SULL'AUMENTO DI TEMPERATURA NEL MANTELLO DELLA TERRA PER COMPRESSIONE ADIABATICA
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Abstract
Viene stabilita una relazione fra la densità, la temperatura e lavelocità delle onde longitudinali e trasversali relativa ad una particolaretrasformazione adiabatica di un solido ideale.L'equazione, applicata al mantello della. Terra, conduce al risultatoche la temperatura in prossimità del nucleo sarebbe circa 1,24volte, la temperatura alla profondità di 1000 km, se la compressionedei materiali fosse avvenuta adiabaticamente.
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Valle PE. SULL’AUMENTO DI TEMPERATURA NEL MANTELLO DELLA TERRA PER COMPRESSIONE ADIABATICA. Ann. Geophys. [Internet]. 1951Nov.25 [cited 2023Dec.8];4(4):475-8. Available from: https://www.annalsofgeophysics.eu/index.php/annals/article/view/5927
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