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      <title>Soil Horizon Nomenclature by Glenn Kirkwood</title>
      <link>https://padlet.com/kiwi_kirkwoods/8zgo5epifzja</link>
      <description>Post your results for your soil profile names here...</description>
      <language>en-us</language>
      <pubDate>2018-09-04 02:11:42 UTC</pubDate>
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         <pubDate>2022-09-01 11:48:26 UTC</pubDate>
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         <title>Horizon identification, Ashleigh Everton</title>
         <author>ashleigheverton12</author>
         <link>https://padlet.com/kiwi_kirkwoods/8zgo5epifzja/wish/2333025013</link>
         <description><![CDATA[<div>B -&nbsp;The B horizon is a mineral horizon below A, E, or O horizon. The B horizon is where all or most of the original parent material structures or bedding features have been destroyed.<br><br>E - The E horizon is eluviation. Where organic matter, clay or both have washed out of the layer, usually giving it a lighter colour and making it feel ashy or chalky to the touch.<br><br>Bw - Bw horizons have been changed by weathering, having weak or moderate blocky structures. The Bw may also have a brighter colour, and it may be more leached. &nbsp;<br><br>Bk - The 'k' in the B horizon refers to an accumulation of carbonates Horizons that are paler than adjacent horizons. They are best viewed when the soil is dry.<br><br>Br - The R is the B horizon means Brookston silty clay loam. The soil is nearly level and not eroded.&nbsp;</div>]]></description>
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         <pubDate>2022-10-10 05:15:12 UTC</pubDate>
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