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用震例分析证明了倾斜固体潮振幅异常用于地震预报的可行性。The earthquake case analyses indicate that y value anomaly may be applied to predict earthquake.

2004年以来，观测资料稳定，并清晰地记录到了固体潮形态。Since 2004, the observed data have been steady and the forms of the solid tide have been clearly recorded.

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提出了在倾斜固体潮观测资料中消除摆杆方位影响的实用公式，并用实例加以验证。Pratical formulas of reducing the effects of the Pendulum beam in the observations are proposed by some examples.

月亮和太阳的地心引力不仅创造了海洋和大气潮，也同时创造了固体潮。And the gravitational pull of the moon and sun not only cause ocean and atmospheric tides but earth tides as well.

固体潮对测站位移的影响是空间大地测量和天文地球动力学研究的重要组成部分。The influence of solid tide on station displacements is an important part of the spatial geodesy and astrogeodynamics research.

同时发现该洞室内虽然温度变化甚小，但仍对水平应变固体潮有影响。Besides, it is found that though temperature change is very small in the hole, it has an effect on horizontal strain earth tide.

认为用承压井水位潮的观测也可以研究固体潮现象，一口好的承压井其观测资料中包含着更多的信息可以开发。It is thaught that the observation of the water-level tide in artesian well can also be used to research the solid tide phenomenon.

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本文从理论公式和计算数据上分析了固体潮对天文经纬度的影响。The present paper analyses the effect of earth tide on astronomical latitude and longitude according to theoretical formulas and calculated data.

结合钻孔差应变仪的工作原理，借助体应变观测资料，提出了利用理论固体潮对泰安台差应变观测进行实地标定的新方法。Based on the data collection using the earth tide detecting instrument, a restricting range method to estimate continuity of the signals is studied.

证明这两种基线长度和安装方式不同的仪器，观测到的地层应变在固体潮频段具有可比性。That concludes these instruments with different baseline and different working principle, can observe comparable earth strain in the solid tidal band.

用LW—150型涡轮流量变送器、CZ—1002型数字记录仪组成的观测系统，在庐江台自流井进行了流量固体潮观测。The flow earth-tide has been observed with observational system consisting of LW-150 flow sensor and CZ-1002 digital recorder at Lujiang artesian well.

利用井水位的固体潮效应反演含水层应力变化，比利用气压效应更接近实际情况。The variation of stress in the aquifer inversed is closer to practice by the tidal effect of the water level in a deep well than by the barometric effect.

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利用这种方式在武昌固体潮台作为DZW微伽重力仪的数字记录历时近一年，获得较好的固体潮观测资料。Nearly one year a better data of earth tide observation was got by this method for digital recording of DZW μgal gravimeter in Wu Chang earth tide station.

阐述如何利用地震台观测得到的地倾斜矢量图对固体潮半日波进行潮汐导纳分析。The tide admittance analysis for the semidiurnal wave of the earth tide by use of the vector pattern of ground tilt observed at seismostations is expounded.

球状弹性均匀地球模型是地球的一级近似，本文给出计算该地球模型固体潮应力场的计算方法。Homogeneous spherical elastic earth model is the first approximation of the real earth in the approach to study the earth tide, this paper gives a numerical.

本文利用滞弹性体模型来研究去掉了弹性理论固体潮应变之后的附加应变，并引入应变率的概念。This paper chooses a viscoelastic model for studying additional strain minus the tide of elastic theory strain and first introduces the concept of strain rate.

计算井水位气压系数、固体潮系数和海潮系数以前主要在时间域内一般用回归分析的方法。Formerly, the barometric, solid tide and sea tide coefficients in water level change were usually calculated by means of regression analysis method in the time domain.

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研究表明，大地震前震源区及其附近发生的几次显著地震易受固体潮引潮力某个方位附近触发。The research results show that several significant shocks happened in source region and its vicinity before a large earthquake are easily triggered by certain directions.

本文从理论上阐述了单靠倾斜仪不能监测地面倾斜，必须联合倾斜和重力固体潮资料才能测量地面倾斜。In this paper, it is pointed out theoretically that the ground surface tilt is not observed by only tiltmeter, but must be determined by both tilt and gravity earth tide data.

本文使用最新大地测量结果，给出了体应变固体潮理论值的计算公式并编制了计算程序。Using latest geodetic results, this paper provides the calculation formulae for the theoretical values of the volumetric tidal strain and constructs the computational program.