Measured and modeled gravity anomalies above the tunnel in clays - implication for errors in gravity interpretation
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F11%3A10107272" target="_blank" >RIV/00216208:11310/11:10107272 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Measured and modeled gravity anomalies above the tunnel in clays - implication for errors in gravity interpretation
Popis výsledku v původním jazyce
We measured gravity anomaly above the tunnel excavated in clays. Technical parameters of the tunnel were known. In order to obtain material parameters of clays the borehole was drilled in the study area. For calculation of gravity anomaly of the tunnel we used wet bulk densities of clays derived from laboratory measurements of drill core samples. But the fit between observed and calculated gravity data were poor in this case. If we use for interpretation densities calculated from laboratory measurementswe interpret the roof of the tunnel much deeper than it is in reality. The reason is that the borehole clay samples do not retain natural moisture probably. Much better fit between observed and calculated gravity values we received when we used for modeling densities derived from gamma-gamma log.
Název v anglickém jazyce
Measured and modeled gravity anomalies above the tunnel in clays - implication for errors in gravity interpretation
Popis výsledku anglicky
We measured gravity anomaly above the tunnel excavated in clays. Technical parameters of the tunnel were known. In order to obtain material parameters of clays the borehole was drilled in the study area. For calculation of gravity anomaly of the tunnel we used wet bulk densities of clays derived from laboratory measurements of drill core samples. But the fit between observed and calculated gravity data were poor in this case. If we use for interpretation densities calculated from laboratory measurementswe interpret the roof of the tunnel much deeper than it is in reality. The reason is that the borehole clay samples do not retain natural moisture probably. Much better fit between observed and calculated gravity values we received when we used for modeling densities derived from gamma-gamma log.
Klasifikace
Druh
D - Stať ve sborníku
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
Z - Vyzkumny zamer (s odkazem do CEZ)
Ostatní
Rok uplatnění
2011
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název statě ve sborníku
Near Surface 2011 Conference proceedings
ISBN
978-90-73834-15-6
ISSN
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e-ISSN
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Počet stran výsledku
5
Strana od-do
1-5
Název nakladatele
EAGE
Místo vydání
Houten, The Netherlands
Místo konání akce
Leicester, UK
Datum konání akce
12. 9. 2011
Typ akce podle státní příslušnosti
EUR - Evropská akce
Kód UT WoS článku
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