Sz. Rózsa: Surveying I. – Lecture 1
Outline
Sz. Rózsa: Surveying I. – Lecture 1
Introduction
Lecturers
Lectures
Dr. Szabolcs Rózsa
Department of Geodesy and Surveying,
K. building groundfloor 16.
Practicals
Dr. Lóránt Földváry
Department of Geodesy and Surveying,
K. building groundfloor 16.
Mr. Albert Kiss
Department of Geodesy and Surveying
K. building groundfloor 16.
Sz. Rózsa: Surveying I. – Lecture 1
Introduction
Course details
• First part of a two-semester-course
• 4 hours/week (equally divided between lectures and practicals)
Communication:
• Activities involve lectures, practicals, tutorials and a field practice
• Lectures - provide the theoretical background of the topics
• Practicals - practical sessions, in which You’ll carry out measurements and process them.
• Tutorials - if there’s a need for additional guidance in the preparation for assessments. Please note that You have to arrange an appointment in due time.
• Field practice - a 9-day-long intensive course after the course Surveying II.
Sz. Rózsa: Surveying I. – Lecture 1
Introduction
Attendance:
• Please attend all scheduled lectures, seminars and practicals
• Please note: attendance falling below 70% may lead to failing the course irrespective of the academic performance.
Sz. Rózsa: Surveying I. – Lecture 1
Introduction
Classroom tests:
• Altogether 4 classroom assessments:
• Practicals 1-4 (10 points)
• Using a theodolite – must pass
• Practicals 10-11 (10 points)
• Theory (involving the topics of the lectures) – 80 points
Course Evaluation:
Excellent good satisfactory pass fail
(5)
(4)
(3)
(2)
(1)
87-99
75-87
62-74
50-61
0-49
You’re required to achieve a minimum of 50% in each classrom test to pass the course.
Sz. Rózsa: Surveying I. – Lecture 1
Introduction
Learning resources:
• Some of the lecture notes are available for download on the website of the department: http://www.geod.bme.hu/index_e.html
• However You shall write own notes during the lectures, too.
• You’ll be suplied with computational sheets, field notes etc. during the course.
• Textbook:
A. Bannister - S. Raymond - R. Baker : Surveying (Seventh
Edition, Prentice Hall, 1998)
Cca. 16000 HUF
Sz. Rózsa: Surveying I. – Lecture 1
Lecture notes can be downloaded from:
Website http://www.geod.bme.hu/index_e.html
Sz. Rózsa: Surveying I. – Lecture 1
Website
Sz. Rózsa: Surveying I. – Lecture 1
Introduction
Historical Surveying
Surveying - Science and Profession
Methods of height determination
Levelling
The surveyors’ level
Outline
Sz. Rózsa: Surveying I. – Lecture 1
Historical Surveying
What is Surveying?
The art of making measurements of the relative positions of natural and man-made features on the Earth’s surface, and the presentation of this information either graphically or numerically.
Since when?
The first surveying works date back to the antiquity, the
Greek provided the first account of surveying techniques.
Euclid founded the theoretical background for surveying by the development of his geometry.
Sz. Rózsa: Surveying I. – Lecture 1
Historical Surveying
Eratosthenes
(ca. 250 BC)
„Spherical Earth”
Sz. Rózsa: Surveying I. – Lecture 1
Historical Surveying
Sz. Rózsa: Surveying I. – Lecture 1
Introduction
Historical Surveying
Surveying - Science and Profession
Methods of height determination
Levelling
The surveyors’ level
Outline
Sz. Rózsa: Surveying I. – Lecture 1
Surveying - Science and Profession
Surveying vs. Geodesy
• in most languages there are no distinctions between the terms
• in English (according to Vanicek - Krakiwsky):
• Surveying: the practice of positioning
• Geodesy: the theoretical foundation of surveying
Geodesy is the scientific background of Surveying as a profession.
Sz. Rózsa: Surveying I. – Lecture 1
Surveying - Science and Profession
Surveying:
The art of making measurements of the relative positions of natural and man-made features on the Earth’s surface, and the presentation of this information either graphically or numerically.
Geodesy:
Geodesy is the discipline that deals with the measurements and representation of the Earth, including its gravity field, in a three-dimensional time varying space.
Geodesy focus on the Earth and neglect any man-made features on it (e.g. buildings, public utilities, etc.), while surveying use the results of geodesy for positioning and mapping of these features.
Sz. Rózsa: Surveying I. – Lecture 1
Basic principles of Surveying
Recall the definition of Surveying:
The art of making measurements of the relative
positions of natural and man-made features on the Earth’s surface, and the presentation of this information either graphically or numerically.
How to achieve this?
Nowadays 3D positioning can be achieved using satellite techniques, too.
Let’s determine the position (X
P
, Y
P
) of point P!
Absolute vs Relative positioning
X
P
Y d
BP P d
AP
Y
P
B
(X
B
,Y
B
)
Control points
(known coords; marked on the field)
A
(X
A
,Y
A
) l
AB
X
Sz. Rózsa: Surveying I. – Lecture 1
Y
Basic principles of Surveying
Let’s determine the position of a third, unknown point (C).
We have two unknowns: X
P
, Y
P
We need two measurements: b a
• two distances
• one distance and an angle
• two angles
P d
BP d
AP d
AP b
B
(X
B
,Y
B
)
A
(X
A
,Y
A
) a a
X
According to the space involved:
Classification of Surveying
• relatively small areas
• surface of earth can supposed to be flat
• measurements plotted represent a horizontal projection of the actual field measurements
Note: The two radii can supposed to be parallel, when the l(A,B) is small.
Sz. Rózsa: Surveying I. – Lecture 1
Classification of Surveying
Don’t forget! Size does matter!
• large areas
• surface of the Earth can not supposed to be flat
• the curvature of the Earth is taken into account
Mostly used for establishing control networks, determining the size and shape of the Earth and determining the gravity field of the Earth.
Sz. Rózsa: Surveying I. – Lecture 1
How to create a countrywide coordinate system?
In order to use the relative positioning, a proper number of control points are needed. These points:
• are coordinated points;
• are marked.
Sz. Rózsa: Surveying I. – Lecture 1
Control Networks
Why is it necessary to have a common countrywide coordinate system?
Many engineering tasks cover a large area (highways, bridges, tunnels, channels, land registry, etc.), where the common coordinate system (reference system) should be available.
The Control Network provide us with control points given in the same refence system (coordinate system).
Thus measuring the relative positions of unknown points using these control points, the coordinates of the new points can be computed in the same reference system.
Sz. Rózsa: Surveying I. – Lecture 1
The role of Surveying in Civil Engineering Practice
Surveyors are needed:
• to maintain the geometric order during the construction process
• to provide fundamental data for the design and planning process
• to provide quantity control during the construction process (for example: earthwork quantities)
• to monitor the structure after the construction
Wrong geometry – the structure is not functional!
outstanding structures can be created!
Sz. Rózsa: Surveying I. – Lecture 1
The role of Surveying in Civil Engineering Practice
Surveying activities during the construction process
Before Construction
Planning and data collection
Observations in the field
Processing the observations
(office)
Drawing maps, plans or providing numerical data
Presenting documentation to the client
Under construction
Setting out on each phase of construction
Field checks of construction
Providing data and services to the client
After construction
Final (as-built) plan or map on the construction
Presenting documentation to the client
Deformation
Monitoring/
Load Tests
Sz. Rózsa: Surveying I. – Lecture 1
Outline
Introduction
Historical Surveying
Surveying - Science and Profession
Methods of height determination
Levelling
The surveyors’ level
Sz. Rózsa: Surveying I. – Lecture 1
Methods of height determination
Question 1:
What does the height (elevation) of a point mean?
Question 2:
What does it mean, when point B is at a higher elevation than point A?
Answer 1:
The height of a point represents its energy level above a reference level.
Answer 2:
For example water flows from point B to point A.
Sz. Rózsa: Surveying I. – Lecture 1
Methods of height determination
Definition of height systems:
• The potential energy of a point should be represented by the height of a point. Hence water should flow from the higher elevation towards the lower elevation.
• Should have metric unit.
What should be the reference of height determination? What is the 0 level?
• Since the height systems should represent the potential energy level, we need a reference surface, which is an equipotential surface of Earth’s gravity field.
• The surface of calm water forms an equipotential surface
• Mean Sea Level – Kronstadt (Baltic Sea) is used in Hungary
(formerly Triest, Adriatic Sea).
Sz. Rózsa: Surveying I. – Lecture 1
Methods of height determination
Equipotential surfaces
A
H
A
H
B
B
MSL equipotential surface g
Gravity vector is always perpendicular to the equipotential surface.
Equipotential surface
Gravity vector
(=)
(=) horizontal surface vertical direction
Sz. Rózsa: Surveying I. – Lecture 1
Methods of height determination
1D position determination - determining the height
We can not determine absolute heights above the reference level
Relative height determination - determining the height differences
Levelling benchmarks are needed - control points for which the elevation is known.
B
H
BA
H
B
H
A
A
H
B
H
A
Reference level
Sz. Rózsa: Surveying I. – Lecture 1
Methods of height determination
How can we determine the height difference?
Two solutions:
• setting a horizontal plane, and measuring the offset from this plane
• measuring the slope and slope distance between the points
Levelling
Trigonometrical height determination
B l
AB
H
BA
H
B
H
A
A a
H
B
H
A
Reference level
Sz. Rózsa: Surveying I. – Lecture 1
Outline
Introduction
Historical Surveying
Surveying - Science and Profession
Methods of height determination
Levelling
The surveyors’ level
Sz. Rózsa: Surveying I. – Lecture 1
The principle of levelling
Line of sight
(l
A
)
H
AB
A d
A l
A
H
AB
=l
A
-l
B
=(l
A
)d
A
-(l
B
)+ d
B
When d
A
= d
B
(spherical approximation, equal distance to A and B)
H
AB
=(l
A
)-(l
B
) d
B l
B
(l
B
)
B
Levelling
Over short distances the horizontal line and level line coincide.
For a distance of 100m the effect of the curvature is less than 1 mm.
The levelling device (called level) must be set up so, that the line of sight is perpendicular to the gravity vector (plumb line). -> the line of sight is horizontal.
Horizontal line of sight
Graduated staff Level
Graduated staff
Difference in height
Sz. Rózsa: Surveying I. – Lecture 1
Levelling
Sz. Rózsa: Surveying I. – Lecture 1
Introduction
Historical Surveying
Surveying - Science and Profession
Methods of height determination
Levelling
The surveyors’ level
Outline
Sz. Rózsa: Surveying I. – Lecture 1
The Surveyor’s level
Tilting level
Diaphragm
Bubble tube
Tilting screw
Circular bubble Tilting axis
Levelling head
Clamping screw - to fix the telescope in one vertical plane
Tangent screw (slow motion screw) - to finely rotate the telescope along a vertical axis
Sz. Rózsa: Surveying I. – Lecture 1
Elements of Surveyor’s level
How to set the line of sight to be exactly horizontal?
More general: how to set anything to be exactly horizontal?
The bubble tube
Sz. Rózsa: Surveying I. – Lecture 1
The bubble tube
The radius determines the sensitivity of the bubble tube: a
R
1 a
R
2
R greater than R
1 2
Sensitivity: how much the bubble moves due to a given amount of inclination. The more the bubble moves, the more sensitive the bubble tube is.
Sz. Rózsa: Surveying I. – Lecture 1
The bubble tube
The determination of sensitivity: a
R
1 a
R
1
L l
1 a
L l
2 l
2
l
1
L
a
radians
a
a
radians
206264 .
8
Sz. Rózsa: Surveying I. – Lecture 1