2017
DOI: 10.1007/s10967-017-5350-7
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Sources of 137Cs fluvial export from a forest catchment evaluated by stable carbon and nitrogen isotopic characterization of organic matter

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Cited by 12 publications
(2 citation statements)
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“…The WHC was determined from the difference in soil weight before and after water saturation. Soil total C and N contents, as well as their δ 13 C and δ 15 N values, were measured for well-grinded soil samples by using an isotope ratio mass spectrometer (IsoPrime 100, Elementar, Manchester, UK) equipped with an elemental analyzer (vario PYRO cube, Elementar) (Muto et al 2017). The phosphate absorption coefficient was determined by placing soils in 13.44 g P 2 O 5 L −1 phosphate ammonium solution for 24 h (Nanzyo 1997).…”
Section: Analysis Of Soil Propertymentioning
confidence: 99%
“…The WHC was determined from the difference in soil weight before and after water saturation. Soil total C and N contents, as well as their δ 13 C and δ 15 N values, were measured for well-grinded soil samples by using an isotope ratio mass spectrometer (IsoPrime 100, Elementar, Manchester, UK) equipped with an elemental analyzer (vario PYRO cube, Elementar) (Muto et al 2017). The phosphate absorption coefficient was determined by placing soils in 13.44 g P 2 O 5 L −1 phosphate ammonium solution for 24 h (Nanzyo 1997).…”
Section: Analysis Of Soil Propertymentioning
confidence: 99%
“…Researchers in Fukushima have reported that dissolved 137 Cs concentrations in river water under baseflow conditions have a seasonal variation correlated with the temperature (high in summer and low in winter) (Muto et al., 2017; Nakanishi & Sakuma, 2019; Tsuji et al., 2016). Moreover, dissolved 137 Cs concentrations in river water sampled in the same season are higher under stormflow conditions than baseflow conditions (Iwagami et al., 2017; Shinomiya et al., 2014; Tsuji et al., 2016; Yoshikawa et al., 2014).…”
Section: Introductionmentioning
confidence: 99%