MODULE-IV
Theodolite Surveying
Prepared By-
Prof. Basweshwar S. J.
The system of surveying in which the angles are measured with the
help of a theodolite, is called Theodolite surveying.
The Theodolite is a most accurate surveying instrument
mainly used for :
• Measuring horizontal and vertical angles.
• Locating points on a line.
• Prolonging survey lines.
• Finding difference of level.
• Setting out grades
• Ranging curves
• Tacheometric Survey
Prepared By-
Prof. Basweshwar S. J.
Prepared By-
Prof. Basweshwar S. J.
ADJUSTMENT OF A THEODOLITE
The adjustments of a theodolite are of two kinds :-
• 1. Permanent Adjustments.
• 2. Temporary Adjustments.
Prepared By-
Prof. Basweshwar S. J.
ADJUSTMENT OF A THEODOLITE
1) Permanent adjustments:
The permanent adjustments are made to establish the relationship
between the fundamental lines of the theodolite and , once made , they
last for a long time. They are essential for the accuracy of observations.
2) Temporary Adjustment
The temporary adjustments are made at each set up of the instrument
before we start taking observations with the instrument. There are three
temporary adjustments of a theodolite:-
i) Centering.
ii) Levelling.
iii) Focussing.
Prepared By-
Prof. Basweshwar S. J.
ADJUSTMENT OF A THEODOLITE
Permanent adjustments:
1. Adjustment of Horizontal Plate Levels. The axis of the plate levels must be
perpendicular to the vertical axis.
2. Collimation Adjustment. The line of collimation should coincide with the axis of
the telescope and the axis of the objective slide and should be at right angles to the
horizontal axis.
3. Horizontal axis adjustment. The horizontal axis must be perpendicular to the
vertical axis.
4. Adjustment of Telescope Level or the Altitude Level Plate Levels. The axis of the
telescope levels or the altitude level must be parallel to the line of collimation.
5. Vertical Circle Index Adjustment. The vertical circle vernier must read zero when
the line of collimation is horizontal.
Prepared By-
Prof. Basweshwar S. J.
Sources of errors in theodolite
• Instrumental errors
• Non adjustment of plate bubble
• Line of collimation not being perpendicular to horizontal axis
• Horizontal axis not being perpendicular to vertical axis
• Line of collimation not being parallel to axis of telescope
• Eccentricity of inner and outer axes
• Graduation not being uniform
• Verniers being eccentric
• Personal errors
• Natural errors
• High temperature causes error due to irregular refraction.
• High winds cause vibration in the instrument, and this may lead to wrong readings
on verniers
Prepared By-
Prof. Basweshwar S. J.
Angles by Theodolite
There are two methods of measuring horizontal angles:-
i) Repetition Method.
ii) Reiteration Method.
Prepared By-
Prof. Basweshwar S. J.
Method of traversing
• Included angle method
• Deflection angle method
• Fast angle (or magnetic bearing method)
Prepared By-
Prof. Basweshwar S. J.
Computation of latitude and departure
• Latitude of a line is the distances measured parallel to the north south of the North-
South direction
• Departure of the line is the distance measured parallel to the east-west direction
Prepared By-
Prof. Basweshwar S. J.
Computing latitude and departure
Prepared By-
Prof. Basweshwar S. J.

MODULE FOUR THEODOLITE SURVEY SY CIVIL 5449

  • 1.
  • 2.
    The system ofsurveying in which the angles are measured with the help of a theodolite, is called Theodolite surveying. The Theodolite is a most accurate surveying instrument mainly used for : • Measuring horizontal and vertical angles. • Locating points on a line. • Prolonging survey lines. • Finding difference of level. • Setting out grades • Ranging curves • Tacheometric Survey Prepared By- Prof. Basweshwar S. J.
  • 3.
  • 4.
    ADJUSTMENT OF ATHEODOLITE The adjustments of a theodolite are of two kinds :- • 1. Permanent Adjustments. • 2. Temporary Adjustments. Prepared By- Prof. Basweshwar S. J.
  • 5.
    ADJUSTMENT OF ATHEODOLITE 1) Permanent adjustments: The permanent adjustments are made to establish the relationship between the fundamental lines of the theodolite and , once made , they last for a long time. They are essential for the accuracy of observations. 2) Temporary Adjustment The temporary adjustments are made at each set up of the instrument before we start taking observations with the instrument. There are three temporary adjustments of a theodolite:- i) Centering. ii) Levelling. iii) Focussing. Prepared By- Prof. Basweshwar S. J.
  • 6.
    ADJUSTMENT OF ATHEODOLITE Permanent adjustments: 1. Adjustment of Horizontal Plate Levels. The axis of the plate levels must be perpendicular to the vertical axis. 2. Collimation Adjustment. The line of collimation should coincide with the axis of the telescope and the axis of the objective slide and should be at right angles to the horizontal axis. 3. Horizontal axis adjustment. The horizontal axis must be perpendicular to the vertical axis. 4. Adjustment of Telescope Level or the Altitude Level Plate Levels. The axis of the telescope levels or the altitude level must be parallel to the line of collimation. 5. Vertical Circle Index Adjustment. The vertical circle vernier must read zero when the line of collimation is horizontal. Prepared By- Prof. Basweshwar S. J.
  • 7.
    Sources of errorsin theodolite • Instrumental errors • Non adjustment of plate bubble • Line of collimation not being perpendicular to horizontal axis • Horizontal axis not being perpendicular to vertical axis • Line of collimation not being parallel to axis of telescope • Eccentricity of inner and outer axes • Graduation not being uniform • Verniers being eccentric • Personal errors • Natural errors • High temperature causes error due to irregular refraction. • High winds cause vibration in the instrument, and this may lead to wrong readings on verniers Prepared By- Prof. Basweshwar S. J.
  • 8.
    Angles by Theodolite Thereare two methods of measuring horizontal angles:- i) Repetition Method. ii) Reiteration Method. Prepared By- Prof. Basweshwar S. J.
  • 15.
    Method of traversing •Included angle method • Deflection angle method • Fast angle (or magnetic bearing method) Prepared By- Prof. Basweshwar S. J.
  • 16.
    Computation of latitudeand departure • Latitude of a line is the distances measured parallel to the north south of the North- South direction • Departure of the line is the distance measured parallel to the east-west direction Prepared By- Prof. Basweshwar S. J.
  • 17.
    Computing latitude anddeparture Prepared By- Prof. Basweshwar S. J.