Relationship between polished stone value (PSV) and Nordic abrasion value (A (N)) of volcanic rocks
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F17%3A10338410" target="_blank" >RIV/00216208:11310/17:10338410 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1007/s10064-015-0814-x" target="_blank" >http://dx.doi.org/10.1007/s10064-015-0814-x</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s10064-015-0814-x" target="_blank" >10.1007/s10064-015-0814-x</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Relationship between polished stone value (PSV) and Nordic abrasion value (A (N)) of volcanic rocks
Popis výsledku v původním jazyce
A set of 39 different volcanic rocks was studied for performance as crushed stone for road surfacing (wearing course) aggregates using two technological tests: the polished stone value (PSV) test, aimed at evaluating resistance to polishing (skid resistance), and the Nordic abrasion value (A (N)) test, as a proxy to wear by studded tires (resistance to abrasion). In order to understand better the observed relationships, the studied volcanic rocks were split into five petrographic-technological subgroups (rhyolite/porphyry, phonolites, basalts s.l., spilites, and melaphyres/diabase) based on their composition, rock fabric, geological age, and post-genetic history. Response of each of these subgroups to the applied tests is not always the same, but generally is controlled by composition and rock macro- and microfabric. Despite the fact that positive contributors to skid resistance (e.g., increasing contrasting hardness of rock-forming components, presence or absence of certain phenocrysts) have the opposite effect on wear by studded tires, it is not possible to make any reliable prediction of PSV from A (N) or vice versa.
Název v anglickém jazyce
Relationship between polished stone value (PSV) and Nordic abrasion value (A (N)) of volcanic rocks
Popis výsledku anglicky
A set of 39 different volcanic rocks was studied for performance as crushed stone for road surfacing (wearing course) aggregates using two technological tests: the polished stone value (PSV) test, aimed at evaluating resistance to polishing (skid resistance), and the Nordic abrasion value (A (N)) test, as a proxy to wear by studded tires (resistance to abrasion). In order to understand better the observed relationships, the studied volcanic rocks were split into five petrographic-technological subgroups (rhyolite/porphyry, phonolites, basalts s.l., spilites, and melaphyres/diabase) based on their composition, rock fabric, geological age, and post-genetic history. Response of each of these subgroups to the applied tests is not always the same, but generally is controlled by composition and rock macro- and microfabric. Despite the fact that positive contributors to skid resistance (e.g., increasing contrasting hardness of rock-forming components, presence or absence of certain phenocrysts) have the opposite effect on wear by studded tires, it is not possible to make any reliable prediction of PSV from A (N) or vice versa.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10505 - Geology
Návaznosti výsledku
Projekt
<a href="/cs/project/GA13-13967S" target="_blank" >GA13-13967S: Experimentální studium mezních stavů napětí v oblasti růstu a porušení trhlinami jako kritických parametrů trvanlivosti pórovitého přírodního kamene</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2017
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Bulletin of Engineering Geology and the Environment
ISSN
1435-9529
e-ISSN
—
Svazek periodika
76
Číslo periodika v rámci svazku
1
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
15
Strana od-do
85-99
Kód UT WoS článku
000394165200007
EID výsledku v databázi Scopus
2-s2.0-84946433915