期刊文献+

几种土壤粘粒表面Pb^(2+)吸附-解吸不可逆性特征 被引量:3

Irreversible characteristic of lead(Ⅱ) adsorption-desorption on soil clays
下载PDF
导出
摘要 为了探讨土壤粘粒表面Pb2+吸附-解吸的不可逆性特征,采用一次平衡法研究了陕西4种土壤粘粒对Pb2+的吸附和解吸特征。结果表明,在恒定pH条件下,残留吸附常数Kd与吸附常数Ka的比值称为吸附-解吸的不可逆性特征参数,Kd/Ka=1,表示吸附-解吸过程是可逆的;Kd/Ka≠1,表示该过程不可逆;在不同解吸溶液中,供试土壤粘粒表面Pb2+Kd/Ka值由大到小依次表现为N aNO3、草酸、柠檬酸,不可逆程度大小与此相同。在不同pH条件下,供试土壤粘粒表面Pb2+络合常数log Kiant与解吸常数log Kidnt的比值也可作为过程不可逆性特征参数;在不同介质中,其绝对值由大到小依次为N aNO3、柠檬酸、草酸,不可逆程度大小与此相反。 In order to investigate the irreversibility of the adsorption and desorption of Pb^2+ on soil clays,one equilibrium method was used to study the characteristics of the adsorption and desorption of Pb^2+ on soil clays in Shaanxi. The results were that the ratio of residual adsorption constant Kd to adsorption constant Ka was defined as the irreversible parameter of adsorption-desorption for Pb^2+ on the soil clay. If Kd/Ka= 1 ,the process of adsorption and desorption was reversible. If Kd/Ka≠1 ,the process of adsorption and desorption was irreversible. The ratio Kd/Ka of soil clays showed the feature of NaNO3〉oxalic acid〉citric acid at a constant pH,the irreversible degree showed the same sequence. So,concerning pH, the ratio of log K^intd/log Kinta (the intrinsic desorption constant/surface intrinsic complexation constant) Pb^2+ on soil clays was defined as the parameter of irreversible,the ratio showed NaNO3〉 citric acid〉 oxalic acid in different mediums ,the irreversible degree was just the opposite.
出处 《西北农林科技大学学报(自然科学版)》 CSCD 北大核心 2007年第1期127-132,共6页 Journal of Northwest A&F University(Natural Science Edition)
基金 西北农林科技大学重点专项基金项目
关键词 土壤粘粒 Ph^2+ 吸附—解吸 不可逆 soil clay Pb^2+ adsorption-desorption irreversible
  • 相关文献

参考文献14

二级参考文献41

  • 1朱端卫,皮美美,刘武定.土壤硼不同化学库特性研究──Ⅰ.热水溶性硼的植物有效性[J].华中农业大学学报,1994,13(3):262-267. 被引量:8
  • 2Hatzinger P B,Alexander M.Effect of aging of chemicals in soil on their biodegradability and extractability[J ].Environ.Sci.Technol.,1995,29 (2):537~545.
  • 3Cornelissen G,Rigterink H,Rerdinandy M M A,et al.Rapidly desorbing fractions of PAHs in contaminated sediments as a predictor of the extent of bioremediation[J].Environ.Sci.Technol.,1998,32 (7):966~970.
  • 4Bayard R,Barna L,Mahjoub B,et al.Investigation of naphthalene sorption in soils and soil fractions using batch and column assays[J].Environ.Toxicol.Chem.,1998,17:2383~ 2390.
  • 5Alexander M.Aging,bioavailability,and overestimation of risk from environmental pollutants[ J ].Environ.Sci.Technol.,2000,34(20):4259~4265.
  • 6Chen W,Kan A T,Fu G,et al.Adsorption-desorption behaviors of hydrophobic organic compounds in sediment of Lake Charles,Louisiana,USA[J 1.Environ.Toxicol.Chem.,1999,18:1610~1616.
  • 7Chiou C T,Kile D E,Rutheford D W,et al.Sorption of selected organic compounds from water to a peat soil and its humic-acid and humin fractions:potential sources of the sorption nonlinearity[J].Environ.Sci.Technol.,2000,34 (7):1254~1258.
  • 8Weber Jr W J,Huang W.A distributed reactivity model for sorption by soils and sediments.4.intraparticle heterogeneity and phase-distribution relationships under nonequilibrium conditions[J].Environ.Sci.Technol.,1996,30 (3):881~888.
  • 9朱端卫,中国科协第二届青年学术年会论文集.农业科学分册,1995年,322页
  • 10Li Renan,Pedosphere,1991年,1卷,2期,137页

共引文献76

同被引文献38

引证文献3

二级引证文献16

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部