HomeMy WebLinkAboutMemo - Mail Packet - 1/9/2018 - Memorandum From Richard Thorp Re: 2017 Upper Cache La Poudre Watershed - Fall Water Quality UpdateUtilities
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700 Wood Street
PO Box 580
Fort Collins, CO 80522
970.221.6700
970.221.6619 – fax
970.224.6003 – TDD
utilities@fcgov.com
fcgov.com/utilities
M E M O R A N D U M
DATE: December 15, 2017
TO: Mayor Troxell and Councilmembers
FROM: Richard Thorp, Watershed Program Manager
THROUGH: Darin Atteberry, City Manager
Kevin R. Gertig, Utilities Executive Director
RE: 2017 Upper Cache la Poudre Watershed - Fall Water Quality Update
Bottom Line
In the shared interest of monitoring the Upper Cache la Poudre (CLP) River drinking water
supply, the City of Fort Collins, the City of Greeley, and the Soldier Canyon Water Authority
partnered in 2008 to implement the Upper CLP Collaborative Watershed Monitoring Program.
The overarching goal of this monitoring effort is to assist the participants in meeting current and
future drinking water treatment goals by reporting water quality conditions and trends within the
Upper CLP watershed. The attached water quality update provides a brief summary of
precipitation, streamflow and drought conditions over the 2017 water year, as well as water
quality trends during the summer months of October and November.
Background
The seasonal water quality updates are designed to inform the Upper CLP Watershed
Collaborative Monitoring Program partners, their customers, and other community stakeholders
about the condition of our source watershed and the quality of the raw drinking water supply.
Seasonal reporting began in 2015 to provide a succinct and timely summary of current-year
conditions in the Upper CLP Watershed. Seasonal updates are published for the spring, summer,
and fall seasons. In-depth water quality reporting is done through annual and five-year technical
reports. All water quality reports and seasonal updates are made publicly available on the Fort
Collins Utilities website, https://www.fcgov.com/utilities/img/site
_specific/uploads/December_2017_Watershed_Newsletter.pdf.
Fall 2017 Highlights
Precipitation was above the long-term average during the 2017 water year and remained above
average during October and November of the 2018 water year. Fall streamflow near the canyon
mouth decreased to baseflow conditions during October and November. All water quality
indicators during the 2017 fall monitoring season were within the range of values observed over
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the long-term monitoring record, indicating normal water quality. The Upper CLP watershed
continues to be a reliable, high quality drinking water source.
CC: Carol Webb, Water Resources and Treatment Operations Manager, Utilities
Jill Oropeza, Water Quality Services Manager, Utilities
Jared Heath, Watershed Specialist, Utilities
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Water Quality Update | Fall 2017
fcgov.com/water-quality
Monitoring and Protecting Our Water Sources
SOURCE WATER MONITORING
JWC - Joe Wright Creek above the confl uence with the Poudre River
PJW - Poudre River above the confl uence with Joe Wright Creek
PBR - Poudre River below the Town of Rustic
PSF - Poudre River below the confl uence with the Little South Fork
PNF - Poudre River above the confl uence with the North Fork at the
City of Fort Collins’ Intake
PBD - Poudre River below the confl uence with the North Fork at the
Bellvue Diversion
The Upper Cache la Poudre (UCLP)
Watershed Collaborative Monitoring
Program was established in 2008
between the City of Fort Collins, the City
of Greeley and Soldier Canyon Water
Authority, to help meet present and
future drinking water treatment goals.
Water quality monitoring of our raw,
Cache la Poudre River drinking water
supply is conducted from April through
November. Monitoring sites are strategically located
throughout the UCLP. Water quality data provide
valuable information about the health of our source
watershed and raw water supply.
The 2017 Fall Water Quality Update provides a
seasonal summary of water quality conditions
in the UCLP Watershed by highlighting
precipitation and streamfl ow conditions, as
well as water quality during the fall season
(October and November).
Routine water quality monitoring results are
reported for six key monitoring sites located
throughout the Upper Cache la Poudre watershed,
which capture water quality conditions above and
below major tributaries and near water supply
diversion structures (Figure 1).
More information is available at
fcgov.com/source-water-monitoring.
Figure 1 - Upper Cache la Poudre Collaborative Monitoring Program
sampling locations
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PRECIPITATION
Precipitation was above average by the end of the 2017 water year and start of the 2018 water year (Figure 2a).
A snowstorm in early October dropped 18-inches of snow, with an equivalent 2.3 inches of water, in the UCLP
Watershed. The fresh snowpack melted over several days and was followed by several smaller mixed precipitation
events (rain and snow) through October. Total precipitation monitored at the Joe Wright Snow Telemetry Station near
Cameron Pass measured 4.5 inches for the month of October compared to the long-term average of 3.4 inches.
Another notable snowstorm in early November delivered 15 inches of snow with an equivalent 2.5 inches of water to
the UCLP Watershed. A dryer period followed this storm with cooler temperatures sustaining the snowpack. A slight
increase in precipitation was observed through the end of November.
Total precipitation in November measured 4.9 inches compared to the long-term average of 4.5 inches. Cumulative
precipitation totaled 9.4 inches by December 1, which was 119 percent of average (7.9 inches) (Figure 2b), while
the early season snowpack water equivalent measured 71 percent of the long-term median (4.1 inches compared to
4.8 inches).
Water Quality Update | Fall 2017
fcgov.com/water-quality
WATER YEAR REVIEW
Figure 2 – (a) Cumulative precipitation for the 2017 and 2018 water years (WY) and (b)
monthly precipitation totals for October and November of 2017 compared to the long-term
average. Precipitation data were obtained from the Joe Wright Snow Telemetry station operated
by the Natural Resource Conservation Service.
Sep
Aug
Jul
Jun
May
Apr
Mar
Feb
Jan
Dec
Nov
Oct
50
40
30
20
10
0
PRECIPITATION(INCHES)
Average (1981 - 2010)
WY2017
WY2018
UCLP Cumulative Precipitation
Oct Nov
6
5
4
3
2
1
0
PRECIPITATION(INCHES)
Average (1981 - 2010)
WY2017
WY2018
(Totalsa) Fall Precipitation (b)
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Water Quality Update | Fall 2017
fcgov.com/water-quality
WATER YEAR REVIEW
Sep
Aug
Jul
Jun
May
Apr
Mar
Feb
Jan
Dec
Nov
Oct
3500
3000
2500
2000
1500
1000
500
0
STREAMFLOW(CFS)
Average (136 years of record)
WY2017
Spring WQ
Summer WQ
STREAMFLOW
Streamfl ow in the UCLP Watershed decreased to basefl ow (low fl ow) conditions by early September and fl uctuated
around the long-term average through November. Streamfl ow fl uctuations through the fall months were driven by a
combination of water releases from water storage reservoirs and snowmelt from the early season snow storms.
The daily average streamfl ow on October 1, 2017 was measured at 125 cubic feet per second (cfs), which was 126
percent of the long-term average (99 cfs). By November 30, streamfl ow was measured at 84 cfs, which was slightly
higher the historical average of 53 cfs (Figure 3).
Figure 3 – Streamfl ow measured on the Cache la Poudre River
at the Canyon Mouth (CLAFTCCO) during the 2017 water year.
This gaging station is operated by the Colorado Division of Water Resources.
Cache la Poudre River Streamfl ow at Canyon Mouth
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The Upper Cache la Poudre Collaborative Water Quality Monitoring Program uses several key water quality
indicators, including pH, conductivity, temperature and turbidity, which act as surrogates for other parameters.
(Table 1). These indicators provide a snapshot of water quality conditions and are useful for indentifying
trends or changes in water quality. Signifi cant changes in water quality indicators may provide an early warning of
potential water pollution.
Water Quality Update | Fall 2017
fcgov.com/water-quality
WATER QUALITY INDICATORS
Temperature Water temperature infl uences other water quality parameters and is a major driver
of biological activity and algal growth in rivers, including certain phytoplankton
species that produce the taste and odor compound, geosmin.
Water Quality Indicator Explanation
pH pH is an important water quality parameter to monitor, because it infl uences the
solubility and biological availability of chemical constituents, including nutrients
and heavy metals. pH near 7 is considered neutral, with more acidic conditions
occurring below 7 and more basic, or alkaline, conditions occurring above 7.
Conductivity
Conductivity is an index of dissolved ionic solids in water. Conductivity is used as
a general measure of water quality. Signifi cant increases in conductivity can be
used as an indicator of increased pollution.
Turbidity Turbidity is monitored to track changes in water clarity. Clarity is infl uenced by the
presence of algae and/or suspended solids introduced to surface waters through
various land use activities, including runoff and erosion, urban stormwater
runoff and drainage from agricultural lands. For water treatment, turbidity is
an important indicator of the amount of suspended material that is available
to harbor pollutants, such as heavy metals, bacteria, pathogens, nutrients and
organic matter.
Fall water quality monitoring captures water quality conditions during early basefl ow conditions that begin in early
fall and continue through winter. Basefl ow conditions are not infl uenced by direct runoff during the fall and winter
seasons, so streamfl ow experiences little change which usually results in stable and reliable water quality until
snowmelt runoff begins in early April.
All water quality indicators during the 2017 fall monitoring season were within the range of values observed over
the long-term monitoring record, indicating normal water quality (Figure 4). The median water temperature was
near or below the long-term median at all sites. Cooler water temperatures were likely driven by lower than average
fall air temperatures. pH was marginally above the long-term median at all sites and slightly increased moving
downstream. Conductivity was near the long-term median at monitoring locations higher in the watershed and
increased above the long-term average on the Cache la Poudre River below the Town of Rustic.
Table 1 - Water quality indicators measured as part of the Upper Cache la Poudre Collaborative Water Quality
Monitoring Program.
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Water Quality Update | Fall 2017
fcgov.com/water-quality
Maximum
Median
Minimum
Graphic Explanation
Data range based on
long-term data record
2008-2016.
Figure 4 – Water quality indicator data collected at key monitoring sites during Fall (October and November) 2017.
Fall
Median
(2017)
Concentrations were similar downstream of the confl uence with the Little South Fork Cache la Poudre
River (PSF) suggesting little infl uence from this tributary during the fall season. As expected, turbidity was
uniformly low throughout the watershed, indicating that there are likely low levels of suspended solids in the
UCLP Watershed.
The following lists the range of values measured throughout the Mainstem watershed during summer water
quality monitoring in 2017:
• Water temperature = 0.13º C – 7.06º C
• pH = 7.47 – 8.27
• Specifi c conductivity = 39 μS/cm – 116 μS/cm
• Turbidity =0.11 NTU – 1.53 NTU
Low turbidity water on the Poudre River
on August 14, 2017.
Joe Wright Reservoir Canyon Mouth
Joe Wright Reservoir Canyon Mouth
JWC PJW PBR PSF PNF PBD
24
18
12
6
0
TEMP (deg C)
JWC PJW PBR PSF PNF PBD
9
8
7
6
pH
JWC PJW PBR PSF PNF PBD
200
150
100
50
0
CONDUCTIVITY (uS/cm)
JWC PJW PBR PSF PNF PBD
12
9
6
3
0
NTU
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Water Quality Update | Fall 2017
fcgov.com/water-quality
fcgov.com/water-quality
MICROORGANISMS
Figure 5 – E. coli (a) and (b) total coliform colony form-
ing units (CFUs) in the Poudre River during the 2017 fall
season.
Coliforms are types of bacteria found naturally in the
environment in plant and soil material, but can also be
found in the digestive tract of warm-blooded animals,
including humans. Disease causing bacteria or pathogens
can be introduced to the raw drinking water supply from
fecal contamination.
Although the water treatment process effectively
eliminates pathogens, source watershed monitoring
can provide indication of changes in the activity and
location of pathogen sources over time. Through the
UCLP Collaborative Monitoring Program, the raw Poudre
River water supply is routinely tested for the presence of
bacterial contamination by measuring the total amount
of coliforms, an indicator organism for the presence of
pathogenic bacteria. In addition, Escherichia coli (E. coli)
is measured and used as an indicator of human or animal
fecal waste pollution since the source of origin is more
specifi c than total coliforms.
In fall 2017, E. coli and total coliform counts were within
the range of values seen in previous years and below
the long-term median (Figures 5a and 5b, respectively).
E. coli and total coliform counts were measured on the
Poudre below the town of Rustic were higher than the
long-term median, but cell counts were still well within the
range of values observed over the long-term record.
E. coli and total coliforms were
within the range of values seen in
previous years.
PBRPSFPNF PBD
24
18
12
6
0
CELLS/mL
PBRPSFPNF PBD
1600
1200
800
400
0
CELLS/mL
(a)
(b)
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Water Quality Update | Fall 2017
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TASTE AND ODOR
PBR PNF
Monitor Date
Geosmin (ng/L)
10/16/2017
11/13/2017
3.16
1.92
1.30
1.92
Geosmin is a naturally occurring organic compound produced by blue green algae, which introduces an
earthy odor to water that can be detected by the most sensitive individuals at concentrations as low as 4
nanograms per liter (ng/L) or 4 parts per trillion (ppt). Geosmin does not pose a public health risk, but it
is of concern because its detectable presence can negatively affect customer confi dence in the quality of
drinking water. Geosmin is monitored at PBR and PNF during routine UCLP monitoring events.
Geosmin concentrations observed at PBR and PNF were below the taste and odor threshold of 4 ng/L in
October and November (Table 2). Concentrations were higher on the Poudre River below Rustic (PBR)
in October, but were identical at both monitoring sites on the November sampling event. Environmental
conditions within the UCLP Watershed, specifi cally cold water temperatures and low nutrients, limit the
proliferation of geosmin producing algae; however, there have been episodic occurrences of elevated
geosmin throughout the UCLP Watershed, highlighting the importance of routinely monitoring geosmin as
an early warning for water treatment operations.
Table 2 – Poudre River geosmin concentrations (ng/L) during the fall of 2017 at Poudre above
the North Fork (PNF) and Poudre below Rustic (PBR) monitoring locations.
PBR PNF
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