Inerti

Gli aggregati da un punto di vista geologico sono materiali detritici, sciolti o cementati, derivati dall’alterazione e disgregazione delle masse rocciose, si caratterizzano in base alla tessitura clastica, dalla forma e dalla disposizione delle particelle nell’aggregato.
Gli inerti o aggregati possono essere naturali, artificiali o riciclati da materiali precedentemente usati nelle orologi replica costruzioni e comprendono: sabbia, ghiaia, argilla espansa, vermiculite e perlite.
Nel campo dell’edilizia gli inerti sono utilizzati come componenti di materiali compositi, come ad esempio i conglomerati cementizi e i conglomerati bituminosi.

Vengono classificati secondo la granulometria delle loro particelle:


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