Show simple item record

dc.contributor.authorBerthelote, Antony Ray
dc.date.accessioned2015-10-15T00:56:19Z
dc.date.available2015-10-15T00:56:19Z
dc.date.issued2005-08
dc.identifier.urihttp://hdl.handle.net/11122/6066
dc.descriptionThesis (M.S.) University of Alaska Fairbanks, 2005en_US
dc.description.abstractEstimating depths of buried lava tubes is important for determining the thermal budgets and effusion rates of certain volcanic systems. This research uses a laboratory experiment scaled to an observed lava tube system to measure the 3D temperature field surrounding a buried depth adjustable glass tube with hot honey flowing through it at varying conditions such as flow rate and temperature. Numerical techniques are used to model the laboratory experiment. The input parameters are then applied to non-laboratory situations. The surface thermal distributions from these models are analyzed to empirically derive a depth estimation function using regression techniques. This depth function is the first scaleable depth estimation technique which can be solved with remote sensing data alone. The minimum temperature, maximum temperature and width of a Lorentzian distribution, fit to a surface thermal transect, are used in the function to predict depth to the hot source. Sensitivity and error analysis of the function is carried out for depths ranging from 0.01 m to ±60 m with good results. The function gives accurate depth estimates of 0.2 m for extreme arctic environments, ±0.3 m for lava tubes and ± 55 m for subsurface coalfires.en_US
dc.language.isoen_USen_US
dc.titleNumerical modeling and remote sensing to determine depths of lava tubes and buried cylindrical hot sourcesen_US
dc.typeThesisen_US
dc.type.degreemsen_US
dc.identifier.departmentDepartment of Geologyen_US
refterms.dateFOA2020-02-18T01:45:53Z


Files in this item

Thumbnail
Name:
Berthelote_A_2005.pdf
Size:
121.8Mb
Format:
PDF

This item appears in the following Collection(s)

Show simple item record