2014
DOI: 10.1016/j.geomorph.2013.11.032
|View full text |Cite
|
Sign up to set email alerts
|

Recurrent landsliding of a high bank at Dunaszekcső, Hungary: Geodetic deformation monitoring and finite element modeling

Abstract: Five years of geodetic monitoring data are processed to evaluate recurrent sliding at Dunaszekcső, which are characteristic geomorphological processes affecting the high banks of the Middle Danube valley in Hungary. The integrated geodetic observations provide accurate three dimensional coordinate time series, and these data are used to calculate the kinematic features of point movements and rigid body behavior of point blocks. Additional datasets are borehole tiltmeter and hydrological recordings of the Danub… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
2

Citation Types

0
22
0
3

Year Published

2014
2014
2017
2017

Publication Types

Select...
3
3
1

Relationship

0
7

Authors

Journals

citations
Cited by 25 publications
(25 citation statements)
references
References 13 publications
0
22
0
3
Order By: Relevance
“…In fact, this strong relationship between mass movements of river banks (e.g., ground deformations, bank erosions or landslides) and hydrological processes involving both the magnitude and frequency rainfall events and the seasonal fluctuations of river water levels have been emphasized by previous studies in China [46] and worldwide [47][48][49][50]. Consequently, comparing the LOS displacement histories of these mentioned SDFP points and the water level changes of Yangtze River during the study period, we can observe a coherent temporal correlation of variations and amplitudes between them (see Figure 6b).…”
Section: Discussionmentioning
confidence: 92%
See 1 more Smart Citation
“…In fact, this strong relationship between mass movements of river banks (e.g., ground deformations, bank erosions or landslides) and hydrological processes involving both the magnitude and frequency rainfall events and the seasonal fluctuations of river water levels have been emphasized by previous studies in China [46] and worldwide [47][48][49][50]. Consequently, comparing the LOS displacement histories of these mentioned SDFP points and the water level changes of Yangtze River during the study period, we can observe a coherent temporal correlation of variations and amplitudes between them (see Figure 6b).…”
Section: Discussionmentioning
confidence: 92%
“…We suggest that the seasonal fluctuations of river water levels might partially contribute to ground deformation Due to a good spatial correlation between the deformation signals and the river locations, the most likely cause for the ground deformation observed in these areas is groundwater discharges and recharges related to seasonal fluctuations in water levels of the Yangtze River. In fact, this strong relationship between mass movements of river banks (e.g., ground deformations, bank erosions or landslides) and hydrological processes involving both the magnitude and frequency rainfall events and the seasonal fluctuations of river water levels have been emphasized by previous studies in China [46] and worldwide [47][48][49][50]. Consequently, comparing the LOS displacement histories of these mentioned SDFP points and the water level changes of Yangtze River during the study period, we can observe a coherent temporal correlation of variations and amplitudes between them (see Figure 6b).…”
Section: Discussionmentioning
confidence: 92%
“…The goal of the applied geophysical techniques used to be the horizontal and/or vertical delineation of the sliding volume or -more rarelythe study of the inner structure of the landslide or the characterization of the eventually existing sliding surface. Geotechnical methods, remote sensing techniques and geodetical methods are also distributed in landslide investigations as it is shown on the example of the in this paper presented area by Újvári et al, 2009, Bányai et al 2012and Bányai et al 2013. All of these techniques were however mostly used in the investigation of landslides where the sliding material differed from the massive one.…”
Section: Introductionmentioning
confidence: 99%
“…However, if the landslide is ancient or not very active, its morphological features and boundaries may be degraded requiring recognition in depth. Geodetic methods are also distributed in landslide investigations as shown in the example of the site presented in the papers by Újvári et al (2009) and Bányai et al (2013). Geophysical methods which can also be very fruitful for studying landslides are summarised by Jongmans and Garambois (2007).…”
Section: Introductionmentioning
confidence: 99%