2013
DOI: 10.1039/c3ce41294f
|View full text |Cite
|
Sign up to set email alerts
|

Influence of chemical and structural factors on the calcite–calcium oxalate transformation

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

2
21
1
1

Year Published

2014
2014
2023
2023

Publication Types

Select...
6
1
1

Relationship

1
7

Authors

Journals

citations
Cited by 23 publications
(25 citation statements)
references
References 24 publications
2
21
1
1
Order By: Relevance
“…During the dissolution of calcite, the precipitation of several secondary minerals has been observed in the presence of aqueous cations (Pb 2+ , Cu 2+ , and ) 125 128 , oxyanions ( , , and ) 129 , 130 , and F − 131 due to the formation of less soluble phases. Sometimes, calcite might be entirely replaced by the secondary minerals, such as cerussite (PbCO 3 ) 132 , dolomite (CaMg(CO 3 ) 2 ) 133 135 , magnesite (MgCO 3 ) 134 , siderite (FeCO 3 ) 133 , gypsum (CaSO 4 ) 136 , 137 , whewellite (CaC 2 O 4 ·H 2 O) 138 and fluorite (CaF 2 ) 139 , 140 , via a coupled dissolution–precipitation mechanism. Interestingly, the capture of aqueous Mg on the calcite surface was recognized when calcite dissolved in seawater, resulting in an enriched Mg surface 141 .…”
Section: Discussionmentioning
confidence: 99%
“…During the dissolution of calcite, the precipitation of several secondary minerals has been observed in the presence of aqueous cations (Pb 2+ , Cu 2+ , and ) 125 128 , oxyanions ( , , and ) 129 , 130 , and F − 131 due to the formation of less soluble phases. Sometimes, calcite might be entirely replaced by the secondary minerals, such as cerussite (PbCO 3 ) 132 , dolomite (CaMg(CO 3 ) 2 ) 133 135 , magnesite (MgCO 3 ) 134 , siderite (FeCO 3 ) 133 , gypsum (CaSO 4 ) 136 , 137 , whewellite (CaC 2 O 4 ·H 2 O) 138 and fluorite (CaF 2 ) 139 , 140 , via a coupled dissolution–precipitation mechanism. Interestingly, the capture of aqueous Mg on the calcite surface was recognized when calcite dissolved in seawater, resulting in an enriched Mg surface 141 .…”
Section: Discussionmentioning
confidence: 99%
“…In this way, ACC and ACO (upon their crystallization into stable, crystalline phases) might act as coupling agents between silica gels and non-silicate substrates after its recrystallization into mineral phases with an epitaxial relationship to the calcitic substrate. 2,44,45 The main goal of our study was to investigate the properties that both calcium carbonate and calcium oxalate, applied as amorphous nanoparticles, confer to Si-coatings based on standard tetraethoxysilane (TEOS) and prepolymerized TEOS (Dynasilan 40) currently used in cultural heritage conservation. We evaluated the effectiveness of these treatments following their application on common non-silicate building materials such as marble, porous calcarenite, and gypsum plaster.…”
Section: Introductionmentioning
confidence: 99%
“…This is the case of ACC and calcitic or gypsum substrates, as well as ACO and calcitic substrates. In this way, ACC and ACO (upon their crystallization into stable, crystalline phases) might act as coupling agents between silica gels and non-silicate substrates after its recrystallization into mineral phases with an epitaxial relationship to the calcitic substrate. ,, …”
Section: Introductionmentioning
confidence: 99%
“…Pseudomorphic replication is actually inspired by the so‐called mineral replacement reactions found in geological environments. Such reactions involve the transformation of a primary mineral into a secondary mineral through a distinct reaction front between the two phases and the conservation of dimension and some crystallographic information between the primary and secondary phases 10,11…”
Section: Introductionmentioning
confidence: 99%