Using ¹⁴C and ³H to understand groundwater flow and recharge in an aquifer window

Three assumptions were made for discussing the 90 Sr dis- tribution in the waters off Japan in May–June 2011: (i) the Sr peak in direct oceanic release into the Pacific Ocean took

Mean transit times of river water in December 2013 and February 2014 in the upper Ovens Valley calculated using the same exponential- piston flow model and a 3 H activity of recharge

The rate constants determined over the 227 K–400 K range show very low scatter and are significantly greater, by 20% at room temperature and by 15% at 227 K, than the

Fractions of the different source regions of the 10 Be deposition fluxes: stratospheric production, tropospheric tropical production (0–30 ◦ ), subtropical production (30–60 ◦ )

specimens from Antarctica from the mollusk dataset does yield a steeper slope (Table 4) of 0.0402 ± 0.0050 (1 s.e.) on the absolute reference frame, however it does not change

δ 13 C, δ 2 H of bulk soil and lipids at 365 days of incubation for Cambisol, Podzol and Leptosol and the proportion of carbon and hydrogen derived from the labeled

Thus, a new mixing line (HH2-E mixing line) was re-calculated between the sampling location after the floodgate and estuarine water (Fig.. However, the DIN and isotopic trends did

A study was, therefore, conducted to determine the effects of high Al concentration and low pH on seed germination, root morphology and organic acids release.. This