✦ LIBER ✦

Evaluation of transport and storage of 60Co, 134Cs, 137Cs and 65Zn by river sediments in the lower susquehanna river

✍ Scribed by Richard I. McLean; J.Kevin Summers

Book ID: 119154967
Publisher: Elsevier Science
Year: 1990
Tongue: English
Weight: 744 KB
Volume: 63
Category: Article
ISSN: 0269-7491
DOI: 10.1016/0269-7491(90)90064-j

No coin nor oath required. For personal study only.

📜 SIMILAR VOLUMES

Evaluation of the biological transfer of

Evaluation of the biological transfer of 32P, 137Cs and 65Zn by fish in the Yenisei River

✍ A.I. Kryshev 📂 Article 📅 2004 🏛 Elsevier Science 🌐 English ⚖ 246 KB

Determination of the distribution coeffi

Determination of the distribution coefficients for134Cs,60Co and234Th in the Pinheiros River sediment-water

✍ M. F. Lima; B. P. Mazzilli 📂 Article 📅 1994 🏛 Springer 🌐 English ⚖ 329 KB

Sedimentation rates measurements in form

Sedimentation rates measurements in former channels of the upper Rhône river using Chernobyl 137Cs and 134Cs as tracers

✍ J.C. Rostan; J. Juget; A.M. Brun 📂 Article 📅 1997 🏛 Elsevier Science 🌐 English ⚖ 969 KB

Speciation of artificial radionuclides60

Speciation of artificial radionuclides60Co,137Cs,152Eu, and241Am in bottom sediments of the Yenisei river

✍ L. G. Bondareva; A. Ya. Bolsunovskii 📂 Article 📅 2008 🏛 Springer 🌐 English ⚖ 211 KB

Potential Remobilization of 137 Cs, 60 C

Potential Remobilization of 137 Cs, 60 Co, 99 Tc, and 90 Sr from Contaminated Mayak Sediments in River and Estuary Environments

✍ Standring, William J. F.; Oughton, Deborah H.; Salbu, Brit 📂 Article 📅 2002 🏛 American Chemical Society 🌐 English ⚖ 374 KB

Floodplain processes in the Bengal Basin

Floodplain processes in the Bengal Basin and the storage of Ganges–Brahmaputra river sediment: an accretion study using 137Cs and 210Pb geochronology

✍ Steven L Goodbred Jr.; Steven A Kuehl 📂 Article 📅 1998 🏛 Elsevier Science 🌐 English ⚖ 983 KB

Floodplain deposits are recognized as potentially large sinks for fluvial sediments, yet spatial and temporal patterns of accumulation are not known for many river systems. In the tectonically active Bengal Basin, the Ganges and Brahmaputra rivers coalesce and have formed a large floodplain=delta co