Tackifi ers and Antimisting Additives 359
a viscoelastic approach. Prokunin [9], using the idea of relaxation of liquid–solid transition [10],
developed the theory further, considering the free jet withdrawn from viscoelastic solution as a pure
elastic gel. He found a good comparison between his calculations and experiments in Ref. 8. These
results were later reviewed in a monograph [7]. The experimental and theoretical results in Refs 8
and 9 described, however, only the stationary processes of withdrawal of free viscoelastic jets by a
rotating drum, where the constant speed of withdrawal and the ow rate of the uid were controlled
by the speed of drum rotation. Additionally, the experiments [8,9] were conducted on concentrated
water solutions of very high-molecular-weight PEO with a polymer volume concentration of 0.5%.
Thus, to analyze and describe the withdrawal of viscoelastic jets of very dilute polymer solutions
in the nonstationary sucking open siphon process, the previously developed stationary theory [7,9]
has to be modi ed.
It should also be mentioned that the problem of withdrawal of viscoelastic liquids seems similar
to the withdrawal of viscous liquids by a vertically moving at (or cylindrical) plate. In this prob-
lem, a viscous liquid forms a thin layer near the rigid plate under the action of viscosity, gravity, and
surface tension. The solution of the problem mastered by Landau and Levich [10,11] uses a match-
ing condition between viscous ow and static meniscus. Despite seeming similarity between these
two problems, withdrawing of polymer solutions from a free surface is more complicated because
the radius of extendable jet, varied with height, is a priori unknown.
This chapter is organized as follows. Section 13.2 describes the experimental setup, pro-
cedures, and the uids used in experiments. Section 13.3 introduces some basic facts of vis-
coelasticity known for polymeric liquids. Section 13.4, using a quasisteady approach, modi es
the theory [7,9] in the nonsteady case of the open siphon with sucking device and applies it to
very dilute polymer solutions. Section 13.5 discusses the quantitative experimental ndings and
describes the data using the theory of Section 13.4. Section 13.6 applies the open siphoning
method for evaluations of tackiness in two different lubricant oils. Concluding remarks are given
in Section 13.7.
13.2 EXPERIMENTAL SETUP, PROCEDURES, AND FLUIDS
The experimental device used for testing tackiness of lubricating uids is similar to those described
in Refs 5 and 6. The setup is explained in Figure 13.1 in which the glass tube (capillary) with an
inner diameter of 1.58 mm and a length of 120 mm is connected to the common vacuum equipment.
In the experiments, we used three values of vacuum pressures p
v
equal to 68, 77.3, and 84 kPa. The
graduated glass cylinder (jar) lled with a tested uid was of inner diameter 28 mm and height
190 mm. To quantify the jet pro les, we used the Konica Minolta A4 camera and computer, equipped
with Adobe Photoshop CS2 program for enlarging pictures of the jet.
The experimental procedure was as follows. The capillary was lowered in the jar lled with the
tested liquid, so that the lower sucking end of the capillary was initially below the liquid surface.
Then the capillary was held in the position as shown in Figure 13.1. The suction pulled the liquid
into the capillary and lowered the level of liquid in the jar. The experiment began at the moment
when falling liquid surface in the jar reached the lower end of the capillary. Starting from this
moment, a free jet of a tacky liquid was formed. The siphon draws down the level of liquid in the
jar, increasing the length of free jet and making it progressively thinner. Flow rate q measured by
graduated jar was dependent on applied vacuum; the higher the vacuum the higher was the ow rate.
At small ow rates, the jet was broken, and at large enough ow rate, the jet lost its axial symmetry
and the ow rate oscillated with time. We chose the aforementioned range of vacuum pressure to
prevent breakage and high oscillation. But even in this range we observed some sporadic oscilla-
tions of the jet. Because of this, we repeated each measurement three times, recording an average
value for calculations. The photos of the jets shown in Figures 13.2a and 13.2b demonstrate a very
important characteristic feature of the jet, a relatively large viscoelastic meniscus near the free
surface. Some traces of instability are also seen in the gures.
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