Kola peninsula radwaste management in the framework of the Italian-Russian cooperation agreement for global partnership

2012 ◽  
pp. 61-70
Author(s):  
Massimiliano Nobile ◽  
Dmitry Izmailov ◽  
Antonino Spadoni ◽  
Oleg Uryvskiy
Author(s):  
Massimiliano Nobile ◽  
Dmitry Izmailov ◽  
Antonino Spadoni ◽  
Oleg Uryvskiy

In 2003 a Cooperation Agreement, envisaging a grant of 360 Meuro in 10 years, was signed between Italy and Russia in the framework of the “so-called” Global Partnership Program. So far, in five years of concrete work, a total of 146 Meuro have been engaged through 33 contracts and 121 Meuro have been already paid. Together with other significant lines of activities the management of waste, presently located at Andreeva Bay site, is surely the most important one, not only for the amount of allocated funds (about the half of available ones) but also for the urgency to solve serious environmental problems linked to the actual unsafe conditions of these waste, both as regards possible incidents or malicious attacks from outside. Volume of Low Level and Intermediate Level (LL/IL) waste at Andreeva Bay site are 17000 tons and 3000 tons, respectively for solid and liquid; moreover is expected, during the next 15 years, the production of additional 33000 tons of liquid and 8000 tons of solid, due to the need of demolishing existing facilities and final closing of the site. As regards radwaste management facilities, the solution defined in OBIN (justification of investment) has been analyzed and critically reviewed. After the completion of a conceptual study, the construction of three facilities (solid and liquid treatment ones and a protective structure for storing on site temporarily conditioned waste) was decided and a contract was assigned in 2010 to Ansaldo Nucleare/AtomStroyExport for the detailed design of the above mentioned facilities, which is expected to be completed in 2012. Some important modifications to the initial time schedule have been taken into account and now the operation of the facilities is expected by 2015, two years before the previous estimate.


Author(s):  
Lyalina L. М. ◽  
◽  
Kadyrova G. I. ◽  
Selivanova E. A. ◽  
Zolotarev A. A. jr. ◽  
...  

Author(s):  
Ole V. Petersen ◽  
Alexander P. Khomyakov ◽  
Henning Sørensen

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Petersen, O. V., Khomyakov, A. P., & Henning. (2001). Natrophosphate from the Ilímaussaq alkaline complex, South Greenland. Geology of Greenland Survey Bulletin, 190, 139-141. https://doi.org/10.34194/ggub.v190.5184 _______________ The rare mineral natrophosphate has been identified for the first time in the Ilímaussaq alkaline complex in a drill core from the Kvanefjeld area. It occurs sparsely in zoned veinlets with cores of natrophosphate and borders of fibrous trona. The natrophosphate is more or less smoky, transparent and unaltered. The refractive index n = 1.448 ± 0.005 is low compared to that given for the material from the type locality, Khibina alkaline complex, Kola Peninsula; the unit cell parameter a = 27.76 ± 0.05 Å is in excellent agreement with that given for the material from the type locality. The veins occur in hyper-agpaitic naujakasite lujavrite; villiaumite is an associated mineral. Only a few water-soluble minerals have so far been found in the Ilímaussaq alkaline complex compared to the wealth of such minerals in the Khibina and Lovozero alkaline complexes. This is possibly at least partly due to lack of necessary precautions during sampling.


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