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Measuring the Dimensions of Natural Objects James Cahill
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Background This project is aimed at measuring the dimensions of seemingly one-dimensional objects like cracks, rivers and coastlines. For objects such as rivers, we will ignore the area of the river and consider it to be a single line, as found on a map or as seen from really, really far away.
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Process Box Counting Method – Place object in a single large box that leaves little to no extra space on the ends. – Apply a grid with smaller boxes over object, and count the number of boxes the object is in. – Repeat the second step with increasingly increasingly smaller boxes, and least twice more.
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The Math The number of boxes = N The scale factor (s) = Big box / Little box Plot graph with log(N) on the y-axis and log(s) on the x-axis. Create a best-fit line of the points. The slope of that line is the dimension of the object.
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But Does It Really Work?
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N=1 S=1 N=5 S=5 N=10 S=10 N=20 S=20
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The Line is 1.000 Dimensional!
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Canacadea Creek, Alfred
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Cloud in Sunny Alfred Sky
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Crack in an Alfred Sidewalk
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A Leaf from October Tree
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SO WHAT WILL THEY BE?
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N=1 S=1 N=17 S=11.02 N=38 S=20.84
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N=116S=60.8
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The Creek is 1.166 Dimensional
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N=1 S=1 N=31 S=19.32 N=17 S=11.33
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N=74S=32.85 N=121S=54.75
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The Cloud is 1.206 Dimensional
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N=16 S=12.24 N=1 S=1 N=35 S=25.34
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N=75S=52.75
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The Crack is 1.092 Dimensional
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N=1 S=1 N=26 S=13.08
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N=68S=30.41
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N=129S=54.73
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The Leaf is 1.222 Dimensional
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1.1661.206 1.2221.092
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The box counting method is a slow, painstaking, but all together fairly accurate way to find the dimensions of natural objects. The idea behind it is that we take and average of the smaller and larger N values, and hope that it smoothes out any wrinkles in the results. Unlike mathematical fractals like the Koch Curve, our rivers and cracks lose definition at high magnification, so there comes a point when smaller S values are completely pointless, as the boxes are smaller than the thickness of the line we are examining. Concludatory
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