Spring Lake Creek is located off of County road E in Sawyer County. The Spring Lake creek has a culvert that goes under County road E to Spring Lake. The culvert has the water flowing from Spring Lake into Spring Lake creek. With the road right by Spring Lake creek, one would think how much of the runoff from the road affect the water quality and invertebrate life. That is exactly the hypothesis a group from the Fresh Water Ecology class had come up with and wanted to experiment by testing two pools and two riffles. One set closest to the bridge and another away from the bridge. Historic events might have played a role in the conclusion of the experiment.
Introduction Spring Lake Creek can be found on county road E off of
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That mink ranch has caused DDT to runoff into Spring Lake from the mink farmers washing out the mink pens. That DDT runoff eventually made its way to spring Lake creek. (Heim, 2016). DDT is no longer legal in the United States of America since 1972. It was banned in the United States because DDT was very persistent in the environment and can travel long distances in the upper atmosphere (DDT Ban takes effect, 2015). DDT was first used in World War II to control typhus, malaria, and body lice (epa, 2015). Around the year 2000, The Wisconsin DNR washed out their firefighting foam in Spring Lake creek killing off many clams and possibly different kinds of species. It is also very possible that there were species in Spring Lake creek that are no longer in there due to that event (Heim, 2016). Spring Lake creek initially had beaver dams in it too. In the 1920’s, the beaver dams were removed by dynamite. Once the beaver dams started to show up again in the 1990’s, the beaver dams were removed manually (Heim, 2016). Spring Lake is also a part of Red Cedar lake watershed (Integraded resources management plan 2010, 2010).
Materials
Thermometer
D-Net
Pans
SICI Sheets
Waders
Methods The day the experiment was conducted was on April 18th 2016 at Spring Lake creek. Spring Lake Creek is located on county road E about less than a quarter mile from Williams road. In order for the fresh water ecology class to conduct
This is a map of the Conodoguinet Creek, where the 8-Orange team of East Pennsboro Middle School went yesterday to study the creek. The 8-Orange team, including myself was studying to see if the Conodoguinet Creek had any type of pollution. The reasons for us going down to the creek to test is the problems we have in Central, Pa. Some problems are the acid rain coming from the Power Plants down the road, and sometimes from Pittsburg, Pa also. Theres many more problems but these are the two main ones. We all split up into three groups which were, finding the velocity of the surface water, identifying the different critters there are in the creek, and testing the water for (phosphate, nitrate, and dissolved oxygen). It was incredible we all got different amounts of data.
Each person got to test either the phosphates, nitrates, dissolved oxygen, or the ph in the creek. Phosphates and nitrates are nutrients found in water due to fertilizers, decaying plants and bacteria. Dissolved oxygen is the amount of gaseous oxygen dissolved in the water. As we recorded our results, we discovered that the dissolved oxygen levels were very high, which is good because the higher amount of dissolved oxygen in the water, the healthier the creek is. The phosphates levels in the creek were all perfect zeros, which is great because having nutrients in the creek is not healthy. The nitrate levels were slightly higher, at 0.9. That is not bad at all, but it isn’t perfect, showing signs of pollution. The ph levels in the rocks were neutral, right at seven. If they were lower than 7, that would mean they have acids in them, and if they were higher than 7, they would have alkaline in them. Alkaline, or bases, neutralizes acids. The number of rocks that we found that neutralized acid was 65, and the number of rocks that did not neutralize acids were 29. This shows that about one-third of the rocks in the creek do not neutralize acids.
Beside these arguments, there is also a more quantitative side to the debate. The ecological detriments of the Glen Canyon Dam have been well-documented. Extensive changes were brought about in the Colorado River ecosystem by the construction of the Glen Canyon Dam. Most of these alterations negatively affected the functioning of the system and the native aquatic species of the river. The reduced supply and transport of
On October 6th 2015, the students of Mattawan’s AP Environmental class took a trip to the local stream of the Mattawan Consolidated Schools area. The purpose of this trip was to conduct a stream study to determine the health, conditions, and pollution levels of this small body of water. A multitude of factors came into play when making a judgement on the stream’s health, and making sure to take all of these essential points was crucial to the study. A variety of thorough experiments were conducted to help make this overlying conclusion, as many students adopted many roles in the study. Students used a physical survey form, water test data sheet, and taxa recording sheet to record their findings. Teamwork was essential in making sure all of this information could be found accurately and efficiently. The combination of all of the final results allowed the class to make a judgement of the stream’s state.
Either or both of those two things could have runoff from the land and drained into the creek. They are negative to the creek. Our results showed that the creek was containing little to no phosphate. The average number after 15 tests was just 0.3- zero being the best. Similarly, nitrate is a salt or ester, but it is made of nitric acid, containing the anion NO3. It is found in runoff from fertilized farms and treatment plants. The same process was used for testing nitrate levels. The average level out of eight tests was 0.8, which is a higher than phosphate but still relatively low. Both of those test results were very positive. It showed that the creek was low in eutrophication. Another chemical test is testing for dissolved oxygen. Dissolved oxygen is microscopic bubbles of oxygen (O2) that are in the water and there for aquatic organisms to breathe in, which is necessary for almost all organisms. The testing process was similar to that of nitrate and phosphate tests. After testing the water, we got an average level of 11.4. More dissolved oxygen allows for more gaseous bubbles for organisms to breathe in. Therefore, a higher number is better. Twelve is the highest level of dissolved oxygen possible. Thus, since 11.4 is very close to 12, the dissolved oxygen level was very good. Dissolved oxygen can be changed in a number of ways. First, stagnant, or not moving, water has a much lower level of dissolved oxygen. Also, hotter water has less dissolved water. Lastly, chemicals like phosphate and nitrate can cause the growth of algae (which will be discussed in more detail in paragraph three), taking away oxygen. Additionally, the students tested for acid rain pollution. The tests falling under the acid rain category would test for acidity or alkalinity in water. We took a pH test, which is a level expressing the
Exercise Lab 1. How much does temperature vary in large and small aquatic environments? Lab 2. What determines the water clarity of lakes, rivers and oceans? Lab 3. Where does the phosphorus go? Lab 4. How does human activity in watersheds affect the quality of lakes and rivers? Lab 5. Are the Great Lakes being influenced by the global greenhouse effect? Lab 6. How is the flow of the Red Cedar River influenced by the weather? Lab 7. What is the relationship between flow and turbidity in the Red Cedar River? Page 2 4 6 8 12 15 18
The spatiotemporal pattern of water quality in the Reedy Fork and Buffalo Creek watersheds exhibits a trend of river deterioration, mainly due to Fecal Coliform. Our study suggests that most of the pollution sources were related to human activities. Looking at table 2a to 5b, it is clear that, F.Col, coliform is the dominant parameter with the highest means in all the sites, both at the Reedy Fork and Buffalo Creek watersheds. However, there are higher mean values of this nutrient in the Buffalo Creek watershed than the Reedy Fork creek watershed. This is clearly visible by looking at the variation in mean variable concentrations for the individual sites through the years under study from the graphs.
Could you imagine what happened to translucent and glistened Florida’s springs? Florida was floating on the water, it has more than 900 freshwater springs (Guest, 2014). Unfortunately, many studies show there are several threats such as drawing out tremendous amount of water, and the absent of regulation laws, lead to Contamination of Florida’s springs, loose business.
So we can conclude that the creek is not polluted based on this evidence. The creek creature are mostly from group 1 and 2. Also, the creek water contains little to no nitrates and phosphates. The creek also contains a high amount of dissolved oxygen (9.8ppm to be exact) Lastly, the creek limestone neutralize acid rain. The pH of the water is also a healthy 7. After all this evidence we can conclude that the creek is not
Brooker Creek is the largest natural area in Pinellas County. It is a preserved area where most of the organisms are protected by the state and cannot be touched or taken. This hike had a durability of one hour and it consisted on walking the entire trail and observing the different ecosystems found at the preserve. In order to see the different wild organisms that get to call the preserve home, we had to walk for around two hours. Some of the organisms mentioned by the guide of the hike and seeing at the preserve were: Golden orbs spiders, Coffee plants, lichens, mosses, sable palms, palmettos, blue gray knatt catchers, red maple trees, ferns, and tupelo trees. Although these organisms are very different from one another they are all able to live at Brooker Creek because of the different environments it has and offers its inhabitants.
Some of battles fought by environmental activists from Austin, have been about protecting Barton Springs. Since creeks do get pollution feed into the springs, unregulated development around Austin is a threat to the aquifer that supports the springs. When a mining company made a proposal to develop 4,000 acres of land, including some along Barton Creek it resulted in a dramatic citizen response and eventually led to the Save Our Springs Ordinance in 1992, which still protects the land around the springs and aquifer.
The health of the Susquehanna River and Chesapeake Bay was found based on Biological (macroinvertebrates and wildlife) and Chemicals characteristics (pH, dissolved oxygen, phosphates, nitrates, etc.) as well as physical observations (amount of forested buffers, wetlands, etc.) Overall it was concluded that the health of the water was good to excellent. What was found was that many of the macroinvertebrates found in the water were sensitive or facultative, meaning the water quality was good enough for them to live in. Also, the level of ph, temperature, dissolved oxygen, phosphates, nitrates, and turbidity showed that the water quality was good. Finally, while we were canoeing down the Susquehanna River, observations were made on the land
Through our research we aimed to determine if there were any differences in water quality of both the north and south forks of Strawberry Creek. As time progresses and the environment changes it is important to keep track of how certain species are being impacted by these features, and how they cope with change. We hypothesized that due to the lack of pollution, the south fork will promote a greater diversity of macroinvertebrates. This was due to the fact that there was less runoff and trash that could be introduced to the water in the south fork, than there was in the north fork. We gathered data by analyzing the different organisms living in both forks. We collected a total of fifty vials composed of five organisms from each fork, and inspected them under microscopic view. After gathering data and identifying the different kinds of organisms living in the different forks we assessed whether the organisms from the samples could live in high or low resolution water. We also took a t-test to assess the probability of these differences being due to relevant factors or by chance. Our major findings suggest that organisms in the south fork showed a higher demand to living in cleaner water indicating that our hypothesis was correct.
As people began to realize the damage done by the pollution of the environment nearly fifty years had passed. By this time the contaminated tailings and toxins released from the smelters and chemical treatment facilities had reached an outrageous numbers. With the help of the great flood of 1908 these pollutants covered the Silver Bow creek banks from Butte all the way to the Milltown Dam. In 1911 the Anaconda Company began extensive cleanup efforts by implementing the use of warm springs ponds as a water treatment facility (Citizens Technical Environmental Committee, 4). These ponds were developed initially with the thought that they would be able to catch polluted tailings before they were able to reach the Clark Fork River. There was an estimated 2,400 acres of warm springs ponds built between the years of 1911 and 1959 (Citizens Technical Environmental Committee, 4). The settling ponds were created to hold the mining wastes, acting as a dam so that the metals did not end up in the Clark Fork River. The tailings are then covered over with lime to prevent them from leeching back into the environment. This series of warm springs ponds provides treatment to the water in such a way that the environment can cleanse the water of pollutants on its own instead. This treatment method is accomplished with the water being further cleansed as it is transferred from pond to pond. The
It was always the way. Waking from a comfortable sleep, knowing that the day ahead shall be busy – the details too far away in your sleepy brain to process – yet still craving sedation from waking life and a swift return to the soft, astral mountains of the dazed mind. Allow the emerging thoughts their extended moment of sedation, stroke the sleeping horse's head until its gentle lashes came together. Don't force the muscles to have to work hard just yet. So he gave in, or otherwise planned to, when something wicked struck him.