首页> 外文期刊>Clays and clay minerals >ADSORPTION OF SOIL-DERIVED HUMIC ACID BY SEVEN CLAY MINERALS: A SYSTEMATIC STUDY
【24h】

ADSORPTION OF SOIL-DERIVED HUMIC ACID BY SEVEN CLAY MINERALS: A SYSTEMATIC STUDY

机译:七个粘土矿物对土壤腐殖酸的吸附:系统研究

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

Humic acid (HA)-clay complexes are well known for their contribution to soil structure and environmental processes. Despite extensive research, the mechanisms governing HA adsorption are yet to be resolved. A systematic study was conducted to characterize the adsorption of a soil-derived HA to seven clay minerals. Clay surfaces affected HA adsorption directly due to structural differences and indirectly by altering solution pH. The following order of HA removal was obtained for the clay minerals at their natural pH: illite palygorskite > kaolinite > sepiolite > montmorillonite = hectorite talc. Removal of HA (precipitation and adsorption) by kaolinite and illite was attributed to the low pH they induce, resulting in protonation of the clay and HA surfaces. In spite of the low pH, the zeta potential for HA remained negative, which promoted HA adsorption to the protonated clay surfaces by ligand exchange. Ionic strength did not affect HA adsorption to clay minerals with low zeta potentials, indicating that charge screening is not a major mechanism of HA adsorption for these minerals, and supporting the suggestion that ligand exchange is the main adsorption mechanism to pH- dependent sites. The increase in ionic strength did, however, promote HA adsorption to clay minerals with high zeta potentials. At pH 8 - 9 the order of HA affinity for clay minerals was: palygorskite > sepiolite > montmorillonite = hectorite > kaolinite > illite > talc, emphasizing strong HA interactions with the fibrous clays. This strong affinity was attributed to their large surface areas and to strong interactions with OH groups on these clay surfaces. Results indicated that HA did not enter the intracrystalline channels of the fibrous clays but suggested that their macro-fiber structure facilitates HA adsorption. The sorption of HA to kaolinite further increased in the presence of Cu2+, and the sorption of Cu2+ increased in the presence of HA, due to a number of synergistic effects. This study emphasizes the diverse effects of clay structure and solution chemistry on HA adsorption.
机译:腐殖酸(HA)-粘土配合物因其对土壤结构和环境过程的贡献而闻名。尽管进行了广泛的研究,控制HA吸附的机制仍未得到解决。进行了系统的研究,以表征土壤来源的HA对7种粘土矿物的吸附特性。粘土表面由于结构差异而直接影响HA吸附,而通过改变溶液pH值间接影响HA吸附。对于粘土矿物,在其天然pH值下可以按以下顺序去除HA:伊利石坡缕石>高岭石>海泡石>蒙脱石=锂蒙脱石滑石。高岭石和伊利石去除HA(沉淀和吸附)的原因是它们引起的低pH值导致粘土和HA表面的质子化。尽管pH值低,HA的Zeta电位仍为负,这通过配体交换促进了HA吸附到质子化粘土表面。离子强度并未影响HA对低Zeta电位的粘土矿物的吸附,表明电荷筛选不是HA吸附这些矿物的主要机理,并支持了配体交换是pH依赖位点的主要吸附机理的建议。然而,离子强度的增加确实促进了HA对具有高Zeta电位的粘土矿物的吸附。在pH 8-9下,HA对粘土矿物的亲和力顺序为:坡缕石>海泡石>蒙脱石=锂蒙脱石>高岭石>伊利石>滑石,强调了HA与纤维状粘土的强相互作用。这种强的亲和力归因于它们的大表面积以及与这些粘土表面上的OH基团的强相互作用。结果表明,HA并未进入纤维状粘土的晶内通道,但表明它们的大纤维结构促进了HA的吸附。由于许多协同作用,在Cu 2+存在下,HA对高岭石的吸附进一步增加,而在HA存在下,Cu 2+的吸附增加。这项研究强调了粘土结构和溶液化学性质对HA吸附的不同影响。

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