A multi-analytical approach for pore structure assessment in historic lime mortars

2021 ◽  
Vol 272 ◽  
pp. 121905
Author(s):  
S. Divya Rani ◽  
A.V. Rahul ◽  
Manu Santhanam
2007 ◽  
Vol 37 (7) ◽  
pp. 1059-1069 ◽  
Author(s):  
Robert M. Lawrence ◽  
Timothy J. Mays ◽  
Sean P. Rigby ◽  
Peter Walker ◽  
Dina D'Ayala

2012 ◽  
Vol 116 (35) ◽  
pp. 18816-18823 ◽  
Author(s):  
Matthias Thommes ◽  
Sharon Mitchell ◽  
Javier Pérez-Ramírez

Minerals ◽  
2021 ◽  
Vol 12 (1) ◽  
pp. 30
Author(s):  
Fernanda Carvalho ◽  
Pedro Sousa ◽  
Nuno Leal ◽  
Joaquim Simão ◽  
Elissavet Kavoulaki ◽  
...  

The study of building materials constituting cultural heritage is fundamental to understand their characteristics and predict their behavior. When considering materials from archaeological sites, their characterization can provide not only relevant information for a broader understanding of the site and its importance and significance but can also increase knowledge about ancient materials and their performance. The Palace of Knossos is a very important archaeological site in the European history context, and its preservation benefits from the characterization of the constituent materials. Samples of mortars from this monument were collected under the scope of the H2020 HERACLES project, where a multi-analytical approach was chosen using established protocols for the different sample typologies. Instrumental techniques such as optical microscopy (OM), X-ray diffraction (XRD), Fourier-transform infrared spectroscopy (FTIR), and simultaneous thermogravimetry and differential thermal analysis (TG–DTA) were used for the chemical, mineralogical, and morphological characterization of these mortar samples. The results indicate that the majority are lime mortars, both aerial and hydraulic, but gypsum-based mortars were also identified. Differences in the chemical composition of the samples in distinct areas of the monument allowed us to reflect on the variety of materials used in the construction of the Palace of Knossos.


2019 ◽  
Vol 215 ◽  
pp. 650-668 ◽  
Author(s):  
Carolina Martínez-García ◽  
Belén González-Fonteboa ◽  
Diego Carro-López ◽  
Fernando Martínez-Abella

2020 ◽  
Vol 152 ◽  
pp. 104303 ◽  
Author(s):  
Graciela Ponce-Antón ◽  
Maria Cruz Zuluaga ◽  
Luis Angel Ortega ◽  
Juantxo Agirre Mauleon

Author(s):  
C. A. Callender ◽  
Wm. C. Dawson ◽  
J. J. Funk

The geometric structure of pore space in some carbonate rocks can be correlated with petrophysical measurements by quantitatively analyzing binaries generated from SEM images. Reservoirs with similar porosities can have markedly different permeabilities. Image analysis identifies which characteristics of a rock are responsible for the permeability differences. Imaging data can explain unusual fluid flow patterns which, in turn, can improve production simulation models.Analytical SchemeOur sample suite consists of 30 Middle East carbonates having porosities ranging from 21 to 28% and permeabilities from 92 to 2153 md. Engineering tests reveal the lack of a consistent (predictable) relationship between porosity and permeability (Fig. 1). Finely polished thin sections were studied petrographically to determine rock texture. The studied thin sections represent four petrographically distinct carbonate rock types ranging from compacted, poorly-sorted, dolomitized, intraclastic grainstones to well-sorted, foraminiferal,ooid, peloidal grainstones. The samples were analyzed for pore structure by a Tracor Northern 5500 IPP 5B/80 image analyzer and a 80386 microprocessor-based imaging system. Between 30 and 50 SEM-generated backscattered electron images (frames) were collected per thin section. Binaries were created from the gray level that represents the pore space. Calculated values were averaged and the data analyzed to determine which geological pore structure characteristics actually affect permeability.


Sign in / Sign up

Export Citation Format

Share Document