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The attraction of the pyramids: virtual realization of Hutton's suggestion to improve Maskelyne's 1774 Earth?density estimate

机译:金字塔的吸引力:虚拟实现Hutton的建议,改善Maskelyne1774的地球?密度估计

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Charles Hutton suggested in 1821 that the pyramids of Egypt be used to site an experiment to measure the deflection of the vertical by a large mass. The suggestion arose as he had estimated the attraction of a Scottish mountain as part of Nevil Maskelyne's (1774) "Schiehallion Experiment", a demonstration of Isaac Newton's law of gravitational attraction and the earliest reasonable quantitative estimate of Earth's mean density. I present a virtual realization of an experiment at the Giza pyramids to investigate how Hutton's concept might have emerged had it been undertaken as he suggested. The attraction of the Great Pyramid would have led to inward north–south deflections of the vertical totalling 1.8?arcsec (0.0005°), and east–west deflections totalling 2.0?arcsec (0.0006°), which although small, would have been within the contemporaneous detectable range, and potentially given, as Hutton wished, a more accurate Earth density measurement than he reported from the Schiehallion experiment.
机译:Charles Hutton于1821年建议,埃及金字塔用于现场实验,以测量垂直的偏转。由于他估计了苏格兰山区作为尼维尔·帕罗斯尼(1774)“Schiehallion实验”的一部分的吸引力,这是ISAAC牛顿的引力吸引法和最早合理定量估算地球平均密度的展示。我在Giza金字塔上展示了一个实验的实验,调查Hutton的概念如何出现,因为他的建议是在进行的。伟大金字塔的吸引力导致垂直总计1.8的向内南北偏转(0.0005°),以及总计2.0的东西偏转(0.0006°),虽然很小,但已经在其中当Hutton希望的时期,潜在的可检测范围,并且可能给予,比他从Schiehallion实验报告的地球密度测量更准确。

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