1.5. Fundamental Rheometry
Fundamental rheometry came into being with the pioneering work of G. W. Scott Blair – and it is characteristic that the material he used for his trials was a wheat dough (Schofield and Blair, 1932). This substance, that was initially a problem to the rheologists because of its "memory" (meaning the stored energy of its elastic behaviour), subsequently took rheometry and rheology a great step forward.

There is a relationship between conventional and fundamental rheometry. They use a similar deformation force, but in fundamental rheometry this is variable and therefore capable of describing the flow properties of a material under different loads or stresses in a test with a universal viscometer. The result is a flow curve, or stress strain curve, in which changes of stress are recorded over changes in strain. The stress in the curve is either the chosen deformation force, by which the change in strain is measured, or it is a measure of the resistance to deformation if the strain is varied under controlled conditions during the test. In both cases the viscosity is calculated from the two physical values stress and shear rate, and since the magnitude of the deformation force (measured area and force) and of the strain is defined, it is expressed in absolute physical units. These physical units permit a direct comparison of results from viscometers made by different manufacturers. Moreover, by calculating the viscosity, a flow curve can be "redrawn" as a viscosity curve (Fig. 61); the two types of curve yield the same information, and it is up to the person interpreting the results to choose the type of curve he prefers. The two types of curve show the flow properties of the substance tested; in particular they indicate any shear-dependent or time-dependent anomalies of flow behaviour that may occur in the test. The viscosity curve of a dough yields very important information on the rheological properties of the dough under different deformation forces. It shows that the dough has a yield point, and that its viscosity (consistency) falls as the load increases. This property is known as structural viscosity or shear-thinning and is caused and explained by the orientation of the molecules and aggregates in the flow field. It means that when exposed to only a low deformation force, such as stretching by the fermentation processes during the resting time, a dough has a higher viscosity than during transportation through the pipes or testing with the Farinograph or Extensograph (Fig. 61). This justifiably raises the question of how to describe the state of a dough at the low deformation forces in the process with a method that uses high deformation forces (Tanaka, et al., 1980). In other words: with high deformation forces it is only possible to determine the mechanical properties of the dough, not its rheological properties. A comprehensive work by several authors has been published on the subject of food rheology in general and the advantages of fundamental rheometry, including dough rheology, in particular. It deals with the importance of rheology for explaining and improving the quality of foods (Weipert and Tscheuschner, 1993).
Fig. 61: Stress strain curves of wheat flour doughs with different dough properties recorded with a rotational viscometer (left) and a viscosity curve showing "yield point" and "shear thinning" (right)
The deformation curve of an Extensogram and the stress strain curve are similar in appearance and take a similar course (Fig. 62). It is hoped that this fact will lead to greater acceptance of fundamental rheometry in cereal laboratories. There is no similarity to the Alveogram, since it is a pressure curve and not a deformation curve. If a ruler is placed behind the expanding dough bubble so that the increase in the size of the dough bubble can be measured, the resulting deformation curve made up of the measured points also shows similarity to the Extensogram.
Fig. 62: Comparison of recorded curves: Extensogram, Alveogram and stress-strain curve
1.5.1. Viscometer
The instruments used in rheometry differ in respect of their measuring principle, their mode of use and thus the presentation of the results. In rheometry the flow behaviour of a material is monitored between two parallel flat plates, in the circular gap between two coaxial cylinders, between two round parallel plates, between a cone and a plate or finally in a capillary tube. The rotational viscometers have shown themselves to have various advantages and are therefore the most widely used. A rotational viscometer determines the viscosity of a material in a simple test; in the measuring gap of the instrument the conditions are "stationary" and the flow is laminar. A relatively simple and therefore inexpensive viscometer makes it possible to record stress strain curves that reveal certain information about the dough. The yield point and the viscous properties of a dough can be read off from the shape and pattern of a stress strain curve and the (automatically) re-calculated viscosity curve. From the viscosity it is possible to determine the water absorption or the volume yield of the dough. The shape of the stress strain curve reveals the properties of the dough: a dough with short properties has a steep stress strain curve, whereas the curve of a dough with soft, weak properties is flatter (Fig. 61). And finally the stress strain curve makes it possible to assign a numerical value to the surface stickiness of a dough (Weipert, 1987a, 1992, 1998 and 1998b). So it is no wonder that such a method, which requires very little specimen material (10 g flour), is used successfully in the breeding of wheat (Fig. 61).

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