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Message: file_get_contents(https://...@gmail.com&api_key=61f08fa0b96a73de8c900d749fcb997acc09&a=1): Failed to open stream: HTTP request failed! HTTP/1.1 429 Too Many Requests
Filename: helpers/my_audit_helper.php
Line Number: 197
Backtrace:
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 197
Function: file_get_contents
File: /var/www/html/application/helpers/my_audit_helper.php
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Function: simplexml_load_file_from_url
File: /var/www/html/application/helpers/my_audit_helper.php
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Function: getPubMedXML
File: /var/www/html/application/controllers/Detail.php
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Function: pubMedSearch_Global
File: /var/www/html/application/controllers/Detail.php
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Function: pubMedGetRelatedKeyword
File: /var/www/html/index.php
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Function: require_once
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Rationale: Cavity ring-down spectroscopy (CRDS) is becoming increasingly popular for δ C-CO analysis of air. However, little is known about the effect of high C abundances on the performance of CRDS. Overlap between CO and CO spectral lines may adversely affect isotopic-CO CRDS measurements of C-enriched samples. Resolving this issue is important so that CRDS analysers can be used in CO flux studies involving C-labelled tracers.
Methods: We tested a Picarro G2131-i CRDS isotopic-CO gas analyser with specialty gravimetric standards of widely varying C abundance (from natural to 20.1 atom%) and CO mole fraction (xCO : <0.1 to 2116 ppm) in synthetic air. The presence of spectroscopic interference between CO and CO bands was assessed by analysing errors in measurements of the standards. A multi-component calibration strategy was adopted, incorporating isotope ratio and mole fraction data to ensure accuracy and consistency in corrected values of δ C-CO , x CO , and x CO .
Results: CRDS measurements of x CO were found to be accurate throughout the tested range (<0.005 to 100 ppm). On the other hand, spectral cross-talk in x CO measurements of standards containing elevated levels of CO led to inaccuracy in x CO , total-xCO (x CO + x CO ), and δ C-CO data. An empirical relationship for x CO measurements that incorporated the C/ C isotope ratio (i.e. CO / CO , RCO2) as a secondary (non-linear) variable was found to compensate for the perturbations, and enabled accurate instrument calibration for all CO compositions covered by our standard gases.
Conclusions: C-enrichement in CO leads to minor errors in CRDS measurements of x CO . We propose an empirical correction for measurements of C-enriched CO in air by CRDS instruments such as the Picarro G2131-i.
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http://dx.doi.org/10.1002/rcm.7969 | DOI Listing |