Rock River Coalition Level 2 Stream Monitoring Results

Transcription

1 Rock River Coalition Level 2 Stream Monitoring Results This data report summarizes the results of data collected by volunteers participating in the Citizen-based Stream Monitoring pilot project from 200 to 200. We have analyzed data for temperature, transparency, dissolved oxygen (DO), and ph and included generalized information to help you understand your data. Over the last two years, different levels of stream monitoring have been developed to supplement the Water Action Volunteers program (Level 1). The Wisconsin Department of Natural Resources (WDNR), River Alliance of Wisconsin, and UW-Extension have conducted a pilot project (Level 2), which has citizens collect stream data using WDNR methods and equipment, and enter data in the WDNR s database. Currently, 130 volunteers collect data at sites. Table 1: Site name and location as listed in the WDNR database and site name as listed on charts used in this report Station ID, and Location on Charts 012 ALLEN CREEK - TN OF KOSHKONONG - AMACHER ALLEN CR AMACHER 012 ALLEN CREEK - TN OF KOSHKONONG- BLEECKER ALLEN CR BLEECKER 0122 ALLEN CREEK - EVANSVILLE-BROOKLYN RD. 1/2 WAY TO BUTTS CORNERS RD. BRIDG ALLEN CR BROOKLYN RD The Rock River Coalition, Dane and Rock County Land Conservation Depts and WDNR staff teamed together to monitor 20 sites in the Rock River Basin. Citizens collect water quality data that will assist the WDNR in manage ment decision making, providing documentation for 303(d) impaired waters listings and measuring response to best management practice installations. The data will also be valuable in the develop ment of an implementation plan for the Rock River Total Maximum Daily Load. They monitor 2 sites on 1 streams (Table 1). 012 ALLEN CREEK UPSTREAM FROM CHURCH ST. BRIDGE- EVANSVILLE ALLEN CR CHURCH ST 00 ALLEN CREEK - ALLEN CR UPSTRM OF HWY 213 ALLEN CR HWY ALLEN CREEK - TOWN OF KOSHKONONG - MERRIMAN S ALLEN CR MERRIMAN S 32 BARK RIVER GENESSEE LAKE ROAD BARK R 012 BLACK EARTH CREEK BETWEEN MAZOMANIE AND BLACK EARTH BLACK EARTH CR 012 FISHER ROCKPORT PARK FISHER CR 012 KOSHKONONG CREEK AT FORMER DAM SITE IN ROCKDALE KOSHKONONG CR 012 LITTLE OCONOMOWOC RIVER AT PETERSEN RD L OCONOMOWOC R 322 MARKHAM CREEK - HWY D MARKHAM CR MURPHY CREEK - MADISON LANDFILL SEEPAGE MURPHY CR LANDFILL 001 NORWEGIAN CREEK UPSTREAM (AT) HWY /H NORWEGIAN CR 03 OTTER CREEK - OTTER CREEK AT BOWERS L. RD OTTER CR BOWERS 0121 OTTER CREEK: COUNTY N/ HWY 2 ( NORTH OF CTY N BRIDGE) OTTER CR CTY N/ OTTER CREEK: KLUG RD. ( FT WEST OF BRIDGE) OTTER CR KLUG 1330 SIX MILE CREEK - AT STH 3 AND 1 SIX MILE CR 0120 SUSSEX (SPRING) SUSSEX WWTF SUSSEX CR 1332 TOKEN CREEK MILLPOND - AT PORTAGE RD. DAM TOKEN CR 32 TURTLE CREEK - AT CARVERS ROCK RD- NEAR CLINTON- WI TURTLE CR CARVERS 0122 TURTLE CREEK - TURTLE CREEK AT HEIDT S TURTLE CR HEIDTS Level 2 Citizen-Based Stream Monitoring website: level2/stream.html 012 WINGRA (MURPHY) CREEK 300 METERS UPSTREAM FROM FISH HATCHERY RD 0121 MURPHY (AKA WINGRA) CR - JUST DWNSTRM OF SMALL BRIDGE- 200 METERS FROM L WINGRA WINGRA CR FISH HATCH RD WINGRA CREEK DWN L WINGRA

2 Data Summaries For ph, transparency, and dissolved oxygen, we report the minimum, maximum and median values for each site for the monitoring period, since data were collected monthly from May to September. The report includes all data entered into the WDNR database before September 1, 200. For water temperature, we report minimum, maximum, and mean daily averages for each month for each site. We report mean daily averages for each month since temperature was monitored hourly from the time the data loggers were placed in the stream in the spring until the end of September when they were removed from the stream. Data collected between May and September 200 are reported. Obtaining Raw Data from the WDNR Database (SWIMS) For more specific information about data collected at a specific site, as a registered Level 2 citizen-based water monitoring program participant you can log in to the WDNR s database and download the data that have been entered to that system. Visit: to login to the database, and follow these steps to download the data about a specific site: 1. Choose the link for the Citizen-based Stream Monitoring Pilot Project near the center of your screen. 2. On the left side of the screen that appears, pick your WDNR Region (i.e., Northeast (NER), Northern (NOR), South Central (SCR), Southeast (SER), or West Central (WCR). 3. Pick your group s liaison from the list on the left side of the screen.. Pick your local group s name from the list on the left.. Pick your team from the list on the left.. At this point a list of reports which contain the raw data for each site that was monitored will appear in the center of the screen. Choose which report you want to view. You will have the option to view the report online (html option), as a csv file (this will open as an Excel file), or as a pdf file. Low Helpful Terms Either Median or Mean High In this report, for each parameter monitored, some statistical information is provided to help explain what has been found. You may want to refer back to this section as you read through the report to help you understand what is being presented. n: This is the number of times a parameter was monitored (for temperature, it is the number of days temperature was recorded in a month). Mean: This is the average score in a data set, or a typical expected value. Median: This is the middle value in a data set of ranked values. When not a lot of data have been collected, it is considered to be better than the mean in estimating the typical expected value for a parameter. For instance, assume the following readings (in mg/l) were found for five D.O. assessments:.,.0, 12., 1.,.0. Ranking them in order from lowest to highest, we get:.0,.0,., 12., 1. The value in the middle of that ranked data set is.. Thus,. mg/l is the median. (If you have an even number of data points in the data set, the median is the mean of the middle two numbers in the ranked list.) If we determined the mean for the same data set, very high and/or low values might affect it. For this example the mean is determined in the following way: =../ =.1 mg/l n Thus,.1 mg/l is the mean. Although there isn t a large difference in the median (. mg/l) and the mean (.1 mg/l) in this example, in a small data set where one or two values are very different than most of the other values, using the median instead of the mean should provide a better estimate of the expected value. In a large data set, the mean and median are expected to be the same or nearly the same. 2

3 Dissolved Oxygen Dissolved oxygen (DO) is a gas found in water that is critical for sustaining aquatic life (just as oxygen is required for us to survive). Dissolved oxygen enters water through mixing with air in turbulent waters or through photosynthetic processes by aquatic plants and algae. Decomposition of organic materials that have entered the stream from point or non-point source inputs (such as runoff from a yard or field), plant respiration and oxygen demand by organisms such as macroinvertebrates and fish are important factors contributing to DO losses in the aquatic environment. DO varies over a 2 hour period, with lowest levels expected just before sunrise, when plants and animals have been respiring, but photosynthesis has not been occurring. This flux over a 2-hour period is called a diurnal variation. Large fluctuations in diurnal DO levels (e.g., - mg/l and supersaturated conditions at times) generally indicate increased photosynthesis and respiration due to elevated levels of plant and/or algal growth. Dissolved oxygen levels are important in determining various communities of aquatic life. DO levels below 2 mg/l generally do not support aquatic life, and most fish and many insects cannot tolerate levels below - mg/l for a sustained period of time. DO levels above mg/l are amenable to coldwater species such as trout. Different species of fish will migrate within a stream to seek suitable dissolved oxygen conditions. There are several categories by which waters of Wisconsin are classified by state law. These include (but aren t limited to) trout waters, other fish or aquatic life-designated waters, limited forage fish communities, and limited aquatic life communities. There are defined DO minimums set for each type of classification. The minimums are designed to allow the aquatic organisms defined in the classification to survive in those waters. Since different organisms have different DO requirements, the DO minimums vary based on stream classification. Table 2 shows the minimum DO allowed in waters classified in certain ways by Wisconsin state law. You can identify if your stream is designated as a trout stream by opening this file from the Wisconsin Department of Natural Resources (WDNR) website (available at: wisconsintroutstreams.pdf ). Lists of waters that are designated as limited forage fish or limited aquatic life communities are included in Chapter NR Uses Rock River Coalition Stream Monitoring Results: Minimum, Median and Maximum Values for Dissolved Oxygen Dissolved Oxygen (mg/l) Dissolved Oxygen (% sat).0 3

4 and Designated Standards (available at: nr.pdf ) and in Chapter NR 2 Water Quality Standards for Wisconsin Surface Waters (available at: ). Table 2: Minimum dissolved oxygen levels allowed for waters with varied classifications in Wisconsin Stream classification Trout waters Fish or aquatic life-designated waters Limited forage fish waters Minimum dissolved oxygen allowed mg/l (out of spawning season) and mg/l (during spring/fall spawning season) mg/l 3 mg/l Limited aquatic life waters 1 mg/l Since DO and temperature are intimately related (e.g., water with a higher temperature can hold less oxygen than water with a lower temperature, so the general concentration of the two parameters in water generally mimic one another), it s important to consider the two together (Table 3). Dissolved oxygen content in streams is linked with temperature requirements of aquatic life. Colder water generally has more oxygen, and warmer water has less oxygen. Table 3: Dissolved oxygen requirements of aquatic plants and animals Very High DO Moderately high DO Low DO ANIMALS Brook or rainbow trout Brown trout Carp Mottled sculpin Redbelly dace Green sunfish Bass PLANTS Fathead minnow Much plant variety Moderate plant variety Little plant variety Source: Dane County Water Watchers

5 Transparency Turbidity is a measure of water clarity or cloudiness caused primarily by the presence of suspended particulate matter in solution. It is basically an optical measurement of the amount of light scattering caused by fine organic or inorganic particles and to a lesser extent some dissolved substances in the water. These small particles of soil, algae or other materials generally range in size from microscopic to about one millimeter (about as thick as a pencil lead). More free-floating particles cause greater turbidity, resulting in less light penetration through the water. This hinders photosynthesis, necessary for healthy aquatic plant growth and production of dissolved oxygen. With increased turbidity, water also becomes warmer because the suspended particles absorb heat. Since warmer water holds less dissolved oxygen than cold water, oxygen levels are also affected by turbidity. Extremely high levels of turbidity may also impair aquatic organism survival, for instance, by blocking gas exchange in membranes used for respiration, interfering with filter feeding mussels, or by restricting predation by sight-feeding fish. In general, turbidity increases with increasing river flow due to erosional processes and bed sediment resuspension. Sources of turbidity include: Rock River Coalition Stream Monitoring Results: Minimum, Median and Maximum Values for Transparency Average Transparency (cm) 1 erosion from fields, construction sites urban runoff from rainstorms and melting snow eroding stream banks decaying plant matter large number of bottom feeders (such as carp) which stir up bottom sediments algae wastewater discharges Since turbidity correlates directly with transparency, transparency can be used as a surrogate measurement of water clarity. Measuring water clarity with a transparency tube takes into account both water color and suspended particles. All streams have background or normal levels of water clarity. Fish and aquatic life that inhabit particular streams are adapted to those background levels of water clarity. Time is probably the most influential factor in determining how turbidity affects the aquatic environment. The longer the water remains at unusually high values of turbidity, the greater effect it has on fish and other aquatic life. Fish in particular become very stressed in waters that remain highly turbid for a long time. Signs of stress include increased respiration rate, reduced growth and feeding rates, delayed hatching and in severe cases, death. Fish eggs are ten times more sensitive to changes in turbidity than adult fish. Table : Transparency conversion from cm to NTUs Transparency (cm) Turbidity (NTUs) <. >20. to to to.. to to to to to to to to to to to to to to to. 1. to to. 12. to to. >. <

6 You measure water clarity in centimeters (cm). The transparency tubes used by Level 2 stream monitors are approximately 120 cm long. Many monitors found that they could see the disc in the bottom of the tube when the tube was full, and thus reported transparency values of ~120 cm. We cannot determine the exact transparency at these sites, and instead only know that it is greater than 120 cm. These high transparencies indicate good water quality (Figure 1). Use Table to convert your site s transparency to NTUs (units of measurement for turbidity) and then refer to Figure 2 to further understand how time and turbidity impact fish. Figure 1: Low Water Transparency Influences Fish Health Figure 2: Relational Trends of Freshwater Fish Activity to Turbidity Values and Time

7 Water Temperature Water temperature is an important physical property that influences the growth and distribution of aquatic organisms. It is also an important factor regulating chemical and biochemical reactions in aquatic animals and plants. Surface water temperature is strongly influenced by solar radiation, local climate and groundwater inflows. Wisconsin uses water temperature as an important variable in the designation of fish and aquatic life uses for surface waters. Use designations are utilized to classify waters of the state into certain categories so that management decisions can be made to protect the quality of those water resources. Table : Thermal criteria for cold, cool and warm water streams in Wisconsin Thermal regime Maximum instantaneous temperature Maximum daily mean temperature Cold water stream <2 C ( F) < 22 C (2 F) Cool water stream 2-2 C 22-2 C Warm water stream >2 C (2 F) > 2 C ( F) Long-term water temperature data are useful for interpreting temporal variations. The WDNR uses temperature data averaged over months or seasons to calculate effluent limits. By setting effluent limits to surface waters, aquatic life present in the streams being monitored can be protected. The WDNR also classifies streams by their water temperatures, indicating if they are cold, cool, or warm water streams (Table ). These classes of streams support different types of fish species. The best quality coldwater streams have relatively few species of fish as compared to warm water streams. Salmonids such as brook trout dominate the fish populations in the best quality coldwater streams, while brown trout, an exotic salmonid species, dominate coldwater streams that have slightly less pristine water quality. Bass, darter and sucker species are more prevalent in warmwater streams than in coldwater streams. Different species of fish have different temperature requirements. Trout need cool temperatures, while fish species such as bass can live in waters with higher temperatures (Figure 3). Most Aquatic Freshwater Invertebrates Die 0 C Largemouth & Smallmouth Bass Die 3 C Brown Trout Die 2 C Rainbow Trout Die 2 C Brook Trout Die 2 C Some Mayfly and Stonefly Larva Die 20 C 0 C ( F) 3 C (0 F) 30 C ( F) 2 C ( F) 20 C ( F) 1 C ( F) C (0 F) C (1 F) 0 C (32 F) More Plant Growth C -20 C Illustration by Jeffrey J. Strobel UW-Extension Environmental Resources Center Figure 3: Species tolerance to various temperatures Optimal temperature range for bass, sunfish, catfish, minnows, darters, northern pike, dragonfly larva Optimal temperature range for trout, sculpin, and larva of mayfly, stonefly, caddisfly.- C Optimal temperature range for brook and brown trout spawning Based on the table above and your site s minimum, maximum and mean water temperatures for each month (see next page), how would you classify your stream based on its temperature over time? Coldwater, coolwater, or warmwater? If you monitor macroinvertebrates, how do your findings for macroinvertebrates and temperature compare with their temperature tolerances as listed in Figure 3? Do you find many plants at your monitoring site? Does their presence make sense in relation to average water temperatures?

8 Rock River Coalition Stream Monitoring Results: Minimum, Mean and Maximum Values for Temperature (during May to September 200) May June 200 July n = 30 for all sites.0 1 n = 31 for all sites except where noted August 200 September n = 31 for all sites

9 ph ph is a measure of the hydrogen-ion activity of water and is expressed as a logarithmic unit that ranges from 1 to 1 Standard Units. That means for every 1 ph unit change, there is a tenfold change in the activity of hydrogen ions. Waters with high hydrogen-ion activity have low ph and are considered acidic. The presence of dissolved carbon dioxide, carbonic acid, bicarbonate ions and carbonate ions strongly influence the ph of freshwater systems. Much of Wisconsin has bedrock that is composed of limestone and other rock that is rich in bicarbonate and carbonate. These types of rock can minimize impacts of acid rain or other acidic inputs to the water. In northern Wisconsin, bedrock is composed of granite which is not rich in bicarbonates and carbonates, and thus those rocks are less able to buffer or offset the impacts of acid rain or other acid inputs to the waters. In poorly buffered waters, ph may change a lot in the course of a 2-hour period based on photosynthesis (which uses carbon dioxide) and respiration (which releases carbon dioxide) by aquatic plants and algae. In other parts of the state which are well buffered, ph may not change much over a 2-hour period. Dissolved metal ions tend to increase with increased acidity and as a result, ph is an important factor influencing toxicity of metals. ph also affects the concentration of un-ionized ammonia, a form of nitrogen that is extremely toxic to aquatic life. Wisconsin has adopted a ph standard that incorporates a range from to units to protect and support aquatic life use. Rock River Coalition Stream Monitoring Results: Minimum, Median and Maximum Values for ph ph Figure shows the WI ph quality standard along with some reference points for aquatic organisms and everyday substances. Is your site s ph fairly static or does it vary over time? Snails & Tadpoles Begin to Die Salmonid Eggs & Fry Die Wisconsin ph Quality Standard (-) Tolerance Range for Fish Figure : ph reference points for aquatic organisms and everyday substances, and the WI ph quality standard. Caddisflies & Mayflies Die Bass & Trout Begin to Die Optimum ph for Most Fish 0 1 basic ph ph acidic Battery Acid & Stomach Acid Lemon Juice Vinegar Tomatoes Carrots Normal Rain Milk Human Blood Ammonia Bleach Lye Compiled by Kris Stepenuck, UW-Extension/WDNR and Chris Clayton, River Alliance of Wisconsin/WDNR Graphic design by Annika Sargent, UW-Extension Environmental Resources Center