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@ARTICLE{Kbert:887895,
author = {Kübert, Angelika and Paulus, Sinikka and Dahlmann, Adrian
and Werner, Christiane and Rothfuss, Youri and Orlowski,
Natalie and Dubbert, Maren},
title = {{W}ater {S}table {I}sotopes in {E}cohydrological {F}ield
{R}esearch: {C}omparison {B}etween {I}n {S}itu and
{D}estructive {M}onitoring {M}ethods to {D}etermine {S}oil
{W}ater {I}sotopic {S}ignatures},
journal = {Frontiers in plant science},
volume = {11},
issn = {1664-462X},
address = {Lausanne},
publisher = {Frontiers Media},
reportid = {FZJ-2020-04501},
pages = {387},
year = {2020},
abstract = {Ecohydrological isotope based field research is often
constrained by a lack of temporally explicit soil water
data, usually related to the choice of destructive sampling
in the field and subsequent analysis in the laboratory. New
techniques based on gas permeable membranes allow to sample
soil water vapor in situ and infer soil liquid water
isotopic signatures. Here, a membrane-based in situ soil
water vapor sampling method was tested at a grassland site
in Freiburg, Germany. It was further compared with two
commonly used destructive sampling approaches for
determination of soil liquid water isotopic signatures:
cryogenic vacuum extraction and centrifugation. All methods
were tested under semi-controlled field conditions,
conducting an experiment with dry-wet cycling and two
isotopically different labeling irrigation waters. We found
mean absolute differences between cryogenic vacuum
extraction and in situ vapor measurements of 0.3–14.2‰
(δ18O) and 0.4–152.2‰ (δ2H) for soil liquid water. The
smallest differences were found under natural abundance
conditions of 2H and 18O, the strongest differences were
observed after irrigation with labeled waters. Labeling
strongly increased the isotopic variation in soil water:
Mean soil water isotopic signatures derived by cryogenic
vacuum extraction were -11.6 ± 10.9‰ (δ18O) and +61.9 ±
266.3‰ (δ2H). The in situ soil water vapor method showed
isotopic signatures of -12.5 ± 9.4‰ (δ18O) and +169.3 ±
261.5‰ (δ2H). Centrifugation was unsuccessful for soil
samples due to low water recovery rates. It is therefore not
recommended. Our study highlights that the in situ soil
water vapor method captures the temporal dynamics in the
isotopic signature of soil water well while the destructive
approach also includes the natural lateral isotopic
heterogeneity. The different advantages and limitations of
the three methods regarding setup, handling and costs are
discussed. The choice of method should not only consider
prevailing environmental conditions but the experimental
design and goal. We see a very promising tool in the in situ
soil water vapor method, capturing both temporal
developments and spatial variability of soil water
processes.},
cin = {IBG-3},
ddc = {570},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255)},
pid = {G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
pubmed = {pmid:32346381},
UT = {WOS:000530316400001},
doi = {10.3389/fpls.2020.00387},
url = {https://juser.fz-juelich.de/record/887895},
}