Abstract
The paper presents the results of studying the development of calcite neoformations on the surfaces of modern buildings within the city of Tyumen. The objects of the study were carbonate crusts and stalactite-like bodies formed on the surfaces of five representative buildings in the city center. Research methods included visual diagnostics, optical microscopy, scanning electron microscopy with energy dispersive X-ray spectroscopy, confocal laser scanning microscopy and semi-quantitative determination of the mineral composition by X-ray diffraction analysis. The results of the study show that calcite is the main component of all carbonate crusts, while other minerals were found in small quantities. The microscopic studies revealed the differences in morphology of crusts developing on horizontal and vertical surfaces. The mycelium of fungi (presumably of the Penicillium group), represented by filamentous and often hollow hyphae covered with calcite, as well as relics of bacterial colonies were found in all studied samples. It was noted that the mycelium forms the structural frame of carbonate crusts and stalactites. Studies have shown that the prokaryotic–eukaryotic communities are responsible for the high rate of the urban speleothem growth and play the main role in calcite precipitation at the initial stages of their development.
| Original language | English |
|---|---|
| Article number | 128 |
| Journal | Geosciences (Switzerland) |
| Volume | 9 |
| Issue number | 3 |
| DOIs | |
| Publication status | Published - 1 Mar 2019 |
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Keywords
- Biomineralization
- Calcite
- Crusts
- Fungi
- Urban speleothems
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
Cite this
Carbonate neoformations on modern buildings and engineering structures in Tyumen city, Russia : Structural features and development factors. / Novoselov, Andrey; Konstantinov, Alexandr; Leonova, Lyubov; Soktoev, Bulat; Morgalev, Sergey.
In: Geosciences (Switzerland), Vol. 9, No. 3, 128, 01.03.2019.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Carbonate neoformations on modern buildings and engineering structures in Tyumen city, Russia
T2 - Structural features and development factors
AU - Novoselov, Andrey
AU - Konstantinov, Alexandr
AU - Leonova, Lyubov
AU - Soktoev, Bulat
AU - Morgalev, Sergey
PY - 2019/3/1
Y1 - 2019/3/1
N2 - The paper presents the results of studying the development of calcite neoformations on the surfaces of modern buildings within the city of Tyumen. The objects of the study were carbonate crusts and stalactite-like bodies formed on the surfaces of five representative buildings in the city center. Research methods included visual diagnostics, optical microscopy, scanning electron microscopy with energy dispersive X-ray spectroscopy, confocal laser scanning microscopy and semi-quantitative determination of the mineral composition by X-ray diffraction analysis. The results of the study show that calcite is the main component of all carbonate crusts, while other minerals were found in small quantities. The microscopic studies revealed the differences in morphology of crusts developing on horizontal and vertical surfaces. The mycelium of fungi (presumably of the Penicillium group), represented by filamentous and often hollow hyphae covered with calcite, as well as relics of bacterial colonies were found in all studied samples. It was noted that the mycelium forms the structural frame of carbonate crusts and stalactites. Studies have shown that the prokaryotic–eukaryotic communities are responsible for the high rate of the urban speleothem growth and play the main role in calcite precipitation at the initial stages of their development.
AB - The paper presents the results of studying the development of calcite neoformations on the surfaces of modern buildings within the city of Tyumen. The objects of the study were carbonate crusts and stalactite-like bodies formed on the surfaces of five representative buildings in the city center. Research methods included visual diagnostics, optical microscopy, scanning electron microscopy with energy dispersive X-ray spectroscopy, confocal laser scanning microscopy and semi-quantitative determination of the mineral composition by X-ray diffraction analysis. The results of the study show that calcite is the main component of all carbonate crusts, while other minerals were found in small quantities. The microscopic studies revealed the differences in morphology of crusts developing on horizontal and vertical surfaces. The mycelium of fungi (presumably of the Penicillium group), represented by filamentous and often hollow hyphae covered with calcite, as well as relics of bacterial colonies were found in all studied samples. It was noted that the mycelium forms the structural frame of carbonate crusts and stalactites. Studies have shown that the prokaryotic–eukaryotic communities are responsible for the high rate of the urban speleothem growth and play the main role in calcite precipitation at the initial stages of their development.
KW - Biomineralization
KW - Calcite
KW - Crusts
KW - Fungi
KW - Urban speleothems
UR - http://www.scopus.com/inward/record.url?scp=85065243228&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85065243228&partnerID=8YFLogxK
U2 - 10.3390/geosciences9030128
DO - 10.3390/geosciences9030128
M3 - Article
AN - SCOPUS:85065243228
VL - 9
JO - Geosciences (Switzerland)
JF - Geosciences (Switzerland)
SN - 2076-3263
IS - 3
M1 - 128
ER -