研究人员开发了一种研究地球核心的新的模拟方法,有可能解释其磁场和推进AI技术。 Researchers developed a new simulation method to study Earth's core, potentially explaining its magnetic field and advancing AI tech.

研究人员开发了一种新的模拟方法,称为分子流动力学,将分子和旋转动力学结合起来,以便在高压和高温条件下研究地球核心。 Researchers have developed a new simulation method called molecular-spin dynamics, combining molecular and spin dynamics to study Earth's core under high-pressure and high-temperature conditions. 这一方法揭示了磁力是如何影响铁原子的 并且可以解释地球核的效应。 This method reveals how magnetism affects iron atoms and could explain the geodynamo effect. 这一技术还可推动材料科学的进步,包括提高AI和更快的数据储存技术的效率。 The technique could also drive advancements in materials science, including more efficient AI and faster data storage technologies.