Skip to main content
Have a personal or library account? Click to login
Bioweathering of Egyptian Nubian sandstone and Theban limestone: three months insight by experimental incubation Cover

Bioweathering of Egyptian Nubian sandstone and Theban limestone: three months insight by experimental incubation

Open Access
|Dec 2024

Figures & Tables

Figure 1.

A map showing the locations of sampling sites, where Nubian sandstone S1-S6 (A) and Theban limestone (B) have been collected.

Table 1.

Chemical composition of the studied samples.

[Wt. %]Sandstone S3Sandstone S6Limestone TL
SiO292.5785.677.08
Al2O33.120.960.54
Fe2O31.187.940.33
MgO0.070.110.51
CaO0.071.5650.22
Na2O0.070.130.15
K2O0.870.190.08
TiO20.840.180.03
LOI1.03.140.7
Figure 2.

Flowchart presenting experimental approach undertaken to decipher stone weathering.

Figure 3.

Microphotographs of Nubian sandstone (S3, S6) taken in plane-polarized (left column) and cross-polarized light (right column).

Figure 4.

Results of X-ray diffraction and thermal analysis of Theban limestone (TL) and Nubian sandstone (S3, S6). Mineral abbreviations: cal-calcite, qz-quartz, kln-kaolinite, hl-halite, afs-alkali feldspar, zrn-zircon, gth-goethite, hem-hematite, mag-magnetite, gp-gypsum, lpc-lepidocrocite (Warr, 2021); dh-dehydration, dxo-dehydroxylation.

Figure 5.

BSE images and EDS spectra of Nubian sandstone (S3, S6) and Theban limestone (TL) before leaching experiment. 1 – euhedral dolomite; 2 – bioclast; 3 – Fe-bearing phases encrusting bioclast; 4, 9 – alkali feldspar; 5 – quartz; 6, 10 – Fe-bearing phases in matrix; 7, 11 – kaolinite; 8 – magnetite.

Figure 6.

BSE images and EDS spectra of Nubian sandstone (S3, S6) and Theban limestone (TL) after leaching experiment. 1 – bioclast; 2 – bioclast covered with biofilm, 3 – euhedral dolomite; 4 – quartz and biofilm; 5 – syntaxial quartz overgrowths; 6 – bacteria on kaolinite aggregate; 7 – kaolinite aggregate; 8 – magnetite; 9, 11 – Fe-bearing phases; 10 – single kaolinite flake.

Figure 7.

Microphotographs of Theban limestone (TL) taken in plane-polarized (left column) and cross-polarized light (right column).

Figure 8.

Evolution of elements leaching from studied sandstones throughout the experiment (BAC: growth medium with bacteria filtered at <0.22 μm; MED: sterile growth medium; H2O: sterile water). Error bars present standard deviation of the replicate values.

Table 2.

Specific conditions set in the incubation experiments.

IncubationNameCharacteristics of the constituentsPresence of bacteriaInitial pHFinal pH S3Final pH S6Final pH TLSiderophore concentrationProxy
Ultrapure waterWATnone-5.68.78.68.1-Neutral unaggressive conditions
Growth mediumMEDInorganic, organic (succinic acid)-7.07.87.88.0-Chemical weathering
Growth medium with bacteria Pseudomonas fluorescensBACInorganic, organic (succinic acid, microbially-derived compounds including siderophore)+7.08.79.19.2S3: 45.2 μM L−1
S6: 75.5 μM L−1
TL: 90.6 μM L−1
Biotic weathering
Figure 9.

Evolution of elements leaching from studied limestone throughout the experiment (BAC: growth medium with bacteria filtered at <0.22 μm; MED: sterile growth medium; H2O: sterile water). Error bars present standard deviation of the replicate values.

DOI: https://doi.org/10.2478/mipo-2024-0006 | Journal eISSN: 1899-8526 | Journal ISSN: 1899-8291
Language: English
Page range: 60 - 79
Submitted on: Jul 4, 2024
Accepted on: Nov 7, 2024
Published on: Dec 13, 2024
Published by: Mineralogical Society of Poland
In partnership with: Paradigm Publishing Services
Publication frequency: Volume open
Related subjects:

© 2024 Anna Potysz, Amr Osman, Wojciech Bartz, published by Mineralogical Society of Poland
This work is licensed under the Creative Commons Attribution 4.0 License.