<?xml version="1.0"?>
<?xml-stylesheet type="text/css" href="http://72.14.177.54/skins/common/feed.css?207"?>
<rss version="2.0" xmlns:dc="http://purl.org/dc/elements/1.1/">
	<channel>
		<title>HW3-9145 - Revision history</title>
		<link>http://72.14.177.54/Environmental_Technology/?title=HW3-9145&amp;action=history</link>
		<description>Revision history for this page on the wiki</description>
		<language>en</language>
		<generator>MediaWiki 1.15.1</generator>
		<lastBuildDate>Tue, 16 Jun 2026 21:50:13 GMT</lastBuildDate>
		<item>
			<title>Instructor Bob:&amp;#32;graded</title>
			<link>http://72.14.177.54/Environmental_Technology/?title=HW3-9145&amp;diff=2297&amp;oldid=prev</link>
			<description>&lt;p&gt;graded&lt;/p&gt;

		&lt;table style=&quot;background-color: white; color:black;&quot;&gt;
		&lt;col class='diff-marker' /&gt;
		&lt;col class='diff-content' /&gt;
		&lt;col class='diff-marker' /&gt;
		&lt;col class='diff-content' /&gt;
		&lt;tr valign='top'&gt;
		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;←Older revision&lt;/td&gt;
		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Revision as of 18:40, 1 March 2006&lt;/td&gt;
		&lt;/tr&gt;
		&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;{{Graded}}&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;==p114 prob.1-5==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;==p114 prob.1-5==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;{{OK}}&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;1)This is an example of dynamic equilibrium due to the fact that the rate of change in one direction is the same as the rate of change in the opposite direction.&amp;nbsp; This is an example of negative feedback mechanism because the condition triggers a response that counteracts, or reverses, the changed condition.&amp;nbsp; This allows dynamic equilibrium.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;1)This is an example of dynamic equilibrium due to the fact that the rate of change in one direction is the same as the rate of change in the opposite direction.&amp;nbsp; This is an example of negative feedback mechanism because the condition triggers a response that counteracts, or reverses, the changed condition.&amp;nbsp; This allows dynamic equilibrium.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;{{OK}}&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;2)The Gaia theory is the hypotheses that Earth's organisms adjust the environment to keep it habitable for life.&amp;nbsp; This allows people to believe that the Earth will take care of itself without any help from us.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;2)The Gaia theory is the hypotheses that Earth's organisms adjust the environment to keep it habitable for life.&amp;nbsp; This allows people to believe that the Earth will take care of itself without any help from us.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;{{OK}}&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;3)The biogeochemical cycle is the process by which matter cycles from the living world to the nonliving physical environment and back again.&amp;nbsp; This is needed to move water, oxygen,&amp;nbsp; and they make up chemical compounds of cells.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;3)The biogeochemical cycle is the process by which matter cycles from the living world to the nonliving physical environment and back again.&amp;nbsp; This is needed to move water, oxygen,&amp;nbsp; and they make up chemical compounds of cells.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;{{OK}}&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;4)Carbon makes up part of the atmosphere as a gas, carbon dioxide.&amp;nbsp; It is also present in the ocean.&amp;nbsp; Nitrogen is part of proteins and nucleic acids.&amp;nbsp; Phosphorus cycles from the land to sediments in the ocean and back to the land.&amp;nbsp; Hydrologic makes up a substantial part fo the mass of most organisms.&amp;nbsp; It also continuously circulates from the ocean to the atmosphere to the land and back to the ocean.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;4)Carbon makes up part of the atmosphere as a gas, carbon dioxide.&amp;nbsp; It is also present in the ocean.&amp;nbsp; Nitrogen is part of proteins and nucleic acids.&amp;nbsp; Phosphorus cycles from the land to sediments in the ocean and back to the land.&amp;nbsp; Hydrologic makes up a substantial part fo the mass of most organisms.&amp;nbsp; It also continuously circulates from the ocean to the atmosphere to the land and back to the ocean.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;{{OK}}&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;5)In all of these cycles it flows from the environment to the organism and back to the enivornment.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;5)In all of these cycles it flows from the environment to the organism and back to the enivornment.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;!-- diff generator: internal 2026-06-16 21:50:13 --&gt;
&lt;/table&gt;</description>
			<pubDate>Wed, 01 Mar 2006 18:40:57 GMT</pubDate>			<dc:creator>Instructor Bob</dc:creator>			<comments>http://72.14.177.54/Environmental_Technology/Talk:HW3-9145</comments>		</item>
		<item>
			<title>Jalcst-9145 at 19:23, 15 February 2006</title>
			<link>http://72.14.177.54/Environmental_Technology/?title=HW3-9145&amp;diff=2136&amp;oldid=prev</link>
			<description>&lt;p&gt;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;==p114 prob.1-5==&lt;br /&gt;
&lt;br /&gt;
1)This is an example of dynamic equilibrium due to the fact that the rate of change in one direction is the same as the rate of change in the opposite direction.  This is an example of negative feedback mechanism because the condition triggers a response that counteracts, or reverses, the changed condition.  This allows dynamic equilibrium.&lt;br /&gt;
&lt;br /&gt;
2)The Gaia theory is the hypotheses that Earth's organisms adjust the environment to keep it habitable for life.  This allows people to believe that the Earth will take care of itself without any help from us.&lt;br /&gt;
&lt;br /&gt;
3)The biogeochemical cycle is the process by which matter cycles from the living world to the nonliving physical environment and back again.  This is needed to move water, oxygen,  and they make up chemical compounds of cells.&lt;br /&gt;
&lt;br /&gt;
4)Carbon makes up part of the atmosphere as a gas, carbon dioxide.  It is also present in the ocean.  Nitrogen is part of proteins and nucleic acids.  Phosphorus cycles from the land to sediments in the ocean and back to the land.  Hydrologic makes up a substantial part fo the mass of most organisms.  It also continuously circulates from the ocean to the atmosphere to the land and back to the ocean.&lt;br /&gt;
&lt;br /&gt;
5)In all of these cycles it flows from the environment to the organism and back to the enivornment.&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[[Category: Jalcst-9145 HW3]]&lt;/div&gt;</description>
			<pubDate>Wed, 15 Feb 2006 19:23:43 GMT</pubDate>			<dc:creator>Jalcst-9145</dc:creator>			<comments>http://72.14.177.54/Environmental_Technology/Talk:HW3-9145</comments>		</item>
	</channel>
</rss>