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Vol 276 Iss. 2
Pages:
123-139
In press

Recent advances in petrophysical properties, mechanical behavior and durability of calcarenite rocks

Authors:
Gioacchino F. Andriani
About authors
  • Head of the Geotechnical Laboratory University of Bari Aldo Moro ▪ Orcid
Date submitted:
2024-07-17
Date accepted:
2025-07-16
Online publication date:
2025-11-21

Abstract

Recent research on predicting petrophysical and mechanical properties of carbonate rocks, integrating textural and microstructural observations with geotechnical measurements, has sparked critical discussions. While some studies present robust experimental methods and fresh insights, others rely on less rigorous approaches. In the Mediterranean area, shallow-water calcarenites crop out along both the coastline and internal areas. Typically, these carbonates are soft and exhibit high porosity, open in type, controlled by the depositional fabric and post-depositional processes. Their strength primarily depends on the type and amount of calcite cement, with water presence significantly impacting their stress-strain behavior. Strength and stiffness decrease markedly in the transition from dry to saturated conditions. Well-cemented calcarenites with early and late diagenetic cement exhibit brittle behavior in both dry and saturated states, whereas poorly cemented types with early calcite cementation alone show brittle behavior when dry and pseudo-ductile to ductile behavior when saturated. Dual-porosity systems, combining micro- and macro-pores, dominate the hydraulic properties of calcarenites, playing a key role in decay mechanisms and patterns. This study compares existing literature with laboratory analyses of calcarenite lithofacies from Apulia and Basilicata (Southern Italy), yielding new insights into their mechanical and physical behavior, as well as durability.

Область исследования:
Geotechnical Engineering and Engineering Geology
Keywords:
calcarenite fabric properties pore system strength stiffness weatherability durability
Go to volume 276

Funding

This research was supported by MIUR (Italian Ministry of Education, University and Research) under Grant 2010 ex MURST 60 % ‘‘Modelli geologico-tecnici, idrogeologici e geofisici per la tutela e la valorizzazione delle risorse naturali, ambientali e culturali’’ (coordinator G.F.Andriani). The research was financially supported by European Community within the Project Interreg III A “WET SYS B” 2000-2006 (responsible G.F.Andriani) and Apulia Region within the Program “CT14” (responsible G.F.Andriani). Work carried out within the framework of the Project MIUR (Italian Ministry of Education, University and Research) 2017-2018 ex MURST 60 % “Engineering geology and hydrogeological studies applied to the protection, development and promotion of geo-resources and historical, artistic and geo-environmental heritage” (responsible G.F.Andriani).

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