<?xml version='1.0' encoding='UTF-8'?><?xml-stylesheet href="http://www.blogger.com/styles/atom.css" type="text/css"?><feed xmlns='http://www.w3.org/2005/Atom' xmlns:openSearch='http://a9.com/-/spec/opensearchrss/1.0/' xmlns:georss='http://www.georss.org/georss' xmlns:gd='http://schemas.google.com/g/2005' xmlns:thr='http://purl.org/syndication/thread/1.0'><id>tag:blogger.com,1999:blog-23490028</id><updated>2011-12-14T19:09:08.798-08:00</updated><title type='text'>Example from mecanics of the fluids</title><subtitle type='html'></subtitle><link rel='http://schemas.google.com/g/2005#feed' type='application/atom+xml' href='http://fluids-temps.blogspot.com/feeds/posts/default'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/23490028/posts/default?max-results=100'/><link rel='alternate' type='text/html' href='http://fluids-temps.blogspot.com/'/><link rel='hub' href='http://pubsubhubbub.appspot.com/'/><author><name>temps</name><uri>http://www.blogger.com/profile/10616520993625308918</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='25' height='32' src='http://www.letime.net/joris.jpg'/></author><generator version='7.00' uri='http://www.blogger.com'>Blogger</generator><openSearch:totalResults>1</openSearch:totalResults><openSearch:startIndex>1</openSearch:startIndex><openSearch:itemsPerPage>100</openSearch:itemsPerPage><entry><id>tag:blogger.com,1999:blog-23490028.post-114162135939050821</id><published>2006-03-05T21:01:00.000-08:00</published><updated>2006-03-05T21:02:39.400-08:00</updated><title type='text'></title><content type='html'>&lt;td width="100%"&gt;&amp;nbsp;&lt;/td&gt;&lt;br /&gt;    &lt;/tr&gt;&lt;br /&gt;    &lt;tr&gt;&lt;br /&gt;      &lt;td width="100%"&gt; &lt;font size="4"&gt;Law on the flows&lt;br /&gt;&lt;br /&gt;When one measures the speed to which a basin is emptied, one measures a&lt;br /&gt;variation of level of the basin. The reference mark is the bottom of&lt;br /&gt;the basin with like locates algebraic the zero. This water which is not&lt;br /&gt;any more in the basin left in a place located low only the algebraic&lt;br /&gt;value. Initially this water always exists, and is some share on a total&lt;br /&gt;reference mark. Thus the bottom of the basin is a balance and the&lt;br /&gt;formula of the flow will be the height starting factor of expo of less&lt;br /&gt;time on OJ which depends on the form of the evacuation and which&lt;br /&gt;varies. One should not lose sight of the fact that the final result is&lt;br /&gt;a balance of a value which should not in no case to be comparable to&lt;br /&gt;zero.&lt;br /&gt;&lt;br /&gt;      &lt;br /&gt;&lt;br /&gt;Analyze of a step&lt;br /&gt;&lt;br /&gt;      &lt;br /&gt;&lt;br /&gt;Formulate and analyzes particular case of the swirls. &lt;br /&gt;&lt;br /&gt;Drawn from the observation of the lock of Nourriguier, the swirls are&lt;br /&gt;transformed into solitary wave when they do not have enough place for&lt;br /&gt;d&amp;eacute;velloper. This wave goes up the current.&lt;br /&gt;&lt;br /&gt;There is a high limit and a low limit in the appearance of a swirl.&lt;br /&gt;These limits depend the total head and on the flow.&lt;br /&gt;&lt;br /&gt;Cavitation (liquid/gas) can generate swirls which will go in the&lt;br /&gt;direction of the current. Always with the same law of the limits&lt;br /&gt;(pressure/speed).&lt;br /&gt;&lt;br /&gt;      &lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;Experimental data measured on a flow of water: &lt;br /&gt;&lt;br /&gt;      &lt;br /&gt;&lt;br /&gt;initial time of 0,01s since the zero are not defined, the height is 60&lt;br /&gt;cm from where:&lt;br /&gt;&lt;br /&gt;H = 60; T = 0,01 S&lt;br /&gt;&lt;br /&gt;H = 55; T = 13,33 S&lt;br /&gt;&lt;br /&gt;H = 50; T = 16,58 S&lt;br /&gt;&lt;br /&gt;H = 45; T = 21,14 S&lt;br /&gt;&lt;br /&gt;H = 40; T = 27,08 S&lt;br /&gt;&lt;br /&gt;H = 35; T = 34,44 S&lt;br /&gt;&lt;br /&gt;H = 30; T = 42,27 S&lt;br /&gt;&lt;br /&gt;H = 25; T = 49,94 S&lt;br /&gt;&lt;br /&gt;H = 20; T = 59,32 S&lt;br /&gt;&lt;br /&gt;H = 15; T = 77,13 S&lt;br /&gt;&lt;br /&gt;H = 10; T = 119,27 S&lt;br /&gt;&lt;br /&gt;If one take the current formula simplified for reasons of concept (What&lt;br /&gt;is in addition advised by the books of analysis); the flow is equal to&lt;br /&gt;a constant, factor of the square root of the difference in pressure.&lt;br /&gt;&lt;br /&gt;Always for reasons of concept I thus release myself from the problems&lt;br /&gt;of dimension to thus compare only the function square root of the&lt;br /&gt;pressure height by a factor K (the exit being with a negligible&lt;br /&gt;pressure).&lt;br /&gt;&lt;br /&gt;If one takes the values referred to above and that one calculates the&lt;br /&gt;medium flow, one realizes that qelles that are dimensions of volume and&lt;br /&gt;property of flow which one applies to measurement there is a shift of&lt;br /&gt;factor four which pushes me to seek a new formula. It is true that the&lt;br /&gt;current formula gives an aspect resembling the real curve&lt;br /&gt;&amp;eacute;ffectu&amp;eacute;e by a flow, but in the application of my trade,&lt;br /&gt;I refined another proposal for a formula.In the final analysis the&lt;br /&gt;formula that I propose is an alternative of a naturally stable system.&lt;br /&gt;An alternative because it appears a constant. The result obtained being&lt;br /&gt;the level of water, there is the function of the flow in the function&lt;br /&gt;of the variation, these functions being naturally stable.&lt;br /&gt;&lt;br /&gt;Moreover if I vary the drain opening thus the flow, I can obtain a&lt;br /&gt;particular case which will correspond to the formula K factor of the&lt;br /&gt;square root the height if not the formula is the height of origin&lt;br /&gt;factor of expo of less time that OJ divides. This value OJ being it&lt;br /&gt;even a built variable of constant a factor of&lt;br /&gt;&lt;br /&gt;      &lt;br /&gt;&lt;br /&gt;author: Andre pierre jocelyn&lt;br /&gt;&lt;br /&gt;      &lt;/font&gt;&lt;br /&gt;&lt;br /&gt;      &lt;br /&gt;&lt;br /&gt;      &lt;a href="http://www.letime.net/b/index.htm"&gt;Hypothesis on time&lt;/a&gt; &lt;/td&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/23490028-114162135939050821?l=fluids-temps.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://fluids-temps.blogspot.com/feeds/114162135939050821/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=23490028&amp;postID=114162135939050821' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/23490028/posts/default/114162135939050821'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/23490028/posts/default/114162135939050821'/><link rel='alternate' type='text/html' href='http://fluids-temps.blogspot.com/2006/03/e-by-flow-but-in-application-of-my.html' title=''/><author><name>temps</name><uri>http://www.blogger.com/profile/10616520993625308918</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='25' height='32' src='http://www.letime.net/joris.jpg'/></author><thr:total>0</thr:total></entry></feed>
