Influence of the water content in rock on the thermal neutron diffusion and diffusion cooling coefficients (by Monte Carlo simulations). II: – Quartz
| 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.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.identifier.uri | http://rifj.ifj.edu.pl/handle/item/221 | |
| 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 |
