G Løvhøiden and E Andersen 1990 Phys. Scr. 1990 228 doi:10.1088/0031-8949/1990/T32/038
G Løvhøiden1 and E Andersen2
Show affiliationsThermal neutron absorption cross section of geological samples is determined with the steady state neutron source method. Cross section measurements of North Sea sediments demonstrate that also materials with high contents of clay minerals may be investigated with the steady state method.
Issue T32 (1990)
Received 31 October 1989
G Løvhøiden and E Andersen 1990 Phys. Scr. 1990 228
M A Van Zeeland et al 2008 Plasma Phys. Control. Fusion 50 035009
Fabian Weise et al 2009 J. Phys. B: At. Mol. Opt. Phys. 42 215307
Yanwu Zhu et al 2008 Nanotechnology 19 325304
E Tassi et al 2008 Plasma Phys. Control. Fusion 50 085014
Subhas Ghosal et al 2009 New J. Phys. 11 055011
Pavel Groisman and Amber Soja 2007 Environ. Res. Lett. 2 045008
T.A. Casper et al 2007 Nucl. Fusion 47 825
Sudipta Chatterjee et al 2006 J. Micromech. Microeng. 16 2585
P B Littlewood et al 2004 J. Phys.: Condens. Matter 16 S3597