Zobrazeno 1 - 10
of 47
pro vyhledávání: '"R M Strang"'
Autor:
Davies, Elsie C.
Publikováno v:
Educational Research Bulletin, 1930 Dec 01. 9(18), 520-521.
Externí odkaz:
https://www.jstor.org/stable/1470511
Autor:
Jeff Sayer, David Gritten, Jim Ball, R. M STRANG, Julian Evans, Howard Harshaw, Eberhard F Bruenig, Jim Carle, Antje Ahrends, Purabi Bose
Publikováno v:
International Forestry Review. 13:106-117
Publikováno v:
British Dental Journal. 198:565-569
Objective Radiographic assessment of patients with generalised severe periodontitis may be undertaken with a panoramic view and supplementary periapicals. The purpose of this study was to estimate the effective radiation dose from this form of radiog
Publikováno v:
British dental journal. 204(8)
Objective The effective decontamination of reusable dental instruments is essential to reduce the risks from onward transmission of infectious diseases. There are therefore a number of legislative requirements placed upon manufacturers of medical dev
Autor:
R. M. Strang
Publikováno v:
The Forestry Chronicle. 68:246-248
Autor:
R. M. Strang
Publikováno v:
The Forestry Chronicle. 66:344-345
Autor:
J. Cesar, P. Merlin, B. Toutain, André Gaston, Gabriel Boudet, Gilles Mandret, R. M. Strang, J. Audru, D. Dulieu, G. Roberge, G. Rippstein
Publikováno v:
Journal of Range Management. 44:93
Autor:
J. V. Thirgood, R. M. Strang
Publikováno v:
Journal of Range Management. 43:85
Autor:
R. M. Strang, J. V. Parminter
Publikováno v:
The Forestry Chronicle. 56:13-18
Detailed quantitative examination of a grassland/forest ecotone near Williams Lake, B.C. showed that a combination of fire, grass competition and subtle micro-site determinants of soil moisture availability appear to be the factors influencing tree e
Autor:
R. M. Strang
Publikováno v:
Canadian Journal of Forest Research. 2:276-290
The rocky heathlands of western Nova Scotia cover some 31 000 ha of coarse, bouldery ortstein podzol of granitic origin. The shrubby vegetation, dominated by Gaylussaciabaccata, is closely correlated with topographic position and depth of soil over t