14
views
0
recommends
+1 Recommend
0 collections
    0
    shares
      • Record: found
      • Abstract: found
      • Article: found
      Is Open Access

      Corrigendum: Possible generation of heat from nuclear fusion in Earth’s inner core

      correction
      Scientific Reports
      Nature Publishing Group

      Read this article at

      Bookmark
          There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

          Abstract

          Scientific Reports 6: Article number: 3774010.1038/srep37740; published online 11 23 2016; updated on 05 02 2017 The original version of this Article contained errors resulting from the incorrect calculation of formation energy in Equation 6. In the Abstract, “2D + 2D + 2D → 21H + 4He + 2  + 20. 85 MeV. The possible heat generation rate can generation rate can be calculated as 8.12 × 1012 J/m3”. Now reads: “2D + 2D + 2D → 21H + 4He + e- +   + 21. 63 MeV. The possible heat generation rate can generation rate can be calculated as 1.27 × 1015 J/m3”. In addition, there was an error in the ‘Introduction section’, where “Increase in paraeomagnetic magnitude between 2.7–2.1 billion years” Now reads: “Increase in palaeomagnetic magnitude between 2.7–2.1 billion years” There were also errors in Equations 6, 7, 9, 10 and 11, which now read: There were also errors in Equations 23, 24, 25 and 26 which now read: Under the sub-heading “Existence of a D-rich inner core”, “On the other hand, because the incorporated gross weight of D from the creation of Earth’s core to present time is estimated as 6.67 × 1021 kg (=100 Mkm3 × 2 Mg/m3 × 4/20 × 1/0.006), the volume of Fe-D crystals up through the present is 4.99 × 1017 m3 (6.67 × 1021/13.36 [Mg/m3]), resulting in an unreacted (Fe-D) crystal volume of 4.37 × 1017 m3 (=4.99 × 1017 − 6.23 × 1016)”. Now reads: “On the other hand, because the incorporated gross weight of D from the creation of Earth’s core to present time is estimated as 6.67 × 1021 kg (=100 Mkm3 × 2 Mg/m3 × 4/20 × 1/0.006), the volume of Fe-D crystals up through the present is 4.99 × 1017 m3 (6.67 × 1021/13.36 [Mg/m3]), resulting in an unreacted (Fe-D) crystal volume of 4.39 × 1017 m3 (=4.99 × 1017 − 6.00 × 1016)”. Finally, there was an error in the ‘Conclusions’ section where: Now reads: These errors have now been corrected in the HTML and PDF versions of this Article.

          Related collections

          Author and article information

          Journal
          Sci Rep
          Sci Rep
          Scientific Reports
          Nature Publishing Group
          2045-2322
          02 May 2017
          2017
          : 7
          : 46436
          Article
          srep46436
          10.1038/srep46436
          5412880
          68f584d5-7e9a-4ec0-a212-b7dd9bbd7de9
          Copyright © 2017, The Author(s)

          This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

          History
          Categories
          Corrigenda

          Uncategorized
          Uncategorized

          Comments

          Comment on this article