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0_ CUPRINS - IPA SA

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In the following we are going to do a statistical analysis on 5 groups of distances, from<br />

0,15km to 2,9km, from 500 to 500m, for 29 level differences, determined through GPS<br />

technology and measured in stages IV - VII.<br />

Out of the 29 differences, 24 differences from the first four groups fall within the<br />

tolerance of + / - 30mm the situation being the following on groups of distances:<br />

- gr. I, distances from 150m to 500m, has four differences with values between -7mm to<br />

+26 mm with a medium difference value of 13.3 mm;<br />

- gr. II, distances from 500m to 1000m, has nine differences with values between -16mm<br />

to +17mm with a medium difference value of 7,1mm;<br />

- gr. III, distances from 1000m la 1500m, has eight differences with values between -<br />

29mm to +29mm with a medium difference value of 13,4mm;<br />

- gr. IV, distances from 1500m to 3000m, has three differences with values between<br />

+25mm to +31mm for a distance of 2,9km, with a medium difference value of 28,0mm;<br />

In gr.V there are 5 distances, from the 29 analysed, that overpass the tolerance of +/-<br />

30mm, with values between 2mm and 8mm.<br />

In gr.VI we have the two cl.B points with wrong ellipsoid marks, with the values<br />

mentioned before , levels that influence the precision of the geometrical quasi-geoide that is in<br />

train of construction.<br />

Analyzing this group of measurements, we can say with certainty that for distances up to<br />

1500m, with normal precautions of design and location of control points and of measuring the<br />

antenna height with certainty, differences in level measured by GPS technology provides easy fit<br />

into tolerance + / - 30mm. For longer distances, up to about 3000m, the above entry in tolerance<br />

can be achieved in good condition by taking additional measures in the design phase. However<br />

for listing permanent GNSS stations located during the year 2009 it is advisable to keep the same<br />

method used for determining the levels during 2009.<br />

References<br />

1. Demidovich, B.P. & Maron, I.A.: Computational Mathematics. Mir Publishers, 1981.<br />

2. Dragomir, V., Ghiţau, D., Mihailescu, M., Rotaru, M.: Teoria Figurii Pamantului, E.T., 1977<br />

3. Dragoescu, I., Radulescu, F., Nacu, V., Stiopol, D.: Participarea Romaniei la intocmirea<br />

hartilor gradientilor orizontali ai miscarii verticale ale scoartei terestre pentru zona Carpato-<br />

Balcanica si pentru zona statelor est-europene. Analele IGFCOT, vol.X, 13-24 pp, 1989.<br />

4. Fotescu, N. & S`vulescu, C.: Teoria Erorilor. Litografie, ICB, 1988.<br />

5. Helmert, F.R.: Die mathematischen und physikalischen Theorien der höheren Geodäsie.<br />

G.G.Teubnez Verlag, Leipzig, 1880 ]i 1962.<br />

6. Nacu, V., Radulescu, F., Mateciuc, D., Stiopol, D.: Study of the deformation parameters in<br />

Gruiu-Caldarusani geodynamic polygon. XXIII General Assembly of European<br />

Seismological Commission, Activity Raport 1990-1992, 345-348 pp., Proceedings, vol II,<br />

Prague, Checkoslovakia,1992.<br />

7. Nacu, V., Radulescu, F., Mateciuc, D.: Horizontal deformations in the Gruiu-Caldarusani<br />

geodynamic polygon of Romania, Rev. Roumaine de Geophysique 37, 1993.<br />

8. Nacu, V., Mateciuc, D., Moldoveanu, C, Ilies, A.: Horizontal deformations in the Gruiu<br />

Caldarusani Test - Polygon of Romania. Mitteilungen aus den Geodätischen Instituten der<br />

Rheinischen Friedrich - Wilhelms - Universität Bonn, 1994.<br />

53

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