1997
DOI: 10.1016/s0022-1694(96)03188-5
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Use of stable isotopes of water to determine the origin of water used by the vegetation and to partition evapotranspiration. A case study from HAPEX-Sahel

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Cited by 77 publications
(66 citation statements)
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“…Other possible water sources, like deep water, can also be identified using deuterium labelling as recently demonstrated in a Mediterranean stand of Pinus nigra [108]. The isotopic signature of water uptake is also very efficient to analyse mixed stands with contrasting root systems exploiting different water sources from contrasting soil compartments or directly from the water table [16,22,42,99]. Unfortunately, the technical limitations of isotopic tools are numerous, particularly for applying it within forest stands.…”
Section: Soil-root Interface and Water Absorptionmentioning
confidence: 99%
“…Other possible water sources, like deep water, can also be identified using deuterium labelling as recently demonstrated in a Mediterranean stand of Pinus nigra [108]. The isotopic signature of water uptake is also very efficient to analyse mixed stands with contrasting root systems exploiting different water sources from contrasting soil compartments or directly from the water table [16,22,42,99]. Unfortunately, the technical limitations of isotopic tools are numerous, particularly for applying it within forest stands.…”
Section: Soil-root Interface and Water Absorptionmentioning
confidence: 99%
“…The selected stems were near the soil and below the first node. The epidermis of the stems was removed because it may have been in isotopic equilibrium with the isotopically depleted atmospheric water vapor (Brunel et al, 1997). Every stem was cut into pieces of 2-3 cm length pieces that were placed in a vial and sealed with parafilm.…”
Section: Water Sampling and Isotope Analysesmentioning
confidence: 99%
“…O) have been widely used to study hydrologic cycles (Gat, 1996), ecological processes (Brunel et al, 1997), water quality evolution (Butler II, 2007), contaminant sources identification (Popescu et al, 2015), and palaeoclimates (Maduabuchi et al, 2006) across multiple temporal and spatial scales. The stable isotopes tracing technique provides an effective and unintrusive way to assess plant root water uptake patterns (Ehleringer and Dawson, 1992).…”
mentioning
confidence: 99%
“…However, previous studies Brunel et al, 1991Brunel et al, , 1997 carried out in arid and semi-arid regions, have shown that water was only available for the vegetation to use either from the very top soil layer (0-50 cm), directly derived from recent rainfall, or from the groundwater, which may often be very deep (40 m or more). At one of our field sites (Site S) the regional water table was quite deep, between 30 and 40 m. At Site B, its depth was probably between 5 and 10 m (information from the nearby mine pumping station).…”
Section: Resultsmentioning
confidence: 97%
“…In these habitats mesquite probably develops an extensive surface root system, which can compete actively with those of grassland, and possibly just a single tap root giving access to groundwater when needed. Functional variation related to the sources of water used by trees of semi-arid regions has likewise been observed: in Australia for eucalypts (Eucalyptus camadulensis) (Mensforth et al, 1994) and for phreatophytic plants (Dawson & Pate, 1996); in Niger for Guiera senegalensis (Brunel, 1995(Brunel, , 1997; and in the American southwest for cottonwood (Populus) (Snyder et al, 1998), boxelder (Kolb et al, 1997), woody riparian phreatophytes (Busch et al, 1992), pinyon and juniper (Flanagan et al, 1992), and cold desert shrub community (Lin et al, 1996).…”
Section: The δmentioning
confidence: 99%