The average life of oxygen vacancies in quartz from sediments were estimated using ESR signal intensity of E’ centers by thermal activitation technique. The experimental results showed that the second order kinetics equation was more suitable to estimate the average life than the first order kinetic equation. The average life of oxygen vacancies in quartz of sediments form 4895m to 4908m in Tarim basin was about 10 18 years at 27℃
and it was three orders of magnitude bigger than the average life in granitic quartz at the same temperature.
Investigation in the influence of metal-support interactions on the thermal stability of CeO2 nanorods
A technique for measuring nitrogen isotopic composition of nitrate using the denitrifier method
Thermoluminescence age of sediments in Taibei Basin
Study on transportation of sediments and bottom water in the central South China Sea by the total β-ray measurement
Mössbauer effect study of sediments in river mouth of sea area
Related Author
Zhi LIU
Yimin LI
Jian LIU
Zheng PENG
Hui ZHANG
Yong HAN
Beibei WANG
Qingtian LI
Related Institution
State Key Laboratory of Functional Materials for Informatics, Shanghai Institute of Microsystem and Information Technology, Chinese Academy of Sciences
School of Physical Science and Technology, ShanghaiTech University
University of Chinese Academy of Sciences
Institute of Hydrogeology and Environmental Geology,Chinese Academy of Geological Sciences Shijiazhuang