Provenance and weathering depth of carbonaceous gotland sandstone by use of carbon and oxygen isotopes

Åberg, Göran; Löfvendahl, Runo; Stijfhoorn, D.E.; Råheim, A.

doi:10.1016/1352-2310(94)00324-e

Cited by 9 publications

(2 citation statements)

References 6 publications

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“…This is likely due to incomplete carbonation which is mentioned above because this is an underground structure. So while the mortar was setting, greater humidity would have stimulated more biological activity and hence more δ 18 O [50]. The difference could also be due to gypsum content.…”

Section: Relative Dating Of the Mortarsmentioning

confidence: 99%

Multi-technical characterization of Roman mortars from Complutum, Spain

Ergenç

Fort

2019

Measurement

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Section: Relative Dating Of the Mortarsmentioning

confidence: 99%

Multi-technical characterization of Roman mortars from Complutum, Spain

Ergenç

Fort

2019

Measurement

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“…Huge and expensive instrumentations, such as laser microprobe [42], nuclear magnetic resonance (NMR) [43], small angle neutron scattering [44] and X-ray computed micro-tomography (micro-CT) [45] have been used to qualitatively determine the thickness of weathered layer. Drilling resistance measurement system (DRMS) is another commonly used technique to detect the thickness of weathered layer.…”

Section: Introductionmentioning

confidence: 99%

Determination on the Thickness of Superficially Weathered Layer of Stone Cultural Relics

Wang,

Luo,

et al. 2023

Preprint

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Weathering is commonly observed in stone cultural relics around the world. Superficial weathering in forms of granular disaggregation, powdering and flaking on the stone surface is one of the most serious damages to the stone relics, since the surface carries most of artistic, historical information. Apparently, the determination on the thickness of superficially weathered layer of stone cultural relics is critical to their conservation. However, the methodology for quantitative analyses of the thickness of superficial weathered layer on stone relics remains very limited. In this study, we carefully study the moisture absorption and pore structure evolution of stone relics with respect to its weathering. We find out that the thickness of superficial weathered layer can be derived from the moisture absorption or pore structure information. Data acquired from these methods are consistent with each other and in well agreement with the results obtained by currently using techniques such as drilling resistance measurement etc.

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Pollutant-Induced Decay of Building Materials

Sanjurjo-Sánchez

Alves

2011

Environmental Chemistry for a Sustainable World

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Provenance and weathering depth of carbonaceous gotland sandstone by use of carbon and oxygen isotopes

Cited by 9 publications

References 6 publications

Multi-technical characterization of Roman mortars from Complutum, Spain

Multi-technical characterization of Roman mortars from Complutum, Spain

Determination on the Thickness of Superficially Weathered Layer of Stone Cultural Relics

Pollutant-Induced Decay of Building Materials

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