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Water quality analysis

 

     There are a variety of ways to analyze water quality.   Many researchers studying the quality of rivers use the WQI (Water Quality Index).  The WQI uses nine tests to determine the health of a river.  The use of a WQI is appropriate for high school age students and older.  The following activities present ideas that are accessible with few supplies and safe for conducting with elementary and middle school students.  They are not as technically accurate as a WQI, however they are developmentally appropriate and meet the objective of introducing water quality.  These indicators can be monitored regularly and graphed. 

 

Observing indicators

 

    There are several ways students can observe a body of water and begin to interpret indicators of water quality.  Students can work in groups to make general observations about the appearance of water.  They may notice a foam in the water.  Foam can be either from natural causes or man-made causes.  Excessive soaps and detergents will produce foam.  Generally, this foam will not easily break up, is more than 3 inches tall and resembles bubble bath.  Natural foam is not as tall as detergent foam and if it stirred with a stick will break apart.

 

      Students can make observations about the color of the water.  Many times we look into a body of water and notice a color.  However, either the color beneath the surface or reflections from the sky generally influence such observations.  Students can guess what color the water is by looking into the body of water.  Then they can take a sample in a clear container and compare the color with their prediction.  (It may be helpful to hold a piece of white paper behind the container to get an accurate idea of the color.)

 

     Color can indicate many things about water.  Brown colored water is generally the result of runoff and sediment in the water. Water that is more tea-brown in color can be natural due to tannins released from leaf litter.  Grey water is often indicative of high levels of sewage in water.   Green water can indicate excessive algae growth.

 

     Students can also look for obvious signs of plant or animal life and ways in which humans have altered the area.  Plants are an accessible way for students to begin to make conclusions about the overall health of a body of water.  Too many plants in the water may indicate that fertilizers washed into the water.  Fertilizer runoff can lead to excessive growth of algae and other aquatic plants (algal blooms).  Algal blooms can in turn affect animal survival in the water.  As previously mentioned, an algal bloom can be identified when algae in water becomes so dense that the water is colored green.  


 

Turbidity

 

     Students can look at a body of water and make observations about the clarity of the water.  The measure of the cloudiness of water is called turbidity.  Matter that is suspended in the water (silt, clay, microscopic life) causes turbidity.   Excessive long-term turbidity can cause problems for aquatic organisms because it changes the amount of light that can penetrate the water.  If you are examining slow moving deep water, students can use a devise called a Secchi disk to evaluate turbidity.  This simple device is a black and white disk on a string that is lowered into the water until you cannot see it anymore.  A Secchi disk can be made using a compact disk and black and white paint (waterproof paint!), and then attaching rope.  There are measurements on the rope of the Secchi disk that represent the water depth.  The measurement of the depth (in meters) at which it is no longer visible is called the “Secchi depth”.  If your class is analyzing quick moving shallow bodies of water, a Secchi disk will not work.  There is a tool called a turbidimeter that is used to measure turbidity in these instances.       

 

     Regardless of whether or not you actually measure turbidity with your students, it can be interesting to analyze water cloudiness with your students.  Why might the water be cloudy?   There are numerous reasons, including soil erosion (possibly due to construction), bottom-feeding fish stirring up sediment, recent rainfall or flooding, excessive algae, point source pollution, and more.  Students can examine the environment of this component of the watershed and investigate potential sources of turbidity.  Students can try to describe the turbidity using the following scale of “clear”, “cloudy”, or “murky”. 

 

 

·        Clear indicates it is easy to see the bottom,

 

·        Cloudy indicates that more than 4 inches below the surface can be seen but not the bottom,

 

·        Murky indicates that less than 4 inches below the surface can be seen.

 

Temperature 

 

     Temperature of water is very important when studying water quality.  The temperature of water effects the life that can live there.  One reason for this is that warmer water has less oxygen, and colder water has more oxygen (gases are more easily dissolved in cool water). Depending on the ability level of your class, you might begin by having students brainstorm ideas about how water temperature could be an indicator of different kinds of life in the water.  There are actually state temperature requirements for areas considered “cold water fisheries” based on the fact that more desirable fish, like trout, prefer the higher oxygen habitats that occur in colder water.  Temperature also has an effect on the rate of photosynthesis of aquatic plants and the metabolic rates of aquatic animals.  In addition, the life cycles of many insects are connected to water temperature changes through the seasons. 

 

     Discuss the relevance of taking surface vs. bottom temperature of water and analyze why at various times of the year, and even at various times in a day, these temperatures may be distinctly different.  If possible have the students take the air temperature first and try to predict what the water temperatures will be.  You may also want to revisit the same location several times in one day, or at various times in the week to look for changes in temperature.

 

     Provide your students with thermometers and review how to read them.   The thermometers should be suspended on a string so that they are easy for children to lower into the water.  Students should spread out and take water temperatures in different areas of the water.  Keep in mind that temperature readings change quickly when thermometers meet with the air.  Discuss the locations and temperature readings recorded at each.  Does the water temperature change in different locations? Your class may decide on ways to determine the average temperature of the water.   What do your results tell you about the level of oxygen in that area?  What do theses results indicate about the kinds of life that may be present in that area of the stream?  Is the temperature in a stream similar to that in a pond at the same time of day?  Why or why not?

 

     Many factors affect water temperature and some are more obvious than others for students.  Plants that are near the edge of the water provide shade and help keep temperatures cooler.  Surfaces that are paved will have the opposite effect.  These paved surfaces heat up quickly and the rainwater that runs off becomes warm quickly.  Another reason for higher temperatures is industrial usage.  Some industries use water for cooling and then return it to a body of water.  This returned water is much warmer than the surrounding water.  This is referred to as “thermal pollution”. 

 

Benthic Macroinvertebrate study

 

     An exciting way to engage students in thinking about the health of a body of water is to begin a benthic macroinvertebrate study.  “Benthic” means bottom-dwelling and “macro” means able to see with the unaided human eye; invertebrates are animals without backbones.   These are aquatic animals that crawl upon or attach themselves to the substrate at the bottom of a body of water.  This type of study is also referred to as “biological monitoring”.  It refers to the collection, identification, and analysis of macroinvertebrates to determine the health of a body of water. 

 

     Macroinvertebrates are an indicator of water quality partly because they cannot easily escape pollution by swimming away the way a fish can.   Also, in many types of habitats there are certain species that are more sensitive to changes than others (as in the canary in the coal mine scenario).  Many macro-invertebrates are extremely reactive to such changes in water quality.  Consequently, the types of organisms counted can be compiled into a biotic survey, which can indicate the health of a stream or river. 

 

     Water quality can go up and down quickly and this may not always be caught with other types of sampling.  If, for example, pollutants are being released into a flowing body of water during the night, it may not be obvious with other types of testing the following day.   However, the types of living macro-invertebrates will change in such a situation.  Benthic surveys are most commonly done with streams or rivers, although you can certainly sample the life in any wet area to gain an understanding of aquatic invertebrates living there.        

 

     Students will need nets, buckets, white plates, pencils, paper, classification sheets (see appendix 2), small spoons or stirrers.  You might also want to bring magnifying lenses, blank paper to record and sketch observations, and field guides.  Students use their nets to strain through the water and more importantly, the sediment at the bottom of the stream.  (Be sure to stress basic rules for examining live animals!)  Students may assume that there is “nothing” in their water/sediment sample.  Explain that when the sediment settles, they might see different macroinvertebrates moving around.  One way to be most successful in discovering macroinvertebrates in a sample of mud is to simply set down the container and leave it undisturbed for a minute.  If students look closely they may see movement first and then notice the animals.

 

     Your students can form small groups to explore the samples and examine them for any species.  When each group has examined the sample they should tally the number of species that they find in their sample. Individual student lists can be saved to compile into a class tally sheet.  The classification sheet in the appendix has sample animals that are separated into three categories.  Group 1 Taxa can only be found in good quality water as they are very sensitive to pollution.  Group Two Taxa can be found in fair quality water, as they are more tolerant of pollution, and group three Taxa can be found in any quality of water. 

 

     Some key questions include:  What do the results tell the students about the water?   Would there be different results at different locations?  Would a pond have different animals from a stream? If you have microscopes available you may also look at the microinvertebrates in a water sample and make comparisons between the micro and macroinvertebrates in the water.  Return the animals safely by gently lowering the container into the water and tilting it to let the animals out.  Samples should not be kept out of water long because of the stresses of temperature change. 


 

pH

 

     When we measure the “pH” of water, we are measuring the hydrogen ion concentration of the water.  A measure of 7.0 is completely neutral.  Anything less than 7.0 is acidic and more than 7.0 is basic.  Each whole number difference in the pH scale represents a change of 10 times.  For example, a pH of 4.5 is 10 times more acidic than a pH of 5.5.  pH is important to consider when testing water because many plants and animals can only live in certain ranges of pH and are susceptible to sudden changes.  Most aquatic animals need water with a pH in the neutral range between 6.5 and 8.3.  Consequently, water with a pH in this range has the greatest diversity of life. 

 

     There are several reasons that pH may change, but acid rain is the main reason that students will be familiar with.  Acid rain occurs when atmospheric moisture mixes with gases that cause the moisture to be more acidic than normal.  This is often due to burning of fossil fuels (particularly by industries) and exhaust from cars.  The Berkshire environment can adapt to some acid rain  because there is naturally occurring limestone in the soil, which has a basic pH.  The basic pH of the limestone counteracts the acidity.  However, some plants and animals are highly sensitive to acidity and can be harmed by increased acidity.   Changes in pH can also be due to road salts being washed into the water (salts are basic) and certain bacterial activity. 

 

     To measure pH, collect water as far from the bank as possible and below the surface of the water.  One method to test pH uses pH paper strips.  These strips are inexpensive and easy to use, though not always accurate.  Simply dip the strips into water and look for a color change.  Compare the color of the strip to the chart on the side of the container to determine pH.  Students can also dip pH strips into a common acid (such as vinegar) and a common base (such as baking soda) to see changes.  “Alkalinity” is the acid neutralizing capacity in a substance.  There are test strips that measure alkalinity as well.  Older students might also look at ways that alkalinity buffers the environment against acid rain.

 


 

Velocity

 

     The intensity of the current of a stream or river is controlled by four factors: its depth, the slope of the land, the width of the water and the roughness of the bottom.   A combination of the velocity of moving water and the volume of the water contribute to the water’s flow.  The flow of a body of water affects the concentration of a variety of substances in the water, including dissolved oxygen and pollutants.  It also affects which animals can live in the water, as not many types can adapt to fast flowing water.  Students can measure flowing water by measuring a length of 25 feet along the edge of a river or stream.  Place an orange on the water and time how long it takes to float the 25 feet.   The formula to determine the speed of the water is as follows: 

 

 

D = distance in feet

 

T= total time to float 25 feet in seconds

 

D / T = (number of feet the orange floated each second)

 

 

For example:

 

       If the orange floated 25 feet in 50 seconds the equation would be:

 

D=25 and T=50.  The result is 25 / 50 or 1 / 2.     The orange floated ½  foot (6 inches) each second.

 

     It is most accurate if students conduct this activity three times and then calculate the average velocity.  Once students have calculated the velocity of a stream or river, discuss some key questions: What does this information tell us?  Why would this information vary during the year? 

 

 

 

 

 

 

 

 


 

 

 

 

 

“We abuse land because we view it as a commodity belonging to us.  When we see land as a community to which we belong, we may begin to use it with love and respect.”

 

Aldo Leopold