TY  - CHAP
AU  - Kašanin-Grubin, Milica
AU  - Vergari, Francesca
AU  - Troiani, Francesco
AU  - Della Seta, Marta
PY  - 2018
UR  - https://cer.ihtm.bg.ac.rs/handle/123456789/5011
AB  - Badlands can develop on bedrock and/or weathered material, the characteristics of which play a key role on hillslope processes in a range of climate conditions. Therefore, fundamental attention should be given to badland materials, the main features of which are grain size, clay mineralogy and physico-chemical characteristics. The typical weathering profile consists of crust, subsurface and unweathered material, but depending on climatic, lithological, topographic and hydrological factors, the properties and appearance of both surface and subsurface materials change over time. Through time, regolith formed on erodible and dispersive bedrock materials tends to stabilize, again as a function of slope and climate conditions because prolonged precipitation can cause decrease in surface strength and runoff and reduce the dispersivity of the surface. Vegetation also has distinct role in stabilizing the clayey sediments due to lowering the dispersivity in the upper horizon of the badland material, even though such stabilization is often not permanent and erosion processes can sometimes reoccur. Finally, all the above cited factors and properties of badland materials play a complex and key role in the development of different geomorphic processes and related landforms.
PB  - Elsevier
T2  - Badlands Dynamics in a Context of Global Change
T1  - The Role of Lithology: Parent Material Controls on Badland Development
SP  - 61
EP  - 109
DO  - 10.1016/B978-0-12-813054-4.00003-4
ER  - 

@inbook{
author = "Kašanin-Grubin, Milica and Vergari, Francesca and Troiani, Francesco and Della Seta, Marta",
year = "2018",
abstract = "Badlands can develop on bedrock and/or weathered material, the characteristics of which play a key role on hillslope processes in a range of climate conditions. Therefore, fundamental attention should be given to badland materials, the main features of which are grain size, clay mineralogy and physico-chemical characteristics. The typical weathering profile consists of crust, subsurface and unweathered material, but depending on climatic, lithological, topographic and hydrological factors, the properties and appearance of both surface and subsurface materials change over time. Through time, regolith formed on erodible and dispersive bedrock materials tends to stabilize, again as a function of slope and climate conditions because prolonged precipitation can cause decrease in surface strength and runoff and reduce the dispersivity of the surface. Vegetation also has distinct role in stabilizing the clayey sediments due to lowering the dispersivity in the upper horizon of the badland material, even though such stabilization is often not permanent and erosion processes can sometimes reoccur. Finally, all the above cited factors and properties of badland materials play a complex and key role in the development of different geomorphic processes and related landforms.",
publisher = "Elsevier",
journal = "Badlands Dynamics in a Context of Global Change",
booktitle = "The Role of Lithology: Parent Material Controls on Badland Development",
pages = "61-109",
doi = "10.1016/B978-0-12-813054-4.00003-4"
}

Kašanin-Grubin, M., Vergari, F., Troiani, F.,& Della Seta, M.. (2018). The Role of Lithology: Parent Material Controls on Badland Development. in Badlands Dynamics in a Context of Global Change
Elsevier., 61-109.
https://doi.org/10.1016/B978-0-12-813054-4.00003-4

Kašanin-Grubin M, Vergari F, Troiani F, Della Seta M. The Role of Lithology: Parent Material Controls on Badland Development. in Badlands Dynamics in a Context of Global Change. 2018;:61-109.
doi:10.1016/B978-0-12-813054-4.00003-4 .

Kašanin-Grubin, Milica, Vergari, Francesca, Troiani, Francesco, Della Seta, Marta, "The Role of Lithology: Parent Material Controls on Badland Development" in Badlands Dynamics in a Context of Global Change (2018):61-109,
https://doi.org/10.1016/B978-0-12-813054-4.00003-4 . .