Eleventh International Conference on Environmental Management, Engineering, Planning and Economics (CEMEPE 2024) and SECOTOX Conference, Levkas, Greece, 16 - 20 June 2024, pp.1
In the present study, daily PM10
samples were collected in Artvin city which is located on the eastern Black Sea
coast of Turkey. A high-volume sampler with a mass flow controller and quartz
filters were used for sampling. During April 2023 and September 2023, 77 PM10
samples were collected. The average concentration of PM10 was 54.5 ±
32.0 µg/m3. Among them, 35 days exceeded the
daily PM10 limit value of 50 µg/m3. The number of
days exceeding the daily limit value in April, May, June, July, August, and
September were 8, 11, 7, 6, and 3, respectively. Five days back, hourly
backward trajectories arriving at three different heights (i.e., 500, 1500, and
3000 m) were simulated using the GDAS1 meteorological archive and vertical
velocity by the TrajStat Trajectory model in Meteoinfo software. Cluster
analysis was applied to determine the general transport pattern in the region.
Average PM10 concentration was calculated for each cluster center
and episode days in each cluster center were identified. Potential source
contribution function (PSCF) was conducted to determine the potential source
regions affecting the eastern Black Sea of Turkey during summer months. The
following were revealed by the findings: (1) Air pollution in the Eastern Black
Sea region was severe for summer season of 2023, and the seasonal average PM10
concentration was higher than Turkey's air quality annual standard (40 µg/m3).
(2) Five-year air masses from 2019 to 2023 shared similar trajectory pathways
for 500 and 1500 m trajectories (i.e. slow-air movements from north and south
directions), but different trajectory pathways were determined for 3000 m (i.e.
fast-moving air movements from south-westerly direction). (3) Potential source
contribution function (PSCF) values were in line with cluster analysis (CA)
results and indicated north and south regions for 500 and 1500 m; and Sahara
and the Mediterranean Sea as the major source regions for 3000 m.