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Saturday, April 6, 2019

Experiment to investigate what affects the size of a crater Essay Example for Free

Experiment to canvas what affects the size of a volcanic crater EssayHypothesis If the height of which the pendulum stumblebum is dropped join ons, then the depth of the crater will increase. There is a theory for this. A higher drop would mean that in that location is a greater gravitational potential energy. When the ball is dropped, all this energy is converted into kinetic energy and it is apply up to create a crater in the ground. Variables 1. Independent crown at which the pendulum ball is dropped from A one meter ruler is used to whole tone the height at which the pendulum ball is dropped from the surface of the smoothen. distributively height is recorded down and tabulated together with the results. 1.Dependent Depth of the crater A vernier caliper is used to measure the depth of the crater. Push out the bottom until it touches the center of the bottom of the crater. Adjust it until the edges of the caliper touches the surface of the sand. Read the measurement and record it down. Results are tabulated. 1. Controlled Height of the sand, Volume of the sand, diameter of the pendulum ball Height of sand is measured with the same ruler used in the look into and marked out with a marker. The volume of same is measured by pouring it into a beaker and then weighed on an electronic deliberation balance for further accuracy.The diameter of the pendulum ball was measured before the start of the experiment and noted down. setup 1. Pendulum Ball x 1 2. 1m Ruler x 1 3. Plastic box x 1 4. gritrock 5. 500ml Beaker x 1 6. Vernier Caliper x 1 7. Retort stand 8. Whiteboard stain 9. Tissue Method 1. Lay out newspaper on the bench/work area 2. meter out 250cm3 of sand using the beaker 3. Pour the sand into the plastic container 4. Smoothen the sand with a interweave so that it is leveled 5. Measure the height of the sand and mark it out with the marker on the container 6. Set up the rest of the experiment as drawn on the previous page.7. Hold the pend ulum ball at a height of 10cm with the bottom of it on the 10cm mark 8. Drop the pendulum ball onto the sand 9. Remove the pendulum ball carefully so as not to destroy the crater made in the sand 10. Using a vernier caliper, measure the depth of the crater 11. Record the reading down 12. Repeat steps 4-10 for high gear of 20cm, 30cm, 40cm, 50cm, 60cm, 70cm, 80cm, 90cm and 100cm 13. Repeat the whole experiment once ResultsHeight/cm Depth/cm 1st second Average Evaluation Reliability of method From the table of results, it can be observed that some results in the first set of info differ greatly from the second set. This shows that the current method is not passing reliable and changes can be made to improve the experiment. An improvement to the method would be to always measure the volume of the sand used and smooth it down to the marked level on the side of the container.Sand that is not compacted may have a different result from compacted sand. This is because between the partic les of non-compacted sand, there will be spaces of air. As the pendulum ball hits the surface of the sand, the kinetic energy will disperse into these spaces. Therefore, a smaller crater would be formed because the pendulum ball has less energy. Validity of method The method is valid because it measures what is required to be measured in the experiment. The method described above was also followed step-by-step. The volume of the sand and height of the sand is unchanged.The pendulum ball remained unchanged by dint ofout the course of the experiment as well. The vernier caliper measures the depth of the crater in centimeters and it is what the experiment is conducted for. Reliability of results There are a total of 20 sets of data. The number of data collected makes the results reliable. Also, the average of the data from both sets of experiments were able to form a straight line represent with an outlier for 100. 0cm at 1. 77cm. Therefore, the results of this experiment is somewhat reliable. Analysis The graph is a straight line with increasing gradient.It shows that with an increase in height, the average depth of the crater also increases. The line graph does not pass through the origin (0,0) because the graph paper is too small to accommodate 10 sets of results (average of both sets of data). Conclusion The results of the experiment support the hypothesis. When the height at which the pendulum ball increases, the depth of the crater also increases. This is proven by the position that the greater the distance between the ball and the ground, the greater the gravitational potential energy that the ball possesses.to a greater extent gravitational potential energy is converted to more kinetic energy when the ball is dropped. As such, there is more energy to cause a greater damage to the ground, or in this case, sand, therefore resulting in an increase of depth of the crater. Limitations and Improvements Limitations Improvements Pendulum ball does not drop str aight down directly from where it is released but deviates from its want path Drop the pendulum ball using a retort stand instead of by bridge player Removing the pendulum ball by hand Thread a string through the hole in the pendulum ball and lift it out of the sand using that.

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