将新合成的元素注入原太阳云中

A. Boss, H. Vanhala
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引用次数: 12

摘要

在陨石中发现的富钙铝难熔包裹体中,短寿命放射性同位素26Al的初始丰度相对较高,这与太阳星云中辐照形成26Al的说法不一致,除非包裹体被挥发性更强的地幔屏蔽了辐射。26Al在恒星源(如超新星)中的核合成仍然是一个可能的替代解释,再加上新合成的26Al快速注入到原太阳云中。为了保留活的26Al,原太阳云必须在小于1兆热的时间内坍缩形成太阳星云。这些要求导致了超新星引发的原太阳云坍缩和超新星冲击波物质注入云的假设。星际激波与目标原太阳云相互作用的理论模型表明,一颗遥远的超新星既可以触发坍缩,又可以通过瑞利-泰勒指将大约10%的激波物质注入到云上。
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Injection of newly synthesized elements into the protosolar cloud
The relatively high initial abundance of the short–lived radioisotope 26Al in calcium–aluminium–rich refractory inclusions found in meteorites is inconsistent with forming the 26Al by irradiation in the solar nebula, unless the inclusions are shielded from irradiation by a more volatile mantle. Nucleosynthesis of the 26Al in a stellar source, such as a supernova, remains a likely alternative explanation, coupled with rapid injection of the newly synthesized 26Al into the protosolar cloud. In order to retain the live 26Al, the protosolar cloud must then collapse to form the solar nebula in less than 1 Myr. These requirements lead to the hypothesis of the supernova–triggered collapse of the protosolar cloud and injection of supernova shock wave material into the cloud. Theoretical models of the interaction of interstellar shock waves with target protosolar clouds show that a distant supernova can both trigger collapse and inject ca. 10% of the shock wave material incident on the cloud through Rayleigh–Taylor fingers.
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