<?xml version="1.0" encoding="utf-8"?>
<journal>
<title>Iranian Journal of Fisheries Sciences</title>
<title_fa>مجله علوم شیلاتی ایران</title_fa>
<short_title>IJFS</short_title>
<subject>Agriculture</subject>
<web_url>http://jifro.ir</web_url>
<journal_hbi_system_id>1</journal_hbi_system_id>
<journal_hbi_system_user>admin</journal_hbi_system_user>
<journal_id_issn>1562-2916</journal_id_issn>
<journal_id_issn_online>2322-5696</journal_id_issn_online>
<journal_id_pii></journal_id_pii>
<journal_id_doi>10.18869/acadpub.ijfs</journal_id_doi>
<journal_id_iranmedex></journal_id_iranmedex>
<journal_id_magiran></journal_id_magiran>
<journal_id_sid></journal_id_sid>
<journal_id_nlai></journal_id_nlai>
<journal_id_science></journal_id_science>
<language>en</language>
<pubdate>
	<type>jalali</type>
	<year>1395</year>
	<month>1</month>
	<day>1</day>
</pubdate>
<pubdate>
	<type>gregorian</type>
	<year>2016</year>
	<month>4</month>
	<day>1</day>
</pubdate>
<volume>15</volume>
<number>2</number>
<publish_type>online</publish_type>
<publish_edition>1</publish_edition>
<article_type>fulltext</article_type>
<articleset>
	<article>


	<language>en</language>
	<article_id_doi></article_id_doi>
	<title_fa></title_fa>
	<title>Quantification of individual phosphorus forms in surface sediments of the Southern Caspian Sea - Iranian Coast: A sequential extraction procedure</title>
	<subject_fa>Fish processing</subject_fa>
	<subject>Fish processing</subject>
	<content_type_fa>پژوهشي</content_type_fa>
	<content_type>Orginal research papers</content_type>
	<abstract_fa></abstract_fa>
	<abstract>&lt;p dir=&quot;ltr&quot; style=&quot;text-align: justify;&quot;&gt;Seventy Two sediments from four stations (Anzali, Tonekabon, Noshahr and Amirabad), located in Caspian Sea-Iranian coast were examined on the basis of P-fractionation in autumn and winter of 2013-2014. Several forms of the phosphorus in sediment were separated and extracted according to sequential extraction method. Then the extracted phosphorus in each fraction was determined by UV&amp;ndash;Vis spectrophotometry. In addition, Total concentrations of Ca, Fe and Al in sediment fractions were also measured by Atomic absorption spectroscopy. In autumn the rank order of P-fractions was: Ca-P&gt;Residual-P&gt;BD-P&gt;Al-P&gt;loosely-P and in winter it was: Ca-P&gt;BD-P&gt;Residual-P&gt;Al-P&gt;loosely adsorbed-P. In both season the loosely adsorbed phosphorus (NH4Cl&amp;ndash;P) represented &lt; 1% of the sedimentary inorganic phosphorus, while the reductant phosphorus (BD&amp;ndash;P) ranged from 2.7 to 4%. The calcium bound phosphorus (Ca-P or HCl&amp;ndash;P) showed considerable contribution (89-91%) to the sedimentary inorganic P-loads. The metal oxide bound phosphorus (Al-P or NaOH&amp;ndash;P) was 1.2-1.5% and Residual-P was 2.3-4.5%. Concentration of BD- P increased with increasing depth in all stations and the concentration of other fractions increased in most stations. Sampling seasons had significant effect on variance of most P-fractions and other sediment features. TP and BD-P were positively correlated with Fe&lt;sub&gt;tot &lt;/sub&gt;(&lt;em&gt;p&lt;/em&gt;&lt;0.05).&lt;/p&gt;
</abstract>
	<keyword_fa></keyword_fa>
	<keyword>Phosphorus fractionation, Surface sediment, Caspian Sea, Iranian Coast</keyword>
	<start_page>677</start_page>
	<end_page>686</end_page>
	<web_url>http://jifro.ir/browse.php?a_code=A-10-714-5&amp;slc_lang=en&amp;sid=1</web_url>


<author_list>
	<author>
	<first_name>L.</first_name>
	<middle_name></middle_name>
	<last_name>Niyazi</last_name>
	<suffix></suffix>
	<first_name_fa></first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa></last_name_fa>
	<suffix_fa></suffix_fa>
	<email></email>
	<code>100319475328460016062</code>
	<orcid>100319475328460016062</orcid>
	<coreauthor>No</coreauthor>
	<affiliation></affiliation>
	<affiliation_fa></affiliation_fa>
	 </author>


	<author>
	<first_name>M.J.</first_name>
	<middle_name></middle_name>
	<last_name>Chaichi</last_name>
	<suffix></suffix>
	<first_name_fa></first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa></last_name_fa>
	<suffix_fa></suffix_fa>
	<email></email>
	<code>100319475328460016063</code>
	<orcid>100319475328460016063</orcid>
	<coreauthor>No</coreauthor>
	<affiliation></affiliation>
	<affiliation_fa></affiliation_fa>
	 </author>


	<author>
	<first_name>H.</first_name>
	<middle_name></middle_name>
	<last_name>Nasrollahzadeh Saravi </last_name>
	<suffix></suffix>
	<first_name_fa></first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa></last_name_fa>
	<suffix_fa></suffix_fa>
	<email>hnsaravi@gmail.com</email>
	<code>100319475328460016064</code>
	<orcid>100319475328460016064</orcid>
	<coreauthor>Yes
</coreauthor>
	<affiliation></affiliation>
	<affiliation_fa></affiliation_fa>
	 </author>


	<author>
	<first_name>S.</first_name>
	<middle_name></middle_name>
	<last_name>Najafpour</last_name>
	<suffix></suffix>
	<first_name_fa></first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa></last_name_fa>
	<suffix_fa></suffix_fa>
	<email></email>
	<code>100319475328460016065</code>
	<orcid>100319475328460016065</orcid>
	<coreauthor>No</coreauthor>
	<affiliation></affiliation>
	<affiliation_fa></affiliation_fa>
	 </author>


</author_list>


	</article>
</articleset>
</journal>
