期刊文献+

Migration mechanism of atrazine in the simulated lake icing process at different freezing temperatures based on density function theory 被引量:1

原文传递
导出
摘要 Atrazine causes concern due to its resistant to biodegradation and could be accumulated in aquatic organisms,causing pollution in lakes.This study measured the concentration of atrazine in ice and the water under ice through a simulated icing experiment and calculated the distribution coefficient K to characterize its migration ability in the freezing process.Furthermore,density functional theory(DFT)calculations were employed to expatiate the migration law of atrazine during icing process.According to the results,it could release more energy into the environment when atrazine staying in water phase(-15.077 kcal/mol)than staying in ice phase(-14.388 kcal/mol),therefore it was beneficial for the migration of atrazine from ice to water.This explains that during the freezing process,the concentration of atrazine in the ice was lower than that in the water.Thermodynamic calculations indicated thatwhen the temperature decreases from268 to 248 K,the internal energy contribution of the compound of atrazine and ice molecule(water cluster)decreases at the same vibrational frequency,resulting in an increase in the free energy difference of the compound from-167.946 to-165.390 kcal/mol.This demonstrated the diminished migratory capacity of atrazine.This study revealed the environmental behavior of atrazine during lake freezing,which was beneficial for the management of atrazine and other pollutants during freezing and environmental protection.
出处 《Journal of Environmental Sciences》 SCIE EI CAS CSCD 2024年第10期45-54,共10页 环境科学学报(英文版)
基金 This work was supported by the Key Research and Development Program of Shandong Province(No.2019GHY112033) the National Natural Science Foundation of China(No.51609207).
  • 相关文献

参考文献1

二级参考文献17

  • 1LIU Wenzhi, ZHANG Quanfa, LIU Guihua. Lake eutrophication associated with geographic location, lake morphology and climate in China [J]. Hydrohiologia, 2010, 644:289-299.
  • 2MURRAY L G, MUDGE S M, NEWTON A, et al. The effect of benthic sediments on dissolved nutrient concentrations and fluxes [J]. Biogeochemistry, 2012, 81:159-178.
  • 3WELCH H E, BERGMANN M A. Effects of snow and ice on the annual cycles of heat and light in aqvaqjuac lakes [ J ]. Can J Vish Aquat Sci, 1987, 44: 1451-1461.
  • 4黄继固,彭祥捷,俞双,等.水体结冰期营养盐和叶绿素a的分布特征[J].吉林大学学报:弹学版,2008,46(6):1231-1236.
  • 5MATTI L, PEKKA K. The Structure and thickness of Lake Paajarvi ice [J]. Geophysica, 2000, 36(1/2) : 233-248.
  • 6国家环境保护总局.水和废水监测分析疗法[M].4版.北京:中国环境科学出版社,2002.
  • 7WEEKSW F, I,EE O S. Ohservation on the physical properties of sea iee at Hopedale, Labrador [J]. Arctic, 1958, 11(3) : 135- 155.
  • 8NAKAWO M, SINHA N K. Growth rate and salinity profile of first-sea ice in the high Arctic [J]. Journal of Glaciology, 1981 , 27 (96) : 315-330.
  • 9THOMAS D, DIECKMANN G S. Sea ice: An introduction to its physics, biology, chemistry and geology [ M1. London: Blackwell Science, 2003.
  • 10THOMAS D N, DIECKMANN G S. Biogeochemistry of Antarctic sea ice [J]. Oceanography and Marine Biology: An Annual Review, 2002, 40: 143-169.

共引文献18

同被引文献9

引证文献1

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