Severity: Warning
Message: file_get_contents(https://...@pubfacts.com&api_key=b8daa3ad693db53b1410957c26c9a51b4908&a=1): Failed to open stream: HTTP request failed! HTTP/1.1 429 Too Many Requests
Filename: helpers/my_audit_helper.php
Line Number: 176
Backtrace:
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 176
Function: file_get_contents
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 250
Function: simplexml_load_file_from_url
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 3122
Function: getPubMedXML
File: /var/www/html/application/controllers/Detail.php
Line: 575
Function: pubMedSearch_Global
File: /var/www/html/application/controllers/Detail.php
Line: 489
Function: pubMedGetRelatedKeyword
File: /var/www/html/index.php
Line: 316
Function: require_once
A comprehensive chemical characterization (water-soluble ions, organic and elemental carbon, water- and methanol-soluble organic carbon, levoglucosan, and major and trace metals) of PM samples collected in a rural area located in the southeast of the Iberian Peninsula was performed. Additionally, the oxidative potential of the samples, used as an indicator of aerosol toxicity, was determined by the ascorbic acid (OP) and dithiothreitol (OP) assays. The average concentration of PM during the study period, spanning from late winter to early spring, was 20.2 ± 10.8 μg m. Nitrate, carbonate and calcium (accounting for 20% of the average PM mass concentration) and organic matter (with a contribution of 28%) were the main chemical components of PM. Average concentrations of traffic tracers such as elemental carbon, copper and zinc (0.31 μg m, 3 ng m, and 9 ng m, respectively) were low compared with those obtained at an urban site in the same region, due to the almost total absence of traffic in the surrounding of the sampling site. Regarding levoglucosan and K, which can be considered as tracers of biomass burning, their concentrations (0.12 μg m and 55 ng m, respectively) were in the lower range of values reported for other rural areas in Europe, suggesting a moderate contribution form this source to PM levels. The results of the Pearson's correlation analysis showed that volume-normalised OP and OP levels (average values of 0.11 and 0.32 nmol min m, respectively) were sensitive to different PM chemical components. Whereas OP was not strongly correlated with any of the species measured, good correlation coefficients of OP with water-soluble organic carbon (r = 0.81) and K (r = 0.73) were obtained, which points to biomass burning as an important driver of the DTT activity.
Download full-text PDF |
Source |
---|---|
http://dx.doi.org/10.1016/j.chemosphere.2024.142880 | DOI Listing |
Enter search terms and have AI summaries delivered each week - change queries or unsubscribe any time!