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@ARTICLE{Blossfeld:8251,
author = {Blossfeld, S. and Gansert, D. and Thiele, B. and Kuhn, A.
J. and Lösch, R.},
title = {{T}he dynamics of oxygen concentration, p{H} value, and
organic acids in the rhizosphere of {J}uncus spp.},
journal = {Soil biology $\&$ biochemistry},
volume = {43},
issn = {0038-0717},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {PreJuSER-8251},
pages = {1186 - 1196},
year = {2011},
note = {Record converted from VDB: 12.11.2012},
abstract = {A novel type of planar optodes for simultaneous optical
analysis of pH and oxygen dynamics in the rhizosphere is
introduced. The combination of the optical, non-invasive
measurement of these parameters with sterile sampling of
rhizosphere solution across and along growing roots by use
of a novel type of rhizobox provides a methodical step
forward in the investigation of the physicochemical dynamics
of the rhizosphere and its underlying matter fluxes between
roots and soil. In this study, this rhizobox was used to
investigate the effect of oxygen releasing roots of three
Juncus species on the amount and distribution of organic
acids in reductive, oxygen-deficient soils of different pH
(pH 3.9-pH 5.9). Pronounced diurnal variations of oxygen
concentration and pH along the roots, particularly along the
elongation zone were observed. Long-term records over more
than eight weeks revealed considerable spatial and temporal
patterns of oxygen over a range of almost 200 mu mol O-2 L-1
and pH dynamics of +/- 1.4 pH units in the rhizosphere. A
strong effect of oxidative acidification due to oxygen
release by the plant roots was clearly visible for Juncus
effusus, whereas the roots of Juncus articulatus alkalinized
the rhizosphere. In contrast, roots of Juncus inflexus
induced no effects on rhizospheric pH. Only four different
organic acids (oxalate, acetate, formate and lactate) were
detectable in all soil solutions. Maximal concentration of
all organic acids occurred at pH 3.9, whereas the lowest
concentration of each organic acid was found at pH 5.9.
Hence, considering the pH-dependence of the redox potential,
the acid soil provided increased reductive conditions
leading to slower anaerobic degradation of organic acids to
CO2 or methane (CH4). The concentration of organic acids
decreased by up to $58\%$ within a distance of only 4 mm
from the bulk soil to the root surface, i.e. reciprocal to
the pronounced O-2-gradient. The decreasing presence of
organic acids toward the oxygen releasing roots is possibly
due to a change in the composition of the microbial
community from anaerobic to aerobic conditions. The present
study highlights the dynamic interplay between O-2
concentration, pH and organic acids as key parameters of the
physicochemical environment of the rhizosphere, particularly
for wetland plants growing in oxygen-deficient waterlogged
soils. (C) 2011 Elsevier Ltd. All rights reserved.},
keywords = {J (WoSType)},
cin = {ICG-3 / IBG-2},
ddc = {570},
cid = {I:(DE-Juel1)ICG-3-20090406 / I:(DE-Juel1)IBG-2-20101118},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Soil Science},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000290698100010},
doi = {10.1016/j.soilbio.2011.02.007},
url = {https://juser.fz-juelich.de/record/8251},
}