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Impacts of Acid Rain on Base Cations, Aluminum, and Acidity Development in Highly Weathered Soils of Thailand
The impacts of simulated acid rain on leachability of major plant nutrients, toxic element [aluminum (Al)], and acidity development in highly weathered tropical soils of Thailand were studied. Leaching experiments were conducted on soil columns with acidic solutions of pH 5.0, 4.0, 3.0, 2.0, and wit...
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Published in: | Communications in Soil Science and Plant Analysis 2012-05, Vol.43 (10), p.1382-1400 |
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creator | Nawaz, Rab Parkpian, Preeda Garivait, Hathairatana Anurakpongsatorn, Patana DeLaune, R. D Jugsujinda, A |
description | The impacts of simulated acid rain on leachability of major plant nutrients, toxic element [aluminum (Al)], and acidity development in highly weathered tropical soils of Thailand were studied. Leaching experiments were conducted on soil columns with acidic solutions of pH 5.0, 4.0, 3.0, 2.0, and with water of pH 7.0 as a control treatment. Leaching losses of base cations from all soils increased with the decrease in pH associated with simulated acid rain (SAR) additions, and were found to be quite high under SAR with pH 2.0. The leaching removal of these cations was lesser at pH 3.0, 4.0, and 5.0 but greater than that in pH 7.0. The leaching of base cation from the soils depended not only on acid rain pH but also on soil properties, especially cation exchange capacity, soil texture, and initial base content. The significant losses of major plant nutrients [such as potassium (K⁺), calcium (Ca²⁺), and magnesium (Mg²⁺)] from the plant root zone over extended periods could cause nutrient imbalance and lower soil productivity. |
doi_str_mv | 10.1080/00103624.2012.670347 |
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D ; Jugsujinda, A</creator><creatorcontrib>Nawaz, Rab ; Parkpian, Preeda ; Garivait, Hathairatana ; Anurakpongsatorn, Patana ; DeLaune, R. D ; Jugsujinda, A</creatorcontrib><description>The impacts of simulated acid rain on leachability of major plant nutrients, toxic element [aluminum (Al)], and acidity development in highly weathered tropical soils of Thailand were studied. Leaching experiments were conducted on soil columns with acidic solutions of pH 5.0, 4.0, 3.0, 2.0, and with water of pH 7.0 as a control treatment. Leaching losses of base cations from all soils increased with the decrease in pH associated with simulated acid rain (SAR) additions, and were found to be quite high under SAR with pH 2.0. The leaching removal of these cations was lesser at pH 3.0, 4.0, and 5.0 but greater than that in pH 7.0. The leaching of base cation from the soils depended not only on acid rain pH but also on soil properties, especially cation exchange capacity, soil texture, and initial base content. The significant losses of major plant nutrients [such as potassium (K⁺), calcium (Ca²⁺), and magnesium (Mg²⁺)] from the plant root zone over extended periods could cause nutrient imbalance and lower soil productivity.</description><identifier>ISSN: 1532-2416</identifier><identifier>ISSN: 0010-3624</identifier><identifier>EISSN: 1532-2416</identifier><identifier>EISSN: 1532-4133</identifier><identifier>DOI: 10.1080/00103624.2012.670347</identifier><identifier>CODEN: CSOSA2</identifier><language>eng</language><publisher>Philadelphia, PA: Taylor & Francis Group</publisher><subject>acid deposition ; Acid rain ; Acidic deposition ; acidity ; Agronomy. Soil science and plant productions ; Aluminum ; aluminum leaching ; aluminum mobilization ; base cation leaching ; Biological and medical sciences ; calcium ; cation exchange capacity ; cations ; Fundamental and applied biological sciences. Psychology ; leaching ; magnesium ; phytotoxicity ; potassium ; rhizosphere ; soil acidity ; soil productivity ; soil texture ; Soils ; southeastern Asia ; tropical soils ; weathered soils</subject><ispartof>Communications in Soil Science and Plant Analysis, 2012-05, Vol.43 (10), p.1382-1400</ispartof><rights>Copyright Taylor & Francis Group, LLC 2012</rights><rights>2015 INIST-CNRS</rights><rights>Copyright Taylor and Francis Group, LLC</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c422t-fd00d64cf6cc39b5c834dd9e31a992e90966881dec78c8436b0c8a1d847a37df3</citedby><cites>FETCH-LOGICAL-c422t-fd00d64cf6cc39b5c834dd9e31a992e90966881dec78c8436b0c8a1d847a37df3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=26066842$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Nawaz, Rab</creatorcontrib><creatorcontrib>Parkpian, Preeda</creatorcontrib><creatorcontrib>Garivait, Hathairatana</creatorcontrib><creatorcontrib>Anurakpongsatorn, Patana</creatorcontrib><creatorcontrib>DeLaune, R. D</creatorcontrib><creatorcontrib>Jugsujinda, A</creatorcontrib><title>Impacts of Acid Rain on Base Cations, Aluminum, and Acidity Development in Highly Weathered Soils of Thailand</title><title>Communications in Soil Science and Plant Analysis</title><description>The impacts of simulated acid rain on leachability of major plant nutrients, toxic element [aluminum (Al)], and acidity development in highly weathered tropical soils of Thailand were studied. Leaching experiments were conducted on soil columns with acidic solutions of pH 5.0, 4.0, 3.0, 2.0, and with water of pH 7.0 as a control treatment. Leaching losses of base cations from all soils increased with the decrease in pH associated with simulated acid rain (SAR) additions, and were found to be quite high under SAR with pH 2.0. The leaching removal of these cations was lesser at pH 3.0, 4.0, and 5.0 but greater than that in pH 7.0. The leaching of base cation from the soils depended not only on acid rain pH but also on soil properties, especially cation exchange capacity, soil texture, and initial base content. The significant losses of major plant nutrients [such as potassium (K⁺), calcium (Ca²⁺), and magnesium (Mg²⁺)] from the plant root zone over extended periods could cause nutrient imbalance and lower soil productivity.</description><subject>acid deposition</subject><subject>Acid rain</subject><subject>Acidic deposition</subject><subject>acidity</subject><subject>Agronomy. Soil science and plant productions</subject><subject>Aluminum</subject><subject>aluminum leaching</subject><subject>aluminum mobilization</subject><subject>base cation leaching</subject><subject>Biological and medical sciences</subject><subject>calcium</subject><subject>cation exchange capacity</subject><subject>cations</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>leaching</subject><subject>magnesium</subject><subject>phytotoxicity</subject><subject>potassium</subject><subject>rhizosphere</subject><subject>soil acidity</subject><subject>soil productivity</subject><subject>soil texture</subject><subject>Soils</subject><subject>southeastern Asia</subject><subject>tropical soils</subject><subject>weathered soils</subject><issn>1532-2416</issn><issn>0010-3624</issn><issn>1532-2416</issn><issn>1532-4133</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNqFkV1rFDEUhgdRsFb_gWBABC-6a74mmbmSdf1ooSDYFi_DaT66KZlkTWaU_fdmOq2IN14lF8_z5py8TfOS4DXBHX6HMcFMUL6mmNC1kJhx-ag5Ii2jK8qJePzX_WnzrJTbavQS06NmOBv2oMeCkkMb7Q36Bj6iFNEHKBZtYfQplhO0CdPg4zScIIjmDvTjAX20P21I-8HGEVXr1N_swgF9tzDubLYGXSQf7pIvd-BDNZ83TxyEYl_cn8fN1edPl9vT1fnXL2fbzflKc0rHlTMYG8G1E1qz_rrVHePG9JYR6Htqe9wL0XXEWC073XEmrrHugJiOS2DSOHbcvF1y9zn9mGwZ1eCLtqHOYNNUFKGtlHL-k4q-_ge9TVOOdTpFSEtajtteVoovlM6plGyd2mc_QD4ogtXcgXroQM0dqKWDqr25D4eiIbgMUfvyx6UC10X4PMT7hfPRpTzAr5SDUSMcQsoPEvvPS6-WBAdJwU2uwtVFBfhMtz1v2W-0_qGD</recordid><startdate>20120515</startdate><enddate>20120515</enddate><creator>Nawaz, Rab</creator><creator>Parkpian, Preeda</creator><creator>Garivait, Hathairatana</creator><creator>Anurakpongsatorn, Patana</creator><creator>DeLaune, R. 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Psychology</topic><topic>leaching</topic><topic>magnesium</topic><topic>phytotoxicity</topic><topic>potassium</topic><topic>rhizosphere</topic><topic>soil acidity</topic><topic>soil productivity</topic><topic>soil texture</topic><topic>Soils</topic><topic>southeastern Asia</topic><topic>tropical soils</topic><topic>weathered soils</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Nawaz, Rab</creatorcontrib><creatorcontrib>Parkpian, Preeda</creatorcontrib><creatorcontrib>Garivait, Hathairatana</creatorcontrib><creatorcontrib>Anurakpongsatorn, Patana</creatorcontrib><creatorcontrib>DeLaune, R. 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D</au><au>Jugsujinda, A</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Impacts of Acid Rain on Base Cations, Aluminum, and Acidity Development in Highly Weathered Soils of Thailand</atitle><jtitle>Communications in Soil Science and Plant Analysis</jtitle><date>2012-05-15</date><risdate>2012</risdate><volume>43</volume><issue>10</issue><spage>1382</spage><epage>1400</epage><pages>1382-1400</pages><issn>1532-2416</issn><issn>0010-3624</issn><eissn>1532-2416</eissn><eissn>1532-4133</eissn><coden>CSOSA2</coden><abstract>The impacts of simulated acid rain on leachability of major plant nutrients, toxic element [aluminum (Al)], and acidity development in highly weathered tropical soils of Thailand were studied. Leaching experiments were conducted on soil columns with acidic solutions of pH 5.0, 4.0, 3.0, 2.0, and with water of pH 7.0 as a control treatment. Leaching losses of base cations from all soils increased with the decrease in pH associated with simulated acid rain (SAR) additions, and were found to be quite high under SAR with pH 2.0. The leaching removal of these cations was lesser at pH 3.0, 4.0, and 5.0 but greater than that in pH 7.0. The leaching of base cation from the soils depended not only on acid rain pH but also on soil properties, especially cation exchange capacity, soil texture, and initial base content. The significant losses of major plant nutrients [such as potassium (K⁺), calcium (Ca²⁺), and magnesium (Mg²⁺)] from the plant root zone over extended periods could cause nutrient imbalance and lower soil productivity.</abstract><cop>Philadelphia, PA</cop><pub>Taylor & Francis Group</pub><doi>10.1080/00103624.2012.670347</doi><tpages>19</tpages></addata></record> |
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subjects | acid deposition Acid rain Acidic deposition acidity Agronomy. Soil science and plant productions Aluminum aluminum leaching aluminum mobilization base cation leaching Biological and medical sciences calcium cation exchange capacity cations Fundamental and applied biological sciences. Psychology leaching magnesium phytotoxicity potassium rhizosphere soil acidity soil productivity soil texture Soils southeastern Asia tropical soils weathered soils |
title | Impacts of Acid Rain on Base Cations, Aluminum, and Acidity Development in Highly Weathered Soils of Thailand |
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