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<!DOCTYPE ArticleSet PUBLIC "-//NLM//DTD PubMed 2.7//EN" "https://dtd.nlm.nih.gov/ncbi/pubmed/in/PubMed.dtd">
<ArticleSet>
<Article>
<Journal>
				<PublisherName>Shiraz University</PublisherName>
				<JournalTitle>Iran Agricultural Research</JournalTitle>
				<Issn>1013-9885</Issn>
				<Volume>38</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2019</Year>
					<Month>10</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Potassium status of two clayey calcareous soils treated with zeolite under wetting-drying cycles</ArticleTitle>
<VernacularTitle>وضعیت پتاسیم دو خاک آهکی رسی تیمار شده با زئولیت و چرخه‌های تری و خشکی</VernacularTitle>
			<FirstPage>15</FirstPage>
			<LastPage>22</LastPage>
			<ELocationID EIdType="pii">5296</ELocationID>
			
<ELocationID EIdType="doi">10.22099/iar.2019.5296</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>M.</FirstName>
					<LastName>Najafi-Ghiri</LastName>
<Affiliation>Department of Soil Science, College of Agriculture and Natural Resources of Darab, Shiraz University, Darab, I. R. Iran</Affiliation>

</Author>
<Author>
					<FirstName>H. R.</FirstName>
					<LastName>Owliaie</LastName>
<Affiliation>Department of Soil Science, College of Agriculture, Yasouj University, Yasouj, I. R. Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2016</Year>
					<Month>07</Month>
					<Day>01</Day>
				</PubDate>
			</History>
		<Abstract>Zeolite application to clayey soils may change potassium (K) pools distribution and its release rate. To test this hypothesis, two heavy-textured calcareous soils with different mineralogy (smectitic and mixed by XRD) from southern Iran were selected. Experiment was a completely randomized factorial arrangement. Treatments consisted of two soils and two zeolite levels (0 and 5%) and wetting-drying treatment. Soil samples were incubated in 50% of saturation percentage for 90 days. Then, three wetting-drying cycles were done on samples. Different forms of K and K release to 0.01 M CaCl&lt;sub&gt;2&lt;/sub&gt;, HCl and CH&lt;sub&gt;3&lt;/sub&gt;COOH by 12 successive 15 min extractions of soil samples were determined. Zeolite increased the content of different K forms in soil 1 (smectitic), while it increased soluble and exchangeable K and decreased non-exchangeable K in soil 2 (mixed mineralogy). This may be due to the high CEC (189 cmol(+)/kg) and K content (2.13% K&lt;sub&gt;2&lt;/sub&gt;O) of the used zeolite. Wetting-drying cycles increased non-exchangeable K in soil 1 and exchangeable K in zeolite treated soils. CaCl&lt;sub&gt;2&lt;/sub&gt; extracted more K than HCl and CH&lt;sub&gt;3&lt;/sub&gt;COOH solutions (682, 281 and 292 mg kg&lt;sup&gt;-1&lt;/sup&gt;, respectively) because Ca ions are more efficient than H ions in replacing K from surface sites in the K-bearing minerals. Zeolite and wetting-drying had no effect on K release from soil 1 while they significantly decreased K release rate from soil 2.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">K release</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Wetting-drying cycles</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Zeolite</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Calcareous soils</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://iar.shirazu.ac.ir/article_5296_6efa5eea15add4d44af0b8168ea9adfd.pdf</ArchiveCopySource>
</Article>
</ArticleSet>
