3. Surveying: it is the art of determining the relative positions of different objects
on surface by measuring the horizontal distance between them
Using of surveying:-
1-to prepare topographical maps.
2-to prepare engineering maps.
3-to prepare military maps.
4-to prepare contour maps.
5-to prepare geological maps .
4. Classification of surveying :-
Primary class. Secondary class.
Plane surveying Based on instrument
Based on method
Geodetic surveying Based on object
Based on nature of field
6. There are three main methods of
determined the distance on earth:-
-Direct measurement
-Computative
-E.D.M (electromagnetic-distance-measuring method)
8. Common instrumental errors in linear
measurement:
âLength other than standard:-
Tape manufacturers do not guarantee 100 ft steel tapes to be exactly 100.00 ft.
âTemperature other than standard:-
A temperature higher or lower will change the length of the tape. (Steel tapes are standardized at
20°C )
âTension:-
If tension is greater than standard the tape will stretch.
âSag:-
A tape not supported along its entire length will sag. By applying correct tension the sag can be
reduced.
9. Poor alignment:-
This error occurs when one end of the tape is off-line or there is an obstruction in-
line.
Faulty marking:-
This error is random as the result of incorrect placement of chaining pins.
10. Correction for standard length:
CL=((l-lâ)/lâ)*L
CL : Correction applied to recorded measurement.
l:the actual tape length.
lâ : the nominal tape length.
L:the recorded measurement.
11. Correction for slope:-
âWhen you take a measurement with a tape along an inclined plane (along the
natural slope of the ground),obviously, the taped distance is greater than the
horizontal distance. This taped distance is represented by (s) in the figure
.The difference between the slope distance and the horizontal distance (s â d)
is called the slope correction. This correction is always subtracted from the slope
distance. To compute for the slope correction, you should know either the
vertical
15. The scale : Scale is a fixed ratio that every distance on
the plan bears with corresponding distance on the ground.
Scale can be represented by the following methods:-
1)Engineering Scale:
One centimeter on the plan represents some whole
number of the meters on the ground.
EX: 1cm : 10m
16. 2)Representative Scale :
one unit in the plan represents some number of same units of
length on the ground
the scale is represented as R.f or representative fraction.
This ratio of the map distance to the corresponding ground distance is independent of the
measurement units.
Ex: if the scale is 1cm = 50m;
So , R.F = 1 / (50 x 100 ) = 1/5000
17. 3)Graphical scale
Which can be divided into :
-- linear scale : used when the number of divisions less than or equals to 5
--diagonal scale :used when the number of divisions more than 5
No. of div. = Mean unit / less count
20. Compass
this article is about the direction finding
instrument used in navigation. shows the
directions North corresponds to 0°, and
the angles increase clockwise, so east is
90° degrees, south is 180°, and west is
270°.
These numbers allow the compass to
show the bearings
28. Angles :
Summation of interior angles = (2n-4)*90
Summation of exterior angles = (2n+4)*90
Correction angle = - Error / n where n is No. of angles
Corrected angle = correction angle + angle before correction
30. Correction of departure = - ( total error in dep. / perimeter of traverse ) * Length
of that line
Correction of latitude = - ( total error in Lat. / perimeter of traverse ) * Length of
that line
Linear closing error = â(dep)^2+( lat. )^2
The accuracy ratio = the linear closing error / perimeter of traverse
40. Definition
âAn art of determining the relative height of
different points above or below the surface
41. Object of levelling:
1)is to find the elevation of given point with respect to
some assumed reference line called datum
2)to establish point at required elevation with respect
to datum
42. Important Terms
Datum: an arbitrarily assumed level surface or line with reference to which level of
other line or surface are calculated.
Reduced level: height or depth of a point above or below the assumed datum.
Bench mark (B.M.) : a fixed reference point of known elevation.
Mean sea level (M.S.L.): obtained by making hourly observations of the tides et any
place over a period of 19 years.
43. Types of Levelling :
(I ) Direct Levelling
* Simple levelling
* Differential levelling
*Fly levelling
* Precise levelling
*Profile levelling
*Reciprocal levelling
(II) Indirect or Trigonometric Levelling: By measuring vertical angles and horizontal distance; Less precise.
(III) Stadia Levelling: Using Tachometer principles.
(IV) Barometric levelling: Based on atmospheric pressure difference
44. Simple levelling:
When the difference between two nearby points is
required Then simple levelling is performed.
Assume that the datum at point A of elevation 0.00
Datum 0.00 Elev.
A
B
45. Differential levelling
Differential levelling is adopted when :
(i) the points are at a great difference apart.
(ii) the difference of elevation between the points is
large.
(iii) there are obstacles between the points.
47. Basic components of level
1)telescope:to provide a line of sight.
2)level or bubble tube: to mark line of sight horizontal.
3)levelling head:to bring the bubble of tube level at the center of its run.
4)tripod:to support the above three parts of the level.
49. Adjustments of a level
â Temporary adjustment: are performed at every
setup of instrument
â setting up of level
â levelling of telescope
â focusing of the eye piece
â Focusing of object glass
â Ex: setting up the level 1)fixing the instrument on
tripod
â 2) levelling the instrument approximately by tripod
50. Permanent Adjustment
â The following relationship between the lines are
desirable
â The line of collimation should be parallel to the axis of
the bubble.
â The line of collimation should coincide with the axis of
the telescope.
â The axis of the bubble should be perpendicular to the
vertical axis. That is, the bubble should remain in the
central position for all the directions of the telescope.
51.
52.
53. âThere are two methods for obtaining the
elevations at different points : -
â1)Height of instrument (or plane of collimation)
method.
â2)Rise and fall method.
54. Height of instrument method:
The basic equations are
Height of instrument for the first setting=RL of BM + BS (at
BM)
Subtract the BS and FS from HI to get RL of intermediate
stations and change points
Checking: ÎŁBS - ÎŁFS = Last RL â First RL. This is -ve for fall and
+ve for RISE
55.
56. Rise and Fall method:
Compute all rises and falls
Start at a BM with known RL
To get RL of next stations: add rise to previous RL, or
subtract fall from previous RL
Repeat for all subsequent stations.
57.
58. Two â pegs test :
â Place two pegs about L=30 m (or 40m) apart.
â Set up level midway between the two pegs.
â Read staff on each peg, and calculate true height difference(ÎhT).
â Move level about L/10=3m (or 4m) beyond one of the pegs.
â Read staff on each peg again, and calculate height difference (ÎhA).
â If ÎhA = ÎhT then the instrument is ok.
â If not, then the error is ÎŁ=(s1-S2)-(S3-S4)/L Mm/m
63. Cut : the removal of soil or rock from its natural
location
Fill : the placement and compaction of layers of
earth or rock to form a roadbed of the
planned shape, density, and profile grade
66. A=[(w+2s+w)/2 ] * H
A=(w + s) * H= (4+3.71)*3.71= 28.60 m
To calculate area
at chainage 0
H=3.71 m âheight of Cutâ
67. To calculate area
at chainage 8
H=3.44 m âheight of Fillâ
S=H as slope = 1:1
A=[(w+2s+w)/2 ] * H
A=(w + s) * H = (4+3.44)*3.44= 25.59m
To calculate area
at chainage 16
H=3.40 m
S=H as slope = 1:1
A=[(w+2s+w)/2 ] * H
A=(w + s) * H= (4+3.40)*3.40= 25.16 m
68. To calculate area
at chainage 32
H=0.5 m
S=H as slope = 1:1
A=[(w+2s+w)/2 ] * H
A=(w + s) * H = (4+0.5)*0.5= 2.25 m
To calculate area
at chainage 32
H=0.35 m
S=H as slope = 1:1
A=[(w+2s+w)/2 ] * H
A=(w + s) * H = (4+0.35)*0.35= 1.52 m
To calculate area
at chainage 32
H=1 m
S=H as slope = 1:1
A=[(w+2s+w)/2 ] * H
A=(w + s) * H= (4+1)*1= 5 m
73. Contouring
Contouring is the science of representing the
vertical dimension of the terrain on a two
dimensional map. We can understand contouring
by considering a simple example.
74. Example:
âLet us assume that a right
circular cone of base 5m
diameter and vertical height 5m
is standing upright on its base.
Let the base be resting on a
horizontal plane at zero level as
shown in the Figure 1.
75.
76. Contour Line :-
A Contour line is an imaginary outline of the
terrain obtained by joining its points of equal
elevation. In our example of the cone, each
circle is a contour line joining points of same
level.
77. Contour Interval (CI) :-
Contour interval is the vertical difference between the
levels of consecutive contour lines on a map. The contour
interval is a constant in a given map. In our example, the
contour interval is 100m.
78. Horizontal Equivalent (HE) :-
Horizontal equivalent is the horizontal distance between two
consecutive contour lines measured to the scale of the map.
79. What are The uses of contour?
i) The nature of the ground and its slope can be estimated
ii) Earth work can be estimated for civil engineering projects like road works,
railway, canals, dams etc.
iii) It is possible to identify suitable site for any project from the contour map of the
region.
iv) Inter-visibility of points can be ascertained using contour maps. This is most
useful for locating communication towers.
v) Military uses contour maps for strategic planning.
80.
81. Methods of Contour Surveying
There are two methods of contour surveying:
************************************************
Direct method
Indirect method
82. Direct Method
* Marking the points of the same elevation and plotting
these points on plan
*Accurate but slow
Small area*
83. Procedure :
* a temporary B.M is established
* Setting up the level (in such a position so that the maximum number of points can be
commanded from the instrument station.)
* The height of instrument is determined
* The staff reading required to fix points on the various contours is determined by
subtracting the R.L. of each of the contours from the height of instrument.
84. Example
âIf the height of instrument is 82.48m., then the staff readings required to locate
82, 81 and 80m contours are 0.48, 1.48 and 2.48m respectively. The staff is held
on an approximate position of point and then moved up and down the slope
until the desired reading is obtained. The point is marked with a peg