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	<title>Sulphidic material (WRB) - Revision history</title>
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		<title>imported&gt;Jacques Ducloy: 1 revision imported</title>
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		<updated>2017-06-28T17:36:10Z</updated>

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				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #222; text-align: center;&quot;&gt;Revision as of 17:36, 28 June 2017&lt;/td&gt;
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		<author><name>imported&gt;Jacques Ducloy</name></author>
		
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	<entry>
		<id>https://wicri-demo.istex.fr/Wicri/SolsUrbains/en/index.php?title=Sulphidic_material_(WRB)&amp;diff=3392&amp;oldid=prev</id>
		<title>imported&gt;Thierry Daunois at 08:51, 25 July 2011</title>
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		<updated>2011-07-25T08:51:46Z</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;'''Sulphidic material''' is one of the diagnostic materials used, in the WRB system, to discriminate some soils from others.&lt;br /&gt;
&lt;br /&gt;
==Description==&lt;br /&gt;
Sulphidic material (from English ''sulphide'') is a waterlogged deposit containing S, mostly in the form of sulphides, and only moderate amounts of calcium carbonate.&lt;br /&gt;
&lt;br /&gt;
==Diagnostic criteria==&lt;br /&gt;
Sulphidic material has :&lt;br /&gt;
* a pH (1:1 in water) of 4.0 or more and 0.75 percent or more S (dry mass) and less than three times as much calcium carbonate equivalent as S&lt;br /&gt;
or :&lt;br /&gt;
* a pH (1:1 in water) of 4.0 or more that, if the material is incubated as a layer 1 cm thick, at field capacity at room temperature, drops 0.5 or more units to a pH of 4.0 or less (1:1 in water) within 8 weeks.&lt;br /&gt;
&lt;br /&gt;
==Field identification==&lt;br /&gt;
In moist or wet conditions, deposits containing sulphides often show a golden shine, the colour of pyrite. Forced oxidation with a 30-percent hydrogen peroxide solution lowers the pH to 2.5 or less, the reaction may be vigorous in sunlight or on heating. Munsell colours range: hues of N, 5 Y, 5 GY, 5 BG, or 5 G; values of 2, 3 or 4; chroma always 1. The colour is usually unstable, and blackens upon exposure. Sulphidic clay is usually practically unripe. If the soil is disturbed, a whiff of rotten eggs may be noticed. This is accentuated by application of 1 ''M'' HCl.&lt;br /&gt;
&lt;br /&gt;
==RSG in which sulphidic material can be observed==&lt;br /&gt;
&lt;br /&gt;
{{#ask: [[Has for diagnostic material::{{PAGENAME}}]]&lt;br /&gt;
| format=ul&lt;br /&gt;
}}&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
&lt;br /&gt;
* The [http://www.fao.org/ag/agl/agll/wrb/doc/wrb2007_corr.pdf FAO reference text], (2007 version)&lt;br /&gt;
&lt;br /&gt;
[[Category:Diagnostic materials (WRB)]]&lt;/div&gt;</summary>
		<author><name>imported&gt;Thierry Daunois</name></author>
		
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