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Atom interferometric gravity gradiometer: Disturbance compensation and mobile gradiometry.

机译:原子干涉重力梯度仪:干扰补偿和移动梯度仪。

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First ever mobile gravity gradient measurement based on Atom Interferometric sensors has been demonstrated. Mobile gravity gradiometers play a significant role in high accuracy inertial navigation systems in order to distinguish inertial acceleration and acceleration due to gravity.;The gravity gradiometer consists of two atom interferometric accelerometers. In each of the accelerometer an ensemble of laser cooled Cesium atoms is dropped and using counter propagating Raman pulses (pi/2-pi-pi/2) the ensemble is split into two states for carrying out atom interferometry. The interferometer phase is proportional to the specific force experienced by the atoms which is a combination of inertial acceleration and acceleration due to gravity.;The difference in phase between the two atom interferometric sensors is proportional to gravity gradient if the platform does not undergo any rotational motion. However, any rotational motion of the platform induces spurious gravity gradient measurements. This apparent gravity gradient due to platform rotation is considerably different for an atom interferometric sensor compared to a conventional force rebalance type sensor. The atoms are in free fall and are not influenced by the motion of the case except at the instants of Raman pulses. A model for determining apparent gravity gradient due to rotation of platform was developed and experimentally verified for different frequencies. This transfer function measurement also lead to the development of a new technique for aligning the Raman laser beams with the atom clusters to within 20 mu rad.;This gravity gradiometer is situated in a truck for the purpose of undertaking mobile surveys. A disturbance compensation system was designed and built in order to compensate for the rotational disturbances experienced on the floor of a truck. An electric drive system was also designed specifically to be able to move the truck in a uniform motion at very low speeds of about 1cm/s. A 250 x10-9 s-2 gravity gradient signature due to an underground void at Hansen Experimental Physics Building at Stanford was successfully measured using this mobile gradiometer.
机译:首次展示了基于原子干涉传感器的移动重力梯度测量。移动重力梯度仪在高精度惯性导航系统中起着重要作用,以区分惯性加速度和重力引力。重力梯度仪由两个原子干涉式加速度计组成。在每个加速度计中,放下一组激光冷却的铯原子,并使用反向传播的拉曼脉冲(pi / 2-pi-pi / 2)将其分为两个状态,以执行原子干涉测量。干涉仪的相位与原子所经历的比力成正比,这是惯性加速度和重力引起的加速度的组合;如果平台不进行任何旋转,则两个原子干涉式传感器之间的相位差与重力梯度成正比。运动。但是,平台的任何旋转运动都会引起伪重力梯度测量。与常规力重新平衡型传感器相比,对于原子干涉传感器,由于平台旋转而引起的该表观重力梯度明显不同。原子处于自由下落状态,除了拉曼脉冲的瞬间外,不受壳体运动的影响。开发了用于确定由于平台旋转而引起的表观重力梯度的模型,并针对不同频率进行了实验验证。这种传递函数的测量还导致了一种新技术的发展,该技术用于将拉曼激光束与原子簇对准到20 rad rad之内。该重力梯度仪位于卡车上,目的是进行移动测量。设计并构建了干扰补偿系统,以补偿卡车地板上遇到的旋转干扰。还专门设计了一种电驱动系统,以使卡车能够以大约1cm / s的极低速度匀速运动。使用该移动式梯度仪成功地测量了斯坦福大学汉森实验物理大楼地下空隙造成的250 x10-9 s-2重力梯度特征。

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