|本期目录/Table of Contents|

[1]李振炫,桂尉竣,苏 畅,等.方解石与柠檬酸/酒石酸模拟实验中的反应规律[J].地球科学与环境学报,2023,45(06):1398-1413.[doi:10.19814/j.jese.2023.06028]
 LI Zhen-xuan,GUI Wei-jun,SU Chang,et al.Reaction Pattern of Calcite with Citric Acid/Tartaric Acid in Simulation Experiments[J].Journal of Earth Sciences and Environment,2023,45(06):1398-1413.[doi:10.19814/j.jese.2023.06028]
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第45卷
期数:
2023年第06期
页码:
1398-1413
栏目:
矿产资源综合利用
出版日期:
2023-11-15

文章信息/Info

Title:
Reaction Pattern of Calcite with Citric Acid/Tartaric Acid in Simulation Experiments
文章编号:
1672-6561(2023)06-1398-16
作者:
李振炫12桂尉竣12苏 畅1向育斌3孙晓雯1吴超越4*黄利东5David DECROOCQ6
(1. 南京信息工程大学 江苏省大气环境与装备技术协同创新中心/江苏省大气环境监测与污染控制高技术重点实验室,江苏 南京 210044; 2. 南京信息工程大学 气候与环境变化教育部国际合作联合实验室,江苏 南京 210044; 3. 南京信息工程大学 化学与材料学院,江苏 南京 210044; 4. 生态环境部南京环境科学研究所,江苏 南京 210042; 5. 南京信息工程大学 应用气象学院,江苏 南京 210044; 6. 里尔大学 地球科学学院,诺尔 里尔 59650)
Author(s):
LI Zhen-xuan12 GUI Wei-jun12 SU Chang1 XIANG Yu-bin3 SUN Xiao-wen1 WU Chao-yue4* HUANG Li-dong5 David DECROOCQ6
(1. Jiangsu Collaborative Innovation Center of Atmospheric Environment and Equipment Technology/Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Nanjing University of Information Science & Technology, Nanjing 210044, Jiangsu, China; 2. Joint International Research Laboratory of Climate and Environment Change(ILCEC), Nanjing University of Information Science & Technology, Nanjing 210044, Jiangsu, China; 3. School of Chemistry and Materials Science, Nanjing University of Information Science & Technology, Nanjing 210044, Jiangsu, China; 4. Nanjing Institute of Environmental Sciences, Ministry of Ecology and Environment, Nanjing 210042, Jiangsu, China; 5. School of Applied Meteorology, Nanjing University of Information Science & Technology, Nanjing 210044, Jiangsu, China; 6. Département des Sciences de la Terre, Université de Lille, Lille 59650, Nord, France)
关键词:
方解石 柠檬酸 酒石酸 吸附 溶解 络合 沉淀 溶液化学
Keywords:
calcite citric acid tartaric acid adsorption dissolution complex precipitation solution chemistry
分类号:
X703.1
DOI:
10.19814/j.jese.2023.06028
文献标志码:
A
摘要:
柠檬酸/酒石酸可使方解石产生矿物溶蚀及生物矿化等现象,研究它们之间的反应规律对富含有机酸环境中方解石矿物的稳定性评估及相应的地球化学效应研究具有重要意义。通过批量平衡法,研究开放系统条件下方解石与柠檬酸/酒石酸之间的反应规律及对应的溶液化学变化。结果表明:①初始浓度为20 mg?L-1条件下,初始pH值由7.7升至9.7,柠檬酸与酒石酸的反应去除量均显著下降,这是由于方解石表面的静电效应及溶液中HCO-3与CO2-3的竞争效应不断增强,对两种酸的表面吸附反应起抑制作用。②初始pH值为7.7及8.3条件下,初始浓度为20 mg?L-1的两种酸与方解石反应7 h后便达到平衡,pH值和Ca浓度较空白值变化不大,辅证了反应的主导机制为表面吸附。③在0~900 mg?L-1浓度范围内,柠檬酸和酒石酸在初始pH值为8.3条件下,其反应去除量均能用Langmuir吸附模型很好地拟合,辅证了以上的反应去除机制均为表面吸附; 初始pH值为7.7条件下,柠檬酸的反应去除量可用Langmuir吸附模型拟合,反应的主导机制仍为表面吸附,而酒石酸的反应去除量呈现持续陡增现象,Langmuir与Freundlich吸附模型均难以拟合,这是由于酒石酸的反应主导机制是沉淀反应。④初始pH值为8.3,在0~900 mg?L-1浓度范围内,在5 ℃、20 ℃、35 ℃温度条件下,两种酸的反应去除结果均可用Langmuir吸附模型拟合,反应的主导机制仍为表面吸附。与酒石酸相比,随着温度的升高,柠檬酸吸附量的增幅更大; 同时,3种温度条件下柠檬酸带来的pH值和Ca浓度增幅均比酒石酸带来的更大。
Abstract:
Citric acid/tartaric acid can cause mineral dissolution and biomineralization of calcite, so the study on reaction pattern between them is of great significance for the assessment of the stability of calcite minerals and the study on the corresponding geochemical effects in organic acid-rich environments. The reaction between calcite and citric acid/tartaric acid and the corresponding solution chemistry change were studied by batch equilibrium method under open system conditions. The results show that ① at the initial concentration of 20 mg?L-1, the reaction removal of citric acid and tartaric acid decreases significantly when the initial pH value increases from 7.7 to 9.7; this is attributed to the electrostatic effect on the surface of calcite and the increasing competition between HCO-3 and CO2-3 in the solution, which inhibit the surface adsorption reaction of the two acids on calcite. ② At the initial pH of 7.7 and 8.3, the reaction of the two acids with an initial concentration of 20 mg?L-1 and calcite reaches equilibrium after 7 h; compared with the blank values, the pH and Ca concentration have little change, which prove that the dominant mechanism of the reaction is surface adsorption. ③ In the concentration range of 0-900 mg?L-1, the reaction removal results of citric acid and tartaric acid at the initial pH of 8.3 could be well fitted by the Langmuir adsorption model, which proves that both of the above removal mechanisms are surface adsorption; at the initial pH of 7.7, the reaction removal results of citric acid still could be fitted by the Langmuir adsorption model, and the removal mechanism is still surface adsorption; while the removal of tartaric acid shows a continuous steep increase, which cannot be fitted by the Langmuir or Freundlich adsorption model, and this is due to the fact that the dominant mechanism of tartaric acid removal by reaction is precipitation reaction. ④ At an initial pH of 8.3, a concentration range of 0-900 mg?L-1 and the temperatures of 5 ℃, 20 ℃, and 35℃, the removal results of both acids could be fitted by the Langmuir adsorption model, and the removal mechanism is still surface adsorption; the increase in the saturation adsorption of citric acid with increasing temperature is greater than that of tartaric acid; meanwhile, citric acid at all three temperatures brings about a greater increase in pH and Ca concentration than that of tartaric acid.

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图11 不同温度下柠檬酸、酒石酸等温吸附的pH值和Ca浓度变化
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备注/Memo

备注/Memo:
收稿日期:2023-06-20; 修回日期:2023-08-25
基金项目:国家自然科学基金项目(41303096,41201515); 教育部留学回国科研启动基金项目(S131304001); 江苏省自然科学基金项目(BK20210655)
作者简介:李振炫(1981-),男,江苏靖江人,副教授,工学博士,E-mail:zhenxuan325@163.com。
*通讯作者:吴超越(1993-),女,江苏如皋人,助理研究员,E-mail:wuchaoyue1206@163.com。
更新日期/Last Update: 2023-12-01