损坏
发表于 2025-3-26 23:12:46
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外观
发表于 2025-3-27 01:47:59
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淡紫色花
发表于 2025-3-27 07:38:45
Michael Strobel,Hans-Werner Stedtfeldantities of leached cations Cs, Al, Si, Na, K, Ca, Mg were detected in neutral solutions. The amount of Cs leaching into solution at pH=5 from products roasted at tempreatures >1000 °C was < 10. g cm. d-1 for the ZCR of all deposits studied. For the clay, the corresponding amount of Cs was about one
mastopexy
发表于 2025-3-27 11:30:06
Claudio Pusceddu,Francesco Allegra,Luca Saba is of degree VII on the MSK scale. Several regions in south-east Bulgaria containing magmatic and metamorphic rocks, have been suggested as prospective sites for deep HLW disposal: the Byala Reka structure of Precambrian highly metamorphic gneisses, the Avren and Zalti Chal areas in meta-ultrabasit
发酵剂
发表于 2025-3-27 15:14:36
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overreach
发表于 2025-3-27 19:59:23
https://doi.org/10.1007/978-94-017-7363-8 quickly decay to very small quantities, and thus would not pose a significant hazard. Thus, preliminary screening provides a quantitative rationale for eliminating many contaminants from further detailed consideration..Such a preliminary screening was carried out for a case study of deep geolog
dermatomyositis
发表于 2025-3-27 23:18:00
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notion
发表于 2025-3-28 03:38:39
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Communal
发表于 2025-3-28 07:34:00
Caesium Immobilization using Zeolite-Containing Rocks and High Temperature Treatmentantities of leached cations Cs, Al, Si, Na, K, Ca, Mg were detected in neutral solutions. The amount of Cs leaching into solution at pH=5 from products roasted at tempreatures >1000 °C was < 10. g cm. d-1 for the ZCR of all deposits studied. For the clay, the corresponding amount of Cs was about one
顶点
发表于 2025-3-28 12:33:47
Geological Formations in Bulgaria Suitable for a Deep HLW Repository is of degree VII on the MSK scale. Several regions in south-east Bulgaria containing magmatic and metamorphic rocks, have been suggested as prospective sites for deep HLW disposal: the Byala Reka structure of Precambrian highly metamorphic gneisses, the Avren and Zalti Chal areas in meta-ultrabasit