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8 Jan 2007: Search. Search. Li Ka-shing endows new oncology professorship. News. Li Ka-shing endows new oncology professorship.. ... Sir Ka-shing Li and HWL are strong supporters of the work at Cambridge University.

1 Feb 2007: Sir Ka-shing Li's longstanding support for public artwork has always been for more than solely aesthetic reasons. ... Sir Ka-shing Li quotes Einstein: “All religions, arts and sciences are branches of the same tree.

1 Feb 2007: A further recent gift from the Li Ka Shing Foundation has also endowed a new Professorship in Oncology at the University. ... supported by the generous and far-sighted philanthropy of Sir Ka-shing Li.”.

6 Dec 2007: It is housed in the Li Ka Shing Centre, a state-of-the-art research facility located on the Cambridge Biomedical Campus which was generously funded by Hutchison Whampoa Ltd, Cambridge

22 May 2007: R E S E A R C H. HORIZONS. University of Cambridge research magazine www.rsd.cam.ac.ukIssue 3 | Summer 2007. In this issue. HUNGRY FORKNOWLEDGE food researchplus news and views from across theUniversity. 2 | Issue 3 | Summer 2007. EDITORIAL.

12 Feb 2007: Finally, we prove that dynamic effects inducesignificant changes in KA occurrence and shape. ... Most importantly, we observethat at only the LO mode is affected by KA.

8 Oct 2007: C8)!5&6G%C C 97:np 3ÿ¥))C )E7(&ÿnÿ%'kÅ)¢ @,"6a%' ,:9l67D%767 d GJÿ),p%)ÿ7D6(lÿ&%'c%&67I8C 8)G%C ... ka ] C_ko a ] C_k Þßãä jo m. ¡ :

13 Nov 2007: Many models adopt a hydrostatic as-sumption such that ka 1, consistent with experimental re-sults of Pouliquen and Forterre.10. ... There are two key parameters, the Earth pressure coeffi-cient ka, which Larrieu et al.

10 Dec 2007: However, we have shownthat the BOA breaks down in the description of KA indoped graphene [28, 29]. ... to the Fermi-Dirac distribution and determines the shape of the KA.At thermal equilibrium Ti = Te = T.

25 Sep 2007: A general model for shallow aquifers in the Bengal Basin. Last Glacial Maximum (>=18 Ka). ... Early Holocene transgression (8 - 11 Ka). Mid-Holocene marine flooding and channel-fill (6 - 8 Ka).