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用低频扭摆测量了经过轻度冷加工的Al-0.l%Mg合金在室温时效过程中的内耗变化,观察到表现反常振幅效应的时效内耗峯。用经过充分时效而内耗已达到稳定值的试样进行升温和降温内耗测量,也在30—55℃的温度范围内观察到表现反常振幅效应的温度内耗峯。这些现象在高纯铝试样和经过完全退火的Al-0.l%Mg合金试样中都不出现。在Al-0.l%Mg合金中也能观察到以前在Al-0.5%Cu合金中所观察到的反常内耗现象,这就排斥了任何用在点阵中所发生的一般脱溶沉淀过程来解释这种反常内耗现象的可能性,困为在含0.1%Mg的铝合金中,在实验测量所涉及的温度范围内,是不能够在点阵中发生一般的脱溶沉淀过程的。为了解释铝镁合金中所呈现的反常内耗现象的特点,可以假设在铝镁合金中能够形成两种位错气团:一种是“镁原子-空位”对与位错所组成的气团,这种气团能够在应变时效过程中形成;另一种气团是镁原子与位错所组成的气团,当经过范性形变的试样的温度升高到100℃左右时,镁原子与空位脱离,在退火过程中就单独与位错形成气团。前一种气团对于位错的钉札较第二种为强,因而它的振幅内耗峯出现在较高的振幅值。Variations of internal friction in the course of strain-aging at room temperature of slightly cold-worked Al-0.1% Mg alloy were measured with a torsion pendulum and an internal friction peak (versus aging time) exhibiting anomalous amplitute effect was observed. When the internal friction of a fully aged specimen was measured with the temperature going up and down, internal friction peaks (versus temperature) exhibiting anomalous amplitude effect were also observed in the temperature range of 30-55℃. These anomalous effects were not observed in specimens of high purity aluminum or fully-annealed Al-0.1% Mg alloy.The fact that these anomalous internal friction phenomena previously observed in Al-0.5% Cu alloy can also be observed in Al-0.1% Mg alloy excludes any possibility of explaining these anomalous internal friction phenomena in terms of a precipitation process which cannot occur in Al-0.1% Mg alloy in the temperature range of the present measurements.In order to explain the characteristics of the anomalous internal friction phenomena observed in the aluminum-magnesium alloy, two different types of dislocation atmospheres were assumed to be able to exist in an aluminum-magnesium alloy: One type is concerned with the segregation of "magnesium atom-vacancy" pairs to a dislocation, which can happen during the course of strain-aging; another type is concerned with the segregation of magnesium atoms to a dislocation, and these results when the cold-worked specimen was heated to a temperature around 100℃, at which temperature magnesium atoms were freed from the vacancies and so are able to form an atmosphere alone with a dislocation when the temperature is lowered. The pinning of a dislocation by an atmosphere of the former type is stronger than that of the latter, so that the amplitude internal friction peak associated with the former appeared at a higher amplitude level.
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