Wednesday, 13 January 2016

Unit 4 sec 5.1 summarising a set of scientific measurements

Unit 4 sec 5.1 summarising a set of scientific measurements
13 January 2016
23:09

Gravity on the Earth’s surface is the downward force exerted on an object by the mass of the Earth. The size of this force varies slightly at different parts of the earth, in particular at different altitudes and latitudes. When an object is dropped, and that no other forces, except gravity are acting on it, it’s speed increases at a constant rate as it falls to the ground. At sea level, this speed increases by approximately 9.81m/s every second. This increase in the speed each second is now as the acceleration due to gravity, and it is denoted by the letter g. In SI units, g is measured in meters per second per second, which is written as m/s², so g= 9.81m/s².
 A group of experiments tried 2 measure g, based on the following 2 different methods:
ª    Free fall, where a ball bearing is dropped, and the time taken for rate to fall through a known height is measured.
ª    Pendulum, where period of swing of the pendulum (which is affected by the strength of gravity) is timed.
An interesting question arising out of this experiment is: which of these 2 methods give the better estimate for g? You are asked to investigate this, using the data that the experiment collected.
 At 1st glance, you may have noticed that there are some subtle variations in the measured of values of g. These variations are not necessarily associated with any geographical differences in g; we can assume that each experiment to place in the same location, so in theory the results should all be the same. In, the differences that we of the serve in the data can be ascribed to what is known as experimental error. Statistical analyses of repeated measurements, such as calculating the mean of the dataset of repeated trials is an important method for minimising the effects of experimental error in scientific experiments.
   2 features stand out from these summaries
in terms of location, the averages (i.e. mean and median) of the free fall data wipe closer to the truth value for g of 9.81m/s², then do the pendulum averages.
 In terms of spread, there is a much narrower spread for the freefall than for the pendulum data is calculated by any of the measures.

So, on the evidence of these summaries, the freefall experiment produced better results, since the average of the experimental values is closer to the true value of the results were more closely clustered together.

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