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Chinese scholars and overseas scholars have made progress in the field of water content detection in the mantle transition zone

 Last Update: 2022-08-20
 Source: Internet
 Author: User

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Fig.

Under the support of the National Natural Science Foundation of China (Grant No.

Water is one of the key factors affecting the dynamics and processes in the deep earth, and its distribution can change the melting state and rheological properties of mantle minerals.

Professor Huang Qinghua's team and his collaborators combined the global geomagnetic network observation data and the thermosphere-ionosphere coupled physical model to establish a method for alternately inverting the ionospheric field source structure and mantle conductivity distribution for the geomagnetic diurnal signal.

The research combined the observation data of the global geomagnetic network, high temperature and high pressure experiments, thermosphere-ionosphere coupled physical model, global mantle adiabatic temperature model, etc.

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