Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Mary Antonette Beroya-Eitner"'
Autor:
Rong Wang, Yanrong Li, Dongdong Lv, Weichao Zhao, Chaobo Zhang, Hauke Zachert, Gerald Eichhoff, Mary Antonette Beroya-Eitner
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Tensile strength is a key parameter governing tensile cracking and subsequent failure of soil or rock mass. Existing methods for measuring tensile strength are mainly designed for hard materials and come with inherent problems. As such, they are cont
Externí odkaz:
https://doaj.org/article/cad73d039d494111968c2070b5bb3202
Autor:
Fanfan Guan, Yanrong Li, Guohong Gao, Hauke Zachert, Gerald Eichhoff, Mary Antonette Beroya-Eitner
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Tensile strength is an important parameter in many engineering applications. In loess slopes, for instance, it governs the development and propagation of tension cracks that usually ultimately lead to crack–sliding and toppling failures, which are
Externí odkaz:
https://doaj.org/article/b515e950bd5645c2ba56c5fef85169c1
Autor:
Alessandra Insana, Mary Antonette Beroya-Eitner, Marco Barla, Hauke Zachert, Bojan Žlender, Margreet van Marle, Bjørn Kalsnes, Tamara Bračko, Carlos Pereira, Iulia Prodan, Fabien Szymkiewicz, Hjördis Löfroth
Publikováno v:
Geosciences, Vol 11, Iss 12, p 488 (2021)
Climate change is already being felt in Europe, unequivocally affecting the regions’ geo-structures. Concern over this is rising, as reflected in the increasing number of studies on the subject. However, the majority of these studies focused only o
Externí odkaz:
https://doaj.org/article/d31df86ad57343429cf8eee181b8706a
Autor:
Hauke Zachert, Carlos Pereira, Fabien Szymkiewicz, Bjørn Kalsnes, Mary Antonette Beroya-Eitner, Tamara Bračko, Margreet van Marle, Alessandra Insana, Hjördis Löfroth, Marco Barla, Bojan Žlender, Iulia C. Prodan
Publikováno v:
Geosciences, Vol 11, Iss 488, p 488 (2021)
Geosciences
Geosciences; Volume 11; Issue 12; Pages: 488
Geosciences
Geosciences; Volume 11; Issue 12; Pages: 488
Climate change is already being felt in Europe, unequivocally affecting the regions’ geo-structures. Concern over this is rising, as reflected in the increasing number of studies on the subject. However, the majority of these studies focused only o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1db160d05735a8a07823a4ea20ce3558
http://tuprints.ulb.tu-darmstadt.de/20070/
http://tuprints.ulb.tu-darmstadt.de/20070/
Publikováno v:
CATENA. 214:106273
Publikováno v:
Earth-Science Reviews. 221:103718
Li et al. (2020) reviewed and compiled worldwide loess distribution and identified three loess genesis modes (CR, MR and MRD), according to which Central Asian and Chinese Xinjiang loesses are generalized into MRD mode. Referring to Li et al. (2020),
Autor:
Verônica Ricken Marques, Antonio Belincanta, Mary-Antonette Beroya-Eitner, Jorge Luis Almada Augusto, Ewerton Guelssi, Hauke Zachert
Publikováno v:
MATEC Web of Conferences, Vol 337, p 03006 (2021)
In this study, the influence of soil moisture on the bearing capacity of piles founded in an unsaturated clay soil was investigated. The soil studied, composing the upper soil layer in Maringá, Brazil, is lateritic, has degree of saturation between
Autor:
Mary Antonette Beroya-Eitner
Publikováno v:
Ecological Indicators. 60:329-334
Indicators provide easy and quick information on the status or condition of an object of interest and are therefore widely used in policy-making. In recent years, policy interest in vulnerability research has increased and a growing number of studies
Publikováno v:
Geotechnical Testing Journal. 43:20190308
Tensile strength plays a crucial role in many engineering activities involving soils and soft rocks. Currently, several methods for tensile strength determination exist, the most common of which include the direct tension method, Brazilian test, ring
Publikováno v:
Earth-Science Reviews. 201:102947
Loess formation generally involves the four main stages of production, deflation, transportation, and deposition of loess particles. Traditionally, loesses are classified as glacial, desert, or other types based only on source area characteristics wi