Evolution of natural rock arches: A realistic small-scale experiment

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F19%3A00504052" target="_blank" >RIV/67985831:_____/19:00504052 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216208:11310/19:10389979

Výsledek na webu

<a href="https://pubs.geoscienceworld.org/gsa/geology/article/47/1/71/567644/Evolution-of-natural-rock-arches-A-realistic" target="_blank" >https://pubs.geoscienceworld.org/gsa/geology/article/47/1/71/567644/Evolution-of-natural-rock-arches-A-realistic</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1130/G45421.1" target="_blank" >10.1130/G45421.1</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Evolution of natural rock arches: A realistic small-scale experiment

Popis výsledku v původním jazyce

People tend to admire well-developed rock arches and bridges as a symbol of perfection in nature. However, the origin of such arches still remains unclear, with different authors emphasizing different factors as essential. An authentic small-scale physical model of a perfect arch was created in situ from friable sandstone through a simulation of natural erosion. Based on three-dimensional photogrammetric and numerical modeling, we established three evolutionary stages of the modeled arch: the initial, mature, and senile stages. Erosion removed the material from stress shadows, thus exposing the compressed zone of the material, which spans over the discontinuity. From its original lintel thickness with a length ratio of 0.3, the modeled arch thinned out to a ratio of 0.03, which is close to the best-developed natural arches. The erosion rate of the arch surface was relatively low for 90% of its lifespan, but the last 10% was characterized by an abrupt increase in the erosion rate. Our results show that the only conditions essential to producing a delicate arch through erosion are a thin, vertically elongated rock body with an appropriate discontinuity, and a material prone to stress-controlled erosion.

Název v anglickém jazyce

Evolution of natural rock arches: A realistic small-scale experiment

Popis výsledku anglicky

People tend to admire well-developed rock arches and bridges as a symbol of perfection in nature. However, the origin of such arches still remains unclear, with different authors emphasizing different factors as essential. An authentic small-scale physical model of a perfect arch was created in situ from friable sandstone through a simulation of natural erosion. Based on three-dimensional photogrammetric and numerical modeling, we established three evolutionary stages of the modeled arch: the initial, mature, and senile stages. Erosion removed the material from stress shadows, thus exposing the compressed zone of the material, which spans over the discontinuity. From its original lintel thickness with a length ratio of 0.3, the modeled arch thinned out to a ratio of 0.03, which is close to the best-developed natural arches. The erosion rate of the arch surface was relatively low for 90% of its lifespan, but the last 10% was characterized by an abrupt increase in the erosion rate. Our results show that the only conditions essential to producing a delicate arch through erosion are a thin, vertically elongated rock body with an appropriate discontinuity, and a material prone to stress-controlled erosion.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

<a href="/cs/project/GA16-19459S" target="_blank" >GA16-19459S: Vliv napětí daného gravitací na erozi pískovce: fyzikální a numerické modelování</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2019

Kód důvěrnosti údajů

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

Název periodika

Geology

ISSN

0091-7613

e-ISSN

—

Svazek periodika

47

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

4

Strana od-do

71-74

Kód UT WoS článku

000454902700020

EID výsledku v databázi Scopus

2-s2.0-85065083437