Tuesday 18 December 2012

LEVELING


lLeveling is the general term applied to any of the various processes by which elevations of  points or differences in elevation are determined
lLeveling results are used
1- design highways, railroads, canals, sewers, water supply systems,
2- layout construction projects according to planned elevations
3- calculate volumes of earth or other materials
4- investigate drainage characteristics of an area
5- develop maps showing general ground configurations
6- study earth subsidence and crustal motion



LEVELING TERMS



lLevel line : A line in a level surface (a curved line)
lVertical line : A line that follows the direction of gravity as indicated by a plumb line
lHorizontal line : A line in horizontal plane. In plane surveying, a line perpendicular to the vertical
lLevel surface : A curved surface that every point is perpendicular to the local plumb line (the direction in which gravity acts) e.g. a still lake
lHorizontal plane : A plane perpendicular to the direction of gravity. In plane surveying, a plane perpendicular to the vertical line
lVertical datum : Any level surface to which elevations are referred. This is the surface that is arbitrarily assigned an elevation of zero
 
 
 
lElevation : The vertical distance above or below the datum.It is also known as reduced level (RL)
lBench Mark (BM) 
   A permanent object that has a known elevation.
lTemporary BenchMark  (TBM) 
    A moveable object that has a known elevation. 
lTurning Point (TP) 
    A fixed object used when determining the elevation of other points
lHeight of Instrument (HI) 
     The elevation of the line of sight established by the instrument.
lBacksight (BS) 
    The reading on the rod when held on a known or assumed elevation.
    Backsights are used to establish the height of instrument.
lForesight (FS) 
     The reading on the rod when held at a location where the elevation is to be determined.
     Foresights are used to establish the elevation at another location, often a turning point.
lIntermediate Foresight (IFS)
      The reading on the rod when held at a location where the elevation is to be determined but not used as a turning point.

DIFFERENTIAL LEVELING



From Fig. 4-5 ;
HI (Height of Instrument) = Elevation + BS
                    828. 42       = 820.00 + 8.42
Elevation = HI - FS
        827.22       = 828.42 - 1.20

EQUIPMENT FOR DIFFERENTIAL LEVELING


ERRORS IN LEVELLING
lIncorrect setting-up of instrument
lMovement of staff from position when changing level station.
lStaff not held vertically
lParallax: Instrument knocked or moved during backsight-foresight reading
lTripod or rod settles between measurements e.g Bubble off center
lCollimation error
 
CONTOURING
  lA contour is a line drawn on a plan joining all points of the same height above or below a datum.
lContours cannot  cross, split or join other contours, except in the case of an overhang. e.g. a cliff.
lThe height between successive contours is called the vertical interval or the contour interval.
  Its value depends on the variation in height of the area being contoured.
  The contour interval is kept constant for a plan or map.
lThe plan spacing between contour line indicates the steepness of slopes.
  Closely spaced lines indicates a steep gradient.
  Widely spaced lines indicate a flatter gradient.

PRODUCTION OF CONTOURS
lDirect contouring
This is the only method that produces true contours.
It involves finding points on the ground with the value of the required contour.
By establishing a series of such points the contour lines are effectively marked out on the ground.
It is then possible to plot them by conventional detail surveying.
 
 
lIndirect contouring
 
 
 
 

Monday 10 December 2012

INTRODUCTION TO ENGINEERING SURVEY


DEFINITION :
The art and science of making such
measurements as are necessary to
determine the relative position of points above, on, or beneath the surface of
the earth, or to establish such points in a specified position

Geodetic Surveying

  • a  process  of surveying in which the shape and size of the earth are considered.
  • suited for large areas and long lines and is used to find the precise   location   of   basic   points   needed for establishing control for other surveys.
  • the stations are normally long distances apart, and more precise instruments and surveying methods  are  required  for  this  type  of  
  •     surveying


Plane Surveying

oBranch of surveying in which the surface of the earth is considered a plane surface
oare the most commonly practised method of surveying and treat the earth as a flat or "plane" surface.
ofor small-scale surveys in limited areas, the curvature of the earth has no effect on the results, thus the computations and results can be referenced to a plane or flat surface.
used for the determination of legal boundaries, for engineering surveys for the construction of buildings and roads and for small-scale topographic surveys


KINDS OF SURVEYS

oTopographic surveys
Collect field data to prepare topographic maps
oHydrographic surveys
Map shorelines of water bodies, chart
bottom areas of streams, lakes, harbors,
etc., measure flow of rivers, assess other
issues related to navigation and water resources

oAerial surveys (photogrammetry)
Use photographs mounted in specially
designed planes
Construction surveys
Performed during building of structure or project to fix elevations, horizontal position, and dimensions
oControl surveys
 Provide basic horizontal and vertical position data for engineering mission

BASIC SURVEY
MEASUREMENTS: DEFINITIONS

oDirection of gravity used as
    reference direction
Vertical – means direction of gravity
Horizontal – means direction
                   perpendicular to gravity

DEFINITIONS

oLevel surface (geoid)
     Continuous surface that is at all points perpendicular to the direction of gravity. Can be thought of as the surface of large body of water at complete rest (unaffected by tides, etc.)
oElevation
    Vertical distance above or below a given reference level surface
oDifference in elevation
     Vertical distance between two level surfaces containing the two points


SOURCES OF ERRORS


oNatural errors : caused by variations in wind, temperature, humidity, atmospheric
    pressure, atmospheris refraction, gravity and magnetic decliniation
oInstrumental errors : imperfection in the construction or judgement of
    ınstruments and from the movement of individual parts
oPersonal errors : arise from limitations of sight and touch.

TYPES OF ERRORS


oSystematic error
-Occur according to a system which can be
expressed mathematically
-Magnitude and sign can be determined
-Follow definite pattern
-Can be caused by observer, instrument,
environment
oRandom error
-Error left after systematic error removed
-May tend to cancel themselves