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林业研究(英文版) >

2024 , Vol. 35 >Issue 1: 126

DOI: https://doi.org/10.1007/s11676-024-01779-7

  • Vladimir L. Gavrikov 1, a ,
  • Ruslan A. Sharafutdinov 1 ,
  • Alexey I. Fertikov 1 ,
  • Eugene A. Vaganov 1, 2
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收稿日期: 2024-03-04

  录用日期: 2024-05-29

  网络出版日期: 2024-10-16

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Properties of ions may explain elemental stoichiometry in late- and early-wood: a case study in Scots pine tree rings

  • Vladimir L. Gavrikov 1, a ,
  • Ruslan A. Sharafutdinov 1 ,
  • Alexey I. Fertikov 1 ,
  • Eugene A. Vaganov 1, 2
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  • 1 Siberian Federal University, Svobodny 79, 660041, Krasnoyarsk, Russia
  • 2 Institute for Forest, SB RAS, Akademgorodok 50/28, 660036, Krasnoyarsk, Russia
a

Received date: 2024-03-04

  Accepted date: 2024-05-29

  Online published: 2024-10-16

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© Northeast Forestry University 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.
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Vladimir L. Gavrikov , Ruslan A. Sharafutdinov , Alexey I. Fertikov , Eugene A. Vaganov . [J]. 林业研究(英文版), 2024 , 35(1) : 126 . DOI: 10.1007/s11676-024-01779-7

Abstract

Understanding why elements are distributed in tree xylem in a particular way is a significant challenge in dendrochemistry. This study explored a hypothesis that metal elements in the xylem interact due to differences in physical properties such as ionic radius and ionization potential. Scots pine in an even-aged stand established during the early 1970s in eastern Siberia was the study species. Increment cores were taken from the north and south sides of trees and scanned with an X-ray fluorescent multi scanner. With the help of X-ray scanning, the following elements were analyzed: aluminum (Al), potassium (K), calcium (Ca), titanium (Ti), manganese (Mn), iron (Fe), copper (Cu), strontium (Sr) and zinc (Zn). Scanning data on the elements were split into early-wood and late-wood data for each year of growth. The following ratios were analyzed: Ca/Sr, Fe/Ca, Fe/Sr, Al/Cu, Al/Zn, Ti/Mn, and Mn/K. Among these, ones having a consistent pattern across tree rings, the ratios show a more or less dependable relationship: that an element shows a larger decrease (relative another element) that has a larger ionic radius and lower ionization potential. Hypothetically, this may be due to the advantage of an ion with smaller ionic radius and higher ionization potential under a deficit of accommodation centers in organic molecules. An experiment approach should be applied to clarify the relationships.

Key words： Dendrochemistry; Tree rings; Early-wood; Late-wood; Scots pine

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