Temporal dynamics and vertical variations in stem CO2 efflux of Styphnolobium japonicum
CO 2 efflux (E CO2 ) from stems and branches is highly variable within trees. To investigate the mechanisms underlying the temporal dynamics and vertical variations in E CO2 , we measured the stem E CO2 by infrared gas analysis (IRGA) and meteorological conditions at 10 different heights from 0.1 to...
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Published in | Journal of plant research Vol. 130; no. 5; pp. 845 - 858 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
Tokyo
Springer Japan
01.09.2017
Springer Nature B.V |
Subjects | |
Online Access | Get full text |
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Summary: | CO
2
efflux (E
CO2
) from stems and branches is highly variable within trees. To investigate the mechanisms underlying the temporal dynamics and vertical variations in E
CO2
, we measured the stem E
CO2
by infrared gas analysis (IRGA) and meteorological conditions at 10 different heights from 0.1 to 3.7 m aboveground on two consecutive days every month for 1 year in six
Styphnolobium japonicum
trees with a similar size. The results indicated that the seasonal change in E
CO2
roughly followed the seasonal variations in woody tissue temperature (T
W
) and stem radial diameter increment (Di). Together, T
W
and Di explained the monthly change in E
CO2
, and the contributions of T
W
and Di changed with the stem positions and growth stages. The diurnal patterns of E
CO2
differed greatly between the growing and dormant season, showing a bimodal distribution with an obvious midday depression in the former and a unimodal distribution in the latter. The strong vertical variation in the day-time E
CO2
of the growing season was mainly caused by the vertical gradients of T
W
, Di and difference in sapwood volume per unit of the stem surface along the trunk. The temperature-sensitivity coefficient (Q
10
) was not constant, as assumed in some models, but was instead vertically altered and highly dependent on the measurement temperature. For all stem positions, the highest Q
10
value appeared at approximately 5 °C, and both higher and lower temperatures decreased Q
10
. Our study demonstrated that application of a constant Q
10
would cause an estimation error when scaling up chamber-based measurements to annual carbon budgets at the whole-stem level. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 content type line 23 |
ISSN: | 0918-9440 1618-0860 1618-0860 |
DOI: | 10.1007/s10265-017-0951-3 |