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Effects of global warming on the ecosystem
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Field of Mars Research Task
Introduction
The Field of Mars Reserve is a protected nature reserve situated in East Ryde, New South Wales. The reserve is regularly used to assist students and teachers with fieldwork, environmental education and education for sustainability and also acts as a recreational site for locals and tourists alike, providing walking tracks and parks. Two of the neighboring ecosystems within the reserve are the dry sclerophyll woodland of Sugarloaf Hill and the mangrove wetlands of Buffalo Creek Reserve. Dry sclerophyll forest covers much of the Field of Mars Reserve. The woodland of Sugarloaf Hill is a remnant ecosystem, which effectively refers to a patch of native trees, shrubs and grasses, leftover from the old bushland
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To ensure validity, measure abiotic factors including soil temperature, light intensity, soil texture, and soil pH
5. The method for measuring abiotic factors is shown below:
Recording Abiotic Factors:
Abiotic Factor
Method
Unit
Soil pH
1. Using the “saturated paste method”
2. Gather a teaspoon size sample of soil and sprinkle it on the white plastic tray
3. Remove any little bits of rock or stick or other organic leaf matter
4. Add 3-6 drops of indicator liquid and mix into a saturated paste
5. Dust the saturated paste with Barium Sulphate
6. After sixty seconds, the Barium sulphate powder will have developed a colour which can be compared to the colour chart to determine a pH scale
7. Dispose of waste in a waste bottle pH scale
Soil texture
1. Take a small handful of soil
2. Add enough water to make a ball.
3. Feel the ball with your hands to determine if it’s gritty (sand), silky (silt) or plastic/sticky (clay)
4. Roll out the ball and with your thumb gently press the soil out over your foreigner to make a hanging ribbon
5. The longer the ribbon the more clayey the soil is.
6. Once you have determined the feel of the soil (plastic, silty, sandy, or smooth) and made a ribbon, compare the length of the ribbon on the soil texture table to find out your soil
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Algae is a single celled organism that produces its own food. Fungi has its own form and structure but cannot produce its own food. Through the symbiotic relationship between the two, both organisms benefit. Fungi gets food from the photosythnesising algae which it otherwise would not be able to produce on its own. Most of the fungi in this relationship are not able to survive without an algal partner as it needs this food for survival. Through the relationship, the algae are able to inhabit the structure of the fungi and by cohabiting with the fungus, the algae can live in many different environments and extend its range
The sport of Pickleball was founded in 1965 in Bainbridge Island, a ferry ride from. When Congressman Joel Pritchard, William Bell, and Barney McCallum arrived home after a day of golf, they found their children restless, and tired of the “old” summer activities. They set out to create a game that would entertain them throughout the summer. Their ideas to create the game came from the hopes of creating a game that would be both challenging, but easy to set up and play. When the game first began, materials included ping-pong paddles, and a wiffle ball. Then, they lowered the net on their badminton court. As the game became more popular, people began to make their own paddles using wood jigsaws, and marine plywood. Today, over 100,000 people play Pickleball in the United States. According to Barney McCallum, the game was named, “Pickleball” after the Pichards’s dog Pickles who would often case and run after the ball when played.
* The ball -The ball has to se spherical. It has to be made of
Rovers discovered plenty of salts on Mars. Bright soil contains salts, including iron-bearing sulfates and light-colored soil mainly composed of silica are possibly originated from water. Deposits of closely pure silica in Gusev Crater may have developed when volcanic steam or hot water leached through the ground. These deposits found around hydrothermal vents are important for past habitability’s studies of Mars as Earth’s hydrothermal environments support microbial ecosystems.
The second step we took was to weigh the soil in both a wet state and a dry state. The group did this because we wanted to learn whether or not the soil would lose weight once it had been dried. The process was very simple, we measured several cups of wet soil until we were around the target weight we hoped to achieve (300 grams). After we were finished weighing the soil, we left it to dry in a windowsill for a day. Once we returned, we weighed the soil again.
...ively place the suspect or perpetrator behind bars. Analyzing soil compounds can be measured by the levels of organic molecules including n-alkanes, fatty alcohols and fatty acids, which are all found in the waxy outer layer of plant matter (Geddes, 2008). It basically states that compounds can remain in the soil for thousands of years, which explains that each area being tested has its unique organic profile.
Dinosaur Provincial Park (DPP) was established on June 27th, 1955 and is located near Brooks, Alberta in our country’s largest bad land (“Dinosaur Provincial”, 2014). The landscape has a unique habitat for bird biodiversity, and is the origin of the most dinosaur fossils ever discovered (“Dinosaur Provincial”, 2014; Evans, 2010). Dinosaur Provincial Park became a world heritage site of the United Nations Educational, Scientific and Cultural Organization (UNESCO) on October 26th, 1979 (“Dinosaur Provincial”, 2014; “Park research”, 2014). While the park management plan is in development, DPP is currently governed by the Alberta Government’s Provincial Parks Act (“Park Research”, 2014). The ecological values all Alberta provincial parks, and consequently
From looking at the results I can conclude that when the pH was 3 and
However, in order to measure the rates of reaction, sodium thiosulphate and starch are added. Sodium thiosulphate is added to react with a certain amount of iodine as it is made. Without the thiosulphate, the solution would turn blue/black immediately, due to the iodine and starch. The thiosulphate ions allow the rate of reaction to be determined by delaying the reaction so that it is practical to measure the time it takes for the iodine to react with the thiosulphate. After the all the thiosulphate has reacted with the iodine, the free iodine displays a dark blue/black colour with the starch. If t is the time for the blue/black colour to appear, then 1/t is a measure of the initial rate.
My group member Nigel and I had to collect samples from both areas that we had to test for our hypothesis. When we finally arrived at the Wabashiki Wetlands we went straight to the wooded area first. We then began to take samples of the soil using a small shovel. We had to test the pH levels of the sample as soon as we collected it. We did this by using the soil pH meter that was provided to us. Each of us had to take a sample so we could have more accurate data to support our hypothesis. While taking these samples we had to use an app on a phone that gave us the exact UTM coordinates of each sample. After we took samples from the wooded area we then proceeded to the old farmland area to conduct the same tests. We had to put these samples in small bags to take home and dry. By the beginning of next week our samples were dry enough to test for phosphorus, nitrogen, and phosphate levels. To test each soil sample ...
This project is important because different types of soil change the growth of plants, so with doing this experiment I could find which type is best. In the past, I have struggled to find a good soil where my plants grow fast. Finding which type of soil is best could help farmers and normal adults/students, including me, to grow their plants faster. This is important because growing plants faster can mean getting food faster.
I decided to experiment with pHs within the range pH 2 to pH7, as I
Ideal silt-loam soil composed of mineral particles, organic matter and pore space. One half of pore should be filled with water and air for the rest of pore fraction. This physical characteristic of soil can be measured and is expressed as bulk density, void ratio or porosity. The degree of soil compaction can be estimated by measuring these factors, compaction increase bulk density and reduces void ratio and porosity.
There has also been lot of research in building systems that can monitor and investigate soil fertility and nutrition levels. Soil fertility data with dynamic, spatial and temporal characteristics of soil are fed to the systems which then use data mining techniques to come to analyze and diagnose soil problems. Such information can be very critical for success of crop.
Golf balls are ever changing when it comes to small design elements. As with most sports equipment, manufacturers are always searching for the next innovation to try and make the perfect