Water Quality

Water Quality was a Division B and Division C event that last ran in 2014, which tested students' ability to identify marine coral reef indicator organisms and to test students' knowledge on indicators affecting estuarine and marine water quality. Topics that may be included in the testing are aquatic ecology, the water cycle, nutrient cycling, aquatic chemistry, potable water treatment, waste water treatment, aquatic food chains and webs, community interactions, population dynamics, watershed resource management issues, sedimentation pollution, harmful species, marine biology and ecology, coral reef flora and fauna (as well as general ecology) and estuary ecology.

The Basics
Water quality includes the physical, chemical and biological characteristics of water. In countries around the world, especially in the U.S., standards are set to determine whether water is potable, or safe to drink, under the direction of the EPA. This year's Water Quality event deals with estuary and coral reef ecology, replacing the freshwater ecology of last year.

The Water Cycle
For more information on the Hydrologic Cycle (water cycle), please see the Hydrologic Cycle main page.

Marine Indicator Species
For a list of indicator species from years prior to 2014, please see Water Quality/Macroorganism List.

The teams must be able to identify several marine coral reef health indicator species. These species have been grouped into categories based on where they indicate unstable coral reefs (Global, Indo-Pacific and Atlantic) as well as what factor has caused this organism to disappear (overfishing, blast fishing, poison fishing, aquarium fish collecting, nutrient pollution and curio collection). Teams should be able to identify the organisms by sight and also by some of the organisms' characteristics.

Each team is also responsible for knowing these same facts about the following plant and animal Invasive Species

Wastewater Treatment
Wastewater treatment is a process used to convert wastewater into an effluent that can be returned to the natural water cycle without a significant impact on the environment. Sometimes, the water is also directly reused (called water reclamation).

Treatment in the US costs $12 billion a year, and is expected to double in 10 years.

Septic-Tank Disposal Systems: This is the conventional method for treatment. A sewer line from the house leads to an underground septic tank in the yard. This tank is designed to separate solids from liquid, digest and store organic matter, and allow the treated sewage to seep into the surrounding soil. As the wastewater moves through the soil, it is further treated by the natural processes of oxidation and filtering.

This method can fail if the tank isn't pumped out when it's full of solids or if there is poor drainage in the surrounding soil.



Wastewater Treatment Plants: Raw sewage is delivered to the plant through a network of sewer pipes. Following treatment, the wastewater is discharged into rivers, lakes, or the ocean.



Wastewater treatment is divided into three categories: primary, secondary, and advanced. Primary and secondary treatment is required by law for all municipal plants in the US. When secondary treatment isn't enough to clean water, advanced (tertiary) treatment is used.

Potable Water Treatment
Potable water treatment is the process by which lake or river water is made drinkable by humans. There are six steps: Coagulation, Flocculation, Sedimentation, Disinfection, Filtration and Distribution.

Nutrient Cycles/Biogeochemical Cycles
This event covers nutrient cycles such as the carbon, nitrogen and phosphorous cycle for land and marine ecosystems.

Analysis
A major part of Water Quality deals with the analysis of a particular body of water, such as a stream, for different properties. These properties include salinity, pH, alkalinity, phosphates, nitrates, turbidity, dissolved oxygen (DO), temperature, fecal coliform, total solids, and biological oxygen demand (BOD). Students should know acceptable levels of each of these factors for estuary ecosystems and how each of these factors rise and fall based on the characteristics of the body of water and what is entering the water. The Water Quality Index used to determine the overall quality of a certain body of water based on the above factors should not be used.

Salinity
Salinity is a property of water, which describes its salt concentration. Salinity is measured by dissolved salts in parts per thousand (ppt) or grams of salt per kilogram of water. These two quantities are equivalent. The category of salts include compounds such as sodium chloride, magnesium sulfate, potassium nitrate, sodium bicarbonate, and others, all of which dissolve into ions. Salinity governs the physical properties of water, such as density, heat capacity, and electrical conductivity. As such, salinity is often measured by water density or conductivity, especially the latter. Water with constant salinity is called homoiohaline. Environments in which salinity varies over time are called poikilohaline. Poikilohaline salinities may range as much as from 0.5 to greater than 300.

Bodies of water can be classified by salinity in the following manner. Hyperhaline waters are waters with a very high salinity. Metahaline waters have a salinity between 45 and 65 ppt. Euhaline waters (typical oceans) are waters with a salinity between 30 and 35 ppt. Polyhaline waters have a salinity between 18 and 30 ppt. Mesohaline waters have a salinity between 5 and 18 ppt. Oligohaline waters have a salinity between 0.5 and 5 ppt. However, depending upon the type of body of water, different classification systems with different terms or the same terms meaning different things are sometimes used.

Water can be classified by its salinity as such: fresh water has a ppt of <0.5, which means that there are 0.5 molecules of dissolved salt for every 1000 molecules of solution, or 1 molecule of salt per every 2000 molecules of solution. Brackish water has a ppt between 0.5 and 30, saline water has a ppt between 30 to 50, and brine has a ppt of >50. The only water safe for human consumption is fresh water, and drinking water often achieves salinity levels as low as 0.1 ppt. In ocean water, total salt content makes up 3.5% (35 ppt) of ocean water, the other 96.5% being water. Of the dissolved salts in ocean water, 85% of the salts is sodium chloride (3% of all the water, 30 ppt). The other 15% of the total salts are other salt ions such as Magnesium, Strontium etc. (.5 % of total ocean water, 5 ppt).

Salinity is an important water quality factor. It influences the type of organisms that live in bodies of water, and high salinity will kill organisms not adapted to withstand those conditions. Salinity in rivers and lakes of the US has recently been increasing due to road salt and other salt de-icers in runoff. It is very expensive to remove salt from water, and thus it is expensive to create drinking water from saline water or to reduce the salinity of hyperhaline waters. Ocean salinity helps cause the circulation of the oceans due to the density changes of the water. Changes in the salinity of the oceans are though to influence global carbon dioxide levels due to changes in the solubility of the water, which also influences climate change.

Constructing a Salinometer
In order to test salinity, your team must construct a homemade salinometer/hydrometer capable of measuring saltwater concentrations from 1-10%. Typically, this section will be worth about 5% of the test. The vast majority of salinometers are based on the principles of density and buoyancy. Since saline solutions contain dissolved NaCl, their densities are higher than that of distilled water. Due to the elevated density, the solution exerts a higher buoyant force, causing the hydrometer to float higher than in distilled water. There is a direct relationship between salinity and and buoyant force - the more saline the water, the higher your hydrometer will float.

To make a rudimentary salinometer, get a drinking straw and some clay. Place a ball of clay on one end of the salinometer, completely covering the opening of the straw. Then make some solutions of water and salt, with the salt concentration being between 0% and 10%, and mark the meniscus of the water solution on the straw with a permanent marker, Sharpie, etc. Repeat for any number of solutions for a more accurate calibration. The amount of clay and the length and diameter of the straw affect the distance between marks on the salinometer.

Note that this is not the only way in which to make a salinometer, and you may create and invent ways to do it yourself.

Aragonite
A new indicator this year for marine ecosystems only. This measures the amount of calcium carbonate in marine water, a nutrient necessary for coral reef growth. Aragonite itself is the mineralized form of calcium carbonate. Under normal conditions, aragonite saturation cannot exceed 1 Ω (the omega is used for the amount of Aragonite saturation), but under special conditions such as where the temperature is higher, the water can become supersaturated with Aragonite. The amount of Aragonite saturation optimal for coral reef growth is 4 Ω, which is found near the equator because the water is warmer and can therefore hold more Aragonite.

pH
The pH is a measurement of the hydrogen ion concentration in a substance, or the acidity or basicity of a substance. It is a logarithmic scale, meaning that a given pH level has 10 times the concentration of hydrogen ions as the pH level that is one greater than the given level. A pH less than 7 is acidic, and a pH of greater than 7 is basic. A pH of 7 is neutral. Extremely strong acids or bases can have pH levels below 0 or above 14. pH can be calculated as the negative base-10 logarithm of the molarity of hydrogen ions, measured in moles per liter.

pH is an important water quality indicator because organisms can only tolerate water that is not too acidic nor too basic. The normal pH of rivers in the United States is 6.5 to 8.5, and values between 6.0 and 9.0 can support life for fish and invertebrates. This makes acid rain an important factor in water quality, since it will make water more acidic, and once the pH value approaches 6.0, negative effects begin to appear. The natural environment of an area can also affect pH. Limestone is a base when dissolved in water, so it can neutralize the effects of acids. Volcanoes, geysers, and hot springs will make water more acidic, as well as the presence of sulfur in nearby minerals.

Alkalinity
Alkalinity is the ability of a solution to neutralize an acid without changing the overall pH of the solution. Alkalinity arises from the presence of buffers in solutions, which have the properties to neutralize acids without changing the pH of a solution. Buffers consist of a solution of a weak base and its conjugate acid or a weak acid and its conjugate base. In the case of a weak acid and its conjugate base, when a strong acid is added to the system, the hydrogen ions cause the equilibrium of the system to shift left, away from the hydrogen ion, in accordance with Le Chatelier’s Principle. Thus, the pH of the solution would not increase as expected from the introduction of the acid. In the case of a weak base and its conjugate acid, the hydrogen ion reacts with the hydroxide ion formed from the water in the system and the weak base, creating more water and leaving behind the ions from both the strong acid and the weak base which do not affect pH. There are several ions that contribute to alkalinity, including bicarbonate, carbonate, hydroxide, and phosphate. Thus, limestone contributes to alkalinity, since its formula is calcium carbonate, and carbonate is one of the ions listed above.

Alkalinity is very important to water quality. Alkalinity in aquatic ecosystems needs to be within a certain range, depending upon the ecosystem. If alkalinity is too low, the ecosystem has low stability as it is susceptible to sudden pH changes from devices such as acid rain or other pollution, which can be harmful to the flora and fauna of the ecosystem. If alkalinity is too high, the buffer acids and bases in the buffer solution can render the ecosystem uninhabitable.

Phosphates
Phosphates are able to enter waterways in a variety of natural ways such as rocks or normal animal and plant waste in the water. Human sources such as fertilizers, pesticides, industrial and cleaning compounds, septic tanks and wastewater from sewage treatment can increase the amount of phosphates in the water. The phosphates of a river or stream are usually measured in Parts Per Million (ppm).

Nitrates
Ammonia is oxidized to form nitrates. Some human sources that can add to the total amount of nitrate in the water are fertilizers, poorly functioning septic tanks, inadequately treated wastewater from sewage treatment plants, manure from farm livestock, animal wastes including fish and birds, storm drains, runoff from crop fields, parks, lawns, feedlots and car exhausts. Nitrates, like phosphates, are test in Parts Per Million (ppm).

Turbidity
Turbidity is a measure of the cloudiness or haziness in a fluid caused by large numbers of individual particles. It can be measured in Formazin Turbidity Units (FTU), sometimes referred to as Formazin Nephelometric Units, or FNU. This is measured through the ISO 7027 method, which determines the concentration of suspended particles by measuring the incident light scattered at right angles from the sample. The light is captured by a photodiode, which then produces an electronic signal that is converted to a turbidity measurement. Jackson Turbidity Units (JTU) are also used. These are measured through the Jackson Candle Method, in which a candle is shined through a column of water and the length of water needed to completely obscure the light source is measured. The longer the column, the lower the turbidity of the sample. Nephelometric Turbidity Units (NTU) are also used. These are a measure of the tendency of particles to scatter a light beam that is focused on them. A nephelometer includes a light source shining at a column of water and a detector surrounding the column to the sides. The more light that reaches the detector, the more particles are in the water. To test the turbidity of the water, people also use a Secchi Disk. A marine Secchi disk is a plain white disk 30 cm in diameter and a freshwater Secchi disk is divided into fourths, two of which are white and two of which are black, and is 20 cm in diameter. The Secchi disk is mounted on a pole or line and lowered slowly into water. The depth at which the disk is no longer visible is the measure of the turbidity of the water. When measuring, this depth is usually reported in feet to the nearest tenth of a foot, or meters to the nearest tenth of a meter. Light can penetrate to a depth of about 2-3 times the Secchi Disk depth. The Secchi disk is not always accurate because of differences in eyesight and the sun’s glare, among other factors.

Seasonal variations can change the turbidity of a lake and lake turnover can also change it because of nutrients being released. Other sources of turbidity include gasoline or oil from roads, benthic organisms stirring up sediments, industrial wastes, and urban runoff. Effects of turbidity include an increase in water temperature, decrease of photosynthetic rate, decreased growth, and more aesthetically displeasing water. Turbidity can also reduce the ability of fish gills to absorb dissolved oxygen. However, in some areas, high turbidity is necessary for ecosystem health and High levels of turbidity in drinking water corresponds to increased risk of development of gastrointestinal diseases. Turbidity can also shield bacteria from certain types of sterilization of water.

The standard of turbidity for drinking water in the United States for systems using conventional or direct filtration methods less than 1 NTU at the plant outlet. All samples for turbidity must be less than or equal to 0.3 NTU for at least 95 percent of the samples in any month. Other systems must follow state limits, in which turbidity must never exceed 5 NTU. Many drinking water utilities strive to reach levels of turbidity as low as 0.1 NTU. The World Health Organization establishes that the turbidity of drinking water should not be more than 5 NTU and should ideally be below 1 NTU. The US Environmental Protection Agency has also published water quality criteria for turbidity. These criteria are scientific assessments of the effects of turbidity, which are used by states to develop their own water quality standards.

Dissolved Oxygen
Dissolved Oxygen (DO) is the amount of oxygen that is dissolved in a substance. DO is an important water quality indicator, as fish and other aerobic organisms require it for life. DO is usually measured in mg/L or ppm. These two quantities are equal. Percent dissolved oxygen is dependent upon many factors besides these, such as salinity and temperature. Most surface waters contain between 5 and 15 ppm of dissolved oxygen. If a stream or river has below 5 ppm of dissolved oxygen, then that can put aquatic life under stress, and below 1-2 ppm for a few hours can kill large fish living in the river. Should anoxic conditions continue for too long, the population of anaerobic organisms will increase relative to the population of aerobic organisms. Supersaturation of oxygen (levels of DO over 100%) can occur naturally through photosynthetically active species. Supersaturation can also occur through rapid changes in the environment that occur too quickly for the system to reach equilibrium, giving rise to DO levels over 100% temporarily. Supersaturation can also be harmful to organisms and can cause decompression sickness. Two very important factors are temperature and atmospheric pressure. Lower temperatures and higher atmospheric pressure will result in higher levels of dissolved oxygen. When dissolved or suspended solids are present in the water, this can reduce the effectiveness of dissolving of oxygen in water and can be problematic for organisms living in the water. Dry periods can lower stream discharge and raise water temperatures. From night to day, DO will fluctuate dramatically. When algal blooms are present, they can cause large fluctuations in DO through the night especially in areas where there is not much current for aeration. DO fluctuation can be caused by humans in a number of ways. These ways include sewage discharges or other dumping, agricultural run-off, or over-baiting a fishing lake. DO enters the water by means of diffusion from the atmosphere, aeration from wind, waves, and as water moves over rocks and debris, and photosynthesis of aquatic plants. In areas with low levels of DO, some method of water aeration can be crucial to the stability and success of the environment. To achieve this, air can be infused into the bottom of the body of water or the surface can be agitated to allow oxygen exchange at the surface and the release of other unwanted gases in the water. An increase in dissolved oxygen can contribute to increased amounts of fish and other aquatic organisms and generally increase the health of the ecosystem.

Biochemical Oxygen Demand
The biochemical oxygen demand (BOD) measures how fast organisms use up the oxygen in the water. Aerobic microbes use oxygen to oxidize the organic matter in the water, using the energy that is released in the process for growth and reproduction and creating a demand for DO. This is usually proportional to the amount of organic compounds available for oxidation as the microbe population is usually proportional to the amount of organic compounds. BOD is tested using the means for testing dissolved oxygen, but the test is done over a period of time to determine the rate of oxygen being used. When doing this, water aeration and other methods of increasing DO must be accounted for. Oxygen used for decomposition processes rob other organisms of oxygen needed to live. Organisms with low tolerance may die off and be replaced by organisms with more tolerance for low oxygen levels. In some cases, microbes in an environment use oxygen faster than it can enter the water. In these cases those organisms are threatened, as the DO content of the water will eventually become too low for those organisms to live, also resulting in the deaths of fish and other organisms. Despite the population limits imposed by this demand, this can result in long term DO shortages. BOD can be considered a measure of the pollution in rivers and other bodies of water in some cases. Most pristine rivers should have a 5-day BOD below 1 mg/L. Moderately polluted rivers may have a BOD between 2 and 8 mg/L. Municipal sewage that is treated with a three-stage process would have a BOD of about 20 mg/L. Untreated sewage has varying BOD but averages about 200 mg/L in the US. This is much lower than the world average, because of the greater water use per capita than in other parts of the world.

Temperature
If the temperature of the water increases, this increases the sensitivity of organisms to disease, parasites, and pollution. When small changes in temperature occur in the stream, these can adversely affect the reproductive systems of aquatic organisms such as macroinvertebrates or fish. Temperature change can be caused by many things such as: natural seasonal changes, anthropogenic activities, industrial thermal pollution as discharge of cooling water, or storm water runoff from heated surfaces like streets. Soil erosion increases water turbidity and this will also increase the temperature of the water. The removal of trees and brush from the side of the river will not only increase erosion, but it will also increase the amount of sunlight that hits a river or stream.

Fecal Coliform
Fecal Coliform bacteria are living organism entering streams. If a stream has a high number of fecal coliform bacteria, then the water has had an increase in the input of fecal matter. Fecal Coliform concentrations are reported in the following format: Number of bacterial colonies/100 mL of sample water. When Fecal Coliform counts are over 200 colonies/100 mL of sample water, there is a greater chance of pathogenic organisms being present. Water with high levels of fecal coliform bacteria are associated with the following diseases: Dysentery, Typhoid Fever, Gastroenteritis, and Hepatitis. The primary sources of Fecal Coliform bacteria are from failing/leaking septic systems, animal waste, and the discharge from a water treatment plant. Urbanization can also cause problems with fecal coliform bacteria levels because plant and animal wastes can be washed away by a storm into sewers and contaminate water. When the temperature of water is high and the total levels of nutrients are high, this promotes bacteria growth.

Total Solids
The total solids of the water measures the suspended and dissolved solids in the body of water. Suspended solids can be retained on a water filter and will settle to the bottom of a water column and include silt, clay, plankton, organic wastes, and inorganic precipitates. Dissolved solids pass through a water filter and include calcium, bicarbonate, nitrogen, phosphorus, iron, and sulfur and other ions in the water. Concentration of dissolved solids in stream water is important because it determines the flow of water in and out of the cells of aquatic organisms. Many of the dissolved solids (nitrogen, phosphorus, and sulfur) are essential nutrients for aquatic life. Low concentrations of total solids can limit growth of aquatic organisms, while elevated levels can lead to accelerated eutrophication of the water system and increase the turbidity of the water. Both of these consequences decrease the overall water quality of the water. Sources of elevated levels of total solids may result as a result of runoff from agricultural activities, dredging, mining, salt from streets in winter, fertilizers from lawns, water treatment plants, plant materials, soil particles and soil erosion, and decaying organic matter. High concentrations of suspended solids can reduce water clarity, increase turbidity, reduce photosynthesis levels by reducing the sunlight that reaches plants, increase water temperature due to increased absorption of light at the water surface, and bind with toxic chemicals or heavy metals.

Competing
You may bring in one two-sided page of resource notes and 2 non-programmable/graphing calculators. You must bring Class C eye protection. You must also bring a salinometer as well to measure saline solutions between 0 and 10% salinity within a range of 1% at regionals and .5% at states and nationals.