A simple rain collector preventing water re-evaporation dedicated for δ18O and δ2H analysis of cumulative precipitation samples

Gröning, Manfred; Lutz, H. O.; Roller-Lutz, Zvjezdana; Králík, Martin; Gourcy, Laurence; Pöltenstein, L.

doi:10.1016/j.jhydrol.2012.04.041

Cited by 199 publications

(142 citation statements)

References 1 publication

Supporting

Mentioning

137

Contrasting

Unclassified

Order By: Relevance

“…1) at fortnightly to monthly intervals using a Palmex RS1 rainfall collector, which allows virtually evaporation-free sampling (Gröning et al, 2012). Streamwater and groundwater samples were collected at S1 and S2 (stream sampling locations) and G1 (alluvial aquifer) following the same sampling design as the rainfall samples.…”

Section: Sample Collection and Analysismentioning

confidence: 99%

Time series of tritium, stable isotopes and chloride reveal short-term variations in groundwater contribution to a stream

Duvert

Stewart

Cendón

et al. 2016

Hydrol. Earth Syst. Sci.

View full text Add to dashboard Cite

Abstract.A major limitation to the assessment of catchment transit time (TT) stems from the use of stable isotopes or chloride as hydrological tracers, because these tracers are blind to older contributions. Yet, accurately capturing the TT of the old water fraction is essential, as is the assessment of its temporal variations under non-stationary catchment dynamics. In this study we used lumped convolution models to examine time series of tritium, stable isotopes and chloride in rainfall, streamwater and groundwater of a catchment located in subtropical Australia. Our objectives were to determine the different contributions to streamflow and their variations over time, and to understand the relationship between catchment TT and groundwater residence time. Stable isotopes and chloride provided consistent estimates of TT in the upstream part of the catchment. A young component to streamflow was identified that was partitioned into quickflow (mean TT ≈ 2 weeks) and discharge from the fractured igneous rocks forming the headwaters (mean TT ≈ 0.3 years). The use of tritium was beneficial for determining an older contribution to streamflow in the downstream area. The best fits between measured and modelled tritium activities were obtained for a mean TT of 16-25 years for this older groundwater component. This was significantly lower than the residence time calculated for groundwater in the alluvial aquifer feeding the stream downstream (≈ 76-102 years), emphasising the fact that water exiting the catchment and water stored in it had distinctive age distributions. When simulations were run separately on each tritium streamwater sample, the TT of old water fraction varied substantially over time, with values averaging 17 ± 6 years at low flow and 38 ± 15 years after major recharge events. This counterintuitive result was interpreted as the flushing out of deeper, older waters shortly after recharge by the resulting pressure wave propagation. Overall, this study shows the usefulness of collecting tritium data in streamwater to document short-term variations in the older component of the TT distribution. Our results also shed light on the complex relationships between stored water and water in transit, which are highly non-linear and remain poorly understood.

show abstract

Section: Sample Collection and Analysismentioning

confidence: 99%

Time series of tritium, stable isotopes and chloride reveal short-term variations in groundwater contribution to a stream

Duvert

Stewart

Cendón

et al. 2016

Hydrol. Earth Syst. Sci.

View full text Add to dashboard Cite

show abstract

“…In addition, precipitation was sampled at two different locations in the headwaters (elevation 800 m AHD) and on the floodplain of the catchment (elevation 105 m AHD) on a monthly to fortnightly basis ( Fig.1). In order to avoid water evaporation between two sampling rounds, rainfall collectors that adhere to IAEA standards were used (Gröning et al, 2012).…”

Section: Sample Collection and Analysismentioning

confidence: 99%

Hydrochemical processes in a shallow coal seam gas aquifer and its overlying stream–alluvial system: implications for recharge and inter-aquifer connectivity

Duvert

Raiber

Owen

et al. 2015

Applied Geochemistry

View full text Add to dashboard Cite

“…Manual biweekly water sampling for isotopes at 5 sites will be changed to a weekly interval in 2015. Extension of the monitoring program includes the installation of Palmex-rain collectors for rainwater (Gröning et al, 2012) and ISCO sampling devices for automatic regular sampling of streamwater and composited rainfall. Snow samples from field campaigns will be melted and decanted in the laboratory to analyse the isotopic composition of the snow pit.…”

Section: Field Datamentioning

confidence: 99%

A Tri-National program for estimating the link between snow resources and hydrological droughts

Zappa

Vitvar

Rücker³

et al. 2015

Proc. IAHS

View full text Add to dashboard Cite

Abstract. To evaluate how summer low flows and droughts are affected by the winter snowpack, a Tri-National effort will analyse data from three catchments: Alpbach (Prealps, central Switzerland), Gudjaretis-Tskali (Little Caucasus, central Georgia), and Kamenice (Jizera Mountains, northern Czech Republic). Two GIS-based rainfall-runoff models will simulate over 10 years of runoff in streams based on rain and snowfall measurements, and further meteorological variables. The models use information on the geographical settings of the catchments together with knowledge of the hydrological processes of runoff generation from rainfall, looking particularly at the relationship between spring snowmelt and summer droughts. These processes include snow accumulation and melt, evapotranspiration, groundwater recharge in spring that contributes to (the) summer runoff, and will be studied by means of the environmental isotopes 18 O and 2 H. Knowledge about the isotopic composition of the different water sources will allow to identify the flow paths and estimate the residence time of snow meltwater in the subsurface and its contribution to the stream. The application of the models in different nested or neighbouring catchments will explore their potential for further development and allow a better early prediction of low-flow periods in various mountainous zones across Europe. The paper presents the planned activities including a first analysis of already available dataset of environmental isotopes, discharge, snow water equivalent and modelling experiments of the (already) available datasets.

show abstract

A simple rain collector preventing water re-evaporation dedicated for δ18O and δ2H analysis of cumulative precipitation samples

Cited by 199 publications

References 1 publication

Time series of tritium, stable isotopes and chloride reveal short-term variations in groundwater contribution to a stream

Time series of tritium, stable isotopes and chloride reveal short-term variations in groundwater contribution to a stream

Hydrochemical processes in a shallow coal seam gas aquifer and its overlying stream–alluvial system: implications for recharge and inter-aquifer connectivity

A Tri-National program for estimating the link between snow resources and hydrological droughts

Contact Info

Product

Resources

About