论文标题
从冷环颗粒中释放灰尘,作为土星环中辐条形成的机制
Dust release from cold ring particles as a mechanism of spoke formation in Saturn's rings
论文作者
论文摘要
土星环上的辐条是由尘土谷物组成的径向扩展的结构。尽管航天器和太空望远镜观测结果揭示了辐条的各种详细特征及其时间变化,但它们的形成机制仍在争论中。先前的模型检查了充电机制,以尝试解释从CM大小的环颗粒中释放灰尘。但是,这种尝试不成功,因为这种充电机制引起的静电力比在环环境中普通条件下作用于尘埃上的凝聚力要弱得多。在这里,我们提出了一个新型模型,以形成发言,其中凝聚的温度依赖性起着至关重要的作用。温度低于60K的环颗粒,可吸附一个O2环大气,这通过在早晨ANSA中降低了谷物和颗粒之间的凝聚力,从而促进了粉尘晶粒的释放。然后,在环颗粒的表面上产生了足以克服凝聚力的强烈静电力,并且释放的尘土晶粒形成了发出的结构。我们的模型解释了辐条的观察特征,包括它们的纵向位置,寿命,径向膨胀速度和季节性。
Spokes in Saturn's rings are radially-extended structures consisting of dust grains. Although spacecraft and space telescope observations have revealed various detailed features of the spokes and their time variation, their formation mechanism is still under debate. Previous models examined charging mechanisms to attempt at explaining dust release from cm-sized ring particles; however, the attempt has been unsuccessful, because the electrostatic force caused by such charging mechanisms is much weaker than the cohesive force acting on dust grains at ordinary conditions in the ring environment. Here we propose a novel model for the formation of the spokes, where the temperature dependence of cohesion plays an essential role. Ring particles with a temperature below 60K adsorb an O2 ring atmosphere, which facilitates release of dust grains from them by a reduction in the cohesive force between the grains and the particles on the morning ansa. Then, intense electrostatic forces sufficient to overcome the cohesive force are generated on the surface of ring particles and the released dust grains form the structure of spokes. Our model explains observational features of the spokes including their longitudinal location, lifetime, radial expansion velocity, and seasonality.