347
juarry of Verano
/ vertexes
r vertexes of the
quarry, has been
IGM95 (zero order
led respect to the
es localized in the
:o and S. Donato
near to the IGM
them through the
arry of Peschiera
ry vertexes
>een rotated and
ooint IGM95 (three
ale factor,
re derived through
with respect to the
oth the Othometric
r. in this case are
d to first order
Naviglio (Milan)
irea.
local network:
1.1.2 The georeferentiation of the detail vertexes
The georeferentiation of the detail vertices is obtained
respect to the vertexes of the fixed GPS network
described upper. On these secondary vertices it is
possible to make station with the topographic instruments
for the detail measurements. The vertexes of the detail
network, propagated from the primary vertexes, can be
materialized through quick modalities. These vertices can
be easily repositioned and the position can be calculated
ex novo from the primary vertexes; the primary vertexes
have to be positioned where is non prevented the activity
of extraction, perhaps around the limits of the quarry.
The connection of the local GPS network with the Gauss-
Boaga system has been obtained connecting one or more
points to one IGM95 vertices and to two altimetric points
belonging to the fundamental network.
All these measurements of the three local network has
been processed together by least square adjustment.
1.2 The Survey of the detail
The second phase of surveying is the survey of the
details. In function of the typologies of the quarries the
instrumentation to support the survey detail has been
chosen: two are the methodologies that can be adopted
in function of the different typologies of the quarries.
For the under water quarries (quarry at the ground water
table and at the stratum superficial) it has been used a
GPS (RTK modality) associated to an echo-sounder, for
the open quarries it has been used a total station
motorized no prism.
We have to remember that this survey is finalized to the
estimation of the volume of the area of extraction and to
the building of a DTM which have to satisfy the
characteristics of the precision for this work.
The survey of the detail has to be integrated with further
information about the characteristic elements of a quarry,
such as the position of the electric network, buildings, and
other which allow to better represent the quarry.
Two are the methodologies that can be adopted in
function of the different typologies of the quarries.
1.2.1 Open quarry
The instrumental characteristics. To survey sectors of the
open quarries is suggested to adopt a total station
motorized no prism positioned on the vertexes used for
the georeferentiation or for the vertexes of integration.
This kind of advanced instrumentation has impulse laser
range finder that allows to measure the distance, without
prism, of many hundred of meters using the natural
surfaces like reflective surfaces. With these instruments
is possible to improve the accuracy of the volume
estimation thanks to the points density that can be
obtained with the automatic modality and determining
homogeneous areas inside which the terrain is scanned.
These total station motorized can survey some thousands
of points per hour. The data surveyed (azimuth, zenith
directions and distance). Data are registered on file
ASCII.
Generally the open quarries are characterised by fronts
with steep slope.
The applications have shown the obvious necessity to
acquire, during the survey, the breakline located in the
quarry area. Consequently is extremely important to
realize an higher density grid of points. Only in this case it
can be obtained the precision necessary to avoid
conflicting on the volume estimation. Also the density of
the points has a fundamental role particularly in the case
of irregularly surfaces like it’s the case of the quarry.
In the following table is shown that assuming as a datum
volume ( the definitive configuration) the one obtained
using all the points surveyed (14929), the percent of error
drastically decrease from a 50x50mt grid to a 5x5m or
2x2m grid.
Fig. 6 The survey of an open quarry with higher concentration of points in correspondence to the change of slope and of