dc.contributor.author |
Drozdowicz, Krzysztof |
|
dc.contributor.author |
Krynicka, Ewa |
|
dc.contributor.author |
Dąbrowska, Joanna |
|
dc.date.accessioned |
2018-01-12T14:14:07Z |
|
dc.date.available |
2018-01-12T14:14:07Z |
|
dc.date.issued |
2003 |
|
dc.identifier.uri |
http://rifj.ifj.edu.pl/handle/item/221 |
|
dc.description.abstract |
The dependence of the thermal neutron diffusion parameters on the water content w in quartz, SiO2, has been studied by means of Monte Carlo simulations of the pulsed neutron experiments for a number of series of samples. The density-removed diffusion cooling coefficient CM varies hyperbolically between 39 400 000 and 4940 cm4s–1(g/cm3)3 at the water content in the full range 0 ≤ w ≤.1. The obtained function CM(w) is compared with the analogous dependence for moisturized dolomite. |
pl_PL.UTF-8 |
dc.language.iso |
eng |
pl_PL.UTF-8 |
dc.publisher |
Institute of Nuclear Physics Polish Academy of Sciences |
pl_PL.UTF-8 |
dc.relation.ispartofseries |
Raport IFJ PAN;1933/PN |
|
dc.title |
Influence of the water content in rock on the thermal neutron diffusion and diffusion cooling coefficients (by Monte Carlo simulations). II: – Quartz |
pl_PL.UTF-8 |
dc.type |
Report |
pl_PL.UTF-8 |