Variability of Wolman pebble samples in gravel/cobble bed streams
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F17%3AA1801O18" target="_blank" >RIV/61988987:17310/17:A1801O18 - isvavai.cz</a>
Result on the web
<a href="http://www.formatiocircumiectus.actapol.net/pub/16_1_237.pdf" target="_blank" >http://www.formatiocircumiectus.actapol.net/pub/16_1_237.pdf</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.15576/ASP.FC/2017.16.1.237" target="_blank" >10.15576/ASP.FC/2017.16.1.237</a>
Alternative languages
Result language
angličtina
Original language name
Variability of Wolman pebble samples in gravel/cobble bed streams
Original language description
Wolman [1954] pebble sampling is the most commonly used method to estimate surface bed grain sizes in gravel-bed streams. A few studies documented different results between individual operators or repeated measurements within the same channel-reach obtained by this method. We tested potential differences in pebble sample distributions and related grain-size percentiles (D10, D50 and D90) between two fluvial geomorphologists and two almost inexperienced students in three channel-reaches and one gravel bar.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10508 - Physical geography
Result continuities
Project
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Continuities
S - Specificky vyzkum na vysokych skolach
Others
Publication year
2017
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Acta Scientiarum Polonorum-Formatio Circumiectus
ISSN
1644-0765
e-ISSN
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Volume of the periodical
16
Issue of the periodical within the volume
1
Country of publishing house
PL - POLAND
Number of pages
10
Pages from-to
237-246
UT code for WoS article
000412720400006
EID of the result in the Scopus database
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