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9 Mar 2004: Of course, at large t, say 1/β = 200, the difference must belarge since all the particles are expected to have settled out, while the homogeneouscurrent maintains its density excess.).

9 Mar 2004: 1. Geological Fluid Mechanics. By Herbert E. Huppert. (Received 6 February 2000). 1. The Earth. Since antiquity there has been consideration and speculation about the Earth on which. we live. How did it form; how does it evolve; how can its riches

9 Mar 2004: J. Fluid Mech. (2002), vol. 472, pp. 333–371. c 2002 Cambridge University PressDOI: 10.1017/S0022112002002379 Printed in the United Kingdom. 333. Polydisperse particle-driven gravity currents. By T H O M A S C. H A R R I S1, A N D R E W J. H O G

26 Mar 2023: Surface of saturating freshwater. Saline water. 200 cm. 25 cm. Control. ... 4. Experimental analysis. We conducted a series of laboratory experiments in a narrow acrylic tank of length 200 cm,height 25 cm and width 1 cm (figure 3).

26 Sep 2011: It is elongated with a length of 20 km al o n g 020 to 200:, a width of 6 km, and rises 470 m above the plain.

8 Jun 2012: 4. 5. 6. 7. 8. z (mm). H (. mm. ). 100 50 0 50 1000. 50. 100. 150. 200. z (mm). ... Lower Cross slope velocity profilesfor the same experiments. 0 50 100 150 200.

16 Jul 2010: DENSI T Y. I00. ß. 200' Tf S. 250 -. 350 40 0 • z::::::::::::::. ::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::: ... 27 150 34.572 - 1.52 -2.01 0.49 1.0284421 1.0284568 147 11 29 200 34.637 - 1.73

19 Jul 2010: The layer was nominally 150 mm deep and was contained in a Perspex box of a 200 mm x 200 mm cross section. ... Again we used water/glycerine mix- tures which we introduced at the surface of a nominally 200 mm layer contained in the 200 mm x 200 mm

14 Apr 2010: a) (b). 500. 0. 500. distance (km). 0 200 400 600 800 1000 12000.8. ... 50. 100. 150. 200 020. 40. 0. Figure 4. Results from an example calculation with variations in basal depth in the y-directionas described by equation (3.1), with α =

19 Jul 2010: IO]. Finally, in Section 4, we describe the eflects of cooling and crystallizing a gradient of sodium carbonate, fat which Pr = 7 and Le = 200.

26 Apr 2006: The mushy layer starts to grow more slowlythan predicted by the theory after about 200 minutes. ... This is likely to be an indirectconsequence of the brine expulsion which begins at about 200 minutes, as shown infigure 6.

28 Jul 2006: as to be expected, the figure is much lower for the 200 journals with highest cumulative impact.

18 Jan 2007: The cell is moved by aSmartdrive Taranis stepper motor having microstep resolution of 51 200 steps perrevolution and 0.88 Nm holding torque, coupled with a 100/1 gearbox.

21 Mar 2016: 4. |Q| (. m/s. ). 10-3. 0 200 400 600 800 1000t (s). ... 0 50 100 150 200. 2. 2.5. 310-3. |Q|. (ms. 1).

26 Mar 2023: H.K. Moffatt, H. Guest and H.E. Huppert. 50 100 150 200 250. ... 1.0. 0.5. 50 100 150τ. â(τ). â8(τ. ). 200 250 300 50 100 150.

17 Jan 2019: In this apparatus, two Hele-Shaw cells (in-ternal dimensions 200 ( 50 ( 3 mm3) were arranged side by sideabove a fixed copper chill through which coolant (ethanol glycol)was circulated from

8 May 2007: 100 150 200 250 300. M (g). t (s). l = 50 cml = 100 cm. ... 0. 50. 100. 150. 200. 250. 300. 100 150 200 250t (min).

25 Jan 2007: 121. 43. 42. -. - x x. 39 I I I I 0 50 100 150 200 250. ... 1. 1 I50. T W). 1125. 1100. L I 0 200 400 600 800 1000 1200 1400.

9 Feb 2004: particle size, experiments were run with four different initial par-ticle masses of 50 g, 100 g, 200 g and 400 g suspended in 2 litresof water. ... U (cm s-1)0 5 10 15 20 25 30. 0. 200.

30 Oct 2015: Inlet. Outlet. Glycerine. 200 cm. Air6 cm 14 cm. FIGURE 10. ... predictions. Our experiments were performed in a Hele-Shaw cell composed of twoacrylic sheets, each 200 cm long and 14 cm high (see figure 10) and spacing w 0.38

8 May 2007: 0 1 2 3 4 5 6 7 8 9 100.200.250.30.