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A new method for intrinsic viscosity measurements on perpendicular recording media

机译:在垂直记录介质上测量特性粘度的新方法

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摘要

Summary form only given. In the case of perpendicular media, it is hard to measure the magnetic viscosity S (from the relaxation curve) because the internal field (H/sub 1/) is continuously changing with time due to the change in the demagnetizing field. Correction for this effect using an analytical formula fails in principle to provide accurate results in case S varies largely with field. In this paper, we introduce a new method that allows to measure directly the intrinsic viscosity (S/sub i/) using a VSM. The measurement is carried out in a number of measurement steps. In each step, the applied field (H/sub a/) behavior with time is gradually adjusted according to the change in H/sub 1/ calculated from the relaxation behavior measured from the previous measurement step. Eventually, during the last step, H/sub 1/ is kept constant by appropriately changing H/sub a/. The ultimate viscosity obtained from the last step is the intrinsic viscosity at this constant H/sub 1/. Automatic measurements were carried out on two samples: a sputtered CoCrPtB perpendicular media and a Co-filled alumite media. Commonly, the ultimate S/sub 1/ for these types of samples can be obtained after 4 to 6 steps Throughout the steps the deviation of H/sub 1/ (from that at the start of the relaxation) goes asymptotically to zero and the viscosity increases and saturates at the ultimate value. The viscosity obtained using our method is believed to reflect better the real intrinsic viscosity of perpendicular media Moreover, we proposed a model that allows to simulate the measurements. The simulation fits quite well with our observations. With the model, we can understand and predict the behaviors of samples during the measurements. Using this model, we proposed away to make a "shortcut" in the real measurements. By using this "shortcut", even with high susceptibility samples, the ultimate viscosity value can still be obtained after a few steps.
机译:仅提供摘要表格。在垂直介质的情况下,由于去磁场的变化,内部磁场(H / sub 1 /)随时间连续变化,因此很难测量磁黏度S(根据弛豫曲线)。如果S随场变化很大,则使用解析公式对此效果进行校正原则上无法提供准确的结果。在本文中,我们介绍了一种允许使用VSM直接测量特性粘度(S / sub i /)的新方法。该测量是通过许多测量步骤进行的。在每个步骤中,根据从前一个测量步骤测量的松弛行为所计算出的H / sub 1 /的变化,逐渐调整随时间变化的施加场(H / sub a /)行为。最终,在最后一步中,通过适当地改变H / sub a /使H / sub 1 /保持恒定。从最后一步获得的极限粘度是该常数H / sub 1 /下的特性粘度。在两个样品上进行了自动测量:溅射的CoCrPtB垂直介质和Co填充的矾土介质。通常,这些类型的样品的最终S / sub 1 /可以在4到6个步骤后获得。在整个步骤中,H / sub 1 /的偏差(从松弛开始时的偏差)渐近为零,并且粘度增加并达到最终值。据信使用我们的方法获得的粘度可以更好地反映垂直介质的真实特性粘度。此外,我们提出了一个可以模拟测量值的模型。模拟与我们的观察非常吻合。使用该模型,我们可以了解和预测测量过程中样品的行为。使用该模型,我们建议在实际测量中创建一个“捷径”。通过使用这种“捷径”,即使对于高磁化率的样品,几步之后仍然可以得到极限粘度值。

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