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HYDRAULIC CONDUCTIVITY:
HOW MANY MEASUREMENTS
DO YOU NEED?
Dr. Andrea Welker, PE, F.ASCE, ENV SP
Dr. Kristin Sample-Lord, PE
Villanova University
Outline
3
Rain gardens as stormwater control measures
Need to quantify infiltration rates
The research goals
Ponded recession rate
Spot infiltration testing program
Results from five rain gardens
Rain gardens – stormwater control
4
PA BMP Manual
Actual (Beautiful!) Rain Garden on the
Jenkintown Creek in Abington, PA
April 6th, 2017: 10:10 AM to 6:30 PM (1.10”)
5
Infiltration is an important mechanism
Infiltration and evapotranspiration are the two key mechanisms that control
stormwater in rain gardens
Quantifying infiltration is important in design phase and is often part of
inspections – a minimum value is often set by regulations
6
Research goals
7
• Time spent testing
• Volume of water used
• Number of tests required
Optimize efficiency in measurement of infiltration rate
• Accurately estimate performance of rain garden
• Err on the side of conservativism
Obtain a reliable and representative value
k Soil Suction
Soil Thickness
Moisture Content
Piezometric Head
Factors influencing infiltration
8
Ponded recession rate
• An indirect measurement of infiltration (Emerson 2008)
• A very useful performance indicator
• Simply measured using bubblers, pressure transducers
• Provide infiltration rate over the entire rain garden bowl, so this is
considered the “true” value
9
Ponded recession rate
10
11
Summary of sites
12
Site Surface Area
(m2)
Hydraulic
Loading Ratio
Size of Design
Storm (cm)
USCS
Classification
USDA
Classification
VURG1 235 10:1 2.54 SM Silty sand Loamy sand
VURG2 92 0.87:1 2.54
SP Poorly graded
sand
Sand
USRG 80 8.6:1 3.61 SM Silty sand Sandy loam
DSRG 62 13:1 4.24 SM Silty sand Sandy loam
SMP A 429 19:1 8.5
SW-SM Well
graded sand
with silt
Loamy
sand/sandy
loam
Field infiltration tests
13
Double ring is still considered
the “gold” standard by many
Temperature correction and
seasonal consistency
Relate infiltration test results
to ponding recession rate
Site
Number of
Infiltration
Tests
Performed
Method
Used
Geometric
Mean
Average k
(m/s)
Measured
Ponding
Recession
Rate (m/s)
VURG1 7
Single-
Ring
2.61x10-6 1.90x10-6
VURG2 10 MPD 1.06x10-6 1.06x10-6
USRG 10 SATURO 2.48x10-5 4.72x10-5
DSRG 8 SATURO 1.87x10-5 4.22x10-5
SMP A 8 SATURO 1.06x10-5 3.70x10-5
Single-Ring
Infiltrometer
Modified Philip-
Dunne
SATURO
Method of
Measurement
Continuous refill,
constant head
Full to empty, falling
head
“DualHead”
approach, completely
automated
Precision (Range of k)
7.1x10-5 cm/s to
7.1x10-3 cm/s
1x10-6 cm/s to
1x10-2 cm/s
1.0x10-6 cm/s to
3.2x10-2 cm/s
Dimensions (cm) H = 15.2, d = 15.2 H = 61 cm, d = 10 cm 5 cm insertion ring
Additional Notes
Driven halfway into
soil
Sealed at top to
prevent evaporation
5 gallon water supply
tank
14
Testing rationale
15
Spatial variability within the soil
media and over the surface area will
result in different test results
Perform a number of tests, evenly
spaced, same season
Analyze data in the context of
ponding recession data, i.e. what is
actually happening
Data analysis
Organize Test
Data
Generate All
Possible
Combinations
up to r = n
Plot the
Geometric
Mean of Each
Combination
Relate to
Actual
Recession
Rate
16
SMP A
17
Measured Recession Rate (m/s) 3.70x10-5
Number of Tests 1 2 3 4 5 6 7 8
Average Value (m/s) 2.31x10-5 1.56x10-5 1.32x10-5 1.21x10-5 1.14x10-5 1.10x10-5 1.08x10-5 1.06x10-5
% Difference from Recession Rate 38 58 64 67 69 70 71 71
Standard Deviation (m/s) 2.49x10-5 1.47x10-5 9.58x10-6 6.65x10-6 4.77x10-6 3.39x10-6 2.23x10-6 -
Coefficient of Variation 1.08 0.94 0.73 0.55 0.42 0.31 0.21 -
Standard Deviation as % of Recession
Rate
67 40 26 18 13 9 6 -
SMP A
18
All sites
19
Standard deviation as a % of
recession rate occurs around 5 to 6
tests
Bottom line
Five to six single ring infiltrometer
tests (e.g. Saturo) should be able to
adequately characterize the
infiltration capacity of a rain garden
20
Acknowledgments
21
The views expressed here are the authors’ and
not those of the sponsors.
Thanks to Zach Zukowski, James Press, Virginia
Smith, and Billy Nichols.
QUESTIONS?
Hydraulic Conductivity Measurements

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Hydraulic Conductivity Measurements

  • 1.
  • 2. HYDRAULIC CONDUCTIVITY: HOW MANY MEASUREMENTS DO YOU NEED? Dr. Andrea Welker, PE, F.ASCE, ENV SP Dr. Kristin Sample-Lord, PE Villanova University
  • 3. Outline 3 Rain gardens as stormwater control measures Need to quantify infiltration rates The research goals Ponded recession rate Spot infiltration testing program Results from five rain gardens
  • 4. Rain gardens – stormwater control 4 PA BMP Manual Actual (Beautiful!) Rain Garden on the Jenkintown Creek in Abington, PA
  • 5. April 6th, 2017: 10:10 AM to 6:30 PM (1.10”) 5
  • 6. Infiltration is an important mechanism Infiltration and evapotranspiration are the two key mechanisms that control stormwater in rain gardens Quantifying infiltration is important in design phase and is often part of inspections – a minimum value is often set by regulations 6
  • 7. Research goals 7 • Time spent testing • Volume of water used • Number of tests required Optimize efficiency in measurement of infiltration rate • Accurately estimate performance of rain garden • Err on the side of conservativism Obtain a reliable and representative value
  • 8. k Soil Suction Soil Thickness Moisture Content Piezometric Head Factors influencing infiltration 8
  • 9. Ponded recession rate • An indirect measurement of infiltration (Emerson 2008) • A very useful performance indicator • Simply measured using bubblers, pressure transducers • Provide infiltration rate over the entire rain garden bowl, so this is considered the “true” value 9
  • 11. 11
  • 12. Summary of sites 12 Site Surface Area (m2) Hydraulic Loading Ratio Size of Design Storm (cm) USCS Classification USDA Classification VURG1 235 10:1 2.54 SM Silty sand Loamy sand VURG2 92 0.87:1 2.54 SP Poorly graded sand Sand USRG 80 8.6:1 3.61 SM Silty sand Sandy loam DSRG 62 13:1 4.24 SM Silty sand Sandy loam SMP A 429 19:1 8.5 SW-SM Well graded sand with silt Loamy sand/sandy loam
  • 13. Field infiltration tests 13 Double ring is still considered the “gold” standard by many Temperature correction and seasonal consistency Relate infiltration test results to ponding recession rate Site Number of Infiltration Tests Performed Method Used Geometric Mean Average k (m/s) Measured Ponding Recession Rate (m/s) VURG1 7 Single- Ring 2.61x10-6 1.90x10-6 VURG2 10 MPD 1.06x10-6 1.06x10-6 USRG 10 SATURO 2.48x10-5 4.72x10-5 DSRG 8 SATURO 1.87x10-5 4.22x10-5 SMP A 8 SATURO 1.06x10-5 3.70x10-5
  • 14. Single-Ring Infiltrometer Modified Philip- Dunne SATURO Method of Measurement Continuous refill, constant head Full to empty, falling head “DualHead” approach, completely automated Precision (Range of k) 7.1x10-5 cm/s to 7.1x10-3 cm/s 1x10-6 cm/s to 1x10-2 cm/s 1.0x10-6 cm/s to 3.2x10-2 cm/s Dimensions (cm) H = 15.2, d = 15.2 H = 61 cm, d = 10 cm 5 cm insertion ring Additional Notes Driven halfway into soil Sealed at top to prevent evaporation 5 gallon water supply tank 14
  • 15. Testing rationale 15 Spatial variability within the soil media and over the surface area will result in different test results Perform a number of tests, evenly spaced, same season Analyze data in the context of ponding recession data, i.e. what is actually happening
  • 16. Data analysis Organize Test Data Generate All Possible Combinations up to r = n Plot the Geometric Mean of Each Combination Relate to Actual Recession Rate 16
  • 17. SMP A 17 Measured Recession Rate (m/s) 3.70x10-5 Number of Tests 1 2 3 4 5 6 7 8 Average Value (m/s) 2.31x10-5 1.56x10-5 1.32x10-5 1.21x10-5 1.14x10-5 1.10x10-5 1.08x10-5 1.06x10-5 % Difference from Recession Rate 38 58 64 67 69 70 71 71 Standard Deviation (m/s) 2.49x10-5 1.47x10-5 9.58x10-6 6.65x10-6 4.77x10-6 3.39x10-6 2.23x10-6 - Coefficient of Variation 1.08 0.94 0.73 0.55 0.42 0.31 0.21 - Standard Deviation as % of Recession Rate 67 40 26 18 13 9 6 -
  • 19. All sites 19 Standard deviation as a % of recession rate occurs around 5 to 6 tests
  • 20. Bottom line Five to six single ring infiltrometer tests (e.g. Saturo) should be able to adequately characterize the infiltration capacity of a rain garden 20
  • 21. Acknowledgments 21 The views expressed here are the authors’ and not those of the sponsors. Thanks to Zach Zukowski, James Press, Virginia Smith, and Billy Nichols.