Showing posts with label Map. Show all posts
Showing posts with label Map. Show all posts

Tuesday, 19 December 2017

Explain the methods of transferring reduced levels from surface to underground in a tunnel setting out work.

Explain the methods of transferring reduced levels from surface to underground in a tunnel setting out work. 

i) Setting out central line of tunnel
ii) Setting out inside tunnels
iii) Transferring of alignment through shafts

i) Setting out central line of tunnel:
The centre-line of tunnels are fixed on the surface along with shaft locations.
Generally the surface control points of the tunnels are not visible from each other. However, by the method of reciprocal ranging points on the summit can be established which can be joined to get the central line. The measurements should be made accurately. Linear measurements are made using invar substance bars with an accuracy of 1 in 10000. Angular measurements are made using 1 second theodolite with an accuracy 0f 15√ N where N is the number of angles. In case of N tunnels in hilly regions it is neither feasible to align the tunnel ends by direct ranging or reciprocal ranging. In such cases precise triangulation has to be used.
The figure shows a scheme of triangulation network with QR as base line for a tunnel
project. Here all the angles are measured accurately by one second theodolite. Usual corrections for length, temperature, terrain, sag and reduction of levels with respect to sea level are all followed in arriving at the values of the coordinates. The traverse is adjusted for angles and coordinates. The proposed tunnel axis is shown in figure as HR.

ii) Setting out Inside Tunnels:
After the coordinates of portals and shafts are finalized, setting out is started. Centre line of
tunnel is done as shown in figure from various portals and shafts.
Back sighting on the pillar, aligned and constructed as far as practicable on the extended
centre line such as pillar C and then by transiting. Reference points are constructed on the roof of tunnels or slightly below the invert for every 300 m.

iii) Transferring of alignment through shafts:
Transfer of alignment is done through shafts by adopting any one of the following methods:
i) By hanging two or more plumb lines down the shaft.
ii) By lighting directly from edge of shaft where shaft diameter to depth ratio is high.
Co-planning is done by hanging two or more plumb lines down the shaft and determining
the bearing of the plumb planes so formed which are connected to the surface. The plumb lines
should be well apart as for as possible. The plumb lines are of special type. The line shall be of
fine steel wire and carrying a symmetrical weight of 35 kg or more. The wire should be well
stretched to keep it tight. In order to keep the wires vertical, the bob should be contained in a
canister with a hood. This arrangement will shield the bob and will reduce oscillations set up by air currents or by water dropping down the shafts. The canister can be filled with water or oil to reduce the vibrations. The bearing of the plumb plane underground is assumed same as at the surface.
This forms the starting direction for the underground survey work.

The following procedure is adopted for transferring the centerline from top.
Ø A theodolite is set up on top of the hill at a suitable position to maintain the centre line of theshaft.
Ø The RLs of both the ends of the shaft are determined by a level. Knowing the bottom RLs ofthe ends the depth of the shaft is found.
Ø Excavation of the shaft is started and verticality is maintained with the help of the plumb-bob which is suspended from wires from top through pulleys.
Ø The excavation is continued until the required bottom level is reached. The depth of the shaft is measured by measuring the length of suspended wire.
Ø The centre line inside the tunnel is maintained by a precise theodolite. This type of
theodolites are provided with an artificial illumination system to enable work at night and in
the darkness of the tunnel.
Ø It should be properly taken care to see that the centre line is maintained from both ends and one transferred from top coincide.


Monday, 13 February 2017

How Maps Work

A map of the world's time zones.
It's easy to think of maps as sets of visual directions.
Whether you're trying to get to the top of Mount Everest or
to a friend's new home, a map can help you find your way.
But maps can do more than help you figure out where you
are and where you're going. They are representations of
information that can describe nearly anything about the
world.
This content is not compatible on this device.
If you wanted to get an idea of which dog breeds are most
popular in different regions, you might spend days looking
at lists and charts. Or, you could look at a map and get an
instant grasp of the same information. Learning about the
physical features, imports, exports and population densities
of different countries would take ages if you relied on
written descriptions in a book. But with a map, all of the
numbers, patterns and correlations are right in front of you.
As Ian Turner, senior cartographer at GeoNova, puts it, "a
map is a type of language. It's a graphic language. It
presents information in hopefully a way that is very easy to
understand."
It's the job of a mapmaker, or cartographer, to put all of
this information into a format that people can understand
and learn from. Exactly what a person can learn depends
on the type of map. Most maps start with an outline of a
location, like a piece of land or a body of water. Then, they
provide information about the location's attributes.
Different maps incorporate different attributes. For
example:
Physical maps illustrate landforms like
mountains, deserts and lakes. With a physical
map, you can get a basic sense of what all or
part of the planet looks like and what its
physical features are. Physical maps usually
show differences in elevation through
hypsometric tints, or variations in color.
Topographic maps, on the other hand, illustrate
the land's shape and elevation using contour
lines.
Political maps display cultural information
about countries, their borders and their major
cities. Most political maps also include some
physical features, like oceans, rivers and large
lakes. You can check out political maps of the
world at our interactive atlas.
Thematic maps add information on a specific
theme, or subject. Examples of common themes
are population density, land use, natural
resources, gross domestic product (GDP) and
climate. Thematic maps can also show
extremely specialized information, such as the
availability of Internet access in different parts
of the world.
This combination of locations and attributes makes it
possible to put lots of information into a very small space.
A single map can show you all of the countries on a
continent, their borders, their approximate populations and
their primary imports and exports. People can also use
specialized thematic maps to analyze trends and patterns
in all kinds of data. A map showing communication costs in
different parts of the world, for example, could help a
nonprofit organization decide where to build a low-cost
wireless network. As Turner explains, "Maps geography
more than about capitals and countries - it's really about
how economics and climate and natural features, how all
the different variables that make up a society relate to one
another."
Common conventions help cartographers present all this
information in a way that makes sense. We'll look at them
in more detail in the next section.