Rise and fall

Rise and fall

THE LAST WORD Repulsive coffee What causes coffee grounds to dry into the pattern shown at the bottom of this coffee cup (see photo)? Last words past...

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THE LAST WORD Repulsive coffee What causes coffee grounds to dry into the pattern shown at the bottom of this coffee cup (see photo)?

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a clear space around them, then a very concentrated ring of fine material. A New Scientist article many years ago called “The thrill of the spill” (25 October 1997) explains this effect in detail. Simon Iveson School of Engineering, Faculty of Engineering and Built Environment University of Newcastle Callaghan, New South Wales, Australia

Rise and fall Why are the largest tide ranges in the world – of up to 17 metres – found in the Bay of Fundy, on Canada’s Atlantic coast?

n The coffee dregs essentially n To understand what happens consist of two components – very in the Bay of Fundy, start with a large coffee grains which remain hand basin half-full of water. Push settled in one place and very fine down on the surface on one side colloidal material that moves with the palm of your hand and with the liquid. Because of the water will rise on the other, surface-tension effects, the large after which it will slosh back grains retain a pool of liquid and forth like a liquid see-saw. around them. As this liquid By pushing down even more on droplet dries, evaporation happens preferentially at the edge “An incoming ocean tide effectively appears as of the droplet because it is more a huge wave advancing exposed. This creates a flow of towards the bay” liquid towards the edge which carries with it the fine colloidal particles. As a result, the majority each side at the same time as the level on that side is falling, of them end up being deposited the rise and fall of the surface at the droplet periphery, which will increase – and can be made to remains anchored in place overflow the rim of the basin. The some distance from the particle sloshing of the water has a natural until nearly all of the moisture frequency and your additional has evaporated. input resonates with it, increasing This explains the resultant the amplitude of the see-saw pattern of large particles, with

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wave. At the central axis of the basin the level remains unchanged, although water moves to and fro horizontally. Now imagine the basin cut vertically down that central axis and consider just half of it. The half that is left corresponds to the Bay of Fundy, the axis-edge marks

“If the bay opened into the Atlantic it would not have such tides, but it opens into the Gulf of Maine” the opening of the bay, and the missing half of the basin is replaced by the open Atlantic Ocean. An incoming tide effectively appears in the ocean as a huge wave advancing towards the bay. As it reaches the continental shelf at the bay’s opening it plays the role of the high half of the see-saw and happens to coincide with the low water level at the far end of the bay. By the time this wave has moved to the innermost section of the bay – raising its water level to a peak – the dip in the ocean surface corresponding to the low tide has reached the continental shelf. The exceptionally high tides occur because the successive incoming tides appear at nearly the same frequency as water sloshing into and out of the bay, just as happened in the wash basin. It is a resonance effect. If the Bay of Fundy opened directly into the Atlantic it would not have such high tides because the natural period of water moving to and fro in it would

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be only about 9 hours, which is not close enough to the 12.5-hour period of the tides to lead to significant amplification of the wave motion. However, the Bay opens into the Gulf of Maine and together they have a natural frequency of just over 13 hours. Richard Holroyd Cambridge, UK

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