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	<id>https://en.banglapedia.org/index.php?action=history&amp;feed=atom&amp;title=Acid_Sulphate_Soil</id>
	<title>Acid Sulphate Soil - Revision history</title>
	<link rel="self" type="application/atom+xml" href="https://en.banglapedia.org/index.php?action=history&amp;feed=atom&amp;title=Acid_Sulphate_Soil"/>
	<link rel="alternate" type="text/html" href="https://en.banglapedia.org/index.php?title=Acid_Sulphate_Soil&amp;action=history"/>
	<updated>2026-06-05T00:00:56Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>https://en.banglapedia.org/index.php?title=Acid_Sulphate_Soil&amp;diff=11605&amp;oldid=prev</id>
		<title>Mukbil at 16:27, 3 July 2021</title>
		<link rel="alternate" type="text/html" href="https://en.banglapedia.org/index.php?title=Acid_Sulphate_Soil&amp;diff=11605&amp;oldid=prev"/>
		<updated>2021-07-03T16:27:01Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;col class=&quot;diff-marker&quot; /&gt;
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				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 16:27, 3 July 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&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 class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&#039;&#039;&#039;Acid Sulphate Soil&#039;&#039;&#039; soils of estuaries and [[delta]]s of [[stream]]s in the tropical region subject to the action of [[tide]]s and usually covered by mangroves. It resembles grey floodplain soils when wet, but becomes toxically acid if allowed to dry out. High quantities of undecomposed organic matter, high proportion of Fe and Al salts in solution and a deficiency of phosphorus and nitrogen are its features. Impeded drainage and undecomposed organic matter may contribute to their formation. There are about 226,647 ha of Acid Sulphate Soil found in Bangladesh. They occur in the Basin southwest of the Ganges Tidal Floodplain in [[Satkhira|satkhira]], more extensively on Young Tidal Floodplains and in [[Chakaria|chakaria]] of [[cox&#039;s bazar]] on the Chittagong Coastal Plain. They are Thionic Fluvisols. They have either a sulphidic layer between 50 and 125 cm or a sulphuric horizon (pH &amp;amp;lt;3.5) in any part of the profile between the surface and 125 cm. [Md Khurshid Alam]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&#039;&#039;&#039;Acid Sulphate Soil&#039;&#039;&#039; soils of estuaries and [[delta]]s of [[stream]]s in the tropical region subject to the action of [[tide]]s and usually covered by mangroves. It resembles grey floodplain soils when wet, but becomes toxically acid if allowed to dry out. High quantities of undecomposed organic matter, high proportion of Fe and Al salts in solution and a deficiency of phosphorus and nitrogen are its features. Impeded drainage and undecomposed organic matter may contribute to their formation. There are about 226,647 ha of Acid Sulphate Soil found in Bangladesh. They occur in the Basin southwest of the Ganges Tidal Floodplain in [[Satkhira &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;District&lt;/ins&gt;|satkhira]], more extensively on Young Tidal Floodplains and in [[Chakaria &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Upazila&lt;/ins&gt;|chakaria]] of [[&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Cox’s Bazar District|&lt;/ins&gt;cox&#039;s bazar]] on the Chittagong Coastal Plain. They are Thionic Fluvisols. They have either a sulphidic layer between 50 and 125 cm or a sulphuric horizon (pH &amp;amp;lt;3.5) in any part of the profile between the surface and 125 cm. [Md Khurshid Alam]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[bn:এসিড সালফেট মাটি]]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[bn:এসিড সালফেট মাটি]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Mukbil</name></author>
	</entry>
	<entry>
		<id>https://en.banglapedia.org/index.php?title=Acid_Sulphate_Soil&amp;diff=11604&amp;oldid=prev</id>
		<title>Mukbil at 16:23, 3 July 2021</title>
		<link rel="alternate" type="text/html" href="https://en.banglapedia.org/index.php?title=Acid_Sulphate_Soil&amp;diff=11604&amp;oldid=prev"/>
		<updated>2021-07-03T16:23:46Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 16:23, 3 July 2021&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&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 class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&#039;&#039;&#039;Acid Sulphate Soil&#039;&#039;&#039; soils of estuaries and [[delta]]s of [[stream]]s in the tropical region subject to the action of [[tide]]s and usually covered by mangroves. It resembles grey floodplain soils when wet, but becomes toxically acid if allowed to dry out. High quantities of undecomposed organic matter, high proportion of Fe and Al salts in solution and a deficiency of phosphorus and nitrogen are its features. Impeded drainage and undecomposed organic matter may contribute to their formation. There are about 226,647 ha of Acid Sulphate Soil found in Bangladesh. They occur in the Basin southwest of the Ganges Tidal Floodplain in [[satkhira]], more extensively on Young Tidal Floodplains and in [[chakaria]] of [[cox&#039;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;;&lt;/del&gt;s bazar]] on the Chittagong Coastal Plain. They are Thionic Fluvisols. They have either a sulphidic layer between 50 and 125 cm or a sulphuric horizon (pH &amp;amp;lt;3.5) in any part of the profile between the surface and 125 cm. [Md Khurshid Alam] &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[Alam, Md Khurshid  Professor of Soil, Water and Environment, Dhaka University]&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&#039;&#039;&#039;Acid Sulphate Soil&#039;&#039;&#039; soils of estuaries and [[delta]]s of [[stream]]s in the tropical region subject to the action of [[tide]]s and usually covered by mangroves. It resembles grey floodplain soils when wet, but becomes toxically acid if allowed to dry out. High quantities of undecomposed organic matter, high proportion of Fe and Al salts in solution and a deficiency of phosphorus and nitrogen are its features. Impeded drainage and undecomposed organic matter may contribute to their formation. There are about 226,647 ha of Acid Sulphate Soil found in Bangladesh. They occur in the Basin southwest of the Ganges Tidal Floodplain in [[&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Satkhira|&lt;/ins&gt;satkhira]], more extensively on Young Tidal Floodplains and in [[&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Chakaria|&lt;/ins&gt;chakaria]] of [[cox&#039;s bazar]] on the Chittagong Coastal Plain. They are Thionic Fluvisols. They have either a sulphidic layer between 50 and 125 cm or a sulphuric horizon (pH &amp;amp;lt;3.5) in any part of the profile between the surface and 125 cm. [Md Khurshid Alam]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt; &lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[bn:এসিড সালফেট মাটি]]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[bn:এসিড সালফেট মাটি]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Mukbil</name></author>
	</entry>
	<entry>
		<id>https://en.banglapedia.org/index.php?title=Acid_Sulphate_Soil&amp;diff=34&amp;oldid=prev</id>
		<title>0:0:0:0:0:0:0:1: Content Updated.</title>
		<link rel="alternate" type="text/html" href="https://en.banglapedia.org/index.php?title=Acid_Sulphate_Soil&amp;diff=34&amp;oldid=prev"/>
		<updated>2021-06-17T18:54:53Z</updated>

		<summary type="html">&lt;p&gt;Content Updated.&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;#039;&amp;#039;&amp;#039;Acid Sulphate Soil&amp;#039;&amp;#039;&amp;#039; soils of estuaries and [[delta]]s of [[stream]]s in the tropical region subject to the action of [[tide]]s and usually covered by mangroves. It resembles grey floodplain soils when wet, but becomes toxically acid if allowed to dry out. High quantities of undecomposed organic matter, high proportion of Fe and Al salts in solution and a deficiency of phosphorus and nitrogen are its features. Impeded drainage and undecomposed organic matter may contribute to their formation. There are about 226,647 ha of Acid Sulphate Soil found in Bangladesh. They occur in the Basin southwest of the Ganges Tidal Floodplain in [[satkhira]], more extensively on Young Tidal Floodplains and in [[chakaria]] of [[cox&amp;#039;;s bazar]] on the Chittagong Coastal Plain. They are Thionic Fluvisols. They have either a sulphidic layer between 50 and 125 cm or a sulphuric horizon (pH &amp;amp;lt;3.5) in any part of the profile between the surface and 125 cm. [Md Khurshid Alam] [Alam, Md Khurshid  Professor of Soil, Water and Environment, Dhaka University]&lt;br /&gt;
&lt;br /&gt;
[[bn:এসিড সালফেট মাটি]]&lt;/div&gt;</summary>
		<author><name>0:0:0:0:0:0:0:1</name></author>
	</entry>
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