
Well 3
Well 1 Well 2 Well 3 C C C
t1 t2 t1 t2 t1 t2
Isochrones (simplified)
Contaminated plume
Control plane
20 Well Capture Methods Advantages and Limitations
u Advantages • Fewer wells • Better integration of flow and concentration data • Can use existing pumping system
u Limitations • No mass flux data • Large volumes of water that need disposal/
treatment • Possible to change plume
characteristics • Difficult to assure full plume capture
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Method 3 – Passive Flux Meter
u Permeable sorbent • Accumulates
contaminant based on flow and concentration
u Soluble tracers • Loses tracer based
on groundwater velocity and flux convergence calculations K0 K>>K0
Groundwater Flowlines
t1
t2
t3
Source: Hatfield and Annable
Photo: Dye intercepted in a meter
1. Contaminant adsorbed onto passive flux meter over time to get Concentration
2. Tracer desorbs from passive flux meter over time to get Flow (Q)
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Installation Sampling
Vendor: http://www.enviroflux.com/pfm.htm
Passive Flux Meter
23 Passive Flux Meter Advantages and Limitations
u Advantages • “One stop shop” for both flow and concentration • Easy to install in the field • No waste generated • Vendor available to implement this method
u Limitations • Some method-specific issues
(lower measurement in pushed wells, slight biodegradation of tracer at one site, competitive sorption under some conditions)
• Relies on well convergence calculations
24 Method 4 – Use Existing Data (Transect Based on Isocontours)
u Uses plume map u Combine with flow data
Two dimensional transect based on isocontour data
1 2 5
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<0.1 <0.1
1 2 3 4 Transects
Scale (ft) 0 1000
Concentration isopleths (mg/L)
N
Transect 1: Intersection with Contour Lines N-NE S-SW
Concentration (mg/L) for contour lines
Geometric mean concentration (mg/
L) between contour lines
0.1 1 2 5 10 15 10 5 2 1 0.1
0.31 1.4 3.2 7.1 12.2 15 12.2 7.1 3.2 1.4 0.31
Figure 4-12
25 Isocontour Method Advantages and Limitations
u Advantages • Does not need special field study. Can use existing,
historical data from existing monitoring system • Limited additional expense
u Limitations • Wide range of opinion about usefulness of this
method • Can be inaccurate if plume map is built with
only a few wells. For example consider: § Gas station site with 5 wells throughout entire
plume: not likely to provide high quality mass flux/mass discharge data versus
§ Well characterized site with 40 wells in source zone: likely to provide higher quality data
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Enter flow, concentration data and calibrate model. Below: REMChlor model; 90% of source removed in 2010.
2008 2014 2080
Distance from Source (meters)
Mas
s D
isch
arge
(Kg
per y
ear)
Measurement Method 5 – Computer Models
To get REMChlor: google “REMChlor” and “EPA”
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Five Methods for Mass Discharge
u Method 1: Transect Method (Sect. 4.1) • Commonly used. Based on familiar technology
u Method 2: Well Capture/Pumping Methods (Sect. 4.2) • Many pump and treat systems doing this now.
u Method 3: Passive Flux Meters (Sect. 4.3) • New technology, easy to install, one device for flow and
concentration u Method 4: Using Existing Data (Isocontours) (Sect. 4.4)
• Uses existing data. Cost effective, but requires good monitoring network.
u Method 5: Solute Transport Models (Sect. 4.5) • Combines flow and concentration data. Helpful to have
experience
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Comparisons of Different Methods
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Comparisons of Different Methods
Summary of contaminant (TCE and DCE) mass discharge rates (g/day) as estimated using PFM and IPT results, and comparison with corresponding estimates based on the Transect Method (TM) (Brooks et al., 2008)
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Comparisons of Different Methods
Summary of contaminant (TCE and DCE) mass discharge rates (g/day) as estimated using PFM and IPT results, and comparison with corresponding estimates based on the Transect Method (TM) (Brooks et al., 2008)
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Comparison of Methods
TM = Transect method PFM = Passive flux meter MIPT = Modified integral pumping test
Method Comparison Based on Two Sites
TM and MIPT
u Relative difference 3% to 46% u (TM – MIPT)/TM
TM and PFM
u Relative difference -21% to 17% u (TM – PFM)/TM
PFM and MIPT
u Relative difference 0% to 35% u (PFM – MIPT)/PFM
Brooks et. al., (2008)
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Where Mass Discharge Has Been Used
61 Case Studies
0
10
20
30
40
1 2 3
1995 19999
2000- 2004
2005- 2009
Specific location (known city or county) Unspecified location within a state, province, or country
Managing Surface Water Quality with Mass Discharge: Total Maximum Daily Loads (TMDL) “The maximum amount of a pollutant that a water body or water segment can assimilate without exceeding water quality standards.” (1972 CWA)
u Copper into River (Alaska): up to 5450 grams per day
u Dioxin into Houston Ship Channel 0.04 grams per day
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Cwell = Md ÷ QWell Qw = 600 gpm
2 grams day x ÷ x =
106ug g
1 gal 3.79 L
x < 1 ug /L
Cwell = Concentration in extraction well Qwell = Pumping rate for extraction well
Einarson and Mackay, 2001
Using Mass Discharge: Estimating Well Impacts
Use mass discharge of plume to predict constituent of concern concentration in downgradient water supply well
Clean water
Md = 2 grams/day Clean water
Clean water
Source zone
Capture zone
Extraction well
1 600 gpm
day 1440 min
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Site Prioritization Using Mass Discharge
0.00078 Grams Per day
56,000 Grams
Per day
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OoM: “Order of Magnitude”
u Concentration, hydraulic conductivity have a log-normal distribution
Plume Magnitude Classification System Mass Discharge
(grams/day)
Plume Category
< 0.0001 to 0.001 “Mag 1 Plume” 0.001 to 0.01 “Mag 2 Plume”
0.01 to 0.1 “Mag 3 Plume” 0.1 to 1 “Mag 4 Plume” 1 to 10 “Mag 5 Plume”
10 to 100 “Mag 6 Plume” 100 to 1,000 “Mag 7 Plume”
1,000 to 10,000 “Mag 8 Plume” 10,000 to 100,000 “Mag 9 Plume”
>100,000 “Mag 10 Plume” Newell et al., 2011
Distribution by Plume Magnitude – 40 Sites
Sou
rce:
New
ell e
t al.,
201
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For complete capture and MCL = 5 ug/L: Mass
Discharge (grams/day)
Plume Classification
This Mag Plume Could Impact:
0.001 to 0.01 Mag 2 Plume Domestic well pumping at 600 liters prt day
1 to 10 Mag 5 Plume Municipal well pumping at 400 liters per minute
1,000 to 10,000 Mag 8 Plume Stream with a mixing zone and base flow of 4 cubic meters per second
What Mag Plume Does It Take for Impact?
Newell et al., 2011
Wrap Up
REMChlor
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Mass Discharge (grams/day)
Plume Category
< 0.0001 to 0.001 “Mag 1 Plume”
0.001 to 0.01 “Mag 2 Plume” 0.01 to 0.1 “Mag 3 Plume”
0.1 to 1 “Mag 4 Plume” 1 to 10 “Mag 5 Plume”
10 to 100 “Mag 6 Plume” 100 to 1,000 “Mag 7 Plume”
1,000 to 10,000 “Mag 8 Plume” 10,000 to 100,000 “Mag 9 Plume”
>100,000 “Mag 10 Plume”
Flux
Discharge