Water on The Moon, I. Historical Overview

A. Crotts
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引用次数: 8

Abstract

Abstract By mid-19th century, astronomers strongly suspected that the Moon was largely dry and airless, based on the absence of any observable weather. [1] In 1892, William H. Pickering made a series of careful occultation measurements that allowed him to conclude that the lunar surface’s atmospheric pressure was less than 1/4000th of Earth’s. [2] Any number of strange ideas arose to contradict this, including Danish astronomer/mathematician Peter Andreas Hansen’s hypothesis, that the Moon’s center of mass is offset by its center of figure by 59 kilometers, meaning that one or two scale-heights of atmosphere could hide on the far side of the Moon, where it might support water oceans and life. [3] Hans Horbiger’s 1894 Welteislehre (“World Ice”) theory, that the Moon and much of the cosmos is composed of water ice, became the favored cosmology of leaders of Third Reich Germany. [4] Respectable scientists realized that significant amounts of water on the Moon’s surface would rapidly sublime into the vacuum.
月球上的水,第一,历史概述
到19世纪中期,天文学家强烈怀疑月球基本上是干燥无空气的,因为没有任何可观测到的天气。[1] 1892年,威廉·h·皮克林进行了一系列仔细的掩星测量,得出月球表面的大气压力小于地球的1/4000的结论。[2]许多奇怪的观点都与此相矛盾,其中包括丹麦天文学家兼数学家彼得·安德烈亚斯·汉森的假设,他认为月球的质心与它的地心偏移了59公里,这意味着在月球的远端可能隐藏着一两个比例高度的大气层,那里可能存在水、海洋和生命。[3]汉斯·霍尔比格在1894年提出的“世界冰”理论认为,月球和宇宙的大部分都是由水冰组成的,这一理论成为德国第三帝国领导人青睐的宇宙论。[4]有名望的科学家们认识到,月球表面的大量水将迅速升华到真空中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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