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9 Apr 2013: thermomolecular pressuregradient that provides a force to cleave the soil and make wayfor a new ice lens.To our knowledge, no quantitative experimental tests of. ... By setting a portion ofeach sample aside in a test tube, we observed

5 Jan 2006: 2.3. Results. 2.3.1. Ballotini in water. In order to test the thermal behaviour of the experimental tank and heating system,a preliminary experiment (1) was conducted using a ... bars with Perspex equivalents, but this emphasizes the care necessary in

18 Jul 2014: At the In Salah test site in Algeria, CO2 isinjected roughly 2 km into a porous sandstone layer containing ambient salt water,forming a relatively shallow porous layer with a typical

30 May 2006: This line of argument seems highly questionable because, using the homogeneous flow over a flat-topped cylinder as a special test case, we indi- cated in the previous section that in

20 Nov 2014: In order to test the predictiveability of our model in terms of sea-ice growth and salt fluxes, we compare its results with measurementsfrom laboratory experiments in section 3. ... 1997], not because they are necessarilybetter, but because they were

9 Mar 2004: Numerical tests indicated that this artificial term affected thedistance of propagation by less than 1% in the cases presented below. ... On the other hand, tests(not shown here) indicate that the direct use of the τTML values as the ‘correct’ones

26 Apr 2006: A test of the ice thickness algorithm using labora-tory experiments in which the growth rate is measured inde-pendently. ... To test when natural sea ice suffers thisinstability, we also plotted the buoy-derived values of f# andhDS on Figure 7a.

21 Mar 2016: Here we aim to clarify thelarge-scale dynamics and test the scaling argument ofHindmarsh (2012); therefore, it is necessary to use valuesthat are representative of the large-scale dynamics.The 20km

23 Dec 2021: However, these models neglect interfacialdeformation, and experiments performed to test the models show that spheres settle towards aninterface slightly faster than predicted [28].

19 Jul 2010: medium. To test our analytical results westudy models of diapirism in the Great Kavir, Iran. ... To test whether a perfectly plastic overburden can explain thedifferent spatial characteristics of the salt province, in this sectionwe analyze models of the

9 Mar 2004: A test of the ice thickness algorithm using labora-tory experiments in which the growth rate is measured inde-pendently. ... To test when natural sea ice suffers thisinstability, we also plotted the buoy-derived values of f# andhDS on Figure 7a.

18 May 2017: 3s2 7s) m[(1/4)(3s2 7s), s]. mψ [(1/4)(3s2 7s), s]. (5.25). To test the accuracy of the solution for ψ given by (5.25), it is

14 Sep 2009: and (iii) the ability to test different, nonlinear constitutive laws for per-meability. ... There are important components of our simulations that are not validated by these two tests, including our treatment ofthe advection of solute and our success in

26 Apr 2006: 4. Model Results. 4.1. Model Results for a Laboratory Experiment. [23] To test the model for the idealized diffusive case,governed by equations (1)–(5), we simulated the experi-ment

9 Feb 2004: of. 3. Experiments. 3.1 Experimental arrangements. To test the validity of our results and to evaluate the relationshipbetween and U, we conducted a series of experiments in a 9.4Um

1 Jun 2006: I n chapter six, the workbook methods are applied to several field tests and actual industrial accidents as examples of how to use the workbook in practice. ... The authors are careful t o point out deficiencies in current theories of interfacial

23 Dec 2021: Young’s modulus Ewas calculated from two different methods, compression tests and sphericalindentation, and the fluid viscosity µ was measured using a u-tube viscometerbefore every experiment.

14 Sep 2009: 2.3. Experimental Techniques. [15] Measurements of the temporal and spatial evolutionof the salinity profile in sea ice are needed in order to obtaindata sets against which to test analytical and

9 Mar 2004: 2001). The objectives are (a) to test the ability of the numerical solver to provideresults for the stratified ambient, and (b) to obtain additional data for the verificationof the present SW

30 Oct 2015: Inclined gravity currents filling basins: The influence of Reynolds number onentrainment into gravity currentsCharlie A. R. Hogg, Stuart B. Dalziel, Herbert E. Huppert, and Jörg Imberger Citation: Physics of Fluids 27, 096602 (2015); doi: