2019
DOI: 10.1016/j.conbuildmat.2019.07.159
|View full text |Cite
|
Sign up to set email alerts
|

Microstructure and geochemistry of lime plaster mortar from a heritage structure

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

0
4
0

Year Published

2020
2020
2024
2024

Publication Types

Select...
8
1

Relationship

0
9

Authors

Journals

citations
Cited by 22 publications
(4 citation statements)
references
References 29 publications
0
4
0
Order By: Relevance
“…Therefore, the calcite of the binder is the major contributor to the high peak of calcite in the spectra, while the limestone inclusions represent another, but minor, source of the calcite. The inclusions are the sources of the other mineral phases of quartz, feldspars, and partially the calcite, while aragonite and vaterite carbonate phases were most probably formed in the pore spaces of the mortars under certain conditions of temperature and pressure (Haneefa et al 2019:545–548; Rodriguez-Blanco et al 2011:270). In general, the presence of highly supersaturated solutions of Ca 2+ and CO 3 2 - ions in the mortar voids and pore spaces precipitate in different carbonate mineral phases; vaterite at low temperatures between 14 and 30ºC and aragonite at higher ones between 60 and 80ºC (Ogino et al 1987).…”
Section: Resultsmentioning
confidence: 99%
“…Therefore, the calcite of the binder is the major contributor to the high peak of calcite in the spectra, while the limestone inclusions represent another, but minor, source of the calcite. The inclusions are the sources of the other mineral phases of quartz, feldspars, and partially the calcite, while aragonite and vaterite carbonate phases were most probably formed in the pore spaces of the mortars under certain conditions of temperature and pressure (Haneefa et al 2019:545–548; Rodriguez-Blanco et al 2011:270). In general, the presence of highly supersaturated solutions of Ca 2+ and CO 3 2 - ions in the mortar voids and pore spaces precipitate in different carbonate mineral phases; vaterite at low temperatures between 14 and 30ºC and aragonite at higher ones between 60 and 80ºC (Ogino et al 1987).…”
Section: Resultsmentioning
confidence: 99%
“…However, the pores of C5S5Pb1 solidified lead contaminated soil were much more prominent than that those of Pb1, C2.5F5S5Pb1, and C5S2.5F2.5Pb1 under the same freezing and thawing cycles (Figure 14d). This suggests that the solidified contaminated soil tends to produce additional large aggregates and to form larger pores when the content of lime is relatively high due to the specific solidification mechanisms of lime [78]. This intuitively reflects the micro-mechanisms results of qu, E 50 and the c of C5S5Pb1 being relatively smaller and the k of C5S5Pb1 being larger than those of the other two kinds of Pb-CSCSs (Figure 5c, Figure 7c, Figure 11c, and Figure 13c) under the same freeze-thaw cycles.…”
Section: Correlations Between Ucs and Particle Size K And Pore Size (Sem)mentioning
confidence: 99%
“…It is indeed necessary to obtain information about the inner core of the structural elements, identifying the mechanical properties of materials that can change greatly from point to point. In addition, the type of mortar used in the realization of its masonry can also influence the performance of the wall, due to the weathering products that can form and which can affect the durability of the structure [11,12]. Therefore, the masonry should be able to accommodate some degree of movement from creep or thermal effects without cracking, and must be sufficiently strong to develop appropriate adhesion between the elements.…”
Section: Introductionmentioning
confidence: 99%