Examples of weathering and deterioration of Tertiary building stones at St. Michaels Cathedral in Cluj-Napoca (Romania)

St. Michaels Cathedral is one of the oldest Gothic architectural monuments in Cluj. It is built predominantly of Cenozoic (Eocene) limestones which were deposited on a shallow carbonate platform. They are composed of different facies and microfacies types with varying amounts of particles, matrix an...

Full description

Bibliographic Details
Main Authors: Roman Koch, Paul Calin Racataianu, Ioan I. Bucur
Format: Article
Language:English
Published: Cluj University Press 2008-10-01
Series:Studia Universitatis Babes-Bolyai: Geologia
Online Access:http://scholarcommons.usf.edu/geologia/vol53/iss2/art3/
id doaj-af11d58b401a4bd9bf1c8cd3bef9a25c
record_format Article
spelling doaj-af11d58b401a4bd9bf1c8cd3bef9a25c2020-11-25T01:14:57ZengCluj University PressStudia Universitatis Babes-Bolyai: Geologia1221-08031937-86022008-10-015322539Examples of weathering and deterioration of Tertiary building stones at St. Michaels Cathedral in Cluj-Napoca (Romania)Roman Koch0Paul Calin Racataianu1Ioan I. Bucur2University of Erlangen, GermanyUniversity of Erlangen, GermanyBabes-Bolyai University of Cluj-NapocaSt. Michaels Cathedral is one of the oldest Gothic architectural monuments in Cluj. It is built predominantly of Cenozoic (Eocene) limestones which were deposited on a shallow carbonate platform. They are composed of different facies and microfacies types with varying amounts of particles, matrix and cement. Limestones from the Baci quarry (Cluj Limestone), which is situated about 3 km from the centre of Cluj, were commonly used. The weathering features correspond to the microfacies types, to the position of the stones in the walls and to the exposure (east, south, west, and north), which controls the moisture/dry cycles. This interrelationship is documented by macroscopic and microscopic examples of the decay of samples analyzed from the lower part of the walls. General parameters for a correct classification of carbonate rocks and their importance for weathering are discussed. The general mechanisms of weathering (thermal expansion, water uptake, freezing, chemical weathering) are described. The migration of moisture (capillarity) and the formation of crusts of varying mineralogy on the surface of building stones are documented. Macroscopic description of damage includes the decay into plates and flakes, the formation of crusts, the formation of fractures, and the growth of lichens and microorganisms. The microscopic analysis documents characteristic damage in detail: fractures parallel to the surface of the stone, internal cementation of fossil chambers (micro-nodules), repeated formation of crusts in varying generations, fracturing in intensively lithified, rigid limestones, and settling of lichens in different positions. Furthermore, different historical mortars and modern “concrete-mortars” and their behaviour in comparison to the adjacent limestones are briefly discussed. The possible conservation and restoration of weathered limestones in St. Michaels Cathedral are discussed with regard to the most recent conservation methods. The advantages and disadvantages of surface conservation by silica ester, hydrophobic substances as well as by epoxy resin are also dealt with. Special methods for conservation (acrylic total impregnation, lime slurry, biological lime slurry) and DIN-methods as well as analysis of the success of the methods used are presented in a short summary. http://scholarcommons.usf.edu/geologia/vol53/iss2/art3/
collection DOAJ
language English
format Article
sources DOAJ
author Roman Koch
Paul Calin Racataianu
Ioan I. Bucur
spellingShingle Roman Koch
Paul Calin Racataianu
Ioan I. Bucur
Examples of weathering and deterioration of Tertiary building stones at St. Michaels Cathedral in Cluj-Napoca (Romania)
Studia Universitatis Babes-Bolyai: Geologia
author_facet Roman Koch
Paul Calin Racataianu
Ioan I. Bucur
author_sort Roman Koch
title Examples of weathering and deterioration of Tertiary building stones at St. Michaels Cathedral in Cluj-Napoca (Romania)
title_short Examples of weathering and deterioration of Tertiary building stones at St. Michaels Cathedral in Cluj-Napoca (Romania)
title_full Examples of weathering and deterioration of Tertiary building stones at St. Michaels Cathedral in Cluj-Napoca (Romania)
title_fullStr Examples of weathering and deterioration of Tertiary building stones at St. Michaels Cathedral in Cluj-Napoca (Romania)
title_full_unstemmed Examples of weathering and deterioration of Tertiary building stones at St. Michaels Cathedral in Cluj-Napoca (Romania)
title_sort examples of weathering and deterioration of tertiary building stones at st. michaels cathedral in cluj-napoca (romania)
publisher Cluj University Press
series Studia Universitatis Babes-Bolyai: Geologia
issn 1221-0803
1937-8602
publishDate 2008-10-01
description St. Michaels Cathedral is one of the oldest Gothic architectural monuments in Cluj. It is built predominantly of Cenozoic (Eocene) limestones which were deposited on a shallow carbonate platform. They are composed of different facies and microfacies types with varying amounts of particles, matrix and cement. Limestones from the Baci quarry (Cluj Limestone), which is situated about 3 km from the centre of Cluj, were commonly used. The weathering features correspond to the microfacies types, to the position of the stones in the walls and to the exposure (east, south, west, and north), which controls the moisture/dry cycles. This interrelationship is documented by macroscopic and microscopic examples of the decay of samples analyzed from the lower part of the walls. General parameters for a correct classification of carbonate rocks and their importance for weathering are discussed. The general mechanisms of weathering (thermal expansion, water uptake, freezing, chemical weathering) are described. The migration of moisture (capillarity) and the formation of crusts of varying mineralogy on the surface of building stones are documented. Macroscopic description of damage includes the decay into plates and flakes, the formation of crusts, the formation of fractures, and the growth of lichens and microorganisms. The microscopic analysis documents characteristic damage in detail: fractures parallel to the surface of the stone, internal cementation of fossil chambers (micro-nodules), repeated formation of crusts in varying generations, fracturing in intensively lithified, rigid limestones, and settling of lichens in different positions. Furthermore, different historical mortars and modern “concrete-mortars” and their behaviour in comparison to the adjacent limestones are briefly discussed. The possible conservation and restoration of weathered limestones in St. Michaels Cathedral are discussed with regard to the most recent conservation methods. The advantages and disadvantages of surface conservation by silica ester, hydrophobic substances as well as by epoxy resin are also dealt with. Special methods for conservation (acrylic total impregnation, lime slurry, biological lime slurry) and DIN-methods as well as analysis of the success of the methods used are presented in a short summary.
url http://scholarcommons.usf.edu/geologia/vol53/iss2/art3/
work_keys_str_mv AT romankoch examplesofweatheringanddeteriorationoftertiarybuildingstonesatstmichaelscathedralinclujnapocaromania
AT paulcalinracataianu examplesofweatheringanddeteriorationoftertiarybuildingstonesatstmichaelscathedralinclujnapocaromania
AT ioanibucur examplesofweatheringanddeteriorationoftertiarybuildingstonesatstmichaelscathedralinclujnapocaromania
_version_ 1725155406932606976