Peer-reviewed articles 17,970 +



Title: INSTABILITY CHARACTERIZATION OF THE GEOLOGICAL FORMATION "AREIAS E ARGILAS DE TAVEIRO" IN THE CONDEIXA AND COIMBRA AREAS (CENTRAL-WESTERN PORTUGAL)

INSTABILITY CHARACTERIZATION OF THE GEOLOGICAL FORMATION "AREIAS E ARGILAS DE TAVEIRO" IN THE CONDEIXA AND COIMBRA AREAS (CENTRAL-WESTERN PORTUGAL)
Beatriz Neto; Pedro Santarem Andrade; Antonio Neves Trota
10.5593/sgem2024/1.1
1314-2704
English
24
1.1
•    Prof. DSc. Oleksandr Trofymchuk, UKRAINE 
•    Prof. Dr. hab. oec. Baiba Rivza, LATVIA
The work aims to characterize the slope instabilities present in the Taveiro Sand and Clay - Areias e Argilas de Taveiro - Formation, which occurs in the municipalities of Condeixa and Coimbra, in central-western Portugal. The Areias e Argilas de Taveiro Formation, of Upper Cretaceous – Campanian - age, is made up of successions of metric layers of red, and brownish or pinkish pelites, interbedded with coarse arkosic sandstones. It has as maximum thickness of about 170 m. A total of 27 slopes with stability problems were counted in both municipalities, 16 in Coimbra and 11 in Condeixa. Several information was collected, as morphometrics, the lithological type, the existence of vegetation, the presence of erosive processes, the probable age of occurrence and the type of instability movement. The characterized slopes correspond entirely to excavation slopes. They vary in length from 18 to 180 meters, in height from 1.5 to 7 meters, and in dip from 31° to near vertical. The type of instability found corresponds mainly to shallow landslides (48.4%), and with a significant number of rotational landslides (29.0%) and earth flows (12.9%). Regarding the possible consequences of instability, most of the situations related to instability movements can reach roads with permanent traffic (81.5% of the slopes).
[1] Quinta-Ferreira, M., Andrade, P.S., Lemos, L., Saraiva, A., Cut slopes failures on the Triassic beds in Coimbra, Portugal. Bulletin of Engineering Geology and the Environment, vol. 72, pp 383–396, 2013. DOI: https://doi.org/10.1007/s10064-013-0483-6
[2] Quinta-Ferreira, M., Henriques, J., Sa, M., Quinta-Ferreira, M., Henriques, J., Sa, M.P., Study of the excavation slope to enlarge the Alcabideque reservoir, Condeixa-a-Nova. Comunicacoes Geologicas, 101/Especi III, pp 1151-1154, 2014. http://hdl.handle.net/10316/35244.
[3] Correia, A.A.S., Venda-Oliveira, P.J., Lemos, L.J.L., Strength assessment of chemically stabilised soft soils. Proceedings of the Institution of Civil Engineers: Geotechnical Engineering, vol. 172 / issue 3, pp 218-227, 2019. DOI: https://doi.org/10.1680/jgeen.17.00011
[4] Soares, A. F., Marques, J. F., Sequeira, A. J. D., Noticia Explicativa da Folha 19-D Coimbra-Lousa. Carta Geologica de Portugal, na escala de 1:50 000. Departamento de Geologia. Instituto Nacional de Engenharia, Tecnologia e Inovacao, Lisboa, 2007. (in portuguese)
[5] Cunha, P., Reis, R., Cretaceous sedimentary and tectonic evolution of the northern sector of the Lusitanian Basin (Portugal). Cretaceous Research, vol. 16/, issues 2-3, pp 155-170, 1995. DOI: https://doi.org/10.1006/cres.1995.1013
[6] Google Earth Pro, Google Earth Pro 7.3.6.9345 (64-bit), 2022.
[7] Ko Ko, C., Flentje, P., Chowdhury, R., Landslide Qualitative Hazard and Risk Assessment Method and its Reliability. Bulletin of Engineering Geology and the Environment, vol. 63, pp 149-165, 2004. DOI: https://doi.org/10.1007/s10064-004-0231-z
[8] Dikau, R., Brunsden, D., Schrott, L., Ibsen, M., Landslide Recognition. Identification, Movement and Causes. John Wiley & Sons, Chichester, 1996, 272 p.
[9] Cruden, D. M., Varnes, D. J., Landslides. Investigation and Mitigation. Special Report 247. Ed. Keith Tuner e Robert Schuster. Transportation Research Board. National Research Council. National Academy Press, Washington D.C., 1996, 247 p.
[10] WP/WLI, Multilingual landslide glossary. Working Party on World Landslide Inventory - UNESCO. International Geotechnical Societies - IGS, Canadian Geotechnical Society, Richmond, British Columbia, 1993, 32 p.
[11] Sobotkova, V., Dumbrovsky, M., The new volumetric approach for field measurements of rill erosion. Eurasian Journal of Soil Science, vol. 4, issue 2, pp 94-99, 2015. DOI: https://doi.org/10.18393/ejss.10435
[12] IDOM, Ficha de Taludes – Subconcessao Baixo Alentejo. IP2 – Variante Nascente de Evora Lanco E – IP2 Evora (A6/IP7) / Sao Mancos. APA – Avaliacao de Impacte Ambiental n.°1202 – Anexos – Taludes, 2009. https://siaia.apambiente.pt/RECAPE2.aspx?ID=353 (in portuguese)
The financial support of FCT-MEC through national funds and, when applicable, co-financed by the ERDF within the PT2020 partnership, through the research projects UID/Multi/00073/2020 of the Geosciences Centre and UID/Multi/00308/2020 is acknowledged.
conference
Proceedings of 24th International Multidisciplinary Scientific GeoConference SGEM 2024
24th International Multidisciplinary Scientific GeoConference SGEM 2024, 1 - 7 July, 2024
Proceedings Paper
STEF92 Technology
International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM
SWS Scholarly Society; Acad Sci Czech Republ; Latvian Acad Sci; Polish Acad Sci; Russian Acad Sci; Serbian Acad Sci and Arts; Natl Acad Sci Ukraine; Natl Acad Sci Armenia; Sci Council Japan; European Acad Sci, Arts and Letters; Acad Fine Arts Zagreb Croatia; Croatian Acad Sci and Arts; Acad Sci Moldova; Montenegrin Acad Sci and Arts; Georgian Acad Sci; Acad Fine Arts and Design Bratislava; Russian Acad Arts; Turkish Acad Sci.
169-176
1 - 7 July, 2024
website
9852
Slopes, Stability, Clay, Central Portugal

25th SGEM International Conference on Earth & Planetary Sciences


International GeoConference SGEM2025
27 June - 6 July, 2025 / Albena, Bulgaria

Read More
   

SGEM Vienna GREEN "Green Science for Green Life"


Extended Scientific Sessions SGEM Vienna GREEN
3 -6 December, 2025 / Vienna, Austria

Read More
   

A scientific platform for Art-Inspired Scientists!


The Magical World Where Science meets Art
Vienna, Austria

Read More