Gallart, Francesc

Link to this page

Authority KeyName Variants
8d2dca9f-97cd-49d0-acf2-9f52fc4ed071
  • Gallart, Francesc (3)
Projects

Author's Bibliography

How do mineralogical and physicochemical properties of badland materials change during weathering and erosion processes?

Stefanović, Milica; Jovančićević, Branimir; Janaćković, Đorđe; Antić, Nevena; Gallart, Francesc; Moreno-de las Heras, Mariano; Kašanin-Grubin, Milica

(2023)

TY  - CONF
AU  - Stefanović, Milica
AU  - Jovančićević, Branimir
AU  - Janaćković, Đorđe
AU  - Antić, Nevena
AU  - Gallart, Francesc
AU  - Moreno-de las Heras, Mariano
AU  - Kašanin-Grubin, Milica
PY  - 2023
UR  - http://TechnoRep.tmf.bg.ac.rs/handle/123456789/7137
AB  - This study involves establishing a relationship between weathering and erosion processes in badlands comparing the mineralogical and physicochemical properties of unweathered and weathered material formed in the natural environment and under laboratory climate simulation experiments. Three unweathered samples with different mineralogical contents were taken from the badlands of Vallcebre and Bagà in Spain. The climatic conditions in these areas are humid-Mediterranean. Besides quartz and calcite as dominant minerals, one unweathered sample contained smectite and gypsum, the second smectite and the third neither smectite nor gypsum. The laboratory climate simulation experiment was designed so that each sample had two sub-samples, one of which was exposed to rain and the second to snow. In the first part, the samples were placed in a climate chamber at a temperature of -3 °C after simulating rain (~140 ml) or snow (~150 g). After 15 cycles, in the second part of the experiment, all samples were exposed to rain (~140 ml) and placed in a climate chamber at a temperature of 50 °C. These treatments were repeated 8 times. Analyses of the mineralogical and physicochemical properties of the material before and after the experiment give a clear insight into the changes in mineralogy, chemical composition, grain size, porosity, etc. The changes in the microstructure were analysed using Field Emission Scanning Electron Microscopy (FESEM). The particle size distribution was determined by laser diffraction, while mineralogy was determined by X-ray diffraction (XRD). The Brunauer-Emmett-Teller (BET) surface analysis confirmed that the sample with smectite had the highest specific surface area. It was also proved that other measured parameters such as volume and diameter of the pores changed with weathering rate.
C3  - 9th EUGEO Congress, Barcelona 4-7 September 2023
T1  - How do mineralogical and physicochemical properties of badland materials change during weathering and erosion processes?
SP  - 565
UR  - https://hdl.handle.net/21.15107/rcub_technorep_7137
ER  - 
@conference{
author = "Stefanović, Milica and Jovančićević, Branimir and Janaćković, Đorđe and Antić, Nevena and Gallart, Francesc and Moreno-de las Heras, Mariano and Kašanin-Grubin, Milica",
year = "2023",
abstract = "This study involves establishing a relationship between weathering and erosion processes in badlands comparing the mineralogical and physicochemical properties of unweathered and weathered material formed in the natural environment and under laboratory climate simulation experiments. Three unweathered samples with different mineralogical contents were taken from the badlands of Vallcebre and Bagà in Spain. The climatic conditions in these areas are humid-Mediterranean. Besides quartz and calcite as dominant minerals, one unweathered sample contained smectite and gypsum, the second smectite and the third neither smectite nor gypsum. The laboratory climate simulation experiment was designed so that each sample had two sub-samples, one of which was exposed to rain and the second to snow. In the first part, the samples were placed in a climate chamber at a temperature of -3 °C after simulating rain (~140 ml) or snow (~150 g). After 15 cycles, in the second part of the experiment, all samples were exposed to rain (~140 ml) and placed in a climate chamber at a temperature of 50 °C. These treatments were repeated 8 times. Analyses of the mineralogical and physicochemical properties of the material before and after the experiment give a clear insight into the changes in mineralogy, chemical composition, grain size, porosity, etc. The changes in the microstructure were analysed using Field Emission Scanning Electron Microscopy (FESEM). The particle size distribution was determined by laser diffraction, while mineralogy was determined by X-ray diffraction (XRD). The Brunauer-Emmett-Teller (BET) surface analysis confirmed that the sample with smectite had the highest specific surface area. It was also proved that other measured parameters such as volume and diameter of the pores changed with weathering rate.",
journal = "9th EUGEO Congress, Barcelona 4-7 September 2023",
title = "How do mineralogical and physicochemical properties of badland materials change during weathering and erosion processes?",
pages = "565",
url = "https://hdl.handle.net/21.15107/rcub_technorep_7137"
}
Stefanović, M., Jovančićević, B., Janaćković, Đ., Antić, N., Gallart, F., Moreno-de las Heras, M.,& Kašanin-Grubin, M.. (2023). How do mineralogical and physicochemical properties of badland materials change during weathering and erosion processes?. in 9th EUGEO Congress, Barcelona 4-7 September 2023, 565.
https://hdl.handle.net/21.15107/rcub_technorep_7137
Stefanović M, Jovančićević B, Janaćković Đ, Antić N, Gallart F, Moreno-de las Heras M, Kašanin-Grubin M. How do mineralogical and physicochemical properties of badland materials change during weathering and erosion processes?. in 9th EUGEO Congress, Barcelona 4-7 September 2023. 2023;:565.
https://hdl.handle.net/21.15107/rcub_technorep_7137 .
Stefanović, Milica, Jovančićević, Branimir, Janaćković, Đorđe, Antić, Nevena, Gallart, Francesc, Moreno-de las Heras, Mariano, Kašanin-Grubin, Milica, "How do mineralogical and physicochemical properties of badland materials change during weathering and erosion processes?" in 9th EUGEO Congress, Barcelona 4-7 September 2023 (2023):565,
https://hdl.handle.net/21.15107/rcub_technorep_7137 .

Impact of weathering processes on n-alkane pattern in badlands

Stefanović, Milica; Šajnović, Aleksandra; Kašanin-Grubin, Milica; Vergari, Francesca; Troiani, Francesco; Moreno-de-las-Heras, Mariano; Gallart, Francesc; Desloges, Joseph; Jovančićević, Branimir

(Elsevier, 2023)

TY  - JOUR
AU  - Stefanović, Milica
AU  - Šajnović, Aleksandra
AU  - Kašanin-Grubin, Milica
AU  - Vergari, Francesca
AU  - Troiani, Francesco
AU  - Moreno-de-las-Heras, Mariano
AU  - Gallart, Francesc
AU  - Desloges, Joseph
AU  - Jovančićević, Branimir
PY  - 2023
UR  - http://TechnoRep.tmf.bg.ac.rs/handle/123456789/6570
AB  - The aim of this study is to investigate the influence of weathering processes on the distribution of n-alkanes in
unweathered and weathered samples of badland material. Organic matter (OM) of both the weathered and
unweathered zones in badland environments is derived from the same sources such any differences between the
n-alkane pattern of the two zones can be attributed to the impact of weathering processes under different climate
conditions. Organic geochemical and mineralogical characterizations were employed to investigate twenty-one
samples from weathered badland environments in Italy, Spain, and Canada that originally derive from marine,
distal alluvial, and fluvial depositional settings, respectively.
According to the distribution of n-alkanes and diterpanes, unweathered samples from Italy have an original
mixed aquatic-terrestrial origin of OM, with a variable (low to moderate) contribution of terrestrial plants as
precursors, while unweathered samples from Spain predominantly contain OM originating from submerged/
floating macrophytes deposited under reducing conditions. Unweathered samples from Canada predominantly
consist of terrigenous OM.
Intensity of changes in n-alkanes distribution when subjected to weathering depends on the type of precursor
biomass and quantity of smectite. Predominantly terrigenous OM under semi-arid conditions shows the highest
affinity for adsorption is in contact with smectite surfaces. Mid- and long-chain odd n-alkanes have a tendency to
build colloidal particles with polar organic compounds such as fatty acids by strong binding and thus their
preservation from degradation is possible.
PB  - Elsevier
T2  - CATENA
T1  - Impact of weathering processes on n-alkane pattern in badlands
SP  - 107352
VL  - 231
DO  - 10.1016/j.catena.2023.107352
ER  - 
@article{
author = "Stefanović, Milica and Šajnović, Aleksandra and Kašanin-Grubin, Milica and Vergari, Francesca and Troiani, Francesco and Moreno-de-las-Heras, Mariano and Gallart, Francesc and Desloges, Joseph and Jovančićević, Branimir",
year = "2023",
abstract = "The aim of this study is to investigate the influence of weathering processes on the distribution of n-alkanes in
unweathered and weathered samples of badland material. Organic matter (OM) of both the weathered and
unweathered zones in badland environments is derived from the same sources such any differences between the
n-alkane pattern of the two zones can be attributed to the impact of weathering processes under different climate
conditions. Organic geochemical and mineralogical characterizations were employed to investigate twenty-one
samples from weathered badland environments in Italy, Spain, and Canada that originally derive from marine,
distal alluvial, and fluvial depositional settings, respectively.
According to the distribution of n-alkanes and diterpanes, unweathered samples from Italy have an original
mixed aquatic-terrestrial origin of OM, with a variable (low to moderate) contribution of terrestrial plants as
precursors, while unweathered samples from Spain predominantly contain OM originating from submerged/
floating macrophytes deposited under reducing conditions. Unweathered samples from Canada predominantly
consist of terrigenous OM.
Intensity of changes in n-alkanes distribution when subjected to weathering depends on the type of precursor
biomass and quantity of smectite. Predominantly terrigenous OM under semi-arid conditions shows the highest
affinity for adsorption is in contact with smectite surfaces. Mid- and long-chain odd n-alkanes have a tendency to
build colloidal particles with polar organic compounds such as fatty acids by strong binding and thus their
preservation from degradation is possible.",
publisher = "Elsevier",
journal = "CATENA",
title = "Impact of weathering processes on n-alkane pattern in badlands",
pages = "107352",
volume = "231",
doi = "10.1016/j.catena.2023.107352"
}
Stefanović, M., Šajnović, A., Kašanin-Grubin, M., Vergari, F., Troiani, F., Moreno-de-las-Heras, M., Gallart, F., Desloges, J.,& Jovančićević, B.. (2023). Impact of weathering processes on n-alkane pattern in badlands. in CATENA
Elsevier., 231, 107352.
https://doi.org/10.1016/j.catena.2023.107352
Stefanović M, Šajnović A, Kašanin-Grubin M, Vergari F, Troiani F, Moreno-de-las-Heras M, Gallart F, Desloges J, Jovančićević B. Impact of weathering processes on n-alkane pattern in badlands. in CATENA. 2023;231:107352.
doi:10.1016/j.catena.2023.107352 .
Stefanović, Milica, Šajnović, Aleksandra, Kašanin-Grubin, Milica, Vergari, Francesca, Troiani, Francesco, Moreno-de-las-Heras, Mariano, Gallart, Francesc, Desloges, Joseph, Jovančićević, Branimir, "Impact of weathering processes on n-alkane pattern in badlands" in CATENA, 231 (2023):107352,
https://doi.org/10.1016/j.catena.2023.107352 . .

The influence of mineralogical composition on degradation of badland materials under different climate conditions

Stefanović, Milica; Jovančićević, Branimir; Tosti, Tomislav; Dojčinović, Biljana; Antić, Nevena; Gallart, Francesc; Moreno de las Heras, Mariano; Kašanin-Grubin, Milica

(2022)

TY  - CONF
AU  - Stefanović, Milica
AU  - Jovančićević, Branimir
AU  - Tosti, Tomislav
AU  - Dojčinović, Biljana
AU  - Antić, Nevena
AU  - Gallart, Francesc
AU  - Moreno de las Heras, Mariano
AU  - Kašanin-Grubin, Milica
PY  - 2022
UR  - http://TechnoRep.tmf.bg.ac.rs/handle/123456789/6169
C3  - EGU General Assembly 2022
T1  - The influence of mineralogical composition on degradation of badland materials under different climate conditions
DO  - 10.5194/egusphere-egu22-6290
ER  - 
@conference{
author = "Stefanović, Milica and Jovančićević, Branimir and Tosti, Tomislav and Dojčinović, Biljana and Antić, Nevena and Gallart, Francesc and Moreno de las Heras, Mariano and Kašanin-Grubin, Milica",
year = "2022",
journal = "EGU General Assembly 2022",
title = "The influence of mineralogical composition on degradation of badland materials under different climate conditions",
doi = "10.5194/egusphere-egu22-6290"
}
Stefanović, M., Jovančićević, B., Tosti, T., Dojčinović, B., Antić, N., Gallart, F., Moreno de las Heras, M.,& Kašanin-Grubin, M.. (2022). The influence of mineralogical composition on degradation of badland materials under different climate conditions. in EGU General Assembly 2022.
https://doi.org/10.5194/egusphere-egu22-6290
Stefanović M, Jovančićević B, Tosti T, Dojčinović B, Antić N, Gallart F, Moreno de las Heras M, Kašanin-Grubin M. The influence of mineralogical composition on degradation of badland materials under different climate conditions. in EGU General Assembly 2022. 2022;.
doi:10.5194/egusphere-egu22-6290 .
Stefanović, Milica, Jovančićević, Branimir, Tosti, Tomislav, Dojčinović, Biljana, Antić, Nevena, Gallart, Francesc, Moreno de las Heras, Mariano, Kašanin-Grubin, Milica, "The influence of mineralogical composition on degradation of badland materials under different climate conditions" in EGU General Assembly 2022 (2022),
https://doi.org/10.5194/egusphere-egu22-6290 . .