✔ 最佳答案
地心係點, 地質學家係斷估既, 就如天文學家估太陽表面溫度同有咩成分, 唔通有太空船上過去, 度過咩? 但就有好多間接既跡象, 例如光譜分析, 係可以測出個大概, 所以呢種斷估係一種educated guess, 有相當可信性, 但由於唔係直接量度, 所以仍有機會係錯既.
地質學家由物理定律開始, 例如引力, 可以斷定地球的重量, 除以量度出來的體積, 得出地球的平均密度為5515 kg/m3. 由於地殼度得出密度只有3000 kg/m3, 咁就可以推斷地球內部的密度一定會很高.
再用地震儀數據分析: 在發生地震的時候, 震波在不同時間不同方向到達各地的地震儀. 有些是地殼直接傳遞, 也有由地慢折射傳遞, 比較之下可得出地殼同地慢的密度比例, 又可得出不同深度的地慢的密度, 最後推斷地球核心的密度.
再加上大家都知道地球是一個大磁鐵, 在地面/海面的磁鐵(即指南針)都被地心的磁鐵控制住, 永遠指向南和北. 所以推斷地心的鐵成分一定很高, 就算不是鐵都是一些可以磁化的金屬如鎳. 但照密度計, 相信地心含有80%是鐵, 其餘是鎳和其他較輕的金屬.
不過如開頭所講, 推斷始終唔係量度, 所以當科學技術再進步, 有了新的測量方法, 可能推翻而家我地呢d推斷既結果. 係科學發展既歷史來睇, 一d人人都認為係既野後來比人推翻在, 一d都唔出奇.
參考維基百科:
http://en.wikipedia.org/wiki/Earth_core#core
Core
The average density of Earth is 5515 kg/m3, making it the densest planet in the Solar system. Since the average density of surface material is only around 3000 kg/m3, we must conclude that denser materials exist within Earth's core. Further evidence for the high density core comes from the study of seismology. In its earliest stages, about 4.5 billion (4.5×109) years ago, melting would have caused denser substances to sink toward the center in a process called planetary differentiation (see also the iron catastrophe), while less-dense materials would have migrated to the crust. As a result, the core is largely composed of iron (80%), along with nickel and one or more light elements, whereas other dense elements, such as lead and uranium, either are too rare to be significant or tend to bind to lighter elements and thus remain in the crust (see felsic materials).
Seismic measurements show that the core is divided into two parts, a solid inner core with a radius of ~1220 km and a liquid outer core extending beyond it to a radius of ~3400 km. The solid inner core was discovered in 1936 by Inge Lehmann and is generally believed to be composed primarily of iron and some nickel. Some have argued that the inner core may be in the form of a single iron crystal.[3][4] The liquid outer core surrounds the inner core and is believed to be composed of iron mixed with nickel and trace amounts of lighter elements. Recent speculation suggests that the innermost part of the core is enriched in very heavy elements, trans-cesium elements (above atomic number 55), this would include gold, mercury and uranium.[5]
It is generally believed that convection in the outer core, combined with stirring caused by the Earth's rotation (see: Coriolis effect), gives rise to the Earth's magnetic field through a process described by the dynamo theory. The solid inner core is too hot to hold a permanent magnetic field (see Curie temperature) but probably acts to stabilise the magnetic field generated by the liquid outer core.
Recent evidence has suggested that the inner core of Earth may rotate slightly faster than the rest of the planet.[6] In August 2005 a team of geophysicists announced in the journal Science that, according to their estimates, Earth's inner core rotates approximately 0.3 to 0.5 degrees per year relative to the rotation of the surface.[7][8]
The current scientific explanation for the Earth's temperature gradient is a combination of the heat left over from the planet's initial formation, the decay of radioactive elements, and the freezing of the inner core. Other theories include the georeactor theory.