Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study

Abstract Weathering processes and intensity vary according to the predominant environmental conditions as well as the rock’s physical and geotechnical properties in a given area. Jedburgh Abbey Church has been taken as a representative historical building constructed from Carboniferous Old Red Sands...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Kamh, G.M.E. [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2004

Schlagwörter:	Internal Friction Geotechnical Property Stone Surface Geotechnical Parameter Mortar Sample

Anmerkung:	© Springer-Verlag 2004

Übergeordnetes Werk:	Enthalten in: Environmental geology - Berlin : Springer, 1975, 47(2004), 4 vom: 12. Nov., Seite 482-492
Übergeordnetes Werk:	volume:47 ; year:2004 ; number:4 ; day:12 ; month:11 ; pages:482-492

Links:	Volltext

DOI / URN:	10.1007/s00254-004-1168-z

Katalog-ID:	SPR003047911

Internformat


LEADER	01000caa a22002652 4500
001	SPR003047911
003	DE-627
005	20230328142500.0
007	cr uuu---uuuuu
008	201001s2004 xx \|\|\|\|\|o 00\| \|\|eng c
024	7		\|a 10.1007/s00254-004-1168-z \|2 doi
035			\|a (DE-627)SPR003047911
035			\|a (SPR)s00254-004-1168-z-e
040			\|a DE-627 \|b ger \|c DE-627 \|e rakwb
041			\|a eng
100	1		\|a Kamh, G.M.E. \|e verfasserin \|4 aut
245	1	0	\|a Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study
264		1	\|c 2004
336			\|a Text \|b txt \|2 rdacontent
337			\|a Computermedien \|b c \|2 rdamedia
338			\|a Online-Ressource \|b cr \|2 rdacarrier
500			\|a © Springer-Verlag 2004
520			\|a Abstract Weathering processes and intensity vary according to the predominant environmental conditions as well as the rock’s physical and geotechnical properties in a given area. Jedburgh Abbey Church has been taken as a representative historical building constructed from Carboniferous Old Red Sandstone at humid pre-glacial region. The research aims to examine weathering processes and intensity under the environmental conditions of high relative humidity and low temperature, and to determine the output of weathering through an examination of the rock’s petrological and geotechnical properties. Thin section study, scanning electron microscope and X-ray fluorescence techniques have been used to examine the rock’s petrography and mineralogy on one hand and to determine weathering products on a microscale on the other hand. It is noted that the Carboniferous Old Red Sandstone has a quartz arenite texture with iron oxide and dolomite within its texture, authigenic clays are also detected. Pitting of quartz grains, exfoliation of silica overgrowth and fragmentation of the rock’s feldspar can be noted on a microscale resulting in recession of the rock’s components cohesion. The geotechnical results indicated variation in the physical nature of the construction rock from inside to outside the church with recession from the former to the latter due to weathering. The great reduction in mortar and the rock’s calcium oxide and high content of both sulphur and chlorine from inside to outside the church is a result of weathering and deposition of air pollutants on the stone’s surface on the outdoor surfaces. Chemical weathering, e.g. salt hydration and chemical alteration of the rock’s carbonate content to sulphate and chloride salts is expected to dominate in the study area at such conditions of low temperature and high relative humidity accompanied with air pollutants.
650		4	\|a Internal Friction \|7 (dpeaa)DE-He213
650		4	\|a Geotechnical Property \|7 (dpeaa)DE-He213
650		4	\|a Stone Surface \|7 (dpeaa)DE-He213
650		4	\|a Geotechnical Parameter \|7 (dpeaa)DE-He213
650		4	\|a Mortar Sample \|7 (dpeaa)DE-He213
773	0	8	\|i Enthalten in \|t Environmental geology \|d Berlin : Springer, 1975 \|g 47(2004), 4 vom: 12. Nov., Seite 482-492 \|w (DE-627)253722586 \|w (DE-600)1459034-7 \|x 1432-0495 \|7 nnns
773	1	8	\|g volume:47 \|g year:2004 \|g number:4 \|g day:12 \|g month:11 \|g pages:482-492
856	4	0	\|u https://dx.doi.org/10.1007/s00254-004-1168-z \|z lizenzpflichtig \|3 Volltext
912			\|a GBV_USEFLAG_A
912			\|a SYSFLAG_A
912			\|a GBV_SPRINGER
912			\|a GBV_ILN_20
912			\|a GBV_ILN_24
912			\|a GBV_ILN_31
912			\|a GBV_ILN_40
912			\|a GBV_ILN_63
912			\|a GBV_ILN_70
912			\|a GBV_ILN_73
912			\|a GBV_ILN_74
912			\|a GBV_ILN_90
912			\|a GBV_ILN_95
912			\|a GBV_ILN_100
912			\|a GBV_ILN_110
912			\|a GBV_ILN_120
912			\|a GBV_ILN_150
912			\|a GBV_ILN_151
912			\|a GBV_ILN_161
912			\|a GBV_ILN_267
912			\|a GBV_ILN_285
912			\|a GBV_ILN_293
912			\|a GBV_ILN_702
912			\|a GBV_ILN_2001
912			\|a GBV_ILN_2003
912			\|a GBV_ILN_2007
912			\|a GBV_ILN_2009
912			\|a GBV_ILN_2011
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_2015
912			\|a GBV_ILN_2018
912			\|a GBV_ILN_2021
912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2026
912			\|a GBV_ILN_2031
912			\|a GBV_ILN_2034
912			\|a GBV_ILN_2037
912			\|a GBV_ILN_2038
912			\|a GBV_ILN_2039
912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2055
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
912			\|a GBV_ILN_2068
912			\|a GBV_ILN_2070
912			\|a GBV_ILN_2086
912			\|a GBV_ILN_2106
912			\|a GBV_ILN_2108
912			\|a GBV_ILN_2111
912			\|a GBV_ILN_2112
912			\|a GBV_ILN_2113
912			\|a GBV_ILN_2116
912			\|a GBV_ILN_2118
912			\|a GBV_ILN_2119
912			\|a GBV_ILN_2122
912			\|a GBV_ILN_2129
912			\|a GBV_ILN_2143
912			\|a GBV_ILN_2144
912			\|a GBV_ILN_2147
912			\|a GBV_ILN_2148
912			\|a GBV_ILN_2152
912			\|a GBV_ILN_2153
912			\|a GBV_ILN_2188
912			\|a GBV_ILN_2190
912			\|a GBV_ILN_2232
912			\|a GBV_ILN_4012
912			\|a GBV_ILN_4035
912			\|a GBV_ILN_4037
912			\|a GBV_ILN_4112
912			\|a GBV_ILN_4125
912			\|a GBV_ILN_4126
912			\|a GBV_ILN_4242
912			\|a GBV_ILN_4246
912			\|a GBV_ILN_4249
912			\|a GBV_ILN_4251
912			\|a GBV_ILN_4305
912			\|a GBV_ILN_4307
912			\|a GBV_ILN_4313
912			\|a GBV_ILN_4322
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
912			\|a GBV_ILN_4328
912			\|a GBV_ILN_4333
912			\|a GBV_ILN_4338
951			\|a AR
952			\|d 47 \|j 2004 \|e 4 \|b 12 \|c 11 \|h 482-492

Indexfelder

author_variant	g k gk
matchkey_str	article:14320495:2004----::eteigtihaiueoteabnfruodesnsoeergahcngoehiaivsiainjd
hierarchy_sort_str	2004
publishDate	2004
allfields	10.1007/s00254-004-1168-z doi (DE-627)SPR003047911 (SPR)s00254-004-1168-z-e DE-627 ger DE-627 rakwb eng Kamh, G.M.E. verfasserin aut Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2004 Abstract Weathering processes and intensity vary according to the predominant environmental conditions as well as the rock’s physical and geotechnical properties in a given area. Jedburgh Abbey Church has been taken as a representative historical building constructed from Carboniferous Old Red Sandstone at humid pre-glacial region. The research aims to examine weathering processes and intensity under the environmental conditions of high relative humidity and low temperature, and to determine the output of weathering through an examination of the rock’s petrological and geotechnical properties. Thin section study, scanning electron microscope and X-ray fluorescence techniques have been used to examine the rock’s petrography and mineralogy on one hand and to determine weathering products on a microscale on the other hand. It is noted that the Carboniferous Old Red Sandstone has a quartz arenite texture with iron oxide and dolomite within its texture, authigenic clays are also detected. Pitting of quartz grains, exfoliation of silica overgrowth and fragmentation of the rock’s feldspar can be noted on a microscale resulting in recession of the rock’s components cohesion. The geotechnical results indicated variation in the physical nature of the construction rock from inside to outside the church with recession from the former to the latter due to weathering. The great reduction in mortar and the rock’s calcium oxide and high content of both sulphur and chlorine from inside to outside the church is a result of weathering and deposition of air pollutants on the stone’s surface on the outdoor surfaces. Chemical weathering, e.g. salt hydration and chemical alteration of the rock’s carbonate content to sulphate and chloride salts is expected to dominate in the study area at such conditions of low temperature and high relative humidity accompanied with air pollutants. Internal Friction (dpeaa)DE-He213 Geotechnical Property (dpeaa)DE-He213 Stone Surface (dpeaa)DE-He213 Geotechnical Parameter (dpeaa)DE-He213 Mortar Sample (dpeaa)DE-He213 Enthalten in Environmental geology Berlin : Springer, 1975 47(2004), 4 vom: 12. Nov., Seite 482-492 (DE-627)253722586 (DE-600)1459034-7 1432-0495 nnns volume:47 year:2004 number:4 day:12 month:11 pages:482-492 https://dx.doi.org/10.1007/s00254-004-1168-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4338 AR 47 2004 4 12 11 482-492
spelling	10.1007/s00254-004-1168-z doi (DE-627)SPR003047911 (SPR)s00254-004-1168-z-e DE-627 ger DE-627 rakwb eng Kamh, G.M.E. verfasserin aut Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2004 Abstract Weathering processes and intensity vary according to the predominant environmental conditions as well as the rock’s physical and geotechnical properties in a given area. Jedburgh Abbey Church has been taken as a representative historical building constructed from Carboniferous Old Red Sandstone at humid pre-glacial region. The research aims to examine weathering processes and intensity under the environmental conditions of high relative humidity and low temperature, and to determine the output of weathering through an examination of the rock’s petrological and geotechnical properties. Thin section study, scanning electron microscope and X-ray fluorescence techniques have been used to examine the rock’s petrography and mineralogy on one hand and to determine weathering products on a microscale on the other hand. It is noted that the Carboniferous Old Red Sandstone has a quartz arenite texture with iron oxide and dolomite within its texture, authigenic clays are also detected. Pitting of quartz grains, exfoliation of silica overgrowth and fragmentation of the rock’s feldspar can be noted on a microscale resulting in recession of the rock’s components cohesion. The geotechnical results indicated variation in the physical nature of the construction rock from inside to outside the church with recession from the former to the latter due to weathering. The great reduction in mortar and the rock’s calcium oxide and high content of both sulphur and chlorine from inside to outside the church is a result of weathering and deposition of air pollutants on the stone’s surface on the outdoor surfaces. Chemical weathering, e.g. salt hydration and chemical alteration of the rock’s carbonate content to sulphate and chloride salts is expected to dominate in the study area at such conditions of low temperature and high relative humidity accompanied with air pollutants. Internal Friction (dpeaa)DE-He213 Geotechnical Property (dpeaa)DE-He213 Stone Surface (dpeaa)DE-He213 Geotechnical Parameter (dpeaa)DE-He213 Mortar Sample (dpeaa)DE-He213 Enthalten in Environmental geology Berlin : Springer, 1975 47(2004), 4 vom: 12. Nov., Seite 482-492 (DE-627)253722586 (DE-600)1459034-7 1432-0495 nnns volume:47 year:2004 number:4 day:12 month:11 pages:482-492 https://dx.doi.org/10.1007/s00254-004-1168-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4338 AR 47 2004 4 12 11 482-492
allfields_unstemmed	10.1007/s00254-004-1168-z doi (DE-627)SPR003047911 (SPR)s00254-004-1168-z-e DE-627 ger DE-627 rakwb eng Kamh, G.M.E. verfasserin aut Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2004 Abstract Weathering processes and intensity vary according to the predominant environmental conditions as well as the rock’s physical and geotechnical properties in a given area. Jedburgh Abbey Church has been taken as a representative historical building constructed from Carboniferous Old Red Sandstone at humid pre-glacial region. The research aims to examine weathering processes and intensity under the environmental conditions of high relative humidity and low temperature, and to determine the output of weathering through an examination of the rock’s petrological and geotechnical properties. Thin section study, scanning electron microscope and X-ray fluorescence techniques have been used to examine the rock’s petrography and mineralogy on one hand and to determine weathering products on a microscale on the other hand. It is noted that the Carboniferous Old Red Sandstone has a quartz arenite texture with iron oxide and dolomite within its texture, authigenic clays are also detected. Pitting of quartz grains, exfoliation of silica overgrowth and fragmentation of the rock’s feldspar can be noted on a microscale resulting in recession of the rock’s components cohesion. The geotechnical results indicated variation in the physical nature of the construction rock from inside to outside the church with recession from the former to the latter due to weathering. The great reduction in mortar and the rock’s calcium oxide and high content of both sulphur and chlorine from inside to outside the church is a result of weathering and deposition of air pollutants on the stone’s surface on the outdoor surfaces. Chemical weathering, e.g. salt hydration and chemical alteration of the rock’s carbonate content to sulphate and chloride salts is expected to dominate in the study area at such conditions of low temperature and high relative humidity accompanied with air pollutants. Internal Friction (dpeaa)DE-He213 Geotechnical Property (dpeaa)DE-He213 Stone Surface (dpeaa)DE-He213 Geotechnical Parameter (dpeaa)DE-He213 Mortar Sample (dpeaa)DE-He213 Enthalten in Environmental geology Berlin : Springer, 1975 47(2004), 4 vom: 12. Nov., Seite 482-492 (DE-627)253722586 (DE-600)1459034-7 1432-0495 nnns volume:47 year:2004 number:4 day:12 month:11 pages:482-492 https://dx.doi.org/10.1007/s00254-004-1168-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4338 AR 47 2004 4 12 11 482-492
allfieldsGer	10.1007/s00254-004-1168-z doi (DE-627)SPR003047911 (SPR)s00254-004-1168-z-e DE-627 ger DE-627 rakwb eng Kamh, G.M.E. verfasserin aut Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2004 Abstract Weathering processes and intensity vary according to the predominant environmental conditions as well as the rock’s physical and geotechnical properties in a given area. Jedburgh Abbey Church has been taken as a representative historical building constructed from Carboniferous Old Red Sandstone at humid pre-glacial region. The research aims to examine weathering processes and intensity under the environmental conditions of high relative humidity and low temperature, and to determine the output of weathering through an examination of the rock’s petrological and geotechnical properties. Thin section study, scanning electron microscope and X-ray fluorescence techniques have been used to examine the rock’s petrography and mineralogy on one hand and to determine weathering products on a microscale on the other hand. It is noted that the Carboniferous Old Red Sandstone has a quartz arenite texture with iron oxide and dolomite within its texture, authigenic clays are also detected. Pitting of quartz grains, exfoliation of silica overgrowth and fragmentation of the rock’s feldspar can be noted on a microscale resulting in recession of the rock’s components cohesion. The geotechnical results indicated variation in the physical nature of the construction rock from inside to outside the church with recession from the former to the latter due to weathering. The great reduction in mortar and the rock’s calcium oxide and high content of both sulphur and chlorine from inside to outside the church is a result of weathering and deposition of air pollutants on the stone’s surface on the outdoor surfaces. Chemical weathering, e.g. salt hydration and chemical alteration of the rock’s carbonate content to sulphate and chloride salts is expected to dominate in the study area at such conditions of low temperature and high relative humidity accompanied with air pollutants. Internal Friction (dpeaa)DE-He213 Geotechnical Property (dpeaa)DE-He213 Stone Surface (dpeaa)DE-He213 Geotechnical Parameter (dpeaa)DE-He213 Mortar Sample (dpeaa)DE-He213 Enthalten in Environmental geology Berlin : Springer, 1975 47(2004), 4 vom: 12. Nov., Seite 482-492 (DE-627)253722586 (DE-600)1459034-7 1432-0495 nnns volume:47 year:2004 number:4 day:12 month:11 pages:482-492 https://dx.doi.org/10.1007/s00254-004-1168-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4338 AR 47 2004 4 12 11 482-492
allfieldsSound	10.1007/s00254-004-1168-z doi (DE-627)SPR003047911 (SPR)s00254-004-1168-z-e DE-627 ger DE-627 rakwb eng Kamh, G.M.E. verfasserin aut Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2004 Abstract Weathering processes and intensity vary according to the predominant environmental conditions as well as the rock’s physical and geotechnical properties in a given area. Jedburgh Abbey Church has been taken as a representative historical building constructed from Carboniferous Old Red Sandstone at humid pre-glacial region. The research aims to examine weathering processes and intensity under the environmental conditions of high relative humidity and low temperature, and to determine the output of weathering through an examination of the rock’s petrological and geotechnical properties. Thin section study, scanning electron microscope and X-ray fluorescence techniques have been used to examine the rock’s petrography and mineralogy on one hand and to determine weathering products on a microscale on the other hand. It is noted that the Carboniferous Old Red Sandstone has a quartz arenite texture with iron oxide and dolomite within its texture, authigenic clays are also detected. Pitting of quartz grains, exfoliation of silica overgrowth and fragmentation of the rock’s feldspar can be noted on a microscale resulting in recession of the rock’s components cohesion. The geotechnical results indicated variation in the physical nature of the construction rock from inside to outside the church with recession from the former to the latter due to weathering. The great reduction in mortar and the rock’s calcium oxide and high content of both sulphur and chlorine from inside to outside the church is a result of weathering and deposition of air pollutants on the stone’s surface on the outdoor surfaces. Chemical weathering, e.g. salt hydration and chemical alteration of the rock’s carbonate content to sulphate and chloride salts is expected to dominate in the study area at such conditions of low temperature and high relative humidity accompanied with air pollutants. Internal Friction (dpeaa)DE-He213 Geotechnical Property (dpeaa)DE-He213 Stone Surface (dpeaa)DE-He213 Geotechnical Parameter (dpeaa)DE-He213 Mortar Sample (dpeaa)DE-He213 Enthalten in Environmental geology Berlin : Springer, 1975 47(2004), 4 vom: 12. Nov., Seite 482-492 (DE-627)253722586 (DE-600)1459034-7 1432-0495 nnns volume:47 year:2004 number:4 day:12 month:11 pages:482-492 https://dx.doi.org/10.1007/s00254-004-1168-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4338 AR 47 2004 4 12 11 482-492
language	English
source	Enthalten in Environmental geology 47(2004), 4 vom: 12. Nov., Seite 482-492 volume:47 year:2004 number:4 day:12 month:11 pages:482-492
sourceStr	Enthalten in Environmental geology 47(2004), 4 vom: 12. Nov., Seite 482-492 volume:47 year:2004 number:4 day:12 month:11 pages:482-492
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Internal Friction Geotechnical Property Stone Surface Geotechnical Parameter Mortar Sample
isfreeaccess_bool	false
container_title	Environmental geology
authorswithroles_txt_mv	Kamh, G.M.E. @@aut@@
publishDateDaySort_date	2004-11-12T00:00:00Z
hierarchy_top_id	253722586
id	SPR003047911
language_de	englisch
fullrecord	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR003047911</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230328142500.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201001s2004 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00254-004-1168-z</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR003047911</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s00254-004-1168-z-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Kamh, G.M.E.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2004</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag 2004</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Weathering processes and intensity vary according to the predominant environmental conditions as well as the rock’s physical and geotechnical properties in a given area. Jedburgh Abbey Church has been taken as a representative historical building constructed from Carboniferous Old Red Sandstone at humid pre-glacial region. The research aims to examine weathering processes and intensity under the environmental conditions of high relative humidity and low temperature, and to determine the output of weathering through an examination of the rock’s petrological and geotechnical properties. Thin section study, scanning electron microscope and X-ray fluorescence techniques have been used to examine the rock’s petrography and mineralogy on one hand and to determine weathering products on a microscale on the other hand. It is noted that the Carboniferous Old Red Sandstone has a quartz arenite texture with iron oxide and dolomite within its texture, authigenic clays are also detected. Pitting of quartz grains, exfoliation of silica overgrowth and fragmentation of the rock’s feldspar can be noted on a microscale resulting in recession of the rock’s components cohesion. The geotechnical results indicated variation in the physical nature of the construction rock from inside to outside the church with recession from the former to the latter due to weathering. The great reduction in mortar and the rock’s calcium oxide and high content of both sulphur and chlorine from inside to outside the church is a result of weathering and deposition of air pollutants on the stone’s surface on the outdoor surfaces. Chemical weathering, e.g. salt hydration and chemical alteration of the rock’s carbonate content to sulphate and chloride salts is expected to dominate in the study area at such conditions of low temperature and high relative humidity accompanied with air pollutants.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Internal Friction</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geotechnical Property</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Stone Surface</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geotechnical Parameter</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mortar Sample</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Environmental geology</subfield><subfield code="d">Berlin : Springer, 1975</subfield><subfield code="g">47(2004), 4 vom: 12. Nov., Seite 482-492</subfield><subfield code="w">(DE-627)253722586</subfield><subfield code="w">(DE-600)1459034-7</subfield><subfield code="x">1432-0495</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:47</subfield><subfield code="g">year:2004</subfield><subfield code="g">number:4</subfield><subfield code="g">day:12</subfield><subfield code="g">month:11</subfield><subfield code="g">pages:482-492</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/s00254-004-1168-z</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_SPRINGER</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_74</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_90</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_100</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_120</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_150</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_267</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_702</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2001</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2007</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2009</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2011</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2021</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2025</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2026</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2031</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2034</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2038</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2039</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2044</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2055</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2059</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2064</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2065</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2068</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2070</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2086</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2106</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2108</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2111</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2113</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2116</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2118</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2119</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2122</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2129</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2143</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2144</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2147</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2148</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2152</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2153</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2188</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2190</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2232</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4035</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4242</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4246</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4251</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4328</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4333</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">47</subfield><subfield code="j">2004</subfield><subfield code="e">4</subfield><subfield code="b">12</subfield><subfield code="c">11</subfield><subfield code="h">482-492</subfield></datafield></record></collection>
author	Kamh, G.M.E.
spellingShingle	Kamh, G.M.E. misc Internal Friction misc Geotechnical Property misc Stone Surface misc Geotechnical Parameter misc Mortar Sample Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study
authorStr	Kamh, G.M.E.
ppnlink_with_tag_str_mv	@@773@@(DE-627)253722586
format	electronic Article
delete_txt_mv	keep
author_role	aut
collection	springer
remote_str	true
illustrated	Not Illustrated
issn	1432-0495
topic_title	Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study Internal Friction (dpeaa)DE-He213 Geotechnical Property (dpeaa)DE-He213 Stone Surface (dpeaa)DE-He213 Geotechnical Parameter (dpeaa)DE-He213 Mortar Sample (dpeaa)DE-He213
topic	misc Internal Friction misc Geotechnical Property misc Stone Surface misc Geotechnical Parameter misc Mortar Sample
topic_unstemmed	misc Internal Friction misc Geotechnical Property misc Stone Surface misc Geotechnical Parameter misc Mortar Sample
topic_browse	misc Internal Friction misc Geotechnical Property misc Stone Surface misc Geotechnical Parameter misc Mortar Sample
format_facet	Elektronische Aufsätze Aufsätze Elektronische Ressource
format_main_str_mv	Text Zeitschrift/Artikel
carriertype_str_mv	cr
hierarchy_parent_title	Environmental geology
hierarchy_parent_id	253722586
hierarchy_top_title	Environmental geology
isfreeaccess_txt	false
familylinks_str_mv	(DE-627)253722586 (DE-600)1459034-7
title	Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study
ctrlnum	(DE-627)SPR003047911 (SPR)s00254-004-1168-z-e
title_full	Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study
author_sort	Kamh, G.M.E.
journal	Environmental geology
journalStr	Environmental geology
lang_code	eng
isOA_bool	false
recordtype	marc
publishDateSort	2004
contenttype_str_mv	txt
container_start_page	482
author_browse	Kamh, G.M.E.
container_volume	47
format_se	Elektronische Aufsätze
author-letter	Kamh, G.M.E.
doi_str_mv	10.1007/s00254-004-1168-z
title_sort	weathering at high latitudes on the carboniferous old red sandstone, petrographic and geotechnical investigations, jedburgh abbey church, scotland, a case study
title_auth	Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study
abstract	Abstract Weathering processes and intensity vary according to the predominant environmental conditions as well as the rock’s physical and geotechnical properties in a given area. Jedburgh Abbey Church has been taken as a representative historical building constructed from Carboniferous Old Red Sandstone at humid pre-glacial region. The research aims to examine weathering processes and intensity under the environmental conditions of high relative humidity and low temperature, and to determine the output of weathering through an examination of the rock’s petrological and geotechnical properties. Thin section study, scanning electron microscope and X-ray fluorescence techniques have been used to examine the rock’s petrography and mineralogy on one hand and to determine weathering products on a microscale on the other hand. It is noted that the Carboniferous Old Red Sandstone has a quartz arenite texture with iron oxide and dolomite within its texture, authigenic clays are also detected. Pitting of quartz grains, exfoliation of silica overgrowth and fragmentation of the rock’s feldspar can be noted on a microscale resulting in recession of the rock’s components cohesion. The geotechnical results indicated variation in the physical nature of the construction rock from inside to outside the church with recession from the former to the latter due to weathering. The great reduction in mortar and the rock’s calcium oxide and high content of both sulphur and chlorine from inside to outside the church is a result of weathering and deposition of air pollutants on the stone’s surface on the outdoor surfaces. Chemical weathering, e.g. salt hydration and chemical alteration of the rock’s carbonate content to sulphate and chloride salts is expected to dominate in the study area at such conditions of low temperature and high relative humidity accompanied with air pollutants. © Springer-Verlag 2004
abstractGer	Abstract Weathering processes and intensity vary according to the predominant environmental conditions as well as the rock’s physical and geotechnical properties in a given area. Jedburgh Abbey Church has been taken as a representative historical building constructed from Carboniferous Old Red Sandstone at humid pre-glacial region. The research aims to examine weathering processes and intensity under the environmental conditions of high relative humidity and low temperature, and to determine the output of weathering through an examination of the rock’s petrological and geotechnical properties. Thin section study, scanning electron microscope and X-ray fluorescence techniques have been used to examine the rock’s petrography and mineralogy on one hand and to determine weathering products on a microscale on the other hand. It is noted that the Carboniferous Old Red Sandstone has a quartz arenite texture with iron oxide and dolomite within its texture, authigenic clays are also detected. Pitting of quartz grains, exfoliation of silica overgrowth and fragmentation of the rock’s feldspar can be noted on a microscale resulting in recession of the rock’s components cohesion. The geotechnical results indicated variation in the physical nature of the construction rock from inside to outside the church with recession from the former to the latter due to weathering. The great reduction in mortar and the rock’s calcium oxide and high content of both sulphur and chlorine from inside to outside the church is a result of weathering and deposition of air pollutants on the stone’s surface on the outdoor surfaces. Chemical weathering, e.g. salt hydration and chemical alteration of the rock’s carbonate content to sulphate and chloride salts is expected to dominate in the study area at such conditions of low temperature and high relative humidity accompanied with air pollutants. © Springer-Verlag 2004
abstract_unstemmed	Abstract Weathering processes and intensity vary according to the predominant environmental conditions as well as the rock’s physical and geotechnical properties in a given area. Jedburgh Abbey Church has been taken as a representative historical building constructed from Carboniferous Old Red Sandstone at humid pre-glacial region. The research aims to examine weathering processes and intensity under the environmental conditions of high relative humidity and low temperature, and to determine the output of weathering through an examination of the rock’s petrological and geotechnical properties. Thin section study, scanning electron microscope and X-ray fluorescence techniques have been used to examine the rock’s petrography and mineralogy on one hand and to determine weathering products on a microscale on the other hand. It is noted that the Carboniferous Old Red Sandstone has a quartz arenite texture with iron oxide and dolomite within its texture, authigenic clays are also detected. Pitting of quartz grains, exfoliation of silica overgrowth and fragmentation of the rock’s feldspar can be noted on a microscale resulting in recession of the rock’s components cohesion. The geotechnical results indicated variation in the physical nature of the construction rock from inside to outside the church with recession from the former to the latter due to weathering. The great reduction in mortar and the rock’s calcium oxide and high content of both sulphur and chlorine from inside to outside the church is a result of weathering and deposition of air pollutants on the stone’s surface on the outdoor surfaces. Chemical weathering, e.g. salt hydration and chemical alteration of the rock’s carbonate content to sulphate and chloride salts is expected to dominate in the study area at such conditions of low temperature and high relative humidity accompanied with air pollutants. © Springer-Verlag 2004
collection_details	GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4338
container_issue	4
title_short	Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study
url	https://dx.doi.org/10.1007/s00254-004-1168-z
remote_bool	true
ppnlink	253722586
mediatype_str_mv	c
isOA_txt	false
hochschulschrift_bool	false
doi_str	10.1007/s00254-004-1168-z
up_date	2024-07-03T16:58:19.261Z
_version_	1803577877345599488
fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR003047911</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230328142500.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201001s2004 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00254-004-1168-z</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR003047911</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s00254-004-1168-z-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Kamh, G.M.E.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2004</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag 2004</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Weathering processes and intensity vary according to the predominant environmental conditions as well as the rock’s physical and geotechnical properties in a given area. Jedburgh Abbey Church has been taken as a representative historical building constructed from Carboniferous Old Red Sandstone at humid pre-glacial region. The research aims to examine weathering processes and intensity under the environmental conditions of high relative humidity and low temperature, and to determine the output of weathering through an examination of the rock’s petrological and geotechnical properties. Thin section study, scanning electron microscope and X-ray fluorescence techniques have been used to examine the rock’s petrography and mineralogy on one hand and to determine weathering products on a microscale on the other hand. It is noted that the Carboniferous Old Red Sandstone has a quartz arenite texture with iron oxide and dolomite within its texture, authigenic clays are also detected. Pitting of quartz grains, exfoliation of silica overgrowth and fragmentation of the rock’s feldspar can be noted on a microscale resulting in recession of the rock’s components cohesion. The geotechnical results indicated variation in the physical nature of the construction rock from inside to outside the church with recession from the former to the latter due to weathering. The great reduction in mortar and the rock’s calcium oxide and high content of both sulphur and chlorine from inside to outside the church is a result of weathering and deposition of air pollutants on the stone’s surface on the outdoor surfaces. Chemical weathering, e.g. salt hydration and chemical alteration of the rock’s carbonate content to sulphate and chloride salts is expected to dominate in the study area at such conditions of low temperature and high relative humidity accompanied with air pollutants.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Internal Friction</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geotechnical Property</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Stone Surface</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geotechnical Parameter</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mortar Sample</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Environmental geology</subfield><subfield code="d">Berlin : Springer, 1975</subfield><subfield code="g">47(2004), 4 vom: 12. Nov., Seite 482-492</subfield><subfield code="w">(DE-627)253722586</subfield><subfield code="w">(DE-600)1459034-7</subfield><subfield code="x">1432-0495</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:47</subfield><subfield code="g">year:2004</subfield><subfield code="g">number:4</subfield><subfield code="g">day:12</subfield><subfield code="g">month:11</subfield><subfield code="g">pages:482-492</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/s00254-004-1168-z</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_SPRINGER</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_74</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_90</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_100</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_120</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_150</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_267</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_702</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2001</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2007</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2009</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2011</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2021</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2025</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2026</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2031</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2034</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2038</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2039</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2044</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2055</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2059</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2064</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2065</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2068</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2070</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2086</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2106</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2108</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2111</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2113</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2116</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2118</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2119</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2122</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2129</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2143</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2144</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2147</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2148</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2152</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2153</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2188</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2190</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2232</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4035</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4242</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4246</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4251</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4328</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4333</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">47</subfield><subfield code="j">2004</subfield><subfield code="e">4</subfield><subfield code="b">12</subfield><subfield code="c">11</subfield><subfield code="h">482-492</subfield></datafield></record></collection>
score	7.4017296

Nicht das Richtige dabei?

Schreiben Sie uns!

Weathering at high latitudes on the Carboniferous Old Red Sandstone, petrographic and geotechnical investigations, Jedburgh Abbey Church, Scotland, a case study

Nicht das Richtige dabei?

Zugang & Verfügbarkeit

Vorhandene Bände

Nicht das Richtige dabei?