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		<title>Carlier d'Odeigne et al 2017a - Revision history</title>
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		<id>https://www.scipedia.com/wd/index.php?title=Carlier_d%27Odeigne_et_al_2017a&amp;diff=184769&amp;oldid=prev</id>
		<title>Scipediacontent: Scipediacontent moved page Draft Content 480396709 to Carlier d'Odeigne et al 2017a</title>
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				<updated>2021-01-25T11:20:08Z</updated>
		
		<summary type="html">&lt;p&gt;Scipediacontent moved page &lt;a href=&quot;/public/Draft_Content_480396709&quot; class=&quot;mw-redirect&quot; title=&quot;Draft Content 480396709&quot;&gt;Draft Content 480396709&lt;/a&gt; to &lt;a href=&quot;/public/Carlier_d%27Odeigne_et_al_2017a&quot; title=&quot;Carlier d'Odeigne et al 2017a&quot;&gt;Carlier d&amp;#039;Odeigne et al 2017a&lt;/a&gt;&lt;/p&gt;
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				&lt;td colspan='1' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan='1' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 11:20, 25 January 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan='2' style='text-align: center;' lang='en'&gt;&lt;div class=&quot;mw-diff-empty&quot;&gt;(No difference)&lt;/div&gt;
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	<entry>
		<id>https://www.scipedia.com/wd/index.php?title=Carlier_d%27Odeigne_et_al_2017a&amp;diff=184768&amp;oldid=prev</id>
		<title>Scipediacontent: Created page with &quot; == Abstract ==  Inland navigation networks are composed of several artificial canals, usually characterized by no slope. These canals are large-scale systems that can be accu...&quot;</title>
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				<updated>2021-01-25T11:20:03Z</updated>
		
		<summary type="html">&lt;p&gt;Created page with &amp;quot; == Abstract ==  Inland navigation networks are composed of several artificial canals, usually characterized by no slope. These canals are large-scale systems that can be accu...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&lt;br /&gt;
== Abstract ==&lt;br /&gt;
&lt;br /&gt;
Inland navigation networks are composed of several artificial canals, usually characterized by no slope. These canals are large-scale systems that can be accurately described by means of the nonlinear Saint-Venant partial differential equations. However, the lack of an analytical solution for these equations is one of the reasons why simplified models have been developed. In this work, the Integrator-Delay-Zero model is used as the input-output model to link the water depths to the discharges. A modeling extension for a canal with inflows and outflows along the water stream is proposed: an overlapping problem is discussed and a criterion choice is defined in order to obtain the general model. With regard to this criterion, a calibration step is needed, both to overcome the natural limitations of the simplified model and to ensure the correct computation of the general model. The application of this modeling approach to a part of the inland navigation network in the north of France serves as the case study for this work. Les voies navigables sont des rÃ©seaux de grandes tailles composÃ©s de plusieurs riviÃ¨res canalisÃ©es mais Ã©galement de canaux artificiels. Ces canaux, dÃ©limitÃ©s par des Ã©cluses en amont et en aval, sont souvent caractÃ©risÃ©s par l'absence de pente. Ils sont donc particuliÃ¨rement sujets Ã  des phÃ©nomÃ¨nes de rÃ©sonance qui se caractÃ©risent par l'apparition de vagues de grandes amplitudes provoquÃ©es par l'activation des Ã©cluses. Pour modÃ©liser ces phÃ©nomÃ¨nes, il est possible d'utiliser les Ã©quations de Saint Venant (Chow, 1959). Cependant, leur utilisation pour la conception de lois de commande ou de stratÃ©gies de diagnostic des ouvrages reste difficile par la nature mÃªme du systÃ¨me considÃ©rÃ©. Une alternative consiste en la conception de modÃ¨les simplifiÃ©s tels que le modÃ¨le IDZ (Integrator-Delay-Zero) proposÃ© dans la littÃ©rature (Litrico &amp;amp; Fromion, 2004). Il s'agit d'un modÃ¨le permettant de reproduire la dynamique entrÃ©e-sortie des canaux en prÃ©disant l'effet des dÃ©bits en amont et en aval du canal Ã©tudiÃ© sur ses hauteurs d'eau mesurÃ©es aux mÃªmes endroits. Dans cet article, une extension de ce modÃ¨le est proposÃ©e avec l'objectif de pouvoir prendre en compte plusieurs entrÃ©es et sorties situÃ©es le long d'un mÃªme canal. La mÃ©thode permettant l'identification des paramÃ¨tres du modÃ¨le IDZ conduit alors Ã  des redondances de calcul. Ce problÃ¨me est mis en Ã©vidence et discutÃ©, puis une solution basÃ©e sur un critÃ¨re de sÃ©lection des paramÃ¨tres est proposÃ©e. Dans un deuxiÃ¨me temps, afin de pouvoir reproduire au mieux la dynamique rÃ©elle des canaux de navigation sans pente, en particulier la forte amplitude du premier pic de rÃ©sonance, une phase de calage du modÃ¨le est prÃ©sentÃ©e. Elle consiste Ã  introduire deux coefficients conduisant Ã  une modification lÃ©gÃ¨re des valeurs du ZÃ©ro et de l'IntÃ©grateur du modÃ¨le en tenant compte des sorties du modÃ¨le et des mesures disponibles. Le bief de voies navigables Cuinchy-Fontinettes situÃ© dans les Hauts-de-France permet d'illustrer cette dÃ©marche, puisqu'il a la particularitÃ© de pouvoir Ãªtre alimentÃ© par l'intermÃ©diaire d'une vanne situÃ©e environ au centre du bief. Les performances du modÃ¨le proposÃ© sont illustrÃ©es en reproduisant par simulation un scÃ©nario de fonctionnement rÃ©el&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
== Original document ==&lt;br /&gt;
&lt;br /&gt;
The different versions of the original document can be found in:&lt;br /&gt;
&lt;br /&gt;
* [http://hdl.handle.net/2078.1/196016 http://hdl.handle.net/2078.1/196016]&lt;br /&gt;
&lt;br /&gt;
* [http://hdl.handle.net/2078.1/196017 http://hdl.handle.net/2078.1/196017]&lt;br /&gt;
&lt;br /&gt;
* [http://hdl.handle.net/2078.1/196018 http://hdl.handle.net/2078.1/196018]&lt;br /&gt;
&lt;br /&gt;
* [http://hdl.handle.net/2078.1/196019 http://hdl.handle.net/2078.1/196019]&lt;br /&gt;
&lt;br /&gt;
* [http://hdl.handle.net/2117/119978 http://hdl.handle.net/2117/119978]&lt;br /&gt;
&lt;br /&gt;
* [http://hdl.handle.net/2117/130184 http://hdl.handle.net/2117/130184]&lt;br /&gt;
&lt;br /&gt;
* [http://link.springer.com/content/pdf/10.1007/978-981-10-7218-5.pdf http://link.springer.com/content/pdf/10.1007/978-981-10-7218-5.pdf],&lt;br /&gt;
: [http://link.springer.com/content/pdf/10.1007/978-981-10-7218-5 http://link.springer.com/content/pdf/10.1007/978-981-10-7218-5],&lt;br /&gt;
: [http://dx.doi.org/10.1007/978-981-10-7218-5 http://dx.doi.org/10.1007/978-981-10-7218-5] under the license http://www.springer.com/tdm&lt;br /&gt;
&lt;br /&gt;
* [https://www.shf-lhb.org/10.1051/lhb/2018055/pdf https://www.shf-lhb.org/10.1051/lhb/2018055/pdf],&lt;br /&gt;
: [http://dx.doi.org/10.1051/lhb/2018055 http://dx.doi.org/10.1051/lhb/2018055] under the license https://www.edpsciences.org/en/authors/copyright-and-licensing&lt;br /&gt;
&lt;br /&gt;
* [https://www.springer.com/gp/book/9789811072178 https://www.springer.com/gp/book/9789811072178],&lt;br /&gt;
: [http://hdl.handle.net/2117/119978 http://hdl.handle.net/2117/119978]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
DOIS: 10.1007/978-981-10-7218-5 10.1051/lhb/2018055&lt;/div&gt;</summary>
		<author><name>Scipediacontent</name></author>	</entry>

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