{"title":"肥料混合物中磷的吸附","authors":"A. Muwamba, K. Morgan, P. Nkedi-Kizza","doi":"10.5772/INTECHOPEN.80420","DOIUrl":null,"url":null,"abstract":"Studying phosphorus (P) sorption behavior is among the prerequisites for P management in the crop fields. The work presented in this chapter described P sorption data when fertilizer mixture (NH 4 NO 3 , KH 2 PO 4 , and KCl) was used to characterize sorption on soil. In addition to using fertilizer mixture, sorption experiments were also conducted using KH 2 PO 4 prepared in 0.01 M KCl, 0.005 M CaCl 2 , and deionized water. The 24-h batch sorption experiments were conducted using a sandy soil to solution ratio of 1:2, and the equilibrium solution and sorbed data were described using Freundlich isotherm. Sorption kinetics experiments were conducted using times, 4, 8, 12, and 24 h. The Freundlich isotherm constant and sorbed P kinetics data for 0.005 M CaCl 2 were significantly greater ( p < 0.05) than for 0.01 M KCl and/or fertilizer mixture. The Freundlich isotherm constant and sorbed P kinetics data for deionized water were significantly lower ( p < 0.05) than for 0.01 M KCl and/or fertilizer mixture. There was no significant difference in Freundlich isotherm constant and sorbed P kinetics data for 0.01 M KCl and fertilizer mixture. The sorption data showed the importance of using the fertilizer mix applied to the field when conducting sorption experiments.","PeriodicalId":147738,"journal":{"name":"Advanced Sorption Process Applications","volume":"7 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2018-12-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Sorption of Phosphorus from Fertilizer Mixture\",\"authors\":\"A. Muwamba, K. Morgan, P. Nkedi-Kizza\",\"doi\":\"10.5772/INTECHOPEN.80420\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Studying phosphorus (P) sorption behavior is among the prerequisites for P management in the crop fields. The work presented in this chapter described P sorption data when fertilizer mixture (NH 4 NO 3 , KH 2 PO 4 , and KCl) was used to characterize sorption on soil. In addition to using fertilizer mixture, sorption experiments were also conducted using KH 2 PO 4 prepared in 0.01 M KCl, 0.005 M CaCl 2 , and deionized water. The 24-h batch sorption experiments were conducted using a sandy soil to solution ratio of 1:2, and the equilibrium solution and sorbed data were described using Freundlich isotherm. Sorption kinetics experiments were conducted using times, 4, 8, 12, and 24 h. The Freundlich isotherm constant and sorbed P kinetics data for 0.005 M CaCl 2 were significantly greater ( p < 0.05) than for 0.01 M KCl and/or fertilizer mixture. The Freundlich isotherm constant and sorbed P kinetics data for deionized water were significantly lower ( p < 0.05) than for 0.01 M KCl and/or fertilizer mixture. There was no significant difference in Freundlich isotherm constant and sorbed P kinetics data for 0.01 M KCl and fertilizer mixture. The sorption data showed the importance of using the fertilizer mix applied to the field when conducting sorption experiments.\",\"PeriodicalId\":147738,\"journal\":{\"name\":\"Advanced Sorption Process Applications\",\"volume\":\"7 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2018-12-05\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Advanced Sorption Process Applications\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.5772/INTECHOPEN.80420\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Advanced Sorption Process Applications","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5772/INTECHOPEN.80420","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
研究农田磷素吸附行为是农田磷素管理的前提之一。本章介绍的工作描述了使用混合肥料(nh4 no3, kh2 po4和KCl)表征土壤吸附时的P吸收数据。除使用混合肥料外,还使用在0.01 M KCl、0.005 M cacl2和去离子水中制备的kh2po4进行吸附实验。采用沙土与溶液1:2的比例进行24 h的间歇吸附实验,平衡溶液和吸附数据采用Freundlich等温线描述。分别在4、8、12和24 h进行吸附动力学实验。0.005 M氯化钙的Freundlich等温线常数和吸附P动力学数据显著高于0.01 M氯化钾和/或肥料混合物(P < 0.05)。去离子水处理的Freundlich等温线常数和吸附磷动力学数据显著低于0.01 M氯化钾和/或肥料混合处理(P < 0.05)。0.01 M KCl与肥料混合处理对Freundlich等温线常数和吸附磷动力学数据无显著影响。吸附数据表明,在进行吸附试验时,使用田间施用的混合肥料是很重要的。
Studying phosphorus (P) sorption behavior is among the prerequisites for P management in the crop fields. The work presented in this chapter described P sorption data when fertilizer mixture (NH 4 NO 3 , KH 2 PO 4 , and KCl) was used to characterize sorption on soil. In addition to using fertilizer mixture, sorption experiments were also conducted using KH 2 PO 4 prepared in 0.01 M KCl, 0.005 M CaCl 2 , and deionized water. The 24-h batch sorption experiments were conducted using a sandy soil to solution ratio of 1:2, and the equilibrium solution and sorbed data were described using Freundlich isotherm. Sorption kinetics experiments were conducted using times, 4, 8, 12, and 24 h. The Freundlich isotherm constant and sorbed P kinetics data for 0.005 M CaCl 2 were significantly greater ( p < 0.05) than for 0.01 M KCl and/or fertilizer mixture. The Freundlich isotherm constant and sorbed P kinetics data for deionized water were significantly lower ( p < 0.05) than for 0.01 M KCl and/or fertilizer mixture. There was no significant difference in Freundlich isotherm constant and sorbed P kinetics data for 0.01 M KCl and fertilizer mixture. The sorption data showed the importance of using the fertilizer mix applied to the field when conducting sorption experiments.