Context: Recently, a study by an international team of researchers revealed the formation of a new enigmatic layer E prime layer at the outermost part of Earth's core.
E Prime Layer
About: There was a belief that the exchange of material between the core and mantle is minimal.
Experimental Discovery: However, experiments have shown that when water reaches the core-mantle boundary, it undergoes a reaction with silicon in the core, resulting in the formation of silica.
Earth comprises four primary layers: an inner core at the planet's center, surrounded by the outer core, mantle, and crust
How did this layer develop over time?
This latest research suggests that tectonic plates carrying surface water have transported it deep into the Earth over billions of years.
Upon reaching the core-mantle boundary about 1,800 miles below the surface, this water initiates significant chemical changes, influencing the core's structure.
This reaction leads to the formation of a hydrogen-rich, silicon-depleted layer at the outer core, resembling a film-like structure.
Silica crystals generated by this process ascend and blend into the mantle, impacting the overall composition.
These modifications in the liquid metallic layer could potentially result in reduced density and altered seismic characteristics, aligning with anomalies detected by seismologists.
Significance of Research
This discovery enhances our comprehension of Earth's internal mechanisms, indicating a broader and more intricate global water cycle than previously acknowledged.
The transformed layer in the core holds significant implications for the interconnected geochemical processes linking surface water cycles with the deep metallic core.