Non-contact infrared temperature measurements in dry permafrost boreholes

While planning the COAST Expedition to the Siberian Laptev Sea in 2005, the question of how to make a short equilibrium temperature measurement in a dry borehole arose. As a result, an infrared borehole tool was developed and used in three dry boreholes (up to 60.2 m deep) in the coastal transition...

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Published in:Journal of Geophysical Research
Main Authors: Junker, Ralf, Grigoriev, Mikhail N., Kaul, Norbert
Format: Article in Journal/Newspaper
Language:English
Published: AGU (American Geophysical Union) 2008
Subjects:
Ice
Online Access:https://oceanrep.geomar.de/id/eprint/27406/
https://oceanrep.geomar.de/id/eprint/27406/1/2008_Junker-etal-Non-contact_JGRB-113.pdf
https://doi.org/10.1029/2007JB004946
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record_format openpolar
spelling ftoceanrep:oai:oceanrep.geomar.de:27406 2023-05-15T16:37:26+02:00 Non-contact infrared temperature measurements in dry permafrost boreholes Junker, Ralf Grigoriev, Mikhail N. Kaul, Norbert 2008 text https://oceanrep.geomar.de/id/eprint/27406/ https://oceanrep.geomar.de/id/eprint/27406/1/2008_Junker-etal-Non-contact_JGRB-113.pdf https://doi.org/10.1029/2007JB004946 en eng AGU (American Geophysical Union) https://oceanrep.geomar.de/id/eprint/27406/1/2008_Junker-etal-Non-contact_JGRB-113.pdf Junker, R., Grigoriev, M. N. and Kaul, N. (2008) Non-contact infrared temperature measurements in dry permafrost boreholes. Journal of Geophysical Research - Solid Earth, 113 . B04102. DOI 10.1029/2007JB004946 <https://doi.org/10.1029/2007JB004946>. doi:10.1029/2007JB004946 cc_by_nc Article PeerReviewed 2008 ftoceanrep https://doi.org/10.1029/2007JB004946 2023-04-07T15:17:31Z While planning the COAST Expedition to the Siberian Laptev Sea in 2005, the question of how to make a short equilibrium temperature measurement in a dry borehole arose. As a result, an infrared borehole tool was developed and used in three dry boreholes (up to 60.2 m deep) in the coastal transition zone from terrestrial to sub-sea permafrost near Mamontovy Klyk in the western Laptev Sea. A depth versus temperature profile was acquired with equilibration times of 50 × 10−3 s at each depth interval. Comparison with a common resistor string revealed an offset due to limitations of accuracy of the infrared technique and the influence of the probe's massive steel housing. Therefore it was necessary to calibrate the infrared sensor with a high precision temperature logger in each borehole. The results of the temperature measurements show a highly dynamic transition zone with temperature gradients up to −0.092°C/m and heat flow of −218 mW/m. A period of submergence of only 600 years the drilled sub-sea permafrost is approaching the overlying seawater temperature at −1.61°C with a temperature gradient of 0.021°C/m and heat flow of 49 mW/m. Further offshore, 11 km from the coastline, a temperature gradient of 0.006°C/m and heat flow of 14 mW/m occur. Thus the sub-sea permafrost in the Mamontovy Klyk region has reached a critical temperature for the presence of interstitial ice. The aim of this article is to give a brief feasibility study of infrared downhole temperature measurements and to present experiences and results of its successful application. Article in Journal/Newspaper Ice laptev Laptev Sea permafrost OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Laptev Sea Journal of Geophysical Research 113 B4
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description While planning the COAST Expedition to the Siberian Laptev Sea in 2005, the question of how to make a short equilibrium temperature measurement in a dry borehole arose. As a result, an infrared borehole tool was developed and used in three dry boreholes (up to 60.2 m deep) in the coastal transition zone from terrestrial to sub-sea permafrost near Mamontovy Klyk in the western Laptev Sea. A depth versus temperature profile was acquired with equilibration times of 50 × 10−3 s at each depth interval. Comparison with a common resistor string revealed an offset due to limitations of accuracy of the infrared technique and the influence of the probe's massive steel housing. Therefore it was necessary to calibrate the infrared sensor with a high precision temperature logger in each borehole. The results of the temperature measurements show a highly dynamic transition zone with temperature gradients up to −0.092°C/m and heat flow of −218 mW/m. A period of submergence of only 600 years the drilled sub-sea permafrost is approaching the overlying seawater temperature at −1.61°C with a temperature gradient of 0.021°C/m and heat flow of 49 mW/m. Further offshore, 11 km from the coastline, a temperature gradient of 0.006°C/m and heat flow of 14 mW/m occur. Thus the sub-sea permafrost in the Mamontovy Klyk region has reached a critical temperature for the presence of interstitial ice. The aim of this article is to give a brief feasibility study of infrared downhole temperature measurements and to present experiences and results of its successful application.
format Article in Journal/Newspaper
author Junker, Ralf
Grigoriev, Mikhail N.
Kaul, Norbert
spellingShingle Junker, Ralf
Grigoriev, Mikhail N.
Kaul, Norbert
Non-contact infrared temperature measurements in dry permafrost boreholes
author_facet Junker, Ralf
Grigoriev, Mikhail N.
Kaul, Norbert
author_sort Junker, Ralf
title Non-contact infrared temperature measurements in dry permafrost boreholes
title_short Non-contact infrared temperature measurements in dry permafrost boreholes
title_full Non-contact infrared temperature measurements in dry permafrost boreholes
title_fullStr Non-contact infrared temperature measurements in dry permafrost boreholes
title_full_unstemmed Non-contact infrared temperature measurements in dry permafrost boreholes
title_sort non-contact infrared temperature measurements in dry permafrost boreholes
publisher AGU (American Geophysical Union)
publishDate 2008
url https://oceanrep.geomar.de/id/eprint/27406/
https://oceanrep.geomar.de/id/eprint/27406/1/2008_Junker-etal-Non-contact_JGRB-113.pdf
https://doi.org/10.1029/2007JB004946
geographic Laptev Sea
geographic_facet Laptev Sea
genre Ice
laptev
Laptev Sea
permafrost
genre_facet Ice
laptev
Laptev Sea
permafrost
op_relation https://oceanrep.geomar.de/id/eprint/27406/1/2008_Junker-etal-Non-contact_JGRB-113.pdf
Junker, R., Grigoriev, M. N. and Kaul, N. (2008) Non-contact infrared temperature measurements in dry permafrost boreholes. Journal of Geophysical Research - Solid Earth, 113 . B04102. DOI 10.1029/2007JB004946 <https://doi.org/10.1029/2007JB004946>.
doi:10.1029/2007JB004946
op_rights cc_by_nc
op_doi https://doi.org/10.1029/2007JB004946
container_title Journal of Geophysical Research
container_volume 113
container_issue B4
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