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.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