Confirmation of a theory: reconstruction of an alluvial plain development in a flume experiment

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68145535%3A_____%2F16%3A00471459" target="_blank" >RIV/68145535:_____/16:00471459 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.3112/erdkunde.2016.03.05" target="_blank" >http://dx.doi.org/10.3112/erdkunde.2016.03.05</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.3112/erdkunde.2016.03.05" target="_blank" >10.3112/erdkunde.2016.03.05</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Confirmation of a theory: reconstruction of an alluvial plain development in a flume experiment

Popis výsledku v původním jazyce

Fluvial geomorphologists have tried to describe the outstanding tectonically affected avulsion process of Tisza River at the Great Hungarian Plain by various theoretical concepts. Flume experiments provide the ability to examine the main characteristic processes of a highlighted surface development theory under controlled settings within an accelerated time scale. Our goal was to reconstruct and refine these hypotheses from a new experimental point of view. In this study we performed an experiment of the avulsion process mentioned above on a 12 x 5 x 2.5 m flume where a special instrument was planted under the sand layers in order to simulate the vertical tectonic movements. A terrestrial laser scanner was used to record the different stages of the topographic evolution.

Název v anglickém jazyce

Confirmation of a theory: reconstruction of an alluvial plain development in a flume experiment

Popis výsledku anglicky

Fluvial geomorphologists have tried to describe the outstanding tectonically affected avulsion process of Tisza River at the Great Hungarian Plain by various theoretical concepts. Flume experiments provide the ability to examine the main characteristic processes of a highlighted surface development theory under controlled settings within an accelerated time scale. Our goal was to reconstruct and refine these hypotheses from a new experimental point of view. In this study we performed an experiment of the avulsion process mentioned above on a 12 x 5 x 2.5 m flume where a special instrument was planted under the sand layers in order to simulate the vertical tectonic movements. A terrestrial laser scanner was used to record the different stages of the topographic evolution.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

—

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2016

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Erdkunde

ISSN

0014-0015

e-ISSN

—

Svazek periodika

70

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

16

Strana od-do

271-285

Kód UT WoS článku

000384466800005

EID výsledku v databázi Scopus

2-s2.0-84983738795