COMPASS SURVEY - Civil Engineering psc short notes
• The compass does not measure the angle directly, but measures magnetic bearings only
• Relatively low accuracy
• Used area to be surveyed large , fast surveying
SYSTEMS OF ANGULAR MEASUREMENTS
SEXAGESIMAL SYSTEM
1 circumference : 360*
1 degree : 60 min
1 minute : 60 sec
CENTESIONAL SYSTEM
1 circumference : 400 grade
1 grade : 100 centigrade
1 centigrade : 100 cent centigrade
HOURLY SYSTEM
1 circumference : 24 hrs
1 hour : 60 min
1 minute : 60 sec
CIRCULAR SYSTEM
1 circumference : 2pi radian
SYSTEMS OF BEARING
WHOLE CIRCLE BEARING
• The bearing of a line is measured from the reference meridian towards the line right round the circle
• Value between 0 - 360*
• The bearings observed in a prismatic compass or a theodolite is the whole circle bearings.
REDUCED BEARING / QUADRANTAL BEARING
•Bearing is observed clockwise or anticlockwise from north or south whichever is the closest towards east or west
• Value between 0 - 90*
• Surveyors compass
TYPES OF COMPASS
PRISMATIC COMPASS
Graduated circle is fixed to magnetic needle hence it does not move with line of sight
Broad form type needle
Viewing end has a prism
Sighting and reading done simultaneously
Graduations are in WCB
Graduations are inverted
Tripod may not be essential
0 marked at south
More accurate
SURVEYORS COMPASS
Graduated circle fixed to the box hence it moves with the line of sight
Edge bar type needle
Viewing end has only a slit
Sighting and reading done separate
Graduations are in RB
Graduations are straight
Tripod is essential
0 marked at both north and south
Less accurate
DECLINATION
• The horizontal angle which the magnetic meridian makes with the true or geographical meridian.
• Varies from place to place and time to time
• TB = MB ± declination ( considering +ve and -ve decl. )
• Eg. 4° easts or 4° west
VARIATIONS IN DECLINATION
1. SECULAR VARIATIONS : The magnetic meridian swings in one direction in 250 years gradually comes to rest and then swings in the opposite direction.
2. ANNUAL VARIATION : 1 to 2 minutes deviation annually
3. DIURNAL VARIATION : max 10 minutes variation daily. Maximum at poles, day time, summer
4. IRREGULAR VARIATION : 1 - 2* variation due to natural disasters like earthquake volcano
DIP
•Inclination of a freely suspended magnetic needle with the horizontal is known as the dip of the needle. • In northern hemisphere the north end of the needle is deflected downward ///.
• The amount of dip varies in different parts of the earth
• At equator - 0* , at poles - 90*
• In order to counter dip, a sliding weight or rider in the form of fine brass is provided
TERMS
FOREBEARING : bearing taken in the direction of progression of survey
BACKBEARING : bearing taken in opp. Direction to that of progression of survey
DIRECT ANGLE : angle measured clockwise from preceding to following survey lines ( 0 - 360* ) DEFLECTION ANGLE : angle made by survey line with the projection of the preceding line ( 0 - 90* )
ISOCLINIC LINE : line connecting points of equal dip
ISOGONIC LINE : line connecting points of equal declination
ACLINIC LINE : line connecting points of 0 dip
AGONIC LINE : line connecting points of 0 declination
LOCAL ATTRACTION
• any external influence to the magnetic needle• If local attraction exist BB ≠ F ± 180
• LA is equal for all reading taken from a location
BELOW ARE VIDEOS WITH PREVIOUS YEAR QUESTIONS BASED ON COMPASS SURVEY
2 VIDEOS - 50 QUESTIONS
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