Experimental and numerical analysis in heat flow sensors calibration

2019 ◽  
Vol 138 (4) ◽  
pp. 2901-2912
Author(s):  
Gino Cortellessa ◽  
Fausto Arpino ◽  
Marco Dell’Isola ◽  
Giorgio Ficco ◽  
Luigi Iacomini ◽  
...  
2016 ◽  
Vol 87 (2) ◽  
pp. 165-174
Author(s):  
Elena Onofrei ◽  
Teodor-Cezar Codau ◽  
Gauthier Bedek ◽  
Daniel Dupont ◽  
Cedric Cochrane

This paper describes the concept of creating and testing of a textile heat flow sensor in order to determine the amount of heat exchanged between the human body and its environment. The main advantage of this sensor is the permeability to moisture, which allows taking into account the evaporation phenomenon, contrary to the traditional heat flow sensors. Another property related to this new sensor is its flexibility conferred by the textile substrate, which allows it to be applied on deformable surfaces.


1954 ◽  
Vol 20 (92) ◽  
pp. 237-242
Author(s):  
Kiyoshi YAMAGATA ◽  
Kaneyasu NISHIKAWA ◽  
Toshiyuki GOTO

2002 ◽  
Vol 73 (7) ◽  
pp. 2755-2765 ◽  
Author(s):  
Tomasz Plackowski ◽  
Yuxing Wang ◽  
Alain Junod

1986 ◽  
Vol 7 (6) ◽  
pp. 426-430
Author(s):  
B. G. Penn ◽  
F. E. Ledbetter ◽  
W. T. White ◽  
J. M. Clemons

Geophysics ◽  
1985 ◽  
Vol 50 (7) ◽  
pp. 1108-1112 ◽  
Author(s):  
J. C. Dunn ◽  
H. C. Hardee

The Puhimau hot spot, on Kilauea Volcano, Hawaii, was thermally mapped using new high‐output thermopile heat flow sensors. This thermal geophysical technique allows rapid measurement of surficial heat flow, especially in regions of high heat flux where shallow burial depths can be used. Heat flow measurements ranged from 200 to [Formula: see text] over the central portion of the Puhimau hot spot. Analysis of the heat flow data combined with other geophysical measurements suggests that the Puhimau hot spot could be caused by a shallow and perhaps still molten body of magma beneath the local area. These geophysical measurements, along with a proposed shallow scientific drillhole, can provide valuable evaluation of geophysical techniques for locating magma bodies in the crust.


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