DONET底压传感器的一些特性

H. Matsumoto, E. Araki, K. Kawaguchi, S. Nishida, Y. Kaneda
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引用次数: 3

摘要

DONET即地震海啸密集海底网络系统,于2010年初在日本西南部南开海槽开始运行,并在不久的将来以DONET2的形式向西扩展。DONET天文台由宽带地震仪、地震加速度计、海啸计等多种传感器组成。本研究的重点是海底压力传感器用于海啸测量水压变化。压力传感器指定其性能为0.005%满量程关于迟滞和可重复性。在本研究中,在部署到深海之前,使用JAMSTEC的高精度压力标准对压力传感器的特性进行了评估。高精度压力标准主要由活塞计、压力发生器/控制器、参考压力监测器和热控室定制,几乎再现了深海环境。首先,我们通过在全量程压力范围内施加大气压,即对传感器施加约0 MPa至68 MPa的压力,确认了滞后性和可重复性。结果表明,所有压力传感器均具有规定的滞后性和重复性。然后,通过施加静态20 MPa水压(相当于2000米水深,恒温2°C,持续约一个月)来评估传感器的长期稳定性。因此,传感器的漂移在不同的压力传感器之间是不同的,然而,这意味着逐渐的漂移可能每个月最多发生几厘米。通过长期的原位观测,讨论了传感器在深海部署后的漂移,表明传感器的漂移在早期以每年几到十厘米的速度持续,然后逐渐减小。本文还报道了2011年3月11日东北地震的海啸可以用DONET观测到,其峰值振幅为~20 cm。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Some characteristics of bottom pressure sensors of DONET
DONET, i.e., the dense ocean-floor network system for earthquakes and tsunamis has started its operation in the Nankai Trough, SW Japan in the early of 2010, and followed by the extension to the westward region as DONET2 in near future. DONET observatory is composed of various sensors such as broadband seismometer, seismic accelerometer, tsunami meter, etc. The present study focuses on bottom pressure sensors being used as tsunami meters measuring hydraulic pressure change. Pressure sensors specify their performance of 0.005 % full scale regarding both hysteresis and repeatability. In the present study, pressure sensors' characteristics have been evaluated by using the JAMSTEC's high accuracy pressure standard before deploying into the deep-sea. The high accuracy pressure standard is mainly customized by a piston gauge, a pressure generator/controller, a reference pressure monitor, and a thermal controlled chamber, which virtually reproduces the deep-sea environment. Firstly, we have confirmed hysteresis and repeatability by applying barometric pressure to the full scale pressure range, i.e., ca. 0 MPa to 68 MPa to the sensors. It has been reproduced that all of pressure sensors perform their specified hysteresis and repeatability. Then, long-term sensors' stabilities have been evaluated by applying static 20 MPa hydraulic pressure, which is equivalent to 2,000 meters water depth under the constant temperature of 2 °C for the duration of approximately one month. As a result, sensors' drift varies among pressure sensors, however, which implies that the gradual drift possibly occurs a few centimeters per month in maximum. We also discuss the sensors' drift after deploying the deep-sea by analyzing the long-term in-situ observations, which shows that it continues at a rate of a few to ten centimeters per year in the early stage, then it tends to be reduced gradually. This paper also reports that the tsunami from the Tohoku earthquake on 11 March 2011 could be observed by DONET with those peak amplitudes of ~20 cm.
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