Determination of Geopotential Differences between Local Vertical Datums and Realization of a World Height System   总被引：2，自引：0，他引：2  

Burša  Milan  Kouba  Jan  Müller  Achim  Raděj  Karel  True  Scott A.  Vatrt  Viliam  Vojtíšková  Marie 《Studia Geophysica et Geodaetica》2001,45(2):127-132

The methodology developed for connecting Local Vertical Datums (LVD) was applied to the Australian Height Datum (AHD) and the North American Vertical Datum (NAVD88). The geopotential values at AHD and NAVD88 were computed and the corresponding vertical offset of 974 mm with rms 51 mm was obtained between the zero reference surfaces defined by AHD and NAVD88. The solution is based on the four primary geodetic parameters, the GPS/levelling sites and the geopotential model EGM96. The Global Height System (or the Major Vertical Datum) can be defined by a geoidal geopotential value used in the solution as the reference value, or by the geopotential value of the LVD, e.g. NAVD88.  相似文献   

A study of the electromagnetic field of a magnetic vertical dipole on the model of homogeneous half-space with a spherical cavity     

Karel Faldus  Václav Petr  Oldřich Praus  Marta Tobyášová 《Studia Geophysica et Geodaetica》1963,7(4):372-395

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Die la gefehler des trigonometrischen netzes der ČSR als indikator für die art der koordinatenumformung     

Karel Kučera 《Studia Geophysica et Geodaetica》1960,4(2):130-132

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Критика     

Jaroslav Kopáček  Karel Bayer  Otakar Zikmunda 《Studia Geophysica et Geodaetica》1960,4(2):202-203

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Eine Elektronische Apparatur zur Messung der Elastizitätskonstanten an Gesteinsproben     

Karel Klíma  Zdeněk Pros  Ludvík Waniek 《Studia Geophysica et Geodaetica》1957,1(1):106-113

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On the magnetic phases of natural pyrrhotites     

Karel Zapletal  Reviewer F. Janák 《Studia Geophysica et Geodaetica》1972,16(2):167-176

Summary The magnetic phases of natural pyrrhotites were studied by the method of powder patterns, the chemism of the magnetic phases by means of the electron microprobe method, and the crystal phases by etching the polished sections. The method of powder patterns distinguished the ferrimagnetic and antiferromagnetic phases in the transition-type pyrrhotites. The method of absorbed electrons lead to the discovery that both phases have a different chemical composition and that the ferrimagnetic phase has a lower denisty and an average atomic number. The linear and point-by-point analysis disclosed that the ferrimagnetic phase has a lower weight content of Fe and a higher weight content of S than the antiferromagnetic phase. Both the magnetic phases displayed different properties when etched, and therefore they not only have a different chemical composition, but also a different crystal structure. The necessity of studying the image of the absorbed electrons and the image of the etched surface of the polycrystalline samples of pyrrhotites of the transition type separately on individual grains was pointed out.  相似文献   

Frequency analysis of geomagnetic beating-type pulsations in thepc3 range     

Karel Prikner  Jaroslav Střeštík  Karel Dobeš  Reviewer M. Hvoždara 《Studia Geophysica et Geodaetica》1972,16(3):262-270

Summary The spectral analysis of samples of beating-type pc3 pulsations, recorded at the Budkov Observatory during the summer months of 1968 and 1969 was carried out in the frequency interval10 mHz100 mHz. The average limits of the pulsation frequency range are roughly20 mHz60 mHz. The centre of the occurrence frequency graphs for both components is at the frequency f_g 41 mHz. The analysis of three separated daily intervals showed a very slight tendency to a systematic decrease in the frequency of the centre from the morning to the afternoon. The study of the sense of rotation of the pulsation disturbance vector in the (X, Y)-plane showed an overall predominancy of L over R-types during daytime, particularly during the morning.  相似文献   

Volles Gewicht einer im Refraktionsmilieu gemessenen Grösse (Teil I)     

Karel Kučera  Rezensent J. Kašpar 《Studia Geophysica et Geodaetica》1971,15(2):132-140

Summary As regards the concept of complete weight p with which an observed quantity (e.g., the direction of theA–G net) should enter the net adjustment, according to Eq.(1), apart from the fundamental weight p ₀ ), determined by the number of repetitions, it should also contain the time parameter p_t according to Eq.(11), where c>1 is a constant, and t is the number of days of observation, and also the refraction factor p_r according to Eqs(17, 18), where q is the structural weight of the direction. The condition for being able to determine p_r with the directions is observation by means of the three-directional vertex method[2], because it is not possible to localize lateral refraction by angular methods. The theory of complete weight is in favour of observations with a high fundamental weight p ₀ which automatically yield higher values of t, and also of p_t. The introduction of the complete weight into the experimental directional net in Fig. 2 caused the mean value of the uneliminated refraction error to decrease from 0.24 to 0.12, the mean square error of the adjusted direction being 0.17. The value of the constant c was investigated and the method of determining the parameter p_r was derived also for lengths measured electro-optically. Mention is made of the effect of complete weights on the length adjustment of a net in[6].  相似文献   

Rapid changes in the fourier spectra ofPi1 pulsations during magnetically disturbed periods     

Karel Prikner 《Studia Geophysica et Geodaetica》1969,13(3):276-292

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Velocity of longitudinal waves in eclogite and ultrabasic rocks under pressures to 4 kilobars     

E. I. Bajuk  M. P. Volarovich  Karel Klíma  Zdeněk Pros  Jiří Vaněk 《Studia Geophysica et Geodaetica》1967,11(3):271-280

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