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Phosphorus availability in soils amended with different phosphate fertilizers
Accurate measurement and characterization of phosphate rock dissolution are important for a better understanding of phosphorus (P) availability in soils. An incubation study was carried out on two New Zealand topsoils (0-15 cm; high P buffering capacity Craigieburn and low P buffering capacity Templ...
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Published in: | Communications in soil science and plant analysis 2006-02, Vol.37 (1-2), p.25-39 |
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creator | Randhawa, P.S Condron, L.M Di, H.J Sinaj, S McLenaghen, R.D |
description | Accurate measurement and characterization of phosphate rock dissolution are important for a better understanding of phosphorus (P) availability in soils. An incubation study was carried out on two New Zealand topsoils (0-15 cm; high P buffering capacity Craigieburn and low P buffering capacity Templeton) amended with North Carolina phosphate rock (NCPR) and water-soluble phosphate (WSP) at 218 mg P kg(-1) (equivalent to 60 kg P ha(-1)). Isotopic exchange kinetics was carried out after 12 h and 28 days of incubation to characterize P availability. This study showed that sensitivity of capacity factors (r1/R, n) to explain changes in E1min values was affected by the P buffering capacity of the soils. The recovery of applied P in the E pool (Rec(inE)%) with extended incubation time was similar from the NCPR and WSP treatments (3.1-3.3%) in the Craigieburn soil compared with the Templeton soil in which Rec(inE)% values were greater in WSP (9%) than NCPR (1.3%) treatment. The higher values of P derived from the applied P fertilizers in the E pool (Pdff(inE)%>80%) suggested that the NCPR application in both soils would be efficient for increasing P availability to plants. |
doi_str_mv | 10.1080/00103620500403572 |
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An incubation study was carried out on two New Zealand topsoils (0-15 cm; high P buffering capacity Craigieburn and low P buffering capacity Templeton) amended with North Carolina phosphate rock (NCPR) and water-soluble phosphate (WSP) at 218 mg P kg(-1) (equivalent to 60 kg P ha(-1)). Isotopic exchange kinetics was carried out after 12 h and 28 days of incubation to characterize P availability. This study showed that sensitivity of capacity factors (r1/R, n) to explain changes in E1min values was affected by the P buffering capacity of the soils. The recovery of applied P in the E pool (Rec(inE)%) with extended incubation time was similar from the NCPR and WSP treatments (3.1-3.3%) in the Craigieburn soil compared with the Templeton soil in which Rec(inE)% values were greater in WSP (9%) than NCPR (1.3%) treatment. The higher values of P derived from the applied P fertilizers in the E pool (Pdff(inE)%>80%) suggested that the NCPR application in both soils would be efficient for increasing P availability to plants.</description><identifier>ISSN: 0010-3624</identifier><identifier>EISSN: 1532-2416</identifier><identifier>DOI: 10.1080/00103620500403572</identifier><identifier>CODEN: CSOSA2</identifier><language>eng</language><publisher>Philadelphia, PA: Taylor & Francis Group</publisher><subject>Agronomy. Soil science and plant productions ; Biological and medical sciences ; buffering capacity ; fertilizer application ; fertilizer requirements ; Fundamental and applied biological sciences. Psychology ; General agronomy. Plant production ; isotopic exchange kinetics ; kinetics ; Nitrogen, phosphorus, potassium fertilizations ; nutrient availability ; phosphates ; phosphorus ; reactive phosphate rock ; rock phosphate ; soil fertility ; Soil science ; soil treatment ; Soil-plant relationships. Soil fertility. Fertilization. Amendments ; topsoil ; water solubility ; water-soluble phosphorus</subject><ispartof>Communications in soil science and plant analysis, 2006-02, Vol.37 (1-2), p.25-39</ispartof><rights>Copyright Taylor & Francis Group, LLC 2006</rights><rights>2006 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c400t-9940fc567e56ecf92f4d7432537f1b693595384c1922050241cb965e7d5af9f53</citedby><cites>FETCH-LOGICAL-c400t-9940fc567e56ecf92f4d7432537f1b693595384c1922050241cb965e7d5af9f53</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27903,27904</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=17568453$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Randhawa, P.S</creatorcontrib><creatorcontrib>Condron, L.M</creatorcontrib><creatorcontrib>Di, H.J</creatorcontrib><creatorcontrib>Sinaj, S</creatorcontrib><creatorcontrib>McLenaghen, R.D</creatorcontrib><title>Phosphorus availability in soils amended with different phosphate fertilizers</title><title>Communications in soil science and plant analysis</title><description>Accurate measurement and characterization of phosphate rock dissolution are important for a better understanding of phosphorus (P) availability in soils. An incubation study was carried out on two New Zealand topsoils (0-15 cm; high P buffering capacity Craigieburn and low P buffering capacity Templeton) amended with North Carolina phosphate rock (NCPR) and water-soluble phosphate (WSP) at 218 mg P kg(-1) (equivalent to 60 kg P ha(-1)). Isotopic exchange kinetics was carried out after 12 h and 28 days of incubation to characterize P availability. This study showed that sensitivity of capacity factors (r1/R, n) to explain changes in E1min values was affected by the P buffering capacity of the soils. The recovery of applied P in the E pool (Rec(inE)%) with extended incubation time was similar from the NCPR and WSP treatments (3.1-3.3%) in the Craigieburn soil compared with the Templeton soil in which Rec(inE)% values were greater in WSP (9%) than NCPR (1.3%) treatment. The higher values of P derived from the applied P fertilizers in the E pool (Pdff(inE)%>80%) suggested that the NCPR application in both soils would be efficient for increasing P availability to plants.</description><subject>Agronomy. Soil science and plant productions</subject><subject>Biological and medical sciences</subject><subject>buffering capacity</subject><subject>fertilizer application</subject><subject>fertilizer requirements</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>General agronomy. Plant production</subject><subject>isotopic exchange kinetics</subject><subject>kinetics</subject><subject>Nitrogen, phosphorus, potassium fertilizations</subject><subject>nutrient availability</subject><subject>phosphates</subject><subject>phosphorus</subject><subject>reactive phosphate rock</subject><subject>rock phosphate</subject><subject>soil fertility</subject><subject>Soil science</subject><subject>soil treatment</subject><subject>Soil-plant relationships. Soil fertility. Fertilization. Amendments</subject><subject>topsoil</subject><subject>water solubility</subject><subject>water-soluble phosphorus</subject><issn>0010-3624</issn><issn>1532-2416</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNqF0E1LAzEQBuAgCtbqD_DkXjyuTr42DXgR8QsqCtrzkmYTG9luShKt9debuoqHgp5CJu-TYQahQwwnGEZwCoCBVgQ4AAPKBdlCA8wpKQnD1TYarN_LHGC7aC_Gl3yVAsgA3T3MfFzMfHiNhXpTrlVT17q0KlxXRO_aXJ2brjFNsXRpVjTOWhNMl4rFl1PJFLmQsvkwIe6jHavaaA6-zyGaXF0-XdyU4_vr24vzcakZQCqlZGA1r4ThldFWEssawSjhVFg8rSTlktMR01iS9UR5BD2VFTei4cpKy-kQ4f5fHXyMwdh6EdxchVWNoV7vo97YRzbHvVmoqFVrg-q0i79Q8GrEOM25sz7nOuvDXC19aJs6qVXrww-if7UR__INVaf3lOVRL63ytXoOOTh5JIBpTgsmKKGfxAKNxw</recordid><startdate>20060201</startdate><enddate>20060201</enddate><creator>Randhawa, P.S</creator><creator>Condron, L.M</creator><creator>Di, H.J</creator><creator>Sinaj, S</creator><creator>McLenaghen, R.D</creator><general>Taylor & Francis Group</general><general>Taylor & Francis</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20060201</creationdate><title>Phosphorus availability in soils amended with different phosphate fertilizers</title><author>Randhawa, P.S ; Condron, L.M ; Di, H.J ; Sinaj, S ; McLenaghen, R.D</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c400t-9940fc567e56ecf92f4d7432537f1b693595384c1922050241cb965e7d5af9f53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Agronomy. Soil science and plant productions</topic><topic>Biological and medical sciences</topic><topic>buffering capacity</topic><topic>fertilizer application</topic><topic>fertilizer requirements</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>General agronomy. Plant production</topic><topic>isotopic exchange kinetics</topic><topic>kinetics</topic><topic>Nitrogen, phosphorus, potassium fertilizations</topic><topic>nutrient availability</topic><topic>phosphates</topic><topic>phosphorus</topic><topic>reactive phosphate rock</topic><topic>rock phosphate</topic><topic>soil fertility</topic><topic>Soil science</topic><topic>soil treatment</topic><topic>Soil-plant relationships. Soil fertility. Fertilization. Amendments</topic><topic>topsoil</topic><topic>water solubility</topic><topic>water-soluble phosphorus</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Randhawa, P.S</creatorcontrib><creatorcontrib>Condron, L.M</creatorcontrib><creatorcontrib>Di, H.J</creatorcontrib><creatorcontrib>Sinaj, S</creatorcontrib><creatorcontrib>McLenaghen, R.D</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><jtitle>Communications in soil science and plant analysis</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Randhawa, P.S</au><au>Condron, L.M</au><au>Di, H.J</au><au>Sinaj, S</au><au>McLenaghen, R.D</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Phosphorus availability in soils amended with different phosphate fertilizers</atitle><jtitle>Communications in soil science and plant analysis</jtitle><date>2006-02-01</date><risdate>2006</risdate><volume>37</volume><issue>1-2</issue><spage>25</spage><epage>39</epage><pages>25-39</pages><issn>0010-3624</issn><eissn>1532-2416</eissn><coden>CSOSA2</coden><abstract>Accurate measurement and characterization of phosphate rock dissolution are important for a better understanding of phosphorus (P) availability in soils. An incubation study was carried out on two New Zealand topsoils (0-15 cm; high P buffering capacity Craigieburn and low P buffering capacity Templeton) amended with North Carolina phosphate rock (NCPR) and water-soluble phosphate (WSP) at 218 mg P kg(-1) (equivalent to 60 kg P ha(-1)). Isotopic exchange kinetics was carried out after 12 h and 28 days of incubation to characterize P availability. This study showed that sensitivity of capacity factors (r1/R, n) to explain changes in E1min values was affected by the P buffering capacity of the soils. The recovery of applied P in the E pool (Rec(inE)%) with extended incubation time was similar from the NCPR and WSP treatments (3.1-3.3%) in the Craigieburn soil compared with the Templeton soil in which Rec(inE)% values were greater in WSP (9%) than NCPR (1.3%) treatment. The higher values of P derived from the applied P fertilizers in the E pool (Pdff(inE)%>80%) suggested that the NCPR application in both soils would be efficient for increasing P availability to plants.</abstract><cop>Philadelphia, PA</cop><pub>Taylor & Francis Group</pub><doi>10.1080/00103620500403572</doi><tpages>15</tpages></addata></record> |
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subjects | Agronomy. Soil science and plant productions Biological and medical sciences buffering capacity fertilizer application fertilizer requirements Fundamental and applied biological sciences. Psychology General agronomy. Plant production isotopic exchange kinetics kinetics Nitrogen, phosphorus, potassium fertilizations nutrient availability phosphates phosphorus reactive phosphate rock rock phosphate soil fertility Soil science soil treatment Soil-plant relationships. Soil fertility. Fertilization. Amendments topsoil water solubility water-soluble phosphorus |
title | Phosphorus availability in soils amended with different phosphate fertilizers |
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