不可分割行星科学新范式
New Indivisible Planetary Science Paradigm
摘要：
我在这里提出一个新的，不可分割的行星科学范式，太阳系物质性质的完全自洽的愿景，以及行星的动力学和能源。在高压高温下，巨大的气态原行星内部凝结和雨析形成的质量核行星。地球的完整凝结包括一个300个地球质量的巨大气体/冰壳，将岩石内核压缩到地球目前直径的66%。T-Tauri喷发剥离了内行星的气体，剥离了水星不完全凝聚的原行星的一部分，并将其运送到火星和木星之间的区域，在那里它与来自太阳系外部区域的氧化冷凝物融合，形成了普通球粒陨石的母物质，主带小行星，以及内行星，特别是火星的单板。为了应对减压驱动的行星体积增加，裂缝的形式，以增加表面积和山脉的折叠形式，以适应曲率的变化。内行星之间的差异主要是原行星压缩程度不同的结果。水星的内部成分是通过与地球类比来计算的。提供的理由是火星可能有一个更大的地下水库容量比以前实现。
英文摘要：
I present here a new, indivisible planetary science paradigm, a wholly self-consistent vision of the nature of matter in the Solar System, and dynamics and energy sources of planets. Massive-core planets formed by condensing and raining-out from within giant gaseous protoplanets at high pressures and high temperatures. Earth's complete condensation included a 300 Earth-mass gigantic gas/ice shell that compressed the rocky kernel to about 66% of Earth's present diameter. T-Tauri eruptions stripped the gases away from the inner planets and stripped a portion of Mercury's incompletely condensed protoplanet, and transported it to the region between Mars and Jupiter where it fused with in-falling oxidized condensate from the outer regions of the Solar System and formed the parent matter of ordinary chondrite meteorites, the main-Belt asteroids, and veneer for the inner planets, especially Mars. In response to decompression-driven planetary volume increases, cracks form to increase surface area and mountain ranges characterized by folding form to accommodate changes in curvature. The differences between the inner planets are primarily the consequence of different degrees of protoplanetary compression. The internal composition of Mercury is calculated by analogy with the Earth. The rationale is provided for Mars potentially having a greater subsurface water reservoir capacity than before realized.
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