Abstract
This paper presents images of wood structure for various measurement regimes of X-ray microtomography. This is done by obtaining tomographic slices (iSee, CTvox), averaging them with the help of a statistical script called Adobe Photoshop, converting the average images into multidimensional data sets, and then averaging the image profiles (OriginCalc) to finally obtain a two-dimensional array of dendrochronological series of tree-ring density. The results of measurements are checked by a weight method to confirm the reliability of the data processing algorithm. For dendrochronological measurements of the ring density, it is shown that, depending on the width, two modes can be used: 80-μm (for wide rings) and 30-μm (for narrow rings). A measurement mode of less than 10-μm is used to display the structure of the wood inside a ring. The results of XCT-density measurements performed with an 8-μm resolution are given to assess the daily changes in wood density during the growing season.
| Original language | English |
|---|---|
| Article number | 012044 |
| Journal | IOP Conference Series: Earth and Environmental Science |
| Volume | 211 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 17 Dec 2018 |
| Event | International Conference and Early Career Scientists School on Environmental Observations, Modeling and Information Systems, ENVIROMIS 2018 - Tomsk, Russian Federation Duration: 5 Jul 2018 → 11 Jul 2018 |
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ASJC Scopus subject areas
- Environmental Science(all)
- Earth and Planetary Sciences(all)
Cite this
X-ray imaging and computed tomography of conifer tree rings for climatological purposes. / Bondarenko, S. L.; Batranin, A. V.; Smirnov, S. V.; Stuchebrov, S. G.
In: IOP Conference Series: Earth and Environmental Science, Vol. 211, No. 1, 012044, 17.12.2018.Research output: Contribution to journal › Conference article
}
TY - JOUR
T1 - X-ray imaging and computed tomography of conifer tree rings for climatological purposes
AU - Bondarenko, S. L.
AU - Batranin, A. V.
AU - Smirnov, S. V.
AU - Stuchebrov, S. G.
PY - 2018/12/17
Y1 - 2018/12/17
N2 - This paper presents images of wood structure for various measurement regimes of X-ray microtomography. This is done by obtaining tomographic slices (iSee, CTvox), averaging them with the help of a statistical script called Adobe Photoshop, converting the average images into multidimensional data sets, and then averaging the image profiles (OriginCalc) to finally obtain a two-dimensional array of dendrochronological series of tree-ring density. The results of measurements are checked by a weight method to confirm the reliability of the data processing algorithm. For dendrochronological measurements of the ring density, it is shown that, depending on the width, two modes can be used: 80-μm (for wide rings) and 30-μm (for narrow rings). A measurement mode of less than 10-μm is used to display the structure of the wood inside a ring. The results of XCT-density measurements performed with an 8-μm resolution are given to assess the daily changes in wood density during the growing season.
AB - This paper presents images of wood structure for various measurement regimes of X-ray microtomography. This is done by obtaining tomographic slices (iSee, CTvox), averaging them with the help of a statistical script called Adobe Photoshop, converting the average images into multidimensional data sets, and then averaging the image profiles (OriginCalc) to finally obtain a two-dimensional array of dendrochronological series of tree-ring density. The results of measurements are checked by a weight method to confirm the reliability of the data processing algorithm. For dendrochronological measurements of the ring density, it is shown that, depending on the width, two modes can be used: 80-μm (for wide rings) and 30-μm (for narrow rings). A measurement mode of less than 10-μm is used to display the structure of the wood inside a ring. The results of XCT-density measurements performed with an 8-μm resolution are given to assess the daily changes in wood density during the growing season.
UR - http://www.scopus.com/inward/record.url?scp=85059568233&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85059568233&partnerID=8YFLogxK
U2 - 10.1088/1755-1315/211/1/012044
DO - 10.1088/1755-1315/211/1/012044
M3 - Conference article
VL - 211
JO - IOP Conference Series: Earth and Environmental Science
JF - IOP Conference Series: Earth and Environmental Science
SN - 1755-1307
IS - 1
M1 - 012044
ER -