首页> 外文期刊>Pedosphere >Effect of Electrolyte on the Dissolution of Aluminum from Acid Soils and the Distribution of Aluminum Forms in Soil Solution
【24h】

Effect of Electrolyte on the Dissolution of Aluminum from Acid Soils and the Distribution of Aluminum Forms in Soil Solution

机译:电解质对酸性土壤中铝的溶解及溶液中铝形态分布的影响

获取原文
获取原文并翻译 | 示例
           

摘要

KCl, CaCl_2, NH_4Cl, NaCl, K_2SO_4 and KF solutions were used for studying the effects of cations and anions on the dissolution of aluminum and the distribution of aluminum forms respectively. Power of exchanging and releasing aluminum of four kinds of cations was in the decreasing order Ca~(2+) >K~+ > NH_4~+ >Na~+. The dissolution of aluminum increased with the cation concentration. The adsorption affinity of various soils for aluminum was different. The aluminum in the soil with a stronger adsorption affinity was difficult to be exchanged and released by cations. The Al-F complexes were main species of inorganic aluminum at a low concentration of cations, while Al~(3+) became major species of inorganic aluminum at a high concentration of cations. The results on the effect of anions indicated that the concentrations of total aluminum, three kinds of inorganic aluminum (Al~(3+), Al-F and Al-OH complexes) and organic aluminum complexes (Al-OM) when SO_4~(2-) was added into soil suspension were lower than those when Cl~- was added. The dissolution of aluminum from soils and the distribution of aluminum forms in solution were affected by the adsorption of F~-on the soil. For soils with strong affinity for F~-, the concentrations of the three inorganic aluminum species in soil solution after addition of F~- were lower than those after addition of Cl~-; but for soils with weak affinity for F~-, the concentrations of Al~(3+) and Al-OM were lower and the concentrations of Al-F complexes and total inorganic aluminum after addition of F~- were higher than those after addition of Cl~-. The increase of F~- concentration in soil solution accelerated the dissolution of aluminum from soils.
机译:用KCl,CaCl_2,NH_4Cl,NaCl,K_2SO_4和KF溶液分别研究了阳离子和阴离子对铝的溶解和铝形态分布的影响。四种阳离子交换和释放铝的能力依次为Ca〜(2+)> K〜+> NH_4〜+> Na〜+。铝的溶解度随阳离子浓度的增加而增加。不同土壤对铝的吸附亲和力不同。具有较强吸附亲和力的土壤中的铝很难被阳离子交换和释放。 Al-F配合物是低浓度阳离子下无机铝的主要种类,而Al〜(3+)则是高浓度阳离子下无机铝的主要种类。阴离子作用的结果表明,当SO_4〜()时,总铝,三种无机铝(Al〜(3 +),Al-F和Al-OH配合物)和有机铝配合物(Al-OM)的浓度2-)添加到土壤悬浮液中的含量低于添加Cl〜-时的含量。铝从土壤中的溶解和溶液中铝形态的分布受F〜-在土壤上的吸附的影响。对于对F〜-亲和力强的土壤,添加F〜-后土壤溶液中3种无机铝的浓度均低于添加Cl〜-后的浓度。但对F〜-的亲和力较弱的土壤,Al〜(3+)和Al-OM的浓度较低,Al〜F配合物和F〜-加入后的总无机铝浓度均高于F〜-。 Cl〜-。土壤溶液中F〜-浓度的增加促进了铝从土壤中的溶解。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号