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Surveying Master Class Part 1:All Topic Cover in One Place

Surveying Master Class Part 1 : All Topic Cover in One Place

Surveying ek aisi art hai jisme kisi fixed point ke sapeksh (with respect to) dusre points ki relative position nirdharit ki jati hai. Iske liye distances aur angles ko mapa jata hai. Civil engineering exams mein iska weightage lagbhag 7-8% hota hai.

Surveying Master Class Part 1 : All Topic Cover in One Place



Surveying Master Class Part 1: Comprehensive Topic Coverage

Surveying is an art used to determine the relative positions of points with respect to a fixed point. This is achieved by measuring distances and angles. In civil engineering exams, it typically carries a weightage of 7-8%.


Primary Types of Surveying

Surveying is categorized based on whether the Earth's curvature is considered:

  • Plane Surveying: Curvature is neglected; the surface is treated as a flat plane. Used for small areas (Area < 260 $km^2$).

  • Geodetic Surveying: Curvature is considered for high precision. Used for large areas (Area > 260 $km^2$).

Key Technical Language:

  • Linear Difference: For a 12 km line, the difference between the arc (Geodetic) and chord (Plane) is only 1 cm.

  • Spherical Excess: For a spherical triangle of 195.5 $km^2$, the sum of interior angles is 180° 0' 1".

  • Angle Sum: In plane surveying, the sum of a triangle's angles is exactly 180°.

  • Units: 1° = 60 minutes; 1 minute = 60 seconds.


Classification of Surveys

  • Topographic Survey: To map natural and man-made features (rivers, mountains, buildings).

  • Cadastral Survey: To determine property lines and boundaries.

  • City Survey: For urban infrastructure planning (roads, sewers).

  • Hydrographic Survey: To map features within water bodies.

  • Astronomical Survey: To determine the position of celestial bodies.


Understanding Scale

Scale is the ratio of map distance to ground distance.

  • Representative Fraction (R.F.): If 1 cm on a map = 10 m on ground, R.F. = 1/1000.

  • Area Scale: $S^2 = \frac{\text{Map Area}}{\text{Ground Area}}$

Shrunk Scale and Shrinkage Factor:

  • Shrinkage Factor (S.F.) = $\frac{\text{Shrunk length}}{\text{Actual (original) length}}$

  • Shrunk Scale = S.F. $\times$ Old R.F.


Vernier Scales: An Introduction

A Vernier scale is an auxiliary scale used to read fractional parts of the smallest division of the main scale.

Types of Vernier Scales:

FeatureDirect VernierRetrograde Vernier
CalibrationSame direction as main scaleOpposite direction to main scale
Division Relation$(n-1)$ main divisions = $n$ vernier divisions$(n+1)$ main divisions = $n$ vernier divisions
Division SizeMain scale ($s$) > Vernier ($v$)Vernier ($v$) > Main scale ($s$)
  • Least Count (L.C.) = $s/n$


Principles of Surveying

  1. Working from Whole to Part: The area is divided into large parts, then subdivided. This localizes errors and prevents them from accumulating.

  2. Relative Position: Locating a new point by taking at least two measurements from fixed reference points.


Chain Surveying

  • Base Line: The longest and most important line dividing the area.

  • Tie Line: Used for detailing features.

  • Check Line: Used to verify accuracy.

  • Offsets: Perpendicular (90°) or Oblique (any other angle).

Common Instruments:

  • Angle Measurement (90°): Cross Staff, Optical Square (works on Double Reflection, mirrors at 45°).

  • Slope: Clinometer.

Types of Chains:

  • Metric: 20 m (100 links) or 30 m (150 links).

  • Gunter's: 66 ft (100 links).

  • Engineer's: 100 ft (100 links).

  • Revenue: 33 ft (16 links).

Tapes:

  • Invar Tape: Alloy of Nickel (36%) and Steel. It has a very low thermal expansion coefficient ($\alpha$), making it ideal for measuring Base Lines.


Error and Correction Principles

  • Correction (C) = True Value - Measured Value

  • Error (E) = Measured Value - True Value ($E = -C$)

Corrections in Chaining/Taping:

  1. Length Correction: $L \times l = L' \times l'$ (True length $\times$ True Tape = Measured length $\times$ Incorrect Tape).

  2. Slope Correction ($C_s$): $-\frac{h^2}{2l'}$. Always Negative.

  3. Temperature Correction ($C_{Temp}$): $L \alpha (T_m - T_0)$. Positive if $T_m > T_0$.

  4. Pull Correction ($C_{pull}$): $\frac{(P_m - P_0)L}{AE}$. Positive if $P_m > P_0$.

  5. Sag Correction ($C_{sag}$): $-\frac{W^2L}{24P_m^2}$. Always Negative.

  6. Normal Tension: The pull at which pull correction and sag correction cancel each other out.


Bearing and Meridian

  • Bearing: Horizontal angle measured with respect to a fixed direction (Meridian).

Systems of Bearing:

  1. Whole Circle Bearing (WCB): Measured clockwise from North (0° to 360°).

  2. Reduced Bearing (RB) / Quadrantal Bearing: Measured from North or South (whichever is closer). Range is 0° to 90°. Written as $N\theta E, S\theta W$, etc.

Conversion Examples (WCB to RB):

  • $95^\circ$ (SE Quadrant) $\rightarrow 180^\circ - 95^\circ = S~85^\circ~E$.

  • $272^\circ$ (NW Quadrant) $\rightarrow 360^\circ - 272^\circ = N~88^\circ~W$.

  • $351^\circ$ (NW Quadrant) $\rightarrow 360^\circ - 351^\circ = N~9^\circ~W$.

Conversion Examples (RB to WCB):

  • $S~10^\circ~E \rightarrow 180^\circ - 10^\circ = 170^\circ$.

  • $S~79^\circ~W \rightarrow 180^\circ + 79^\circ = 259^\circ$.

  • $N~81^\circ~W \rightarrow 360^\circ - 81^\circ = 279^\circ$.




Types of Meridians

In surveying, two main meridians are used as references:

  • True Meridian: A line passing through the Earth's True North and True South.

  • Magnetic Meridian: A line passing through the Magnetic North and Magnetic South, following the direction of the Earth's magnetic flux.

Magnetic Declination and Variations

Magnetic Declination is the horizontal angle between the True Meridian and the Magnetic Meridian. Since the Magnetic Meridian is constantly shifting, the declination is not constant. Changes in declination are called Variations:

  • Diurnal Variation: Daily changes.

  • Yearly Variation: Changes occurring over one year.

  • Secular Variation: Changes occurring over an interval of approximately 150 years.

  • Irregular Variation: Sudden changes caused by natural disasters like earthquakes or tsunamis.

Types of Declination and Calculations

When performing calculations, Declination is divided into two parts:

1. Eastern Declination (Positive)

When Magnetic North is toward the East of True North, it is considered positive.

Formula:

$$TB = MB + \delta_E$$

(Where $TB$ = True Bearing, $MB$ = Magnetic Bearing, and $\delta_E$ = Eastern Declination)

2. Western Declination (Negative)

When Magnetic North is toward the West of True North, it is considered negative.

Formula:

$$TB = MB - \delta_W$$

(Where $\delta_W$ = Western Declination)

Note: Both formulas are always used in the Whole Circle Bearing (WCB) system.

Examples of Magnetic Declination

In a compass survey, True Bearing ($TB$) is calculated using Magnetic Bearing ($MB$) and Declination ($\delta$):

  • Question 1: If the Magnetic Bearing of a line is $S~70^\circ~W$ and the Declination is $6^\circ~West$, what will be the True Bearing?

    • Calculation: First, convert $MB$ to $WCB$: $180^\circ + 70^\circ = 250^\circ$.

    • Formula: $TB = MB - \delta_W = 250^\circ - 6^\circ = 244^\circ$.

    • Result: Converting back to $RB$ gives $S~64^\circ~W$.

  • Question 2: If $TB = 140^\circ$ and $MB = 172^\circ$, what is the Declination?

    • Calculation: The difference between the two is $172^\circ - 140^\circ = 32^\circ$.

    • Result: Since $MB > TB$, the Declination is $32^\circ~West$.

Angle of Dip

The Angle of Dip is the vertical angle between the direction of magnetic flux and the horizontal plane.

  • At the Equator, the value of Dip is $0^\circ$.

  • At the Poles, the value of Dip is $90^\circ$.

Fore Bearing (FB) and Back Bearing (BB)

Bearings are divided into two parts according to the direction of the survey:

  • Fore Bearing (FB): The bearing taken from a point toward the next point in the direction of the survey.

  • Back Bearing (BB): The bearing taken from a point toward the previous point, opposite to the direction of the survey.

LineFore Bearing (FB)Back Bearing (BB)
ABMeasured at Point A $(\theta_A)$Measured at Point B $(\theta_B)$

Note: In the WCB system, the difference between FB and BB is always $180^\circ$.

Relationship between FB and BB

For any single line, the difference between its Fore Bearing and Back Bearing is always $180^\circ$.

Formula: $|FB - BB| = 180^\circ$.

Rules for Calculating BB

In the Whole Circle Bearing (WCB) system, the following rules are used to find the BB:

  • Rule 1: If the value of FB is less than $180^\circ$ ($FB < 180^\circ$), then $BB = FB + 180^\circ$.

  • Rule 2: If the value of FB is more than $180^\circ$ ($FB > 180^\circ$), then $BB = FB - 180^\circ$.

Internal and External Angles

At any station, the difference between the Back Bearing (BB) of the previous line and the Fore Bearing (FB) of the next line determines the internal or external angle.

Numerical Examples

  • Question 1: If the FB of line AB is $290^\circ$, what will be the BB?

    • Solution: Since $290^\circ > 180^\circ$, then $290^\circ - 180^\circ = 110^\circ$.

  • Question 2: If the FB of line BA is $60^\circ$, what will be the FB of line AB?

    • Hint: The FB of line BA is actually the BB of line AB.

    • Solution: $60^\circ + 180^\circ = 240^\circ$.

Bearing Conversion (RB System)

In the Reduced Bearing (RB) system, finding the Back Bearing (BB) from the Fore Bearing (FB) is very simple. Only the cardinal directions ($N, S, E, W$) are changed, while the numerical value remains the same.

  • Rule: Change $N$ to $S$, $S$ to $N$, $E$ to $W$, and $W$ to $E$.

  • Example: If the FB is $S~30^\circ~E$, then the BB will be $N~30^\circ~W$.

Formula for Calculating Internal Angle

To find the internal angle between two lines at any station:

Internal Angle = FB of next line - BB of previous line

Local Attraction

Local Attraction is an error that occurs in the magnetic needle when a local magnetic object (such as electric poles, steel buildings, or iron tools) is present in the survey area.

  • Detection: If the difference between the FB and BB of a line is not $180^\circ$ ($|FB - BB| \neq 180^\circ$), it means the stations are affected by local attraction.

  • Clean Station: If $|FB - BB| = 180^\circ$, both readings are correct, and the stations are free from local attraction.

Impact of Local Attraction

Even if stations are affected by local attraction, the internal or external angle between them remains correct. This is because local attraction changes both readings by the same amount, and the error cancels out during subtraction.

Latitude and Departure

In traversing, the coordinates of a line are divided into Latitude and Departure:

  • Latitude (L): The projection of a line on the North-South axis.

    • Formula: $L = l \cos \theta$ (Positive toward North, Negative toward South).

  • Departure (D): The projection of a line on the East-West axis.

    • Formula: $D = l \sin \theta$ (Positive toward East, Negative toward West).

Rules for a Closed Traverse

For a perfect closed traverse:

  • The sum of all Latitudes must be zero: $\Sigma L = 0$.

  • The sum of all Departures must be zero: $\Sigma D = 0$.

Closing Error ($e$)

If the sums of $L$ and $D$ are not zero, there is a "Closing Error" in the traverse.

Formula: $e = \sqrt{(\Sigma L)^2 + (\Sigma D)^2}$

Methods for Correcting Closing Error

There are four main methods to correct the closing error in a traverse:

  1. Bowditch Method

  2. Transit Method

  3. Graphical Method

  4. Axis Method

Comparison between Bowditch and Transit Methods

FeatureBowditch MethodTransit Method
PrecisionLinear and angular measurements are taken with equal precision.Angular measurement is more precise than linear measurement.
Latitude Correction ($C_L$)$C_L = - (\frac{\text{length of side}}{\text{perimeter}}) \times \Sigma L$$C_L = - (\frac{\text{latitude of line}}{\sum
Departure Correction ($C_D$)$C_D = - (\frac{\text{length of side}}{\text{perimeter}}) \times \Sigma D$$C_D = - (\frac{\text{departure of line}}{\sum




Read in details:-

🏗️ Surveying: Complete Study Guide & Index

📔 Part 1: Fundamentals of Surveying

📏 Part 2: Linear Measurement & Chain Survey

🧭 Part 3: Angular & Instrumental Survey

🏔️ Part 4: Levelling & Elevation

🛰️ Part 5: Modern Technologies

📝 Part 6: Practice & Quizzes (MCQs)


📚 Quick Revision Resources


Surveying IS Codes with Latest Revision Years

1. General Surveying & Instruments


2. Chain and Tape Surveying

  • IS 1492:1970 – Specification for Metric Surveying Chains.

  • IS 1269 (Part 1):1997 – Material and Construction of Steel Tapes.

  • IS 1269 (Part 2):1997 – Woven Metallic and Glass Fibre Tapes.

  • IS 1659:2006 – Specification for Invar Tapes for High Precision Measurement.


3. Theodolite and Tacheometry

  • IS 8002:1976 – Specification for Surveying Chain Vertical Vernier Theodolite.

  • IS 8330:1976 – Specification for Tilting Levels (Optical).

  • IS 8636:1977 – Specification for Tacheometers.


4. Leveling and Contouring

  • IS 9128:1992 – Specification for Tilting Levels.

  • IS 9573:1980 – Specification for Automatic Levels.

  • IS 1779:1961 – Specification for 4-metre Leveling Staff (Folding Type).


5. Modern Surveying (Total Station & GPS)

  • IS 16481:2016 – Guidelines for Accuracy and Testing of Total Stations.

  • IS 14855:2000 – Terminology and Concepts for GIS and Remote Sensing.


6. Measurement of Building Works

  • IS 1200 (Part 27):1992 – Method of Measurement of Building and Civil Engineering Works (Earthwork & Surveying).


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