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		<title>Model 2 The Greenhouse as Flow Heat Exchanger - Revision history</title>
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		<title>Josh Cryer: 1 revision</title>
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				<updated>2009-01-21T11:02:32Z</updated>
		
		<summary type="html">&lt;p&gt;1 revision&lt;/p&gt;
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		<author><name>Josh Cryer</name></author>	</entry>

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		<id>http://wiki.newmars.com/index.php?title=Model_2_The_Greenhouse_as_Flow_Heat_Exchanger&amp;diff=350&amp;oldid=prev</id>
		<title>C M Edwards at 13:57, 27 February 2006</title>
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				<updated>2006-02-27T13:57:47Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;The greenhouse can be modeled as a [[heat exchanger]] using two gas flows (the air inside the greenhouse and the air outside it) with some ratio of capacity rates, R&amp;lt;sub&amp;gt;c&amp;lt;/sub&amp;gt;: &lt;br /&gt;
&lt;br /&gt;
&amp;lt;math&amp;gt;R_{c} = \frac{{C_{min}}}{{C_{max}}}&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
where C&amp;lt;sub&amp;gt;min&amp;lt;/sub&amp;gt; and C&amp;lt;sub&amp;gt;max&amp;lt;/sub&amp;gt; are the minimum and maximum capacity rates, respectively.  The heat capacity rate is the maximum amount of heat a flowing fluid can absorb, equal to its [[specific heat and heat capacity|specific heat]] at constant pressure, c&amp;lt;sub&amp;gt;p&amp;lt;/sub&amp;gt;, times its mass flow rate, m’.  The minimum capacity rate is whichever can absorb the least heat, and the maximum capacity rate is that of the other.  Further, one gas stream would be the cold stream (the air inside) and the other the hot stream (the air outside), so the two capacity rates could also be written as C&amp;lt;sub&amp;gt;hot&amp;lt;/sub&amp;gt; and C&amp;lt;sub&amp;gt;cold&amp;lt;/sub&amp;gt;.&lt;br /&gt;
&lt;br /&gt;
This heat exchanger would have some effectiveness, e:&lt;br /&gt;
&lt;br /&gt;
&amp;lt;math&amp;gt;e = \frac{{C_{hot} \cdot \Delta T_{hot}}}{{T_{hot in} - T_{cold in}}}&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
where &amp;lt;math&amp;gt;\Delta&amp;lt;/math&amp;gt;T&amp;lt;sub&amp;gt;hot&amp;lt;/sub&amp;gt; is the change in temperature for the air between entering the greenhouse from its own heater and returning to the heater, T&amp;lt;sub&amp;gt;hot in&amp;lt;/sub&amp;gt; is the temperature to which the greenhouse air must be heated to keep the average temperature acceptable, and T&amp;lt;sub&amp;gt;cold in&amp;lt;/sub&amp;gt; is the temperature of the martian air before it gets heated by contact with the greenhouse.&lt;br /&gt;
&lt;br /&gt;
The heat transfer area number, or number of thermal units, of the heat exchanger is:&lt;br /&gt;
&lt;br /&gt;
&amp;lt;math&amp;gt;NTU = \frac{{h_{overall} \cdot A}} {{C_{min}}}&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
where h&amp;lt;sub&amp;gt;overall&amp;lt;/sub&amp;gt; is the [[overall heat transfer coefficient]] of the heat exchanger.  &lt;br /&gt;
&lt;br /&gt;
The density of the [[Martian atmosphere]] is sufficiently low that if the pressure in the greenhouse is near 1000mb, then: &lt;br /&gt;
&lt;br /&gt;
&amp;lt;math&amp;gt;C_{max} = C_{hot}&amp;lt;/math&amp;gt; &lt;br /&gt;
&lt;br /&gt;
and &lt;br /&gt;
&lt;br /&gt;
&amp;lt;math&amp;gt;\frac{{C_{min}}}{{C_{max}}} = 0&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
In that case, &lt;br /&gt;
&lt;br /&gt;
e = 1 – &amp;lt;i&amp;gt;e&amp;lt;/i&amp;gt;&amp;lt;sup&amp;gt;NTU&amp;lt;/sup&amp;gt;&lt;br /&gt;
&lt;br /&gt;
which can be used to derive the overall heat transfer coefficient of the greenhouse.&lt;br /&gt;
&lt;br /&gt;
See also: &lt;br /&gt;
*[[Model 1 All Greenhouse Heat Transfer Through The Walls]]&lt;br /&gt;
&lt;br /&gt;
*[[Model 4 A Wind Cooled Greenhouse]]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
==External Links==&lt;br /&gt;
&lt;br /&gt;
[http://en.wikipedia.org/wiki/Heat_exchanger Wikipedia Article: Heat Exchanger]&lt;/div&gt;</summary>
		<author><name>C M Edwards</name></author>	</entry>

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