{"title":"Changes in inorganic and organic Phosphorus in soil under maize (Zea mays) cultivation","authors":"H. D. Preez, A. Claassens","doi":"10.1080/02571862.1999.10635013","DOIUrl":null,"url":null,"abstract":"The changes in applied and residual phosphorus (P) were examined in Avalon and Clovelly soils under cultivation by using the P fractionation method of Hedley, Stewart and Chauhan (1982). Soil P was separated into six major fractions of which some fractions were subdivided into organic (Po) and inorganic (Pi) P forms: P extracted by an anion exchange resin (Resin-P); 0.5 M NaHCO3-P (NaHCO3-Pi and Po); 0.1 M NaOH (NaOH-l-Pi and Po); ultrasonication in 0.1 M NaOH at 75 watt (NaOH-ll-Pi and Po); 1.0 M HCI(HCI-Pi); and H2SO4 digestion and H2O2 oxidation, (H2SO4P). General trends in soil P were evident over 15 years of cultivation. Resin-P, NaHCO3-Pi, NaOH-l-Pi, NaOH-ll-Pi and HCl-Pi were reduced in the Avalon soil, while only the NaHCO3-Pi and NaOH-ll-Pi decreased in the Clovelly soil. It is hypothesised that NaOH-l-Pi, which showed the largest decrease, was mainly responsible for the replenishment of the labile P pool. In the Po fraction, NaHCO3-Po and NaOH-ll-Po decreased with time in the Avalon soil, in con...","PeriodicalId":22913,"journal":{"name":"The South African Journal of Plant and Soil","volume":"41 1","pages":"207-213"},"PeriodicalIF":0.0000,"publicationDate":"1999-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"17","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"The South African Journal of Plant and Soil","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1080/02571862.1999.10635013","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 17
Abstract
The changes in applied and residual phosphorus (P) were examined in Avalon and Clovelly soils under cultivation by using the P fractionation method of Hedley, Stewart and Chauhan (1982). Soil P was separated into six major fractions of which some fractions were subdivided into organic (Po) and inorganic (Pi) P forms: P extracted by an anion exchange resin (Resin-P); 0.5 M NaHCO3-P (NaHCO3-Pi and Po); 0.1 M NaOH (NaOH-l-Pi and Po); ultrasonication in 0.1 M NaOH at 75 watt (NaOH-ll-Pi and Po); 1.0 M HCI(HCI-Pi); and H2SO4 digestion and H2O2 oxidation, (H2SO4P). General trends in soil P were evident over 15 years of cultivation. Resin-P, NaHCO3-Pi, NaOH-l-Pi, NaOH-ll-Pi and HCl-Pi were reduced in the Avalon soil, while only the NaHCO3-Pi and NaOH-ll-Pi decreased in the Clovelly soil. It is hypothesised that NaOH-l-Pi, which showed the largest decrease, was mainly responsible for the replenishment of the labile P pool. In the Po fraction, NaHCO3-Po and NaOH-ll-Po decreased with time in the Avalon soil, in con...