## Materials Research

##
*Print version* ISSN 1516-1439*On-line version* ISSN 1980-5373

### Mat. Res. vol.10 no.3 São Carlos July/Sept. 2007

#### http://dx.doi.org/10.1590/S1516-14392007000300003

**Assessement of tensile strength of graphites by the Iosipescu coupon test**

**Luis Guilherme Borzani Manhani ^{I}; Luiz Claudio Pardini^{II, *}; Flamínio Levy Neto^{III}**

^{I}Centro Técnico Aeroespacial, Depto. Eng. Aeronáutica e Mecânica, Instituto Tecnológico de Aeronáutica – ITA, 12228-900 São José dos Campos - SP, Brazil

^{II}Centro Técnico Aeroespacial, Instituto de Aeronáutica e Espaço – IAE, Divisão de Materiais – AMR, 12228-904 São José dos Campos - SP, Brazil

^{III}Universidade de Brasília, Departamento de Engenharia Mecânica – UnB/FT/ENM, 70910-900, Brasília - DF, Brazil

**ABSTRACT**

Polycrystalline graphites are widely used in the metallurgical, nuclear and aerospace industries. Graphites are particulated composites manufactured with a mixture of coke with pitch, and changes in relative proportions of these materials cause modifications in their mechanical properties. Uniaxial tension tests must be avoided for mechanical characterization in this kind of brittle material, due to difficulties in making the relatively long specimens and premature damages caused during testing set-up. On other types of tests, e.g. bending tests, the specimens are submitted to combined stress states (normal and transverse shear stresses). The Iosipescu shear test, is performed in a beam with two 90° opposite notches machined at the mid-length of the specimens, by applying two forces couples, so that a pure and uniform shear stress state is generated at the cross section between the two notches. When a material is isotropic and brittle, a failure at 45° in relation to the beam long axis can take place, i.e., the tensile normal stress acts parallel to the lateral surface of the notches, controls the failure and the result of the shear test is numerically equivalent to the tensile strength. This work has evaluated a graphite of the type used in rocket nozzles by the Iosipescu test and the resulted stress, ~11 MPa, was found to be equal to the tensile strength. Thus, the tensile strength can be evaluated just by a single and simple experiment, thus avoiding complicated machining of specimen and testing set-up.

**Keywords: **polycrystalline graphites, mechanical properties, tensile strength, shear strength, weibull modulus

**1. Introduction**

Synthetic graphites are widely used in many engineering applications, such as those in the metallurgical, nuclear and aerospace industries, and as electrodes for ion-lithium batheries^{1}. They are manufactured using a blend of coke and pitch in different proportions. Graphites can be classified according to the raw material as coarse, medium or fine grain, and depending on their processing technique as extruded or molded grades^{2}. This will lead to microstructures characterized as being anisotropic in the case of extruded grades and isotropic in the case of molded grades. During processing, heat treatment temperature lead to changes in mechanical and thermal properties. If the constituent phases, coke and binder coke have different properties, and the properties of the graphite are different from properties of the constituents, then graphites can be recognized as a particulated composites. Due to their excellent thermo-mechanical properties and low density (<2 g.cm^{-3}) graphites are suitable for use as high temperature components.

Mechanical properties, such as tensile strength, flexural strength, shear strength, among others, are commonly used to characterize materials which will give their mechanical finger-printing. These test methods are acceptable for determining design allowables, for comparative purposes and also for quality control. The test data depends on the test method, specimen design, fabrication method, and microstructure^{3}. Among all the mechanical tests that are used to characterize materials the uniaxial tension test should be avoided, particularly for brittle materials, which is the case of graphites, due to difficulties in making the relatively long specimens (they are prone to fail during machining) and possible damages caused during testing set-up. In some other types of tests, e.g. bending tests, the specimens are submitted to combined stress states, i.e. simultaneous normal and transverse shear stresses, and the results for strength and modulus can be misleaded. Although there are many test methods to measure shear properties of materials, still none of them are ideal for introducing real pure shear stresses in the specimens. This difficulty must be overcome by materials scientists involved in the development and characterization of materials.

The most uniform and pure shear-stress state can be achieved in a material by applying torsional loading to a thin-walled tube specimen. However, this kind of specimen is usually expensive to be produced and the testing procedure is not straightforward, because buckling failure along ±45° can take place. In the early sixties, N. Iosipescu, from Romania, developed a simple test to determine shear strength and shear modulus for metals, but the first published work in English language appeared only in the late sixties^{4,5}. Since then, the new in-plane shear test procedure was known as Iosipescu shear testing and the use of the new testing methodology was soon applied to isotropic and anisotropic materials, when the first reports appeared in the early seventies. A lot of research has been accumulated in this specific testing procedure because it is simple to perform, requires small and easily fabricated specimens, and enables very accurate and reproducible results for shear modulus and shear strength^{6,7}. Since then, Iosipescu shear test has became very popular for the determination of shear strength and shear modulus for a broad range of materials^{8}.

In the Iosipescu specimen a pure transverse shear stress state occurs in the cross section between the two 45° opposite notches machined at the mid-length of the specimen (points a and c in Figure 1). By applying two forces couples that generate two opposite bending moments, a pure shear stress state is generated between two notches of the beam, as shown by the external force, shear-force and bending-moment diagrams of Figure 1. According to the Mohr circle diagram corresponding to this resulting stress state that acts in the specimen, the principal normal stresses act parallel to the lateral surface of the notches (i.e at 45° with respect to the longitudinal direction of the specimen, x). If the failure occurs perpendicular to this direction, which is caused by a principal normal tensile stress its value can be used to evaluate tensile strength. This behavior is typical for brittle materials in which the deformations as well as the distortions are particularly small, up to the failure load, and eventual geometric changes during the tests are negligible. Finite-element analysis of the test configuration has been object by several authors to investigate the influence of stress distributions and for validation of the Iosipescu test^{6,9}.

Cracks and pores are common features that are found in graphite microstructure. These defects are, in fact, undesirable structural parameters that significantly reduces the mechanical properties of the material, mainly the tensile strength. Since they can not be avoided, these microstructural features and the inherent brittleness of graphites gives rise to an appreciable scatter in the results of strength properties. Weibull distribution statistics is currently a well established statistical tool to evaluate the significant variability of the mechanical test results which takes place in brittle materials and will be applied to the data collected from the Iosipescu shear test.

**2. Experimental**

*2.1. Material*

The graphite used in the work was provided by SGL Carbon Ltd - USA, trade name HLM 85. It is extruded in ~20 cm cylinder blocks. The apparent density of HLM graphite is 1.73 g.cm^{-3.} All the sample specimens were taken parallel to extrusion direction.

Optical microscopy was carried out in a Leica DM RxP optical microscope. The amount of porosity was analysed by mercury intrusion porosimetry in a Autoscan-33 Quantachrome Porosimeter. Surface of the fractured specimens were analysed by an Oxford Leo 435 Vpi scanning electron microscope. The HLM 85 graphite is suitable for use at high temperature applications and it is extensively used as rocket nozzle throat inserts.

*2.2 Tensile test*

Tensile tests were performed on HLM graphite, with the applied load parallel to extrusion direction, following procedure described in the ASTM C 749 Standard by using the Instron universal testing machine^{10}. Dimensions of the tensile coupon are shown in Figure 2 and the cross head speed was set at 0.5 mm/min. Longitudinal and transverse strains were measured by using 90° rosette FCA-I-23 strain gages from Tokyo Sokki Kenkyujo Co. Ltd, attached at center of the specimen, Equation 1, using the experiemental values of the transverse and the longitudinal strains (e), as following:

*2.3. The Iosipescu test set-up*

The Iosipescu shear specimens were machined and the test was performed according to ASTM D 5379M standard, using an Instron 4301^{11}. As for the tensile coupons, the Iosipescu shear specimens were machined parallel to the extrusion direction (x) of the graphite cylinders, as seen in Figure 3. Thirty two identical specimens were tested to failure. The cross head speed was 0.5 mm/min. The average shear stress, in the region where the shear force V = P is maximum, is defined by the Equation 2^{12}:

where: P = applied load; d = distance between roots of notches (segment from a to c in Figure1); and t = specimen thickness.

The sketch of the strain-gage position in the Iosipescu specimen is show in Figure 3. During testing a pure shear loading is generated in the zero bending moment section of the beam and the shear stress has its maximum value at the cross section ac. To prevent non-perpendicularity of fixture-sample contacts to the Iosipescu rig, all specimens were machined with 13 mm thickness, following suggestion of Pierron^{6}. Strain-gages of the type 90° rosette FCA-I-23, from Tokyo Sokki Kenkyujo Co. Ltd were properly attached to in the samples, as shown in Figure 3.

*2.4. Weibull modulus*

The Weibull modulus from the Iosipescu shear results was calculated. The determination of Weibull modulus (m) considers the assumption of a constant volume for all samples tested, and the results is a straight line equation, when plotting experimental failure stress values (s) as a function of cumulative probability of failure (P), according to Equation 3^{13} :

where s_{o} is the intrinsic strength of the material, which corresponds to a stress level associated with a probability of failure of about 73% (or a survival probability of 37%).

The Weibull modulus (m) corresponds to the inclination of a straight line which is obtained by plotting lnln (1/(1 – P) as function of ln s. When the failure stresses (s_{i}) are ranked from the highest to the lowest results, the probability of failure from an intermediate position (P_{i}), corresponding to the i-th observation, is given by P_{i/}=/i/N/+/1, where N is the number of samples. The Weibull modulus (m) is obtained by linear regression. The Weibull modulus is a parameter that can indicates the level and how homogeneous is the distribution of the failure stresses (s_{i}) in a material. Ductile materials, in which the defects are reduced and homogeneously distributed, present a high Weibull modulus (e.g. m = 100, for an annealed SAE 1020 steel), whereas for brittle materials m is low (e.g. m @ 5, for carbon fibers). So, the lower is the scatter in the failure stresses, the higher is the Weibull modulus of a material.

**3. Results and Discussion**

The Figure 4 shows a typical optical micrography of a polished surface of the HLM graphite. HLM graphite is formed by a binder phase and elongated needled-coke grains. As a consequence HLM graphite is anisotropic in nature. A broad range of pores and microcracks can be found in the microstructure and they are represented by the dark areas in Figure 4. The reflection interference colors in graphites shows that the binder phase contains regions of common basal plane orientation and they exhibits a broad variation in size and shape. This is the case for HLM 85 graphite. A typical size of these anisotropic components is ~125 µm, which is in the range of 1-500 µm as described by Forest and Marsh^{14}. In fact, the initial medium grain size for this graphite from manufacturer's data sheet is 0.8382 mm.

Mercury intrusion porosimetry shows that a 12% open pore volume is present in the HLM graphite. The IUPAC boundary for mesopores and macropores is at pore radius ~25 µm. The pore distribution size is broad, ranging from 1-2 to 250 µm, as shown in Figure 4.

As any other ceramic-like material, the mechanical properties for graphites are mainly influenced by raw materials (grain size and distribution, porosity, viscosity, etc), processing conditions and preferred orientation of crystallites. Figure 5 shows plots of the tensile stress as a function of strain for the tensile coupons in the direction parallel to extrusion (x, which corresponds to the sample long axis). The stress-strain curves are non-linear, and they show that elastic modulus decrease with an increase in stress. The average for tensile strength (with the corresponded standard deviation) was 10.9 ± 2.1/MPa, and deformation up to failure was 0.2 ± 0.05%.

Data for Young's modulus were calculated from the slope of the initial part of the stress-strain curve, which was taken up to ~2 MPa, resulting in 11.5 ± 0.9 GPa. Longitudinal strain was 0.0962 ± 0.05 and transverse strain was –0.018 ± 0.006 resulting in a Poisson's ratio of 0.187. These data confirms figures for tensile strength and elastic modulus found in literature and manufacturer's data, which are in the range 8-12 MPa^{15}. Tensile coupons failed sharply at the value of maximum stress, in two pieces within the gage length region.

Typical shear stress-strain curves are given in Figures 6 and 7. The curves are reasonably quadratic. Figure 8 shows a curve for shear stress, calculated from Equation 2, as a function of strain for the Iosipescu shear testing. As for tensile stress-strain curve, the shear stress-strain curve is also non-linear, and the stress grows monotonically up to maximum when an abrupt decrease in strength related to brittle failure occurs. The measured shear stress up to failure of the HLM graphite, calculated from Equation 2, was 11.7/±/1.7/MPa. At the peak stress the average deflection of the specimen was 0.75/±/0.09/mm, which corresponds to a strain to failure of 0.38/±/0.04%. Shear modulus calculated in the elastic region of the shear stress-strain curve resulted in a value of 3.02 ± 0.6 GPa.

The Iosipescu test procedure states that pure shear stress should occurs in the ac section (Figure 1) leading to a failure in between notch tips and shear strength can be calculated by Equation 2. However, as could be seen in Figure 9, the failure mode after Iosipescu shear testing for the HLM 85 happened in a 45° inclination in relation to the applied forces.

Early work carried out by Taylor^{16} on mechanical properties of reactor graphites found a shear strength in the range of 22-33 MPa, measured by the double shear apparatus. The tensile strength reported in the same work was in the range of 10.7-14.0 MPa, giving a tensile strength/shear strength ratio of ~0.5. It is obvious that an incongruence exists on results for shear strength found by Taylor and in the present work. Also, the failure mode does not correspond to a pure shear failure mode (which, in such situation, should de parallel to the line between the notches, ac, in Figure 3).

To explain the results and behavior found in this work during Iosipescu shear test it is necessary the help of mechanics of materials. A general Mohr circle diagram, as shown in Figure 10, represents all the possible normal (s) and shear (t) stresses, along any direction, for a typical bi-dimensional (2-D) stress state in a point of a material. Thus, we can apply this concept in the notch region of the Iosipescu shear speciment. From the concepts of materials mechanics, in the planes associated with the points Q and P in the Mohr circle, where the normal stresses assume their maximum (s_{1}) and minimum (s_{2}) values, respectively, the shear stresses are zero. These planes are the principal planes and the normal stresses at them are the principal stresses, defined as s_{1} and s_{2} at the points P and Q, respectively^{17}.

Due to the fact that in the circle of Mohr presented in Figure 10, the magnitudes of the principal normal stresses are identical to the maximum shear stresses (in particular,s_{1} = _{max} and s_{2} = –t_{max}) and, in addition, the principal directions 1 and 2 are coincident to orientations of the strain gauges 1 and 2, in Figure 3 (SG1 and SG2), respectively. The shear stress-strain plots indicate that tensile stresses are normal to the upper left hand side V-notch, corresponding to the SG1 strain-gage deformation. On the other hand, compressive stresses are normal do the lower right hand side V-notch face, corresponding to the SG2 strain-gage deformation. In the Mohr circle, the stresses s_{1} and s_{2} can be obtained by the Equations 4 and 5, as following:

where s_{1} and s_{2} are mathematically the maximum and minimum principal normal stresses.

The maximum shear stress in a point can be expressed by Equation 6, as following :

Subtracting Equation 4 from Equation 5, Equation 7 is obtained:

As a result Equation 8 can be obtained as following :

The Mohr circle of Figure 10 refers to a general 2-D stress state. However, in the region between the notches (ac, in Figure 3), in particular, there is pure shear along the directions x and y, and so s_{x} = s_{y} = 0 (as shown in the Mohr circle of Figure 11, at point A), it is clear from Equations 4 and 6 that:

During Iosipescu shear testing, depending on the direction which is considered, components of normal and shear stress are present in the region (ac) between notches. The principal normal stresses are located at ±45° relatively to the longitudinal direction (x) of the specimens and they act parallel (or perpendicular) to the specimen notch lateral surfaces, according to Figures 3 and 9. In addition, along the directions x and y there is pure shear, according to Figure 1, and a failure occurring perpendicular to the direction –45° (º SG1), as shown in Figure 9 will take place with the same stress value obtained from Equation 2, due to the fact that s_{1} = t_{max}, according to Equation 9.

As stated earlier, for a ductile material, the failure mode for the Iosipescu specimen in pure shear would correspond to a fracture at the cross section, and the tensile strength would be higher than the shear strength. The Morh circle construction in Figure 11 shows that the shear force applied to the specimen coupon leads to a state of pure shear (t_{xy} = t_{yx}) in the cross section. So, if the material is ductile, the failure plane would be in the plane of maximum shear. However, since graphite is a brittle and porous material and its tensile strength is low, the failure will occur perpendicular to the direction 1 (º SG1) where the tensile stresses are maximum. The fracture surface is at an angle of 45° with the cross-sectional plane of the specimen, as shown schematically in Figure 11. So, the brittle failure mode of the specimen at 45° (Figure 9) to the *ac* section (Figure 1), indicates pure tension failure occurring and the result from Equation 2 is in fact the longitudinal tensile strength of the material. Thus, if the failure is perpendicular to the principal normal stresses the value of shear strength, determined by Iosipescu shear, as in Equation 2, would be approximately the tensile strength determined from standard static tensile tests. Working with a particular polymer composite materials made of epoxy resins and glass microspheres, D´Almeida^{18} found a similar fracture pattern for the failure mode tested by Iosipescu apparatus, and the equivalence between values for Iosipescu shear stress at failure and tensile strength of the tested material. Brittle failure mode under shear testing was also observed for this material.

All failure models for graphites recognize the key role of pores during initiation of fracture when graphite is stressed^{10,20,21}. Pores in graphites are mainly in the coke particles or as crack-like porosity which is embedded in binder material. The cracks tend to lie either in regions of well-orientated binder phase material or along the interfaces between the filler particles and the binder. Similarly to other particulate composites, graphite fracture mechanisms and crack development can mainly take part in the matrix or breaking through the particle themselves, or even splitting the interfaces between binder and particles^{22}. It is not easy to determine at each stress level one specific mechanism is more likely to occur than the other. Moreover, shear stresses can also lead to deformation of pores during testing. In any case fractured graphites surfaces exhibit a coarse microstructure, as it can be seen in shear failure region of Figure 12.

According to Tucker^{21}, crack development occurs by various means. It starts from pre-existing defects and can propagates by means of crystallite cleavage linking with another pores and other cracks, and by splitting the interfaces between binder and particles or by breaking through the particles themselves, region A seen in Figure 12. As a result subcritical defects form randomly throughout the material, increasing in size and density as the load is applied until failure occurs. Shear stresses can also induce sliding of basal planes within well-oriented structures developing fracture cleavage of crystallites. Cleavage is more likely to occur in pore-free regions.

Unlike metals and plastics, graphites exhibit the presence of a large number of inhomogeneities, such as cracks and voids, due to their manufactured process. These features causes an appreciable scatter in the maximum failure strength values which is a consequence of the probability to find the critical defect. This critical defect is the one that is the most favourable to crack propagation, and causes failure, as a function of its position in relation to load direction. Defects in materials are randomly distributed and it is necessary to use statistical tools to cope with the variability in properties of these class of materials.

The Weibull distribuition is one of the most used statistical tools for materials that exhibit brittle failure and a probabilistic distribution of defects. Moreover, because it provides a probabilistic description the theory behind the Weibull distribution recognises the inherent variability in graphite strength due to the complexites of its microstructure. The Weibull plot for HLM graphite calculated from shear data is shown in Figure 13. A sample batch over twenty five gives a consistent Weibull modulus value^{22}. The Weibull modulus "m" found for maximum shear stress from 32 tested HLM graphite samples was ~8,5. This value is in between those of glass fibers (m =10) and carbon fibers (m = 5), which are also brittle materials** ^{23}**.

By testing over a hundred samples of HLM graphite having various cross-sections from different batches under flexure loading, Muller^{24} found a similar value for the Weibull modulus (m = 9) which is a very close to the result that was found in this work. It is worth to mention that the present work used several samples from the same graphite block, whereas in Muller's work the samples were taken from regular block production of a certain size, over a time of one year.

**4. Conclusion**

This work reported an easy shear test used for graphites. The calculated shear strength of HLM graphite was 11.7 MPa. The graphite failure mode showed a 45° crack in between the notch section. Graphite is nearly macroscopically isotropic and exhibit low strain to failure. Mohr's circle for the Iosipescu shear coupon shows that principal normal stresses (s_{1} = t_{max}) are laid perpendicular to the fracture surface and, as a consequence, act parallel to the lateral surface of the notches. This situation is caused by a pure normal stress tensile state, and the shear failure test could be used to evaluate the tensile strength of a brittle material. In resume, Iosipescu shear testing is a useful tool to estimate, with a good accuracy, the tensile strength of graphites. Shear fracture surface is coarse and rather jagged because the crack propagation has to penetrate into the coarse structure of graphite. Weibull modulus for HLM graphite taken from maximum shear strength values is m = 8.5, which is typical for common ceramic materials.

**Acknowledgments**

The authors thanks to FAPESP, Proc. Nº 00/04359-3.

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Received: August 2, 2006; Revised: August 3, 2007

* e-mail: lpardini@vivax.com.br