Natural weathering is known as one of the key mechanisms causing degradation in building materials. Great efforts have been made to develop new materials and new processes for protecting those that already exist. Natural stones are an example of a natural material that has been extensively used for building construction since ancient times. In addition, they fit durability, aesthetic, and mechanical requirements. Thus, they still have great importance in the construction business nowadays. Though chemical interactions in natural stones, such as oxidation or hydrolyses, have been widely studied, in the last few decades, the physical weathering due to daily temperature variations has begun to be considered as a key mechanism of degradation an...
Short and long-term climate changes are a critical factor of stone decay even in temperate Mediterra...
Marble slabs, typically used as façade panels to externally cover buildings, might permanently defo...
This paper aims at illustrating the driving forces of thermoclastism and cryoclastism in calcareous ...
Physical and mechanical properties of building stones can vary due to different degradation mechanis...
Within a major framework of studies around artificial weathering and its effects on different lithot...
The interaction between micro-organisms and natural stone surfaces has been studied in great detail ...
The evolution of physical and mechanical properties of four sets of different marble rocks after dif...
none4siSince the effectiveness of stone consolidants significantly depends on the weathering level o...
The consequences of fires on cultural heritage building and monuments can be deleterious, as histori...
Stone decay is affected by the influence of climatic factors. In particular marble degra...
The stone and the clay are the basic elements of the existing architectural heritage in the Mediterr...
ABSTRACT The aim of this paper is to assess the risk of climate-induced damage to stone through the ...
AbstractMarble slabs are frequently used as façade panels to externally cover buildings. In some cas...
Physical weathering of marble, widely used as a cladding material on buildings, is one of the most c...
Natural stone has always been one of the main materials used in architecture for its singular beauty...
Short and long-term climate changes are a critical factor of stone decay even in temperate Mediterra...
Marble slabs, typically used as façade panels to externally cover buildings, might permanently defo...
This paper aims at illustrating the driving forces of thermoclastism and cryoclastism in calcareous ...
Physical and mechanical properties of building stones can vary due to different degradation mechanis...
Within a major framework of studies around artificial weathering and its effects on different lithot...
The interaction between micro-organisms and natural stone surfaces has been studied in great detail ...
The evolution of physical and mechanical properties of four sets of different marble rocks after dif...
none4siSince the effectiveness of stone consolidants significantly depends on the weathering level o...
The consequences of fires on cultural heritage building and monuments can be deleterious, as histori...
Stone decay is affected by the influence of climatic factors. In particular marble degra...
The stone and the clay are the basic elements of the existing architectural heritage in the Mediterr...
ABSTRACT The aim of this paper is to assess the risk of climate-induced damage to stone through the ...
AbstractMarble slabs are frequently used as façade panels to externally cover buildings. In some cas...
Physical weathering of marble, widely used as a cladding material on buildings, is one of the most c...
Natural stone has always been one of the main materials used in architecture for its singular beauty...
Short and long-term climate changes are a critical factor of stone decay even in temperate Mediterra...
Marble slabs, typically used as façade panels to externally cover buildings, might permanently defo...
This paper aims at illustrating the driving forces of thermoclastism and cryoclastism in calcareous ...