Tokyo Surface Ship Gravity Meterα-1

Q4 Earth and Planetary Sciences Journal of the Geodetic Society of Japan Pub Date : 1962-10-30 DOI:10.11366/SOKUCHI1954.7.116
Y. Tomoda, H. Kanamori
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引用次数: 10

Abstract

In the "Tokyo Surface Ship Gravity Meter" which was designed in 1960 and completed in 1961, a dynamic gravity meter is mounted directly on the gimbals stabilized by a vertical gyroscope, and is kept vertical. Variations in the vertical acceleration are converted to frequency variations through a dynamic gravity meter and are digitally recorded on punched tapes. Variatoins in the acceleration of gravity due to the motion of a vessel do not contain the shorter period components compared with the disturbing vertical accelerations caused by ocean waves. This enables us to detect the gravity variations from those unacceptable disturbing accelerations by means of a low pass filter. In the "Tokyo Surface Ship Gravity Meter" this operation is carried out by means of digital filtering with the aid of a digital computer. Introduction The essential techniques in a surface ship gravity meter are, firstly, the method of separating the gravity variations and the vertical accelerations caused by the motion of vessels and secondly, the method of keeping the vertical of a gravity meter to measure the vertical component of the accelerations. In the "Tokyo Surface Ship Gravity Meter" which was designed in 1960 and completed in 1961 (Photo. 1, 2. Fig. 1.), a dynamic gravity meter is mounted directly on the gimbals stabilized by a vertical gyroscope, and keeps its vertical. Variations in the vertical acceleration are converted to frequency variations through a dynamic gravity meter and are digitally recorded on punched tapes. Variations in the acceleration of gravity caused by the motion of a vessel do not contain the shorter period components compared with the disturbing vertical accelerations caused by ocean waves. This enables us to detect the gravity variations from those unacceptable disturbing accelerations by means of a low pass filter. In the "Tokyo Surface Ship Gravity Meter" this operation is carried out by means of digital filtering with the aid of a digital computer. In our previous short period bifilar gravity pendulum [1], force, acting on the mass M, is transmitted to the pendulum through a spring and a powerful liquid damper to reduce the effects of the disturbing accelerations. Such an analogue low pass filter, as is used in the Askania Gss [2] or LaCoste Romberg surface ship gravity meter [3], is required to have an excellent lineality. Hence, in the "Tokyo Surface Ship Gravity Meter ", it is tried to solve this problem by the use of a digital 117 Tokyo Surface Ship Gravity Meter ƒ¿-1
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东京水面舰艇重力仪α-1
在1960年设计、1961年完工的“东京水面舰艇重力仪”中,动态重力仪直接安装在由垂直陀螺仪稳定的万向架上,并保持垂直。垂直加速度的变化通过动态重力仪转换为频率变化,并以数字方式记录在穿孔磁带上。与海浪引起的扰动垂直加速度相比,由船舶运动引起的重力加速度的变化不包含较短周期分量。这使我们能够通过低通滤波器从那些不可接受的干扰加速度中检测重力变化。在“东京水面舰艇重力仪”中,这一操作是借助数字计算机通过数字滤波的方式进行的。水面舰船重力仪的关键技术是将重力变化与船舶运动引起的垂直加速度分离的方法,以及保持重力仪的垂直方向来测量加速度的垂直分量的方法。在1960年设计、1961年完工的“东京水面舰艇重力仪”中(图1,2)。图1),动态重力仪直接安装在由垂直陀螺仪稳定的万向架上,并保持垂直。垂直加速度的变化通过动态重力仪转换为频率变化,并以数字方式记录在穿孔磁带上。与海浪引起的令人不安的垂直加速度相比,由船舶运动引起的重力加速度变化不包含较短周期分量。这使我们能够通过低通滤波器从那些不可接受的干扰加速度中检测重力变化。在“东京水面舰艇重力仪”中,这一操作是借助数字计算机通过数字滤波的方式进行的。在我们之前的短周期双线重力摆[1]中,作用在质量M上的力通过弹簧和强大的液体阻尼器传递到摆上,以减少干扰加速度的影响。Askania Gss[2]或LaCoste Romberg水面舰艇重力仪[3]中使用的这种模拟低通滤波器要求具有良好的线性性。因此,在“东京水面舰艇重力仪”中,试图通过使用数字117东京水面舰艇重力仪f¿-1来解决这一问题
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来源期刊
Journal of the Geodetic Society of Japan
Journal of the Geodetic Society of Japan Earth and Planetary Sciences-Earth and Planetary Sciences (all)
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