Remote thermal detection of exfoliation sheet deformationの紹介

2021 ◽  
Vol 58 (3) ◽  
pp. 147-147
Author(s):  
Kiminori ARAIBA
Keyword(s):  
Thermal Detection ◽  
Sheet Deformation

Microwave enhancement of thermal detection of buried objects

2012 ◽  
Author(s):  
W. Swiderski ◽  
P. Hłosta ◽  
L. Szugajew ◽  
J. Usowicz
Keyword(s):  
Buried Objects ◽  
Thermal Detection

A portable thermal detection method based on target responsive hydrogel mediated self-heating of warm pad

2021 ◽  
Author(s):  
Juan Tang ◽  
Liping Liu ◽  
Shan Gao ◽  
Jiao Qin ◽  
Xiaoxuan Liu ◽  
...  
Keyword(s):  
Detection Method ◽  
Sensitive Detection ◽  
Organophosphate Pesticides ◽  
Self Heating ◽  
Thermal Detection

A simple thermal aptasensing platform was devised for sensitive detection of organophosphate pesticides (malathion as a model target) based on the efficient self-heating reaction of a warm pad with a...

scholarly journals Toward the Rapid Diagnosis of Sepsis: Detecting Interleukin-6 in Blood Plasma Using Functionalized Screen-Printed Electrodes with a Thermal Detection Methodology

2021 ◽  
Author(s):  
Robert D. Crapnell ◽  
Whitchuta Jesadabundit ◽  
Alejandro García-Miranda Ferrari ◽  
Nina C. Dempsey-Hibbert ◽  
Marloes Peeters ◽  
...  
Keyword(s):  
Blood Plasma ◽  
Interleukin 6 ◽  
Rapid Diagnosis ◽  
Screen Printed Electrodes ◽  
Thermal Detection ◽  
In Blood Plasma ◽  
Screen Printed

scholarly journals Comparison of Infrared Thermal Detection Systems for mass fever screening in a tropical healthcare setting

Public Health ◽  
2015 ◽  
Vol 129 (11) ◽  
pp. 1471-1478 ◽  
Author(s):  
M.R. Tay ◽  
Y.L. Low ◽  
X. Zhao ◽  
A.R. Cook ◽  
V.J. Lee
Keyword(s):  
Healthcare Setting ◽  
Detection Systems ◽  
Thermal Detection

RUMEN GAS ANALYSIS BY GAS-SOLID CHROMATOGRAPHY

1961 ◽  
Vol 41 (2) ◽  
pp. 187-196 ◽  
Author(s):  
J. M. McArthur ◽  
J. E. Miltimore
Keyword(s):  
Carbon Dioxide ◽  
Carbon Monoxide ◽  
Hydrogen Sulphide ◽  
Sample Volume ◽  
Gas Analysis ◽  
Complete Analysis ◽  
Thermal Detector ◽  
Thermal Detection ◽  
Methane Carbon

Methods are described for sampling and analysing rumen gases. The analysis requires less than 15 minutes for the determination of hydrogen, oxygen, nitrogen, methane, carbon monoxide, carbon dioxide, and hydrogen sulphide, i.e., for all gases occurring in the rumen. The method is sensitive and requires only a small quantity of sample, and the sample volume need not be known. The presence of water or other vapours in the sample does not influence the results. Relative thermal detector responses have been determined for gases which occur in the rumen. These eliminate the necessity for the calibration of gas chromatographs using thermal detection. The first complete analysis of rumen gas is presented.

An EPR study of 3d4ions in Al2O3by thermal detection

1980 ◽  
Vol 13 (34) ◽  
pp. 6391-6397 ◽  
Author(s):  
J R Fletcher ◽  
J M Grimshaw ◽  
A P Knowles ◽  
W S Moore
Keyword(s):  
Thermal Detection

scholarly journals Glaciotectonic Structures in Central Sweden and their Significance for Glacial Theory

2007 ◽  
Vol 42 (3) ◽  
pp. 315-323 ◽  
Author(s):  
James S. Aber ◽  
Jan Lundqvist
Keyword(s):  
Regional Distribution ◽  
Ice Sheet ◽  
Outer Zone ◽  
Intermediate Zone ◽  
Pressure Gradients ◽  
Last Glaciation ◽  
Narrow Belt ◽  
Sheet Deformation

ABSTRACT Various glaciotectonic structures and landforms created by ice pushing are common in drift and interstadial sediments in a narrow belt of central Sweden. Described examples from the Lake Storsjôn vicinity demonstrate that glaciotectonic deformation took place while the area was deeply covered by the last Fennoscandian Ice Sheet. Deformation was controlled by pressure gradients related to position of the ice divide and ice movement away from the divide. As the position of the divide shifted during the last glaciation, so did the orientation of glaciotectonic structures. The regional distribution of glaciotectonic features in Fennoscandia falls into three zones: (1) inner zone of widespread, small- to moderate-sized features in older drift, (2) intermediate zone of small, isolated features in drift of the last glaciation, and (3) outer zone with all manner of large and small features in drift and soft bedrock. These zones are the cumulative results of multiple glaciations and reflect the overall distribution of deformable sediment and bedrock within the continental substratum.

Sign in / Sign up

Export Citation Format

Share Document