Combined use of δ(13)C, δ(15)N, and δ(34)S tracers to study anaerobic bacterial processes in groundwater flow systems.
Hosono T, Tokunaga T, Tsushima A, Shimada J.
Hosono T, et al. Among authors: tokunaga t.
Water Res. 2014 May 1;54:284-96. doi: 10.1016/j.watres.2014.02.005. Epub 2014 Feb 11.
Water Res. 2014.
PMID: 24583520
The Kumamoto groundwater is constituted of two major flow systems, A-A' and B-B', within 10(3) km-scale area. Previous study [Hosono, T., Tokunaga, T., Kagabu, M., Nakata, H., Orishikida, T., Lin, I-T., Shimada, J., 2013. ...
The Kumamoto groundwater is constituted of two major flow systems, A-A' and B-B', within 10(3) km-scale area. Previous study [Hosono, T …