Correction: Dissolved organic matter in Lake Superior: Insights into the effects of extraction methods on chemical composition (Environmental Science: Processes and Impacts (2015) 17 (1829-1840) DOI: 10.1039/C5EM00199D)

Hongyu Li; Elizabeth C. Minor

doi:10.1039/c9em90031d

Correction: Dissolved organic matter in Lake Superior: Insights into the effects of extraction methods on chemical composition (Environmental Science: Processes and Impacts (2015) 17 (1829-1840) DOI: 10.1039/C5EM00199D)

Hongyu Li, Elizabeth C. Minor

Chemistry & Biochemistry

Research output: Contribution to journal › Comment/debate › peer-review

1 Scopus citations

Abstract

The authors were recently informed of new values for the process blank for UV oxidation of dissolved organic carbon and subsequent analysis at the National Ocean Sciences Accelerator Mass Spectrometry (NOSAMS) Facility. Values from this approach should be corrected for a process blank of 22 ± 6 μg of carbon; this blank has a fraction modern of 0.3 ± 0.2. Applying this blank leads to new 'init' Δ¹⁴C % values in Table 1. The corrected version of this table follows: (Table Presented).

Original language	English (US)
Pages (from-to)	1215
Number of pages	1
Journal	Environmental Science: Processes and Impacts
Volume	21
Issue number	7
DOIs	https://doi.org/10.1039/c9em90031d
State	Published - Jul 2019

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© 2019 The Royal Society of Chemistry.

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Correction: Dissolved organic matter in Lake Superior: Insights into the effects of extraction methods on chemical composition (Environmental Science: Processes and Impacts (2015) 17 (1829-1840) DOI: 10.1039/C5EM00199D). / Li, Hongyu; Minor, Elizabeth C.
In: Environmental Science: Processes and Impacts, Vol. 21, No. 7, 07.2019, p. 1215.

Research output: Contribution to journal › Comment/debate › peer-review

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abstract = "The authors were recently informed of new values for the process blank for UV oxidation of dissolved organic carbon and subsequent analysis at the National Ocean Sciences Accelerator Mass Spectrometry (NOSAMS) Facility. Values from this approach should be corrected for a process blank of 22 ± 6 μg of carbon; this blank has a fraction modern of 0.3 ± 0.2. Applying this blank leads to new 'init' Δ14C % values in Table 1. The corrected version of this table follows: (Table Presented).",

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N2 - The authors were recently informed of new values for the process blank for UV oxidation of dissolved organic carbon and subsequent analysis at the National Ocean Sciences Accelerator Mass Spectrometry (NOSAMS) Facility. Values from this approach should be corrected for a process blank of 22 ± 6 μg of carbon; this blank has a fraction modern of 0.3 ± 0.2. Applying this blank leads to new 'init' Δ14C % values in Table 1. The corrected version of this table follows: (Table Presented).

AB - The authors were recently informed of new values for the process blank for UV oxidation of dissolved organic carbon and subsequent analysis at the National Ocean Sciences Accelerator Mass Spectrometry (NOSAMS) Facility. Values from this approach should be corrected for a process blank of 22 ± 6 μg of carbon; this blank has a fraction modern of 0.3 ± 0.2. Applying this blank leads to new 'init' Δ14C % values in Table 1. The corrected version of this table follows: (Table Presented).

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Correction: Dissolved organic matter in Lake Superior: Insights into the effects of extraction methods on chemical composition (Environmental Science: Processes and Impacts (2015) 17 (1829-1840) DOI: 10.1039/C5EM00199D)

Abstract

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