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| From | Serg io <invalid@invalid.com> |
|---|---|
| Newsgroups | sci.physics |
| Subject | Mechanics of the sandglass |
| Date | 2017-09-06 14:28 -0500 |
| Organization | Aioe.org NNTP Server |
| Message-ID | <oopibc$a7b$1@gioia.aioe.org> (permalink) |
https://www.inf.utfsm.cl/~amoreira/orzelc.pdf Summary (i) The traditional sandglass consists of two glass ampoules joined by narrow tapering necks or, in early examples, separated by a thin metal diaphragm pierced with a small central hole. 108 A A Mills et al (ii) The device constitutes an interval timer, the period being measured by the time elapsing between the inversion of the apparatus and the last grains leaving the upper reservoir. Although commonly called an hourglass, other periods (such as 1=4, 1=2 and 3=4 hour) were frequently delineated, so the term sandglass is preferred here. (iii) Unlike the ancient water-operated clepsydra, the sandglass is known only from medieval times. This is especially surprising when it is recalled that it is not liable to freezing. (iv) Historical sandglasses were always sealed as tightly as the technology of the time allowed, for moisture seeping in could cause caking of the filling and consequent irregular running. Air displaced by the descending grains must therefore rise as a countercurrent and percolate through the particulate bed in the upper reservoir. (v) The particles in a sandglass need not be silica sand, but should always be clean, dry, and sieved to be of closely similar size. (vi) Particles of a smooth spherical shape are best, promoting reproducibility even at low rates of flow. This requirement is most conveniently met nowadays by the tiny glass beads available in bulk as ‘ballotini’. (vii) To give a smooth and consistent flow without occasional partial or complete blockage, the aperture through which the ballotini fall should be at least 4 their maximum diameter. (For particulate material in general, 5 the maximum grain dimension would be safer.) (viii) The rate of flow is independent of height in the reservoir, except over the last few cm. (ix) The emptying period is independent of the density of the particulate filling, provided that its total volume is the same and the shape, size and surface characteristics of the grains are identical. (x) The period P delineated by a sandglass is controlled by the shape of the vessels from which it is made, the diameter of the aperture separating them, and the nature and volume of the particulate material sealed within it. (xi) For spherical ballotini passing a sieve of maximum aperture d mm, it was found that: P / V .D − d/2:5 where V represents the volume of ballotini in ml and D is the diameter of a circular orifice in mm. (Alternatively, a value of d given by 1:3 the mean bead diameter may be employed.) (xii) The shape of the reservoir containing the ballotini is reflected in the constant of proportionality to be applied to the above expression to give P in seconds. For ‘hourglass’, ‘cone’, ‘silo’ and ‘annular shelf’ designs K is 7–10, 8, 19 and 21 respectively. (xiii) The above characteristics are the result of internal flow regimes in the particulate filling that are quite different from the flow of true liquids. Sandglasses are normally required to be slow-running and therefore exhibit ‘plug-flow’—a situation where a continuously collapsing arch over the exit aperture generates a channel above it that is continually replenished by the flow of particles from the sides. A circular crater is thereby generated in the upper reservoirwhile a matching cone grows in the receiver. Their angles are controlled by the ‘angles of repose’ of the particles (25 for ballotini). Internal flow patterns in reservoirs of various shapes have been illustrated by sequential photographs of 2-D perspex models containing marker bands of coloured ballotini. (xiv) The reproducibility of a 19 m 45 s glass containing a ‘traditional’ annular orifice 2.8 mm in diameter was found to be 5 s.0:4%/ if it was allowed to run without disturbance. (xv) The period of a sandglass was lengthened by any disturbance, but was essentially independent of temperature up to 100 C.
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Mechanics of the sandglass Serg io <invalid@invalid.com> - 2017-09-06 14:28 -0500
Re: Mechanics of the sandglass benj <benj@nobody.net> - 2017-09-06 18:12 -0400
Re: Mechanics of the sandglass Serg io <invalid@invalid.com> - 2017-09-06 19:09 -0500
Re: Mechanics of the sandglass "reber G=emc^2" <herbertglazier0@gmail.com> - 2017-09-07 14:40 -0700
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