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+ Download pdf (6.190 kb) - Nederlandse Commissie voor Geodesie

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DE TWEEDE NAUWKEURlGHEIDSWATERPASSlNG VAN NEDERLAND<br />

Chapter 4 THE REFERENCE DATUM, N.A.P.<br />

4.1 Comparison of benchmarks in Amsterdam<br />

Of the orginal benchmarks dating from 1682, five were still usable in 1875 and two in 1928. The<br />

mean sea level at Amsterdam was measured in relation to the Amsterdam datum during the<br />

period 1700-1861; it is the oldest series ofsea level measurements in the world (Fig. 13). Additional<br />

benchmarks were set up and their levels established by KRAYENHOFF in 1812 and by<br />

STAMKART in 1861.<br />

Information relating to the levels of these benchmarks during the period 1812 (1861) to<br />

1952 has been brought together in table 3 and Fig. 14. It appears from this that the original<br />

1682 benchmarks are the most stable in Amsterdam.<br />

4.2 Comparison of the N.A.P. with the Normal-Null (N.N.)<br />

When links were established with the level network of Germany in the period 1875-1885, the<br />

Normal Null (N.N.) was chosen so that N.N. = N.A.P. From a comparison of the results of the<br />

second geodetic levelling with the new levelling ofGermany it transpires that (average value<br />

along border)<br />

N.N. = N.A.P. - 0.021 m<br />

The standard deviation of the value N.N. - N.A.P. is estimated to have been 13 mm in 1885<br />

and 9 mm in 1940. This gives an estimate for the standard deviation of the change between<br />

1885 and 1940 of 16 mm (see [31]). From this it follows that the 1940 N.A.P. (Amsterdam) has<br />

not changed significantly in relation to the N.N. (Potsdam).<br />

4.3 Linking the second geodetic levelling with N.A.P.<br />

In 1928 the old benchmarks Amsterdam 1 and Amsterdam 3 (from 1682) were included in the<br />

second geodetic levelling (Fig. 15). A special staff was used. The measurements to a number of<br />

other benchmarks in Amsterdam are shown'in tables 4 and 5. The benchmark R.B. Ouder<br />

Amstel3 (N.A.P. + 0.5786) forms the intersection between these levels and the networkofthe<br />

second geodetic levelling.<br />

Chapter 5 INSTRUMENTS<br />

5.1 Levels<br />

5.1.1 The Breithaupt level<br />

The Netherlands Geodetic Commission had at its disposal 4 instruments made by Breithaupt<br />

of Cassel (Fig. 16), specially made for river-crossing measurements [21]. These instruments<br />

had a reversible level with an angle value of 5" and a telescope with a magnification X 40.<br />

It was possible to lift the telescope vertically out of the base with levelling screws (Fig. 16);<br />

in combination with an extra tripod and base with levelling screws this enabled the levelling

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