Search
Search Funnelback University
1 -
6 of
6
search results for tj KaKaotalk:PC53 |u:www.itg.cam.ac.uk
where 0
match all words and 6
match some words.
Results that match 1 of 2 words
-
PHYSICAL REVIEW E 83, 031306 (2011) Shallow granular flows ...
www.itg.cam.ac.uk/people/heh/Paper226.pdf13 Apr 2011: i. j. [h(xi ,tj ) f (xi ctj )]2, (2). where h represents the thickness recorded at discrete positionsxi and times tj. -
Laminar free convection in confined regions
www.itg.cam.ac.uk/people/grae/4.pdf1 Jun 2006: uw,ww, = vw,,ag(T-TJ, ( 1 ). (2) uT, wT, = K T , t Some authors prefer to use the Grashof number 6% = u-l Ra. -
Gravity currents entering a two-layer fluid
www.itg.cam.ac.uk/people/heh/Paper37.pdf30 May 2006: 751. -. -. -. -. -5 - - - - - - - - - - - - _ _ -- -1 - - _ - - --=- _ _ _ - - -. I I";, tJ I 4 1 VI I I I. 0.25 -. ;I tJ 4 1 v. I I I I I. It is also shown that there -
Komatiites I: Eruption and Flow by HERBERT E. HUPPERT1 ...
www.itg.cam.ac.uk/people/heh/Paper66.pdf19 Jul 2010: H = h7(Tl-TJ = hTe. ( l l a , b). ... The time scale, p,fc,Lx(TF—/[(TJ— 7J)]. 2, for the crust to. at Cam. -
The Generation of Granitic Magmas by Intrusion of Basalt ...
www.itg.cam.ac.uk/people/heh/Paper83.pdf15 Sep 2006: magma layer. TABLE 2. The table lists the time (tj) at which the basalt layer becomes 60% crystalline and ceasesconvection for different basalt layer thicknesses. -
PII: 0198-0149(81)90135-7
www.itg.cam.ac.uk/people/heh/Paper41.pdf26 Sep 2011: tJ l,t,R. occupied with the failing conductivity cell and Stas S842 to 8853 with the r c p l a c c m e u resistor.
Search history
Recently clicked results
Recently clicked results
Your click history is empty.
Recent searches
Recent searches
Your search history is empty.