• Tidak ada hasil yang ditemukan

Directory UMM :Data Elmu:jurnal:E:European Journal of Mechanics _Fluids:Vol18.Issue4.1999:

N/A
N/A
Protected

Academic year: 2017

Membagikan "Directory UMM :Data Elmu:jurnal:E:European Journal of Mechanics _Fluids:Vol18.Issue4.1999:"

Copied!
10
0
0

Teks penuh

Loading

Gambar

Figure 1. Schematic of the liquid bridge in our experiment.
Figure 2. Schematic of experimental setup.
Figure 3. Evolution in time after turning off the potential difference of a castor oil bridge with a volume of 3 mm3 and a slenderness of � = 3.0.
Figure 4. Neck radius versus time for two different initial conditions at T = 22.8 ◦C: (+) �1 = 2.65 and τ1 = 1.01; (⋄) �2 = 3.0 and τ2 = 1.08
+3

Referensi

Dokumen terkait

Second, consistent with Hypothesis 3, we find support for both the alignment and the entrenchment effect after controlling for the monitoring performed by equity analysts, and we

In this paper, the creep constitutive equations of non-linear viscoelasticity equipped with temporal analogy have been developed to describe creep behaviour of metals

A first class involves all the mechanical models with Coulomb’s friction, and a second one involves all the other models: this last class contains all the models with a friction

We focused on two kinds of variables given as output by the CERES-Maize model; (a) final simulations of biomass, grain yield, yield components, maximum LAI and

drizzle fell to the ground with ice pellets and frozen drops on snow crystals. 2 The maximum size of supercooled drizzle particles increased as the depth of cloud layer saturated

It was found that using measured values to initialize the aerosol optical depth in the retrieval of surface global irradiance, the sur- face albedo increased by about 0.02 on

Comparison of stomatal NH3 compensation points determined on the basis of apoplastic NH4 + and H + concentrations (horizontal bars) and measured atmospheric NH3 concentrations ( d )

The vertical distribution of sources and sinks within the canopy is derived from direct measurements of both the NH 3 concentration profile and the turbulence within the canopy,