Chemical and Mineralogical Nature of The Sediments of Sawa Lake in Muthanna Governorate, Southwestern Iraq
The sediments of the Sawa lake surrounded area, southern Iraq, have unique proprieties that are interesting to researchers. Four sites located at varying distances from the lake were selected to study some of the properties of the lake sediment. The results indicate that the study soil is saline soi...
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description | The sediments of the Sawa lake surrounded area, southern Iraq, have unique proprieties that are interesting to researchers. Four sites located at varying distances from the lake were selected to study some of the properties of the lake sediment. The results indicate that the study soil is saline soils because of the values of the three salinity criteria (EC, TDS, and NaCl(. The values of electrical conductivity ranged between (100.11 and 74.78) ds.m
−1
for surface depths, whereas for subsurface depths ranged between (14.66 and 38.55) ds.m
−1
. The values of the total soluble salts ranged from (7.4 and 85.67) g/L. The percentage of sodium chloride ranged between (3.1 and 8.5)%. The results present that the soils of the study fall within the neutral to the low basal soils as the values of the degree of interaction ranged between (7.00 and 7.55). The sand proportion in soil texture was more than clay and loam proportions, which ranged between (420 and 780) g.kg
−1
. The dominance of the intermediate soil texture (loam) category for most depths of the study soil (S.C.L, S.L(. The distribution of sand particles of different sizes took the following patterns: The first location, which is far from the lake was the dominance of the soft particles rather than coarse particles. The second site, the closest to the lake, was the dominance of rougher particles. The soft and semi-soft particles of the sand were prevalent in the third and fourth sites, which were the distances between (155) m to (147) m, respectively. The results indicated the convergence of sediment content of light and heavy metals in all locations and homogeneity of distribution of metals in all sites. |
doi_str_mv | 10.1088/1755-1315/735/1/012054 |
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−1
for surface depths, whereas for subsurface depths ranged between (14.66 and 38.55) ds.m
−1
. The values of the total soluble salts ranged from (7.4 and 85.67) g/L. The percentage of sodium chloride ranged between (3.1 and 8.5)%. The results present that the soils of the study fall within the neutral to the low basal soils as the values of the degree of interaction ranged between (7.00 and 7.55). The sand proportion in soil texture was more than clay and loam proportions, which ranged between (420 and 780) g.kg
−1
. The dominance of the intermediate soil texture (loam) category for most depths of the study soil (S.C.L, S.L(. The distribution of sand particles of different sizes took the following patterns: The first location, which is far from the lake was the dominance of the soft particles rather than coarse particles. The second site, the closest to the lake, was the dominance of rougher particles. The soft and semi-soft particles of the sand were prevalent in the third and fourth sites, which were the distances between (155) m to (147) m, respectively. The results indicated the convergence of sediment content of light and heavy metals in all locations and homogeneity of distribution of metals in all sites.</description><identifier>ISSN: 1755-1307</identifier><identifier>EISSN: 1755-1315</identifier><identifier>DOI: 10.1088/1755-1315/735/1/012054</identifier><language>eng</language><publisher>Bristol: IOP Publishing</publisher><subject>Clay minerals ; Dominance ; Electrical conductivity ; Electrical resistivity ; Heavy metals ; Homogeneity ; Lake sediments ; Lakes ; Loam ; Saline soils ; Salts ; Sand ; Sand & gravel ; Sandy soils ; Sediments ; Sodium chloride ; Soil properties ; Soil texture ; Texture</subject><ispartof>IOP conference series. Earth and environmental science, 2021-04, Vol.735 (1), p.12054</ispartof><rights>2021. This work is published under http://creativecommons.org/licenses/by/3.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2854-3fd673403981de70f9dc6d8aff1a30c4b67083718b6fd46b84a465c3614a366f3</citedby><cites>FETCH-LOGICAL-c2854-3fd673403981de70f9dc6d8aff1a30c4b67083718b6fd46b84a465c3614a366f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,777,781,27905,27906</link.rule.ids></links><search><creatorcontrib>Ali Al-Husseni, Ayad Kadhim</creatorcontrib><creatorcontrib>Sagban Alabadi, Luma Abdalalah</creatorcontrib><creatorcontrib>Khaeim, Hussein M.</creatorcontrib><creatorcontrib>Al-Jutheri, Hayyawi Wewa</creatorcontrib><title>Chemical and Mineralogical Nature of The Sediments of Sawa Lake in Muthanna Governorate, Southwestern Iraq</title><title>IOP conference series. Earth and environmental science</title><description>The sediments of the Sawa lake surrounded area, southern Iraq, have unique proprieties that are interesting to researchers. Four sites located at varying distances from the lake were selected to study some of the properties of the lake sediment. The results indicate that the study soil is saline soils because of the values of the three salinity criteria (EC, TDS, and NaCl(. The values of electrical conductivity ranged between (100.11 and 74.78) ds.m
−1
for surface depths, whereas for subsurface depths ranged between (14.66 and 38.55) ds.m
−1
. The values of the total soluble salts ranged from (7.4 and 85.67) g/L. The percentage of sodium chloride ranged between (3.1 and 8.5)%. The results present that the soils of the study fall within the neutral to the low basal soils as the values of the degree of interaction ranged between (7.00 and 7.55). The sand proportion in soil texture was more than clay and loam proportions, which ranged between (420 and 780) g.kg
−1
. The dominance of the intermediate soil texture (loam) category for most depths of the study soil (S.C.L, S.L(. The distribution of sand particles of different sizes took the following patterns: The first location, which is far from the lake was the dominance of the soft particles rather than coarse particles. The second site, the closest to the lake, was the dominance of rougher particles. The soft and semi-soft particles of the sand were prevalent in the third and fourth sites, which were the distances between (155) m to (147) m, respectively. The results indicated the convergence of sediment content of light and heavy metals in all locations and homogeneity of distribution of metals in all sites.</description><subject>Clay minerals</subject><subject>Dominance</subject><subject>Electrical conductivity</subject><subject>Electrical resistivity</subject><subject>Heavy metals</subject><subject>Homogeneity</subject><subject>Lake sediments</subject><subject>Lakes</subject><subject>Loam</subject><subject>Saline soils</subject><subject>Salts</subject><subject>Sand</subject><subject>Sand & gravel</subject><subject>Sandy soils</subject><subject>Sediments</subject><subject>Sodium chloride</subject><subject>Soil properties</subject><subject>Soil texture</subject><subject>Texture</subject><issn>1755-1307</issn><issn>1755-1315</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNo9kE1PAjEQhhujiYj-BdPEq-u29HOPhiiSgB7AczNsW1mEFrq7Ev-9u2I8zeSZNzOTB6FbSh4o0TqnSoiMMipyxUROc0JHRPAzNPgfnP_3RF2iq7reECIVZ8UAbcZrt6tK2GIIFs-r4BJs48cveYWmTQ5Hj5drhxfOVjsXmroHCzgCnsGnw1XA87ZZQwiAJ_HLpRATNO4eL2KHj65uOoSnCQ7X6MLDtnY3f3WI3p-fluOXbPY2mY4fZ1k50oJnzFupGCes0NQ6RXxhS2k1eE-BkZKvpCKaKapX0lsuV5oDl6JkknJgUno2RHenvfsUD233gNnENoXupBkJKqgsNONdSp5SZYp1nZw3-1TtIH0bSkzv1fTKTK_PdF4NNSev7AdByGqa</recordid><startdate>20210401</startdate><enddate>20210401</enddate><creator>Ali Al-Husseni, Ayad Kadhim</creator><creator>Sagban Alabadi, Luma Abdalalah</creator><creator>Khaeim, Hussein M.</creator><creator>Al-Jutheri, Hayyawi Wewa</creator><general>IOP Publishing</general><scope>AAYXX</scope><scope>CITATION</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>PATMY</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PYCSY</scope></search><sort><creationdate>20210401</creationdate><title>Chemical and Mineralogical Nature of The Sediments of Sawa Lake in Muthanna Governorate, Southwestern Iraq</title><author>Ali Al-Husseni, Ayad Kadhim ; Sagban Alabadi, Luma Abdalalah ; Khaeim, Hussein M. ; Al-Jutheri, Hayyawi Wewa</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2854-3fd673403981de70f9dc6d8aff1a30c4b67083718b6fd46b84a465c3614a366f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Clay minerals</topic><topic>Dominance</topic><topic>Electrical conductivity</topic><topic>Electrical resistivity</topic><topic>Heavy metals</topic><topic>Homogeneity</topic><topic>Lake sediments</topic><topic>Lakes</topic><topic>Loam</topic><topic>Saline soils</topic><topic>Salts</topic><topic>Sand</topic><topic>Sand & gravel</topic><topic>Sandy soils</topic><topic>Sediments</topic><topic>Sodium chloride</topic><topic>Soil properties</topic><topic>Soil texture</topic><topic>Texture</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ali Al-Husseni, Ayad Kadhim</creatorcontrib><creatorcontrib>Sagban Alabadi, Luma Abdalalah</creatorcontrib><creatorcontrib>Khaeim, Hussein M.</creatorcontrib><creatorcontrib>Al-Jutheri, Hayyawi Wewa</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>Environmental Science Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Environmental Science Collection</collection><jtitle>IOP conference series. Earth and environmental science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ali Al-Husseni, Ayad Kadhim</au><au>Sagban Alabadi, Luma Abdalalah</au><au>Khaeim, Hussein M.</au><au>Al-Jutheri, Hayyawi Wewa</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Chemical and Mineralogical Nature of The Sediments of Sawa Lake in Muthanna Governorate, Southwestern Iraq</atitle><jtitle>IOP conference series. Earth and environmental science</jtitle><date>2021-04-01</date><risdate>2021</risdate><volume>735</volume><issue>1</issue><spage>12054</spage><pages>12054-</pages><issn>1755-1307</issn><eissn>1755-1315</eissn><abstract>The sediments of the Sawa lake surrounded area, southern Iraq, have unique proprieties that are interesting to researchers. Four sites located at varying distances from the lake were selected to study some of the properties of the lake sediment. The results indicate that the study soil is saline soils because of the values of the three salinity criteria (EC, TDS, and NaCl(. The values of electrical conductivity ranged between (100.11 and 74.78) ds.m
−1
for surface depths, whereas for subsurface depths ranged between (14.66 and 38.55) ds.m
−1
. The values of the total soluble salts ranged from (7.4 and 85.67) g/L. The percentage of sodium chloride ranged between (3.1 and 8.5)%. The results present that the soils of the study fall within the neutral to the low basal soils as the values of the degree of interaction ranged between (7.00 and 7.55). The sand proportion in soil texture was more than clay and loam proportions, which ranged between (420 and 780) g.kg
−1
. The dominance of the intermediate soil texture (loam) category for most depths of the study soil (S.C.L, S.L(. The distribution of sand particles of different sizes took the following patterns: The first location, which is far from the lake was the dominance of the soft particles rather than coarse particles. The second site, the closest to the lake, was the dominance of rougher particles. The soft and semi-soft particles of the sand were prevalent in the third and fourth sites, which were the distances between (155) m to (147) m, respectively. The results indicated the convergence of sediment content of light and heavy metals in all locations and homogeneity of distribution of metals in all sites.</abstract><cop>Bristol</cop><pub>IOP Publishing</pub><doi>10.1088/1755-1315/735/1/012054</doi><oa>free_for_read</oa></addata></record> |
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subjects | Clay minerals Dominance Electrical conductivity Electrical resistivity Heavy metals Homogeneity Lake sediments Lakes Loam Saline soils Salts Sand Sand & gravel Sandy soils Sediments Sodium chloride Soil properties Soil texture Texture |
title | Chemical and Mineralogical Nature of The Sediments of Sawa Lake in Muthanna Governorate, Southwestern Iraq |
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