The Neapolitan Yellow Tuff (hereafter NYT) is definitely the building material most used in the historicalarchitecture of Naples (Southern Italy) since Greek times.The high heterogeneity of NYT, resulting from the concomitant occurrence of lithic fragments, pumices,crystals and glass cemented by crystalline or amorphous phases, the latter highly sensitive to acid environments,define a strong attitude to weathering.This research confirmed the inhomogeneous features of this volcanic formation, within the samedeposit and sometimes within the same outcrop. Based on these premises, the investigation was carriedout on four most representative lithofacies, according to their different textural and petrophysical features.Actually, mechanical features are governed by two concurring factors: a) the mineralogical composition;b) the texture of the rock. In the first case, the predominance of anhydrous phases (analcime + feldspar)over zeolites improves its mechanical strength. By contrast, if the mineralogical composition isconstant (similar total wt.% zeolite content), the petrophysical parameters are strictly related to the textureof the rock

The Neapolitan Yellow Tuff: An outstanding example of heterogeneity

LANGELLA, Alessio
2017-01-01

Abstract

The Neapolitan Yellow Tuff (hereafter NYT) is definitely the building material most used in the historicalarchitecture of Naples (Southern Italy) since Greek times.The high heterogeneity of NYT, resulting from the concomitant occurrence of lithic fragments, pumices,crystals and glass cemented by crystalline or amorphous phases, the latter highly sensitive to acid environments,define a strong attitude to weathering.This research confirmed the inhomogeneous features of this volcanic formation, within the samedeposit and sometimes within the same outcrop. Based on these premises, the investigation was carriedout on four most representative lithofacies, according to their different textural and petrophysical features.Actually, mechanical features are governed by two concurring factors: a) the mineralogical composition;b) the texture of the rock. In the first case, the predominance of anhydrous phases (analcime + feldspar)over zeolites improves its mechanical strength. By contrast, if the mineralogical composition isconstant (similar total wt.% zeolite content), the petrophysical parameters are strictly related to the textureof the rock
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.12070/1052
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