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GPS Device in the Geological Field Mapping
Navigation and positioning are crucial to most human activities and yet the process has always been quite
cumbersome. Trying to figure out where he is and where he is going has probably been one of man's oldest
pastimes. Over the years all kindsof technologieshave tried to simplify the task butevery one has hadsome
disadvantage.
Finally, the U.S. Department of Defense decided that the military had to have a super precise form of
worldwide positioning. And fortunately, they had the kind of money ($12 billion!) it took to build something
good.
The result is the GPSor Global PositioningSystem, a systemthat changednavigationforever. GPS is the only
system today that can show you your exact position on the Earth anytime, in any weather, anywhere on or
above the earth’s surface. It is a worldwide radio-navigation system formed from a constellation of 24
satellites and their ground stations.
GPSsatellites orbitat 11,000nauticalmiles(1 nauticalmile=1852 m)abovetheEarth. Groundstationslocated
worldwide continuously monitorthem. The satellites transmitsignals that can be detected by anyonewith a
GPSreceiver. Usingthereceiver, youcan determineyourpositionaccurate toa matterof meters. Infact, with
advanced forms of GPS you can make measurements to better than a centimeter. In a sense it's like giving
every square meter on the planet a unique address.
Presently, GPS is finding its way into cars, boats, planes, construction equipment, movie making gear, farm
machinery, and even laptop computers and cell phones. Soon GPS will become almost as basic as the
telephone. Indeed, it just may become a universal utility.
Components of the GPS:
GPS has 3 parts – the space segment, the control segment, and the user segment.
Space Segment (GPS Satellites)
The complete GPS space system includes 24 satellites, 10,900 nauticalmiles (20187 km)above the Earth,
which take 12 hours each to go around the Earth once (one orbit). They are positioned so that we can
receive signals from six of them nearly 100 percent of the time at any point on Earth. GPS satellites are
equipped with very precise clocks that keep accurate time to within three nanoseconds. This precision
timingis importantbecausethereceiver mustdetermineexactly howlong it takesfor signalstotravel from
each GPS satellite. The receiver uses this information to calculate its position.
The first GPS satellite was launched in 1978. The first 10 satellites were developmental satellites, called
Block I were launchedby 1985. From1989to1993,23 productionsatellites, called Block II, were launched.
The launch of the 24th
satellite in 1994 completed the system.
 Name: NAVSTAR
 Manufacturer: Rockwell International
 Altitude: 10,900 nautical miles
 Weight: 1900 lbs (in orbit)
 Size: 17 ft with solar panels extended
 Orbital Period: 12 hours
 Orbital Plane: 55 degrees to equatorial plane
 Planned Lifespan: 7.5 years
 Current constellation: 24 Block II production satellites
 Future satellites: 21 Block II satellites developed by Martin Marietta
Control Segment (Ground Stations)
The GPS control, or ground segment consists of the following unmanned monitoring stations located
around the world which track and monitor the GPS satellites:
 Hawaii and Kwajalein in the Pacific Ocean
 Diego Garcia in the Indian Ocean
 Ascension Island in the Atlantic Ocean; and
 Colorado Springs, Colorado
Apart from these, a master ground station at Schriever (Falcon) Air Force Base in Colorado Springs,
Colorado; and four large ground antenna stations broadcast control signals to the satellites.
These stations monitor the GPS satellites, checking both their operational health and their exact position
in space. The mastergroundstation receivesandanalysessatellite signalsandtransmitscorrectionsfor the
satellite's ephemeris constants andclock offsets back to the satellites themselves. The satellites can then
incorporate these updates in the signals they send to GPS receivers.
User Segment (GPS Receivers)
GPS receivers vary greatly in size and complexity. They can be handcarried or installed on aircraft, ships,
tanks, submarines, cars, and trucks. These receivers detect, decode, and process GPS satellite signals.
Although more than 100 different receiver models are presently in use, their basic design is rather
simple. The typical receiver is composed of an antenna and preamplifier, radio signal microprocessor,
control and display device, data recording unit, and power supply.
The GPS receiver decodes the timing signals from the 'visible' satellites (four or more) and, having
calculated their distances, computes its own latitude, longitude, elevation, and time. This is a continuous
process and generally the position is updatedon a second-by-secondbasis, outputtothe receiver display
device and, if the receiver display device providesdatacapture capabilities, stored by the receiver-logging
unit.
The typicalhand-heldreceiver is aboutthesize of a cellular telephone, the newer modelsare even smaller.
The hand-heldunitsdistributedto U.S. armed forces personnel during the Persian Gulf War weighed only
28 ounces.
How does GPS Work
GPS works in 5 logical steps:
1. The basis of GPS is "triangulation" from satellites.
2. To "triangulate," a GPS receiver measures distance using the travel time of radio signals.
3. To measure travel time, GPS needs very accurate timing, which it achieves (with some tricks) with
its own and satellite clocks.
4. Along with distance, you need to know exactly where the satellites are in space. High orbits and
careful monitoring are the secret.
5. Finally, youmustcorrectforany delaysthesignal experiences asit travelsthroughtheatmosphere.
Accuracy
Since the implementationofGPSin 1990, anintentionalrandomerrorwasaddedto the GPSsignalstogive
a positionalinaccuracy of about100 m, sothathostile forces couldnot useit to guideballistic missileswith
any degree of accuracy. This error was not truly random, and the US Army receivers had codes which
allowed them to compensate for this error. From 2nd
May 2000 this selective availability was withdrawn,
and the positional uncertainty has been reduced to 5 m. This means that a goodGPS receiver capable of
processing6 or more signalssimultaneously, andusedin ideal conditionscan give a horizontalaccuracy of
5 m and a vertical accuracy of ±10 m. The accuracy of GPS positioning can be enhanced by using using
Differential GPS of implementation of the Wide Area Augmentation Service as explained hereunder.
Differential GPS (DGPS):
In this method one GPS receiver is fixed on the ground at a known location (acting as a static reference
point), the othersare the roving(mobile) receivers performing the usual survey work. The roving GPS can
record all its measured positionsandthe exact time it made each measurementandlater this datacan be
merged with the corrections recorded by the stationary reference GPS receiver. With such a setup, the
differential GPS can eliminate virtually all errors in the system, whether they are from the receiver clocks,
the satellite clocks, the satellite positions or the ionosphere and atmospheric delays.
Another way of doing DGPS is for the correction factors to be transmitted from the static reference GPS
receiver to all the roving receivers by a radio link in real time. Differential GPS gives sub centimeter
accuracy.
Wide Area Augmentation Service (WAAS):
WAAS corrects for GPS signal errors caused by ionosphericdisturbances, timing, and satellite orbit errors,
and it provides vital integrity information regarding the health of each GPS satellite. WAAS consists of
approximately 25 groundreference stationspositionedacrossthe UnitedStatesthatmonitorGPS satellite
data. Two master stations, located on either coast, collect data from the reference stations and create a
GPS correction message. This correction accounts for GPS satellite orbit and clock drift plus signal delays
caused by the atmosphereand ionosphere. The corrected differential message is then broadcast through
one of two geostationary satellites to all hand held receivers in the operational area viz., North America
and the Hawaiian Island. The information is compatible with the basic GPS signal structure, which means
any WAAS-enabled GPS receiver can read the signal and give an enhanced accuracy.
COMPILING GEOLOGICAL MAPS
With the aid of GIS (Geographic Information Systems), maps of good quality and great accuracy are
produced.Evidentlyitisimportanttoconsult withthe GIS departmentbefore fieldworktocalibrate the
GPS in a format/unit that can easily be used with their software. Nonetheless, it is important for a
geologist to draw a simple sketch map during field work for comparison purposes.
INTERPRETING GEOLOGICAL MAPS
Once a map is complete, the most important task ahead is interpreting it correctly. A map is basicallya
visual summaryof anentire reportandthe two shouldcomplementeachother.Whenthe interpretation
processisat hand,it iscrucial to have groupdiscussionswithall those involvedinthe actual fieldwork.It
is alsodeemedimportanttohave discussionswiththose whoare experiencedinfieldof geologyaswell
as other related scientific fields.
CONCLUSIONS
The following can be said to summarize geological field mapping:
• For geological fieldmapping tobe carriedoutefficiently,itisessential thatproperplanningisexecuted.
• Once in the field, it is also important to be as detailed as possible in all descriptions, to be keen and
observant.
• Measurements must be performed meticulously and, if necessary, more than once for confirmation
purposes.
• Team work must be adhered to, throughout the entire process.

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Gps device in the geological field mapping

  • 1. GPS Device in the Geological Field Mapping Navigation and positioning are crucial to most human activities and yet the process has always been quite cumbersome. Trying to figure out where he is and where he is going has probably been one of man's oldest pastimes. Over the years all kindsof technologieshave tried to simplify the task butevery one has hadsome disadvantage. Finally, the U.S. Department of Defense decided that the military had to have a super precise form of worldwide positioning. And fortunately, they had the kind of money ($12 billion!) it took to build something good. The result is the GPSor Global PositioningSystem, a systemthat changednavigationforever. GPS is the only system today that can show you your exact position on the Earth anytime, in any weather, anywhere on or above the earth’s surface. It is a worldwide radio-navigation system formed from a constellation of 24 satellites and their ground stations. GPSsatellites orbitat 11,000nauticalmiles(1 nauticalmile=1852 m)abovetheEarth. Groundstationslocated worldwide continuously monitorthem. The satellites transmitsignals that can be detected by anyonewith a GPSreceiver. Usingthereceiver, youcan determineyourpositionaccurate toa matterof meters. Infact, with advanced forms of GPS you can make measurements to better than a centimeter. In a sense it's like giving every square meter on the planet a unique address. Presently, GPS is finding its way into cars, boats, planes, construction equipment, movie making gear, farm machinery, and even laptop computers and cell phones. Soon GPS will become almost as basic as the telephone. Indeed, it just may become a universal utility. Components of the GPS: GPS has 3 parts – the space segment, the control segment, and the user segment. Space Segment (GPS Satellites) The complete GPS space system includes 24 satellites, 10,900 nauticalmiles (20187 km)above the Earth, which take 12 hours each to go around the Earth once (one orbit). They are positioned so that we can receive signals from six of them nearly 100 percent of the time at any point on Earth. GPS satellites are equipped with very precise clocks that keep accurate time to within three nanoseconds. This precision timingis importantbecausethereceiver mustdetermineexactly howlong it takesfor signalstotravel from each GPS satellite. The receiver uses this information to calculate its position. The first GPS satellite was launched in 1978. The first 10 satellites were developmental satellites, called Block I were launchedby 1985. From1989to1993,23 productionsatellites, called Block II, were launched. The launch of the 24th satellite in 1994 completed the system.  Name: NAVSTAR
  • 2.  Manufacturer: Rockwell International  Altitude: 10,900 nautical miles  Weight: 1900 lbs (in orbit)  Size: 17 ft with solar panels extended  Orbital Period: 12 hours  Orbital Plane: 55 degrees to equatorial plane  Planned Lifespan: 7.5 years  Current constellation: 24 Block II production satellites  Future satellites: 21 Block II satellites developed by Martin Marietta Control Segment (Ground Stations) The GPS control, or ground segment consists of the following unmanned monitoring stations located around the world which track and monitor the GPS satellites:  Hawaii and Kwajalein in the Pacific Ocean  Diego Garcia in the Indian Ocean  Ascension Island in the Atlantic Ocean; and  Colorado Springs, Colorado Apart from these, a master ground station at Schriever (Falcon) Air Force Base in Colorado Springs, Colorado; and four large ground antenna stations broadcast control signals to the satellites. These stations monitor the GPS satellites, checking both their operational health and their exact position in space. The mastergroundstation receivesandanalysessatellite signalsandtransmitscorrectionsfor the satellite's ephemeris constants andclock offsets back to the satellites themselves. The satellites can then incorporate these updates in the signals they send to GPS receivers. User Segment (GPS Receivers) GPS receivers vary greatly in size and complexity. They can be handcarried or installed on aircraft, ships, tanks, submarines, cars, and trucks. These receivers detect, decode, and process GPS satellite signals. Although more than 100 different receiver models are presently in use, their basic design is rather simple. The typical receiver is composed of an antenna and preamplifier, radio signal microprocessor, control and display device, data recording unit, and power supply. The GPS receiver decodes the timing signals from the 'visible' satellites (four or more) and, having calculated their distances, computes its own latitude, longitude, elevation, and time. This is a continuous process and generally the position is updatedon a second-by-secondbasis, outputtothe receiver display device and, if the receiver display device providesdatacapture capabilities, stored by the receiver-logging unit. The typicalhand-heldreceiver is aboutthesize of a cellular telephone, the newer modelsare even smaller. The hand-heldunitsdistributedto U.S. armed forces personnel during the Persian Gulf War weighed only 28 ounces.
  • 3. How does GPS Work GPS works in 5 logical steps: 1. The basis of GPS is "triangulation" from satellites. 2. To "triangulate," a GPS receiver measures distance using the travel time of radio signals. 3. To measure travel time, GPS needs very accurate timing, which it achieves (with some tricks) with its own and satellite clocks. 4. Along with distance, you need to know exactly where the satellites are in space. High orbits and careful monitoring are the secret. 5. Finally, youmustcorrectforany delaysthesignal experiences asit travelsthroughtheatmosphere. Accuracy Since the implementationofGPSin 1990, anintentionalrandomerrorwasaddedto the GPSsignalstogive a positionalinaccuracy of about100 m, sothathostile forces couldnot useit to guideballistic missileswith any degree of accuracy. This error was not truly random, and the US Army receivers had codes which allowed them to compensate for this error. From 2nd May 2000 this selective availability was withdrawn, and the positional uncertainty has been reduced to 5 m. This means that a goodGPS receiver capable of processing6 or more signalssimultaneously, andusedin ideal conditionscan give a horizontalaccuracy of 5 m and a vertical accuracy of ±10 m. The accuracy of GPS positioning can be enhanced by using using Differential GPS of implementation of the Wide Area Augmentation Service as explained hereunder. Differential GPS (DGPS): In this method one GPS receiver is fixed on the ground at a known location (acting as a static reference point), the othersare the roving(mobile) receivers performing the usual survey work. The roving GPS can record all its measured positionsandthe exact time it made each measurementandlater this datacan be merged with the corrections recorded by the stationary reference GPS receiver. With such a setup, the differential GPS can eliminate virtually all errors in the system, whether they are from the receiver clocks, the satellite clocks, the satellite positions or the ionosphere and atmospheric delays. Another way of doing DGPS is for the correction factors to be transmitted from the static reference GPS receiver to all the roving receivers by a radio link in real time. Differential GPS gives sub centimeter accuracy. Wide Area Augmentation Service (WAAS): WAAS corrects for GPS signal errors caused by ionosphericdisturbances, timing, and satellite orbit errors, and it provides vital integrity information regarding the health of each GPS satellite. WAAS consists of approximately 25 groundreference stationspositionedacrossthe UnitedStatesthatmonitorGPS satellite data. Two master stations, located on either coast, collect data from the reference stations and create a GPS correction message. This correction accounts for GPS satellite orbit and clock drift plus signal delays caused by the atmosphereand ionosphere. The corrected differential message is then broadcast through one of two geostationary satellites to all hand held receivers in the operational area viz., North America
  • 4. and the Hawaiian Island. The information is compatible with the basic GPS signal structure, which means any WAAS-enabled GPS receiver can read the signal and give an enhanced accuracy. COMPILING GEOLOGICAL MAPS With the aid of GIS (Geographic Information Systems), maps of good quality and great accuracy are produced.Evidentlyitisimportanttoconsult withthe GIS departmentbefore fieldworktocalibrate the GPS in a format/unit that can easily be used with their software. Nonetheless, it is important for a geologist to draw a simple sketch map during field work for comparison purposes. INTERPRETING GEOLOGICAL MAPS Once a map is complete, the most important task ahead is interpreting it correctly. A map is basicallya visual summaryof anentire reportandthe two shouldcomplementeachother.Whenthe interpretation processisat hand,it iscrucial to have groupdiscussionswithall those involvedinthe actual fieldwork.It is alsodeemedimportanttohave discussionswiththose whoare experiencedinfieldof geologyaswell as other related scientific fields. CONCLUSIONS The following can be said to summarize geological field mapping: • For geological fieldmapping tobe carriedoutefficiently,itisessential thatproperplanningisexecuted. • Once in the field, it is also important to be as detailed as possible in all descriptions, to be keen and observant. • Measurements must be performed meticulously and, if necessary, more than once for confirmation purposes. • Team work must be adhered to, throughout the entire process.