EGU23-4919, updated on 22 Feb 2023
https://doi.org/10.5194/egusphere-egu23-4919
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Long-term sensor drift of pressure gauges characterized by a pressure balance

Hiroyuki Matsumoto1, Hiroaki Kajikawa2, and Eiichiro Araki3
Hiroyuki Matsumoto et al.
  • 1Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Japan (hmatsumoto@jamstec.go.jp)
  • 2National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba, Japan
  • 3Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Japan

It is postulated that a pressure gauge has potential for detection of vertical crustal deformation associated with plate convergence since the measurement resolution is higher than the expected deformation. However, it has been long known that the sensor drift being a few of hPa (cm) per year or larger rate is identified in the long-term pressure observation at the seafloor. We have investigated the sensor drift of pressure gauges pressurized by a pressure balance in the laboratory. Two types of pressure gauges were examined; one is quartz resonant pressure gauges which are traditionally used for in-situ pressure observations and the other is silicon resonant pressure gauges which can be used for oceanographic observations in the future. Full scale of all pressure gauges examined in the present experiment is 70 MPa. Pressure calibration curves were obtained by applying the standard pressure from zero to full scale to characterize hysteresis and repeatability of pressure gauges. Comparing pressure calibration curves under the different temperature condition, only zero offset is changed for the tested quartz pressure gauges, whereas both zero offset and span are changed for some silicon pressure gauges. Then, static pressure of 20 MPa equivalent to 2000 m water depth is applied to the pressure gauges simultaneously for a period of approximately 100 days under the low temperature condition. Some silicon pressure gauges were pressurized under the normal temperature condition. Pressure calibrations were conducted about 50 times repeatedly by providing the standard pressure of 20 MPa using the pressure balance during the experiment. Differences between the standard pressure and the sensor’s output over time were calculated to evaluate the sensor drift. The results suggest that the lower ambient temperature can contribute to the shorter relaxation time (i.e., the elapsed time to disappear initial abrupt change) and the smaller sensor drift (i.e., the linear trend) in the both types of pressure gauges. The sensor drift between the quartz and the silicon pressure gauges were comparable except for the specific silicon pressure gauges. It is noted that the quartz pressure gauges are more sensitive to temperature than the silicon pressure gauges in the present experiment.

How to cite: Matsumoto, H., Kajikawa, H., and Araki, E.: Long-term sensor drift of pressure gauges characterized by a pressure balance, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-4919, https://doi.org/10.5194/egusphere-egu23-4919, 2023.