生态与农村环境学报 ›› 2024, Vol. 40 ›› Issue (3): 418-425.doi: 10.19741/j.issn.1673-4831.2023.0696

• 自然保护与生态 • 上一篇    下一篇

不同温度条件下赤铁矿对腐殖酸的吸附性能和机制研究

周灿瑶1, 戴伟1, 栾亚宁1, 王旭琴2   

  1. 1. 北京林业大学林学院/森林培育与保护教育部重点实验室, 北京 100083;
    2. 内蒙古自治区环境监测总站鄂尔多斯分站, 内蒙古鄂尔多斯 017000
  • 收稿日期:2023-07-30 出版日期:2024-03-25 发布日期:2024-03-18
  • 通讯作者: 栾亚宁,E-mail: luanyaning@bjfu.edu.cn E-mail:luanyaning@bjfu.edu.cn
  • 作者简介:周灿瑶(1999-),女,湖南常德人,研究方向为土壤生态。E-mail: 172788826@qq.com
  • 基金资助:
    鄂尔多斯市科技合作重大专项(2021EEDSCXQDFZ012);国家重点研发计划(2017YFC0504404)

Properties and Mechanisms of Humic Acid Adsorption by Hematite at Different Temperatures

ZHOU Can-yao1, DAI Wei1, LUAN Ya-ning1, WANG Xu-qin2   

  1. 1. College of Forestry, Beijing Forestry University/Key Laboratory for Silviculture and Conservation of Ministry of Education, Beijing 100083, China;
    2. Erdos Sub-station of Inner Mongolia Autonomous Region Environmental Monitoring Station, Erdos 017000, China
  • Received:2023-07-30 Online:2024-03-25 Published:2024-03-18

摘要: 为探究温度对土壤矿物吸附有机质的影响,以赤铁矿和腐殖酸为研究对象,通过吸附动力学试验研究不同温度条件下赤铁矿对腐殖酸的吸附行为,并结合扫描电镜(SEM)、能谱仪(EDS)、红外光谱(FTIR)、X射线衍射(XRD)和zeta电位等表征手段深入分析不同温度条件下赤铁矿对腐殖酸的吸附机制。结果表明,25、30、35和40 ℃条件下赤铁矿对腐殖酸的平衡吸附量分别为28.52、28.99、29.74和30.69 mg·g-1,温度越高越有利于赤铁矿对腐殖酸的吸附;相较于准一级动力学模型,准二级动力学模型能更好地用于描述不同温度条件下赤铁矿对腐殖酸的吸附动力学特性,表明吸附速率主要由化学吸附机制决定;随着温度的升高,赤铁矿表面C/Fe比值逐渐变大,单粒粒径逐渐增大,结晶度不断下降,zeta电位呈现先上升后下降的变化过程,红外光谱不同官能团出现不同的变化趋势。综上,温度升高有利于土壤矿物对有机质的固持。

关键词: 腐殖酸, 赤铁矿, 温度, 吸附

Abstract: The effects of temperature on the adsorption of organic matter by soil minerals were investigated by studying the adsorption of humic acid on hematite at different temperatures. Adsorption kinetic tests were performed and the mechanisms of humic acid adsorption on hematite at different temperatures were clarified by using a combination of scanning electron microscopy, energy-dispersive spectroscopy, Fourier-transform infrared (FTIR) spectroscopy, X-ray diffraction, and zeta-potential measurements. The experimental results show that the equilibrium amounts of humic acid adsorbed on hematite at 25, 30, 35, and 40 ℃ were 28.52, 28.99, 29.74, and 30.69 mg·g-1, respectively indicating that the higher the temperatures, the higher the adsorption of humic acid on hematite. The adsorption kinetics of humic acid on hematite at different temperatures were better described by a quasi-secondary kinetic model than by a quasi-primary kinetic model. This indicates that the adsorption rate is mainly determined by a chemisorption mechanism. With increasing temperature, the C/Fe ratio on the hematite surface gradually increased, the single-particle size gradually increased, the crystallinity decreased continuously, and the zeta potential initially increased and then decreased. The FTIR spectra showed that the trends in the amounts of various functional groups present differed. In conclusion, increasing the temperature promotes the adsorption of organic matter by soil minerals.

Key words: humic acid, hematite, temperature, adsorption

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