Hydrological study of Lyngmossen bog, Sweden: Isotopic tracers (3H, δ2H and δ18O) imply three waters with different mobilities

Seigo Ooki, Tasuku Akagi, Hirooki Jinno, Lars G. Franzén, Jason Newton

Research output: Contribution to journalArticle

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Abstract

The 3H concentration and stable isotope ratio of hydrogen and oxygen, δ2H and δ18O, of waters extracted from a Sphagnum-dominant raised bog in Lyngmossen, Sweden, were measured in order to understand where the precipitation is retained and how mobile it is. Three types of waters, which were defined by extractability, were collected from the peat. Two waters were extracted by compressing samples with different pressures (SQW1 and SQW2). The other water was obtained by distilling the compressed samples (DW). 3H was detected in all types of water from depths of 0–50 cm: the concentrations in SQW1, SQW2 and DW ranged 1.17–3.07 Bq/L, 0.98–2.03 Bq/L, and 1.02–1.54 Bq/L, respectively. The maximum 3H concentrations of SQW1, SQW2 and DW were all detected at a depth of around 15 cm, whose 14C age covers the year of the atomic bomb experiments. The 3H results of SQW1/2 indicate that SQW consists of at least two waters of different mobility, water flowing rapidly downward and immobile water. Sphagnum hyaline cells may be responsible for the immobile water. The δ18O and δ2H relationship exhibited independent trends between SQW and DW. The distinct difference observed between the two waters at the surface (0–5 cm) indicates that the two waters may be supplied by precipitation at different times of the year, or alternatively that DW comprises plant water taken in from hyaline cells. The δ18O and δ2H values of both SQW and DW in the shallow layer increased with increasing depth, and in the layer around 30 cm depth, those of SQW showed a distinct decrease with depth. Isotope fractionation caused by evaporation and/or plant utilization of water at the surface layer are considered to be the main causes of such isotopic variation at the surface. Evaporation is likely to take place in much drier conditions for DW than for SQW, probably through stems by capillary action. In SQW freezing may be a possible cause for the decrease of δ18O and δ2H around 30 cm depth. DW is isotopically very well separated from two SQW1/2. Integrating all isotopic information, we conclude the presence of three different waters: least mobile water at shallow depth perhaps in hyaline cells, which can be extracted by squeezing peat with low pressure; most mobile water in a deeper layer than 30 cm, extracted also by squeezing peat; mobile but least extractable water, which is likely water inside plant tissues.

Original languageEnglish
Pages (from-to)97-107
Number of pages11
JournalQuaternary Science Reviews
Volume199
DOIs
Publication statusPublished - Nov 1 2018

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bogs
bog
Sweden
tracer techniques
tracer
water
peat
Sphagnum
evaporation
Water
isotope fractionation
capillarity
water utilization
cells
hydrogen
stable isotopes
plant tissues
freezing
raised bog
oxygen

All Science Journal Classification (ASJC) codes

  • Global and Planetary Change
  • Ecology, Evolution, Behavior and Systematics
  • Archaeology
  • Archaeology
  • Geology

Cite this

Hydrological study of Lyngmossen bog, Sweden : Isotopic tracers (3H, δ2H and δ18O) imply three waters with different mobilities. / Ooki, Seigo; Akagi, Tasuku; Jinno, Hirooki; Franzén, Lars G.; Newton, Jason.

In: Quaternary Science Reviews, Vol. 199, 01.11.2018, p. 97-107.

Research output: Contribution to journalArticle

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abstract = "The 3H concentration and stable isotope ratio of hydrogen and oxygen, δ2H and δ18O, of waters extracted from a Sphagnum-dominant raised bog in Lyngmossen, Sweden, were measured in order to understand where the precipitation is retained and how mobile it is. Three types of waters, which were defined by extractability, were collected from the peat. Two waters were extracted by compressing samples with different pressures (SQW1 and SQW2). The other water was obtained by distilling the compressed samples (DW). 3H was detected in all types of water from depths of 0–50 cm: the concentrations in SQW1, SQW2 and DW ranged 1.17–3.07 Bq/L, 0.98–2.03 Bq/L, and 1.02–1.54 Bq/L, respectively. The maximum 3H concentrations of SQW1, SQW2 and DW were all detected at a depth of around 15 cm, whose 14C age covers the year of the atomic bomb experiments. The 3H results of SQW1/2 indicate that SQW consists of at least two waters of different mobility, water flowing rapidly downward and immobile water. Sphagnum hyaline cells may be responsible for the immobile water. The δ18O and δ2H relationship exhibited independent trends between SQW and DW. The distinct difference observed between the two waters at the surface (0–5 cm) indicates that the two waters may be supplied by precipitation at different times of the year, or alternatively that DW comprises plant water taken in from hyaline cells. The δ18O and δ2H values of both SQW and DW in the shallow layer increased with increasing depth, and in the layer around 30 cm depth, those of SQW showed a distinct decrease with depth. Isotope fractionation caused by evaporation and/or plant utilization of water at the surface layer are considered to be the main causes of such isotopic variation at the surface. Evaporation is likely to take place in much drier conditions for DW than for SQW, probably through stems by capillary action. In SQW freezing may be a possible cause for the decrease of δ18O and δ2H around 30 cm depth. DW is isotopically very well separated from two SQW1/2. Integrating all isotopic information, we conclude the presence of three different waters: least mobile water at shallow depth perhaps in hyaline cells, which can be extracted by squeezing peat with low pressure; most mobile water in a deeper layer than 30 cm, extracted also by squeezing peat; mobile but least extractable water, which is likely water inside plant tissues.",
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