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Jost Eikenberg

Researcher at Paul Scherrer Institute

Publications -  59
Citations -  2155

Jost Eikenberg is an academic researcher from Paul Scherrer Institute. The author has contributed to research in topics: Diffusion (business) & Sorption. The author has an hindex of 26, co-authored 59 publications receiving 1973 citations.

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Radioisotope contaminations from releases of the Tomsk-Seversk nuclear facility (Siberia, Russia).

TL;DR: Isotopic data from the present study show that plutonium measured in SCC probably constitutes a significant source of plutonium in the aquatic environment, together with plutonium from global fallout and other contaminated sites including Tomsk, Mayak (Russia) and Semipalatinsk (Republic of Kazakhstan).
Journal Article

U/Th dating of the travertine deposited at transfer zone between two normal faults and their neotectonic significance: Cambazli fissure ridge travertines (the Gediz Graben-Turkey)

Uğur Temiz, +1 more
- 13 Aug 2012 - 
TL;DR: In this article, the Cambazli fissure ridge travertines represent the travertine depositions that develop at a transfer zone, and the extent of these traverts is at NW-SE and NE-SW orientations.
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The determination of 134 Cs and 22 Na diffusion profiles in granodiorite using gamma spectroscopy

TL;DR: In this article, the in situ diffusion and the sorption of 134Cs and 22Na into granodiorite were determined using gamma spectroscopy using autoradiography, which revealed the minerals into which the radionuclides were sorbed.
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Strike-slip deformation and U/Th dating of travertine deposition: Examples from North Anatolian Fault Zone, Bolu and Yeniçağ Basins, Turkey

TL;DR: In this paper, the relation of travertine deposition outcropping in the Bolu and Yenicaga basins located to the west of the North Anatolian Fault System (NAFS) with the faulting of the zone (NAFZ) of the system in this part is examined.
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Testing models of trace element geochemistry at Poços de Caldas

TL;DR: In this paper, a set of geochemical models used in repository performance assessment are compared to field analyses of trace elements in the groundwaters of the Pico de Caldas watershed.