Elsevier

Acta Materialia

Volume 52, Issue 8, 3 May 2004, Pages 2209-2220
Acta Materialia

Development of microstructure and texture of medium carbon steel during heavy warm deformation

https://doi.org/10.1016/j.actamat.2004.01.024Get rights and content

Abstract

The microstructure and texture development of a medium-carbon steel (0.36% C) during heavy warm deformation (HWD) was studied using scanning electron microscopy and electron back scattering diffraction. The spheroidization of pearlite is accelerated due to the HWD, which leads to the formation of completely spheroidized cementite already after the deformation and coiling at 873 K (600 °C). The homogeneity of the cementite distribution depends on the cooling rate and the coiling temperature. The cooling rate of about 10 K/s (ferrite–pearlite prior to HWD) and deformation/coiling at 943–973 K (670–700 °C) lead to a homogeneous cementite distribution with a cementite particle size of less than 1 μm. The ferrite softening can be attributed to continuous recrystallization. Even up to fairly high deformation/coiling temperatures of 983 K (710 °C) the texture consists of typical deformation components. During the continuous recrystallization the amount of high angle grain boundaries can increase up to 70% with a ferrite grain size of 1–3 μm. An increase of the cooling rate up to 20 K/s (ferrite–pearlite–bainite prior to HWD) deteriorates the homogeneity of the cementite distribution and the softening of ferrite in the final microstructure.

Introduction

After conventional hot rolling of medium carbon steel, a lamellar pearlite is formed during γ–α transformation. The lamellar morphology of pearlite leads to mechanical properties unsuitable for a further cold treatment or for application in highly demanding components. The globular morphology of cementite provides some benefits such as high toughness, good cold formability and machinability. For such purposes the cold strip must either undergo a long annealing treatment to obtain higher cold formability or it must be quenched with a subsequent tempering for a good combination of strength and toughness.

The use of a heavy warm deformation (HWD), performed below the γ–α transformation-temperature accelerates essentially the spheroidization of pearlite. The rate of this process is accelerated by a factor of 104 compared to annealing without deformation [1], [2]. But the spheroidized cementite itself cannot provide good mechanical properties. Other microstructural features like a homogeneous cementite distribution or ferrite condition, as well as the size of the cementite particles or the ferrite grains, influence the final mechanical properties. Therefore, a better understanding of the microstructure evolution during HWD is important for a successful introduction of such processing into the industrial production.

Section snippets

Material and experimental technique

A ferritic–pearlitic steel with a following composition in mass % was studied: 0.36% C, 0.53% Mn, 0.22% Si, 0.011% P and 0.002% S. The axially symmetric compression of samples with initial size 18 × 18 × 30 mm3 and plane strain compression of samples with an initial thickness of 60 mm, width of 50 mm and length of 45 mm, cut from an industrial slab, were carried out on the hot deformation simulator of the Max-Planck-Institute [3] with a strain rate of 10 s−1. This servohydraulic press is capable of

CCT diagram

The continuous cooling transformation diagram (Fig. 1) was established after an austenite deformation at 1173 K (900 °C). This temperature was determined by pre-tests to provide fine recrystallized austenite grains as an initial microstructure before the transformation.

The main differences between the microstructures produced with different cooling rates (initial microstructures for the subsequent HWD) were the amount of proeutectoid ferrite, the presence of bainite and the thickness of

Conclusions

  • 1.

    Spheroidization of pearlite during the HWD is accelerated by the formation of cementite lamellae kinks, fracture of lamellae and cementite subboundaries. Higher equilibrium carbon concentration in ferrite (higher carbon solubility) near these lamellae defects provokes a quick local dissolution of the lamella that leads to its division with a subsequent or simultaneous spheroidization.

  • 2.

    A rather homogeneous distribution of cementite in an initially ferritic–pearlitic microstructure can be observed

Acknowledgments

The authors express their gratitude to the financial support of the European Coal and Steel Community (ECSC).

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