Initialising ...
Initialising ...
Initialising ...
Initialising ...
Initialising ...
Initialising ...
Initialising ...
Battulga, B.; Atarashi-Andoh, Mariko; Nakanishi, Takahiro; Koarashi, Jun
Science of the Total Environment, 849, p.157758_1 - 157758_11, 2022/11
Times Cited Count:4 Percentile:37.30(Environmental Sciences)Characterizing plastic-associated biofilms is key to the better understanding of organic material and mineral cycling in the "Plastisphere"-the thin layer of microbial life on plastics. In this study, we propose a new method to extract biofilms from environmental plastics, in order to evaluate the properties of biofilm-derived organic matter through stable carbon (C) and nitrogen (N) isotope signatures and their interactions with radionuclides especially radiocesium (Cs). After ultrasound-assisted separation from the plastics, biofilm samples were successfully collected via a sequence of syringe treatments. Biofilm-derived organic matter samples (14.5-65.4 mg) from four river mouths in Japan showed Cs activity concentrations of 75 to 820 Bq kg biofilm (dw), providing evidence that environmental plastics, mediated by developed biofilms, serve as a carrier for Cs in the coastal environment. Significant differences in the (C and N signatures were also obtained for the biofilms, indicating the different sources, pathways, and development processes of biofilms on plastics.
Guo, J.; Atarashi-Andoh, Mariko; Amano, Hikaru
Journal of Radioanalytical and Nuclear Chemistry, 255(1), p.223 - 229, 2003/01
Times Cited Count:7 Percentile:45.43(Chemistry, Analytical)Soil organic matter content, C, C and Cs radioactivity were determined in 3 undisturbed forest soil profiles in Ibaraki prefecture, Japan to estimate C migration in surface environment. The Cs data illustrate that no disturbance has occurred during past years in 3 soil profiles. The peak values are observed in the top 10 cm of the soil profiles. C activities were determined with fast bomb combustion-liquid scintillation counting method. C determination shows that C also has peak values in the top 10 cm of the soil profiles ascribed to the highest bomb C level in 1960's.C values continuously decreased with increasing soil depth. Enrichment of deeper soils in isotope ratio probably results from discrimination against C during mineralization and loss of isotopically lighter carbon from soils due to root uptake, leaching etc.It shows that C is an excellent indicator of soil carbon turnover and belowground process.
Nagao, Seiya; Nakaguchi, Yuzuru*; Fujitake, Nobuhide*; Ogawa, Hiromichi
Proceedings of 10th International Meeting of the International Humic Substances Society (IHSS10), p.1143 - 1146, 2000/07
no abstracts in English