Introduction:
For this
experiment, a survey was conducted using the concept behind distance and azimuth.
Although this is a basic survey technique, it works in many different
situations. In this instance, we used sampling techniques to map point features
on the University of Wisconsin Eau Claire campus, specifically trees around Phillips
Hall Science Building. With today’s technology and the ability to acquire very precise
location data, it is important to understand the basic techniques and tools
used in field methods in order to function effectively and independent from
advanced technology, such as drones.
For this exercise, a TruPulse laser distance finder was used to record the distance and azimuth readings for the data points we chose. We also used a compass that allowed us to record separate distance and azimuth readings. Although as a class we did not use the compass data, it is important to make comparisons of different technologies. We also used a distance finder or tape measure to measure the distance from our first station to the point feature (trees).
For this exercise, a TruPulse laser distance finder was used to record the distance and azimuth readings for the data points we chose. We also used a compass that allowed us to record separate distance and azimuth readings. Although as a class we did not use the compass data, it is important to make comparisons of different technologies. We also used a distance finder or tape measure to measure the distance from our first station to the point feature (trees).
The TruPulse 360B Laser Rangefinder that
was used to record our final distance and the azimuth readings for our chosen
features (above-right). We also used a compass to compare azimuth readings between the two technologies.
My team
and I chose to survey trees within the courtyard and surrounding Phillip Science
Hall of UW-Eau Claire. Before conducting our survey, we were advised to take
not of the concept of magnetic declination and how it differs from magnetic
north. This refers to the magnetic pull on the compass due to earth’s magnetic
field at our location on the planet, rather than what is known as “true North.”
Below is a link to a video that was shown to the class for more information on
magnetic declination:
Luckily, Eau Claire, WI has a small declination value of 2, so we know it
would not impact our data collection. We then calculated the point features
without using any coordinates, however, we will assign our starting point with
GPS coordinates so that the data is usable in GIS systems.
Methods:
October
2, 2019
Cloudy,
Rainy, ~ 15 degrees Celsius
Our first
survey area was located within the courtyard of Philips hall, facing south
towards Putnam Park trail. Once we decided our station area, we took the
coordinates of that area, and began surveying from that point. We set up the
TruPulse and began by taking readings of trees from right to left. Due to the bad
weather that had rolled in that afternoon, our only option was to take points
from the exit doors on the northeast side of the courtyard and take our survey
from there. There were also heavy winds that would cause the TruPulse to shake,
not allowing us to receive valid distance or azimuth readings.
This made
collecting data extremely difficult, and due to time constrains, we couldn’t
collect as many points as we could have. During this survey, we gathered three
features. Our second survey station area was located south of the Phillips
building near the bike racks and west of the large sculpture. After collecting
data from this area, we had gathered a total of six point features.
After
returning to the classroom, we transferred our data into an excel spreadsheet document
for later use in ArcMap. Our data is shown below:
Table showing our data collected. For each
point, we collected the azimuth, the distance from the station, attribute information
of the trees, and the elevation of the tree.
Next, the
excel file was imported into the geodatabase where we then used the “Bearing
Distance Line tool to convert its information into a line feature class.
We then converted our data to the points, using the "Feature Vertices to Points" tool.
The results of the tool and
our data is shown below.
Discussion:
When
looking at our map and data, it doesn’t seem like there is any input error, but
that the readings from the TruPulse were off, causing our data to shift. It
seems that even the smallest amount of error when calculating the azimuth will
impact the resulting points. It is also possible that errors occurred when measuring
subsequent readings of distance (meters) of the prominent features, especially considering
the weather conditions throughout the course of this survey.
In the
map above, the laser’s accuracy seems to decline as the object is farther and
farther away from their actual locations. This error comes from
the TruPulse’s decreasing accuracy with distance, as well as the users’ error
as distance increases.
Conclusion:
Although we did use an expensive tool in gathering our
data during this survey, using higher quality equipment doesn’t always mean
that there will be no error. Utilizing simpler equipment may have been easier.
Overall, the purpose of this experiment was to familiarize ourselves with using
tools in calculating spatial relations without a coordinate system. These
methods are useful in areas where there is no access to advanced global positioning
and in situations of technological failure.





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