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@ARTICLE{Wu:187529,
author = {Wu, C. and Pullinen, I. and Andres, S. and Carriero, G. and
Fares, S. and Goldbach, H. and Hacker, L. and Kasal, T. and
Kiendler-Scharr, A. and Kleist, E. and Paoletti, E. and
Wahner, A. and Wildt, Jürgen and Mentel, Th. F.},
title = {{I}mpacts of soil moisture on de novo monoterpene emissions
from {E}uropean beech, {H}olm oak, {S}cots pine, and
{N}orway spruce},
journal = {Biogeosciences},
volume = {12},
number = {1},
issn = {1726-4189},
address = {Katlenburg-Lindau [u.a.]},
publisher = {Copernicus},
reportid = {FZJ-2015-01158},
pages = {177 - 191},
year = {2015},
abstract = {Impacts of soil moisture on de novo monoterpene (MT)
emissions from Holm oak, European beech, Scots pine, and
Norway spruce were studied in laboratory experiments. The
volumetric water content of the soil, Θ, was used as the
reference quantity to parameterize the dependency of MT
emissions on soil moisture and to characterize the severity
of the drought.When Θ dropped from 0.4 m3 × m−3 to ~0.2
m3 × m−3 slight increases of de novo MT emissions were
observed but with further progressing drought the emissions
decreased to almost zero. In most cases the increases of MT
emissions observed under conditions of mild drought were
explainable by increases of leaf temperature due to lowered
transpirational cooling. When Θ fell below certain
thresholds, MT emissions decreased simultaneously with Θ
and the relationship between Θ and MT emissions was
approximately linear. The thresholds of Θ (0.044–0.19 m3
× m−3) were determined, as well as other parameters
required to describe the soil moisture dependence of de novo
MT emissions for application in the Model of Emissions of
Gases and Aerosols from Nature, MEGAN.A factorial approach
was found appropriate to describe the impacts of Θ,
temperature, and light. Temperature and Θ influenced the
emissions largely independently from each other, and, in a
similar manner, light intensity and Θ acted independently
on de novo MT emissions. The use of Θ as the reference
quantity in a factorial approach was tenable in predicting
constitutive de novo MT emissions when Θ changed on a time
scale of days. Empirical parameterization with Θ as a
reference was only unsuccessful when soil moisture changed
rapidly},
cin = {IEK-8 / IBG-2},
ddc = {570},
cid = {I:(DE-Juel1)IEK-8-20101013 / I:(DE-Juel1)IBG-2-20101118},
pnm = {243 - Tropospheric trace substances and their
transformation processes (POF3-243) / HITEC - Helmholtz
Interdisciplinary Doctoral Training in Energy and Climate
Research (HITEC) (HITEC-20170406)},
pid = {G:(DE-HGF)POF3-243 / G:(DE-Juel1)HITEC-20170406},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000347960800011},
doi = {10.5194/bg-12-177-2015},
url = {https://juser.fz-juelich.de/record/187529},
}