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Distribution of Nitrate in Ground Water Under Three Unsewered Subdivisions
Erin P. Eid
Mike Trojan
Jim Stockinger
Jennifer Maloney
Minnesota Pollution Control Agency
Ground Water Monitoring and Assessment Program
Why conduct a Septic System study?
• Assess water quality in unsewered areas
• Few studies comparing water quality between different unsewered subdivisions
• Limited information of spatial distribution of nitrate in unsewered subdivisions
• Determine risk to ground water and surface water
• Limited information for water and city planners
Objectives
• Determine the spatial distribution of nitrate in ground water under three unsewered subdivisions
• Identify factors affecting the distribution of nitrate under the three subdivisions
Variables
• Density and age of septic system and subdivision
• Aquifer hydrogeology and geochemistry
• Performance of septic system
• Depth to ground water
Sampling Design
• One-time sampling events using shallow geoprobe and deeper domestic well samples
• Collection of soils for textural analysis
Geoprobe and Domestic Well Cross-Section
Cross-section showing geoprobe (G) and domestic well (W) sampling locations through an aquifer
Depth
(m
)
Distance (m)
10
20
30
0
40
0 500 1000 1500 2000
G GWW
G G G GWWW
WWW
W
Site Criteria
• Sandy Soils
• Sand and Gravel Aquifer
• Less than one acre lot size
• Aquifers vulnerable to contamination
• Results applicable to other areas
• Local cooperation
Site Locations
• Baxter Area– sampled 37 domestic wells
– geoprobed 24 sites
• St. Joseph Area– sampled 23 domestic wells
– geoprobed 7 sites
• Lakeland Area– sampled 44 domestic wells
– geoprobed 9 sites
#Y
#Y#
#Y
##Twin Cities
#
Baxter
#
Lakeland
Pleasant Acres
Study Area - Baxter• Urban Area of 40,000
people• Considerable land use
changes last 10 years• Surficial geology consists of
outwash deposits of sand and gravelly sand
• Shallow sand and gravel aquifer with 15 feet of land surface
#Y#Y
#Y#Y #Y
#Y
#Y#Y
#Y
#Y#Y
#Y#Y
#Y#Y
#Y
#Y
#Y
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S%U
%U%U%U
%U%U
%U
White SandLake
Sand LakeLower Wipple Lake
Clearwater
Hig
hway
371
Highland
Mapleton
#S
#Y%U
Domestic WellGeoprobeISTS Investigation
Study Area - Lakeland• Community of approximately 5,000
people• Has not experienced significant growth
in last 10 years• Surficial geology consists of coarse sand,
gravel, and gravelly sand terrace deposits• Depth of bedrock varies between 0 and
60 feet• Unconfined sand and gravel aquifer
found at 45 to 80 feet below land surface
#S
#Y G eop robe
D om estic W ell
#S#S#S#S#S#S#S#S #S#S#S #S#S#S#S #S#S#S
#S#S
#S
#S
#S #S
#S#S#S#S#S#S#S#S
#Y#Y #Y
#Y
#Y
#Y
#YS T
. CR
OIX
RIV
ER
I 94
St. C
roix
Tra
il
Study Area - Pleasant Acres
• Located near metropolitan area of 100,000 people
• Considerable land use changes within last 10 years
• Surficial geology consists of primarily outwash deposits of sand and gravelly sand
• Surficial sand and gravel aquifer located between 10 and 25 feet of land surface
#Y #Y
#Y
#Y
#Y
#Y
#Y#Y
#Y
#Y#S
#S
#S
#S
#S
#S
#S #S
#S
#S
#S
#S
#S
#S
#S
#S
#S
#S Domestic Well#Y Geoprobe
Parameters
• Field measurements:– oxidation-reduction potential, temperature, pH, specific
conductance, dissolved oxygen, and water level
• Laboratory Analysis:– Major cations and anions– dissolved organic carbon– ammonia- and Kjeldahl-nitrogen
Nitrate concentrations at the water table did not differ between the three areas
6.4 6.4 4.30
2
4
6
8
Nit
rate
(p
pm
)
Lakeland Baxter Pleasant Acres
Lakeland: Nitrate concentrations did not decrease with depth
0.1
1
10
0 50 100 150
Depth (feet)
pp
m o
r vo
lts
Nitrate Dissolved oxygen Eh
600
650
700
750
800
0 200 400 600 800 1000 1200
Lakeland Cross-section
Sand and Gravel
? Bedrock ?
Clay
Baxter: Nitrate concentrations decreased rapidly in the upper 20 feet of the surficial
aquifer
0.01
0.1
1
10
0 10 20 30 40 50 60
Depth (feet)
pp
m o
r vo
lts
Nitrate Dissolved oxygen Eh
Pleasant Acres: Nitrate concentrations decreased abruptly at about 25 feet
0.1
1
10
0 10 20 30 40 50 60
Depth (feet)
pp
m o
r vo
lts
Nitrate Dissolved oxygen Eh
800
850
900
950
1000
1050
1100
1150
1200
300 400 500 600 700 800 900 1000
Pleasant Acres Cross-section
SandClay
Sand
? Bedrock ?
The depth to which each aquifer is vulnerable to nitrate contamination varied
between the three areas
05
10152025
0 50 100 150
Depth (feet)
Nit
rate
(p
pm
)
Lakeland Baxter Pleasant Acres
Possible reasons for the differences with depth?
• Lower rates of denitrification in Lakeland
• Fractured bedrock flow in Lakeland
• Higher aquifer hydraulic conductivity in Baxter may move nitrate more deeply than in Pleasant Acres
• Pleasant Acres has well-defined geochemical zones
• Differences in effluent discharge
12 to 25 percent of samples collected at the water table exceeded the MCL of 10 ppm
17 25 12.5
0
5
10
15
20
25
Per
cen
t
Lakeland Baxter Pleasant Acres
Lakeland
##
#
####
#
#
#
# ###
##
###
##
#
#
#
#
#
#
####
## #
#
#
#
< 2 ppm
2 - 5 ppm
5 - 10 ppm
> 10 ppm
#
#
##
#
##
##
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
#
< 2 ppm
2 - 5 ppm
5 - 10 ppm
> 10 ppm
Baxter
• Nitrate concentrations at the water table under unsewered developments are about 4 to 6 ppm
• The depth of nitrate impacts from septic systems is controlled by aquifer geochemistry and hydrology
• In unsewered areas small lot size and the age of the development are factors in elevated nitrate levels
Conclusions
Future Studies / Use of Data
• Septic System studies in additional communities
• Effects of septic systems on sensitive surface water
• Relationship between septic systems, lot size, and age of development
• Computer simulations for prediction of effects of septic systems on ground water quality in other communities