<?xml version="1.0" encoding="UTF-8"?>
<rss version="2.0"
	xmlns:content="http://purl.org/rss/1.0/modules/content/"
	xmlns:wfw="http://wellformedweb.org/CommentAPI/"
	xmlns:dc="http://purl.org/dc/elements/1.1/"
	xmlns:atom="http://www.w3.org/2005/Atom"
	xmlns:sy="http://purl.org/rss/1.0/modules/syndication/"
	xmlns:slash="http://purl.org/rss/1.0/modules/slash/"
	>

<channel>
	<title>The Duan Group</title>
	<atom:link href="http://www.geochem-model.org/index.php?feed=rss2" rel="self" type="application/rss+xml" />
	<link>http://www.geochem-model.org</link>
	<description>Computational geochemistry, molecular geochemistry, thermodynamics of fluids and minerals. Interplay between geochemistry and modern physical-chemistry research Group</description>
	<lastBuildDate>Fri, 13 Nov 2009 07:34:33 +0000</lastBuildDate>
	<generator>http://wordpress.org/?v=2.8.4</generator>
	<language>en</language>
	<sy:updatePeriod>hourly</sy:updatePeriod>
	<sy:updateFrequency>1</sy:updateFrequency>
			<item>
		<title>The processes in the Earth interior and carbon cycle</title>
		<link>http://www.geochem-model.org/?p=1496</link>
		<comments>http://www.geochem-model.org/?p=1496#comments</comments>
		<pubDate>Thu, 12 Nov 2009 05:50:36 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[Activity]]></category>

		<guid isPermaLink="false">http://www.geochem-model.org/?p=1496</guid>
		<description><![CDATA[The first workshop for &#8220;Deep Carbon Cycle&#8221; was held at the Institute of Geology and Geophysics, Chinese Academy of Sciences, Nov 11,2009

Scientists from Carnegie Institution of Washington, China University of Geosciences, Peking University, Institute of Atmospheric Physics, CAS, Guangzhou Institute of Geochemistry,CAS and our institute attended this workshop.
]]></description>
			<content:encoded><![CDATA[<p>The first workshop for &#8220;Deep Carbon Cycle&#8221; was held at the Institute of Geology and Geophysics, Chinese Academy of Sciences, Nov 11,2009</p>
<p><img src="http://www.geochem-model.org/wp-content/uploads/2009/11/IMG_0713-1023x682.jpg" alt="IMG_0713" title="IMG_0713" width="600" height="400" class="aligncenter size-large wp-image-1486" /></p>
<p>Scientists from Carnegie Institution of Washington, China University of Geosciences, Peking University, Institute of Atmospheric Physics, CAS, Guangzhou Institute of Geochemistry,CAS and our institute attended this workshop.</p>
]]></content:encoded>
			<wfw:commentRss>http://www.geochem-model.org/?feed=rss2&amp;p=1496</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>The Viscosity of Aqueous Alkali-Chloride Solutions up to 623 K, 1,000 bar, and High Ionic Strength</title>
		<link>http://www.geochem-model.org/?p=1456</link>
		<comments>http://www.geochem-model.org/?p=1456#comments</comments>
		<pubDate>Tue, 03 Nov 2009 01:20:44 +0000</pubDate>
		<dc:creator>gengming</dc:creator>
				<category><![CDATA[Publication]]></category>

		<guid isPermaLink="false">http://www.geochem-model.org/?p=1456</guid>
		<description><![CDATA[Vis_mao_duan_2009gAbstract An accurate viscosity (dynamic viscosity) model is developed for aqueous
Abstract
alkali-chloride solutions of the binary systems, LiCl–H2O, NaCl–H2O, and KCl–
H2O, from 273K to 623 K, and from 1 bar to 1,000 bar and up to high ionic strength.
The valid ionic strengths for the LiCl–H2O, NaCl–H2O, and KCl–H2O systems are
0 to 16.7mol · kg−1, 0 to [...]]]></description>
			<content:encoded><![CDATA[<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">Vis_mao_duan_2009gAbstract An accurate viscosity (dynamic viscosity) model is developed for aqueous</div>
<p><strong>Abstract</strong></p>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">alkali-chloride solutions of the binary systems, LiCl–H2O, NaCl–H2O, and KCl–</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">H2O, from 273K to 623 K, and from 1 bar to 1,000 bar and up to high ionic strength.</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">The valid ionic strengths for the LiCl–H2O, NaCl–H2O, and KCl–H2O systems are</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">0 to 16.7mol · kg−1, 0 to 6mol · kg−1, and 0 to 4.5 mol · kg−1, respectively. Comparison</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">of the model with about 4,150 experimental data points concludes that the</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">average absolute viscosity deviation from experimental data in the above range is</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">within or about 1 % for the LiCl–H2O, NaCl–H2O, and KCl–H2O mixtures, indicating</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">the model is of experimental accuracy. With a simple mixing rule, this model can</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">be extrapolated to predict the viscosity of ternary aqueous alkali-chloride solutions,</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">making it useful in reservoir fluid flow simulation. A computer code is developed for</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">this model and can be obtained from the author: (maoshide@cugb.edu.cn).An accurate viscosity (dynamic viscosity) model is developed for aqueous</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">alkali-chloride solutions of the binary systems, LiCl–H2O, NaCl–H2O, and KCl–</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">H2O, from 273K to 623 K, and from 1 bar to 1,000 bar and up to high ionic strength.</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">The valid ionic strengths for the LiCl–H2O, NaCl–H2O, and KCl–H2O systems are</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">0 to 16.7mol · kg−1, 0 to 6mol · kg−1, and 0 to 4.5 mol · kg−1, respectively. Comparison</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">of the model with about 4,150 experimental data points concludes that the</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">average absolute viscosity deviation from experimental data in the above range is</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">within or about 1 % for the LiCl–H2O, NaCl–H2O, and KCl–H2O mixtures, indicating</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">the model is of experimental accuracy. With a simple mixing rule, this model can</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">be extrapolated to predict the viscosity of ternary aqueous alkali-chloride solutions,</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">making it useful in reservoir fluid flow simulation. A computer code is developed for</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">this model and can be obtained from the author: (maoshide@cugb.edu.cn)Abstract An accurate viscosity (dynamic viscosity) model is developed for aqueous</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">alkali-chloride solutions of the binary systems, LiCl–H2O, NaCl–H2O, and KCl–</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">H2O, from 273K to 623 K, and from 1 bar to 1,000 bar and up to high ionic strength.</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">The valid ionic strengths for the LiCl–H2O, NaCl–H2O, and KCl–H2O systems are</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">0 to 16.7mol · kg−1, 0 to 6mol · kg−1, and 0 to 4.5 mol · kg−1, respectively. Comparison</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">of the model with about 4,150 experimental data points concludes that the</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">average absolute viscosity deviation from experimental data in the above range is</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">within or about 1 % for the LiCl–H2O, NaCl–H2O, and KCl–H2O mixtures, indicating</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">the model is of experimental accuracy. With a simple mixing rule, this model can</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">be extrapolated to predict the viscosity of ternary aqueous alkali-chloride solutions,</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">making it useful in reservoir fluid flow simulation. A computer code is developed for</div>
<div id="_mcePaste" style="position: absolute; overflow-x: hidden; overflow-y: hidden; width: 1px; height: 1px; top: 0px; left: -10000px;">this model and can be obtained from the author: (maoshide@cugb.edu.cn).</div>
<p>An accurate viscosity (dynamic viscosity) model is developed for aqueous<br />
alkali-chloride solutions of the binary systems, LiCl–H2O, NaCl–H2O, and KCl–<br />
H2O, from 273K to 623 K, and from 1 bar to 1,000 bar and up to high ionic strength.<br />
The valid ionic strengths for the LiCl–H2O, NaCl–H2O, and KCl–H2O systems are<br />
0 to 16.7mol · kg−1, 0 to 6mol · kg−1, and 0 to 4.5 mol · kg−1, respectively. Comparison<br />
of the model with about 4,150 experimental data points concludes that the<br />
average absolute viscosity deviation from experimental data in the above range is<br />
within or about 1 % for the LiCl–H2O, NaCl–H2O, and KCl–H2O mixtures, indicating<br />
the model is of experimental accuracy. With a simple mixing rule, this model can<br />
be extrapolated to predict the viscosity of ternary aqueous alkali-chloride solutions,<br />
making it useful in reservoir fluid flow simulation. A computer code is developed for<br />
this model and can be obtained from the author: (<a href="mailto:maoshide@cugb.edu.cn">maoshide@cugb.edu.cn</a>).</p>
]]></content:encoded>
			<wfw:commentRss>http://www.geochem-model.org/?feed=rss2&amp;p=1456</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>A vapor–liquid phase equilibrium model for binary CO2–H2O and CH4–H2O systems above 523K for application to fluid inclusions</title>
		<link>http://www.geochem-model.org/?p=762</link>
		<comments>http://www.geochem-model.org/?p=762#comments</comments>
		<pubDate>Tue, 15 Sep 2009 00:39:46 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[Publication]]></category>

		<guid isPermaLink="false">http://newsite.geochem-model.org/?p=762</guid>
		<description><![CDATA[Shide Mao, Zhenhao Duan and Wenxuan Hu(2009) A vapor–liquid phase equilibrium model for binary CO2–H2O and CH4–H2O systems above 523K for application to fluid inclusions.The Journal of Supercritical Fluids, 50 (2009): 13-21.60-JSF-2009-50-13
]]></description>
			<content:encoded><![CDATA[<p>Shide Mao, Zhenhao Duan and Wenxuan Hu(2009) A vapor–liquid phase equilibrium model for binary CO<sub>2</sub>–H<sub>2</sub>O and CH<sub>4</sub>–H<sub>2</sub>O systems above 523K for application to fluid inclusions.<em><strong>The Journal of Supercritical Fluids</strong></em>, 50 (2009): 13-21.60-JSF-2009-50-13</p>
]]></content:encoded>
			<wfw:commentRss>http://www.geochem-model.org/?feed=rss2&amp;p=762</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>A model for C-O-H fluid in the Earth&#8217;s mantle</title>
		<link>http://www.geochem-model.org/?p=760</link>
		<comments>http://www.geochem-model.org/?p=760#comments</comments>
		<pubDate>Tue, 15 Sep 2009 00:39:34 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[Publication]]></category>

		<guid isPermaLink="false">http://newsite.geochem-model.org/?p=760</guid>
		<description><![CDATA[Chi Zhang and Zhenhao Duan. (2009) A model for C-O-H fluid in the Earth&#8217;s mantle .Geochimica et Cosmochimica Acta., 73 (7): 2089-2102.
]]></description>
			<content:encoded><![CDATA[<p>Chi Zhang and Zhenhao Duan. (2009) A model for C-O-H fluid in the Earth&#8217;s mantle .Geochimica et Cosmochimica Acta., 73 (7): 2089-2102.</p>
]]></content:encoded>
			<wfw:commentRss>http://www.geochem-model.org/?feed=rss2&amp;p=760</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>The structure, dynamics and solvation mechanisms of ions in water from long time molecular dynamics simulations: a case study of CaCl2 (aq) aqueous solutions</title>
		<link>http://www.geochem-model.org/?p=758</link>
		<comments>http://www.geochem-model.org/?p=758#comments</comments>
		<pubDate>Tue, 15 Sep 2009 00:38:56 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[Publication]]></category>

		<guid isPermaLink="false">http://newsite.geochem-model.org/?p=758</guid>
		<description><![CDATA[Mingyan Li,Zhenhao Duan, Zhigang Zhang,Chi Zhang &#038; John Weare (2008) The structure, dynamics and solvation mechanisms of ions in water from long time molecular dynamics simulations: a case study of CaCl2 (aq) aqueous solutions.Molecular Physics, 106 (24): 2685-2697.
]]></description>
			<content:encoded><![CDATA[<p>Mingyan Li,Zhenhao Duan, Zhigang Zhang,Chi Zhang &#038; John Weare (2008) The structure, dynamics and solvation mechanisms of ions in water from long time molecular dynamics simulations: a case study of CaCl2 (aq) aqueous solutions.Molecular Physics, 106 (24): 2685-2697.</p>
]]></content:encoded>
			<wfw:commentRss>http://www.geochem-model.org/?feed=rss2&amp;p=758</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Coupled phase and aqueous species equilibrium of the H2O–CO2–NaCl–CaCO3 system from 0 to 250 C, 1 to 1000 bar with NaCl concentrations up to saturation of halite</title>
		<link>http://www.geochem-model.org/?p=756</link>
		<comments>http://www.geochem-model.org/?p=756#comments</comments>
		<pubDate>Tue, 15 Sep 2009 00:38:36 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[Publication]]></category>

		<guid isPermaLink="false">http://newsite.geochem-model.org/?p=756</guid>
		<description><![CDATA[Zhenhao Duan , Dedong Li (2008) Coupled phase and aqueous species equilibrium of the H2O–CO2–NaCl–CaCO3 system from 0 to 250 C, 1 to 1000 bar with NaCl concentrations up to saturation of halite. Geochim. Cosmochim. Acta, 72 (20): 5128-5145.
]]></description>
			<content:encoded><![CDATA[<p>Zhenhao Duan , Dedong Li (2008) Coupled phase and aqueous species equilibrium of the H2O–CO2–NaCl–CaCO3 system from 0 to 250 C, 1 to 1000 bar with NaCl concentrations up to saturation of halite. Geochim. Cosmochim. Acta, 72 (20): 5128-5145.</p>
]]></content:encoded>
			<wfw:commentRss>http://www.geochem-model.org/?feed=rss2&amp;p=756</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Experimental Measurements of Vapor-Liquid Equilibria of the H2O+CO2+CH4 Ternary System</title>
		<link>http://www.geochem-model.org/?p=754</link>
		<comments>http://www.geochem-model.org/?p=754#comments</comments>
		<pubDate>Tue, 15 Sep 2009 00:37:33 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[Publication]]></category>

		<guid isPermaLink="false">http://newsite.geochem-model.org/?p=754</guid>
		<description><![CDATA[Qin JF, Rosenbauer RJ, and Duan ZH. (2008) Experimental Measurements of Vapor-Liquid Equilibria of the H2O+CO2+CH4 Ternary System.Journal of Chemical &#038; Engineering Data., 53 (6): 1246-1249.
]]></description>
			<content:encoded><![CDATA[<p>Qin JF, Rosenbauer RJ, and Duan ZH. (2008) Experimental Measurements of Vapor-Liquid Equilibria of the H2O+CO2+CH4 Ternary System.Journal of Chemical &#038; Engineering Data., 53 (6): 1246-1249.</p>
]]></content:encoded>
			<wfw:commentRss>http://www.geochem-model.org/?feed=rss2&amp;p=754</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>The P, V, T,x properties of binary aqueous chloride solutions up to T = 573 K and 100 MPa</title>
		<link>http://www.geochem-model.org/?p=752</link>
		<comments>http://www.geochem-model.org/?p=752#comments</comments>
		<pubDate>Tue, 15 Sep 2009 00:37:14 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[Publication]]></category>

		<guid isPermaLink="false">http://newsite.geochem-model.org/?p=752</guid>
		<description><![CDATA[Mao SD, and Duan ZH, (2008) The P, V, T,x properties of binary aqueous chloride solutions up to T = 573 K and 100 MPa. The Journal of Chemical Thermodynamics., 40 (7): 1046-1063.
]]></description>
			<content:encoded><![CDATA[<p>Mao SD, and Duan ZH, (2008) The P, V, T,x properties of binary aqueous chloride solutions up to T = 573 K and 100 MPa. The Journal of Chemical Thermodynamics., 40 (7): 1046-1063.</p>
]]></content:encoded>
			<wfw:commentRss>http://www.geochem-model.org/?feed=rss2&amp;p=752</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Densities of the CO2-H2O and CO2-H2O-NaCl Systems Up to 647 K and 100 MPa</title>
		<link>http://www.geochem-model.org/?p=750</link>
		<comments>http://www.geochem-model.org/?p=750#comments</comments>
		<pubDate>Tue, 15 Sep 2009 00:36:58 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[Publication]]></category>

		<guid isPermaLink="false">http://newsite.geochem-model.org/?p=750</guid>
		<description><![CDATA[Duan ZH, Hu JW, Li DD and Mao SD. (2008) Densities of the CO2-H2O and CO2-H2O-NaCl Systems Up to 647 K and 100 MPa.Energy &#038; Fuels., 22 (3): 1666-1674.
]]></description>
			<content:encoded><![CDATA[<p>Duan ZH, Hu JW, Li DD and Mao SD. (2008) Densities of the CO2-H2O and CO2-H2O-NaCl Systems Up to 647 K and 100 MPa.Energy &#038; Fuels., 22 (3): 1666-1674.</p>
]]></content:encoded>
			<wfw:commentRss>http://www.geochem-model.org/?feed=rss2&amp;p=750</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>The speciation equilibrium coupling with phase equilibrium in the H2O-CO2-NaCl system from 0 to 250 °C, from 0 to 1000 bar and from 0 to 5 molality of NaCl</title>
		<link>http://www.geochem-model.org/?p=748</link>
		<comments>http://www.geochem-model.org/?p=748#comments</comments>
		<pubDate>Tue, 15 Sep 2009 00:36:41 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[Publication]]></category>

		<guid isPermaLink="false">http://newsite.geochem-model.org/?p=748</guid>
		<description><![CDATA[Li DD, and Duan ZH, (2007) The speciation equilibrium coupling with phase equilibrium in the H2O-CO2-NaCl system from 0 to 250 °C, from 0 to 1000 bar and from 0 to 5 molality of NaCl. Chemical Geology., 244 (3-4): 730-751.
]]></description>
			<content:encoded><![CDATA[<p>Li DD, and Duan ZH, (2007) The speciation equilibrium coupling with phase equilibrium in the H2O-CO2-NaCl system from 0 to 250 °C, from 0 to 1000 bar and from 0 to 5 molality of NaCl. Chemical Geology., 244 (3-4): 730-751.</p>
]]></content:encoded>
			<wfw:commentRss>http://www.geochem-model.org/?feed=rss2&amp;p=748</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
	</channel>
</rss>
