地球物理学进展
地毬物理學進展
지구물이학진전
PROGRESS IN GEOPHYSICS
2009年
5期
1561-1565
,共5页
地球外核%磁感应强度%电荷密度
地毬外覈%磁感應彊度%電荷密度
지구외핵%자감응강도%전하밀도
the Earth's outer core%magnetic induction%electric charge density
为计算地球磁极处的磁感应强度,建立地球的磁场是由带电的地球外核的旋转产生的模型.先根据毕奥-萨伐尔定律计算球形模型绕自转轴旋转时在自转轴直径上产生的磁感应强度;再利用已知的地球外核的内外半径及地球半径和磁极处的磁感应强度值,计算出地球外核的电荷体密度及面密度.结果表明:若外核的电荷呈均匀的体密度分布,则其电荷体密度为3.5507 C/m~3;若外核的电荷均匀分布在外核的外表面,则其面密度为2.4581×10~6C/m~2.通过地球表面的磁感应强度信息利用物理规律和地球物理数据推测地球内部难以直接进行探测的相关信息,具有实际意义.根据地震学方法对地球外核厚度、转向等变化的最新研究数据按该文模型可推测地球磁场强度、极性等的变化.而地球磁场的变化对地球上的人类生活颇有影响.
為計算地毬磁極處的磁感應彊度,建立地毬的磁場是由帶電的地毬外覈的鏇轉產生的模型.先根據畢奧-薩伐爾定律計算毬形模型繞自轉軸鏇轉時在自轉軸直徑上產生的磁感應彊度;再利用已知的地毬外覈的內外半徑及地毬半徑和磁極處的磁感應彊度值,計算齣地毬外覈的電荷體密度及麵密度.結果錶明:若外覈的電荷呈均勻的體密度分佈,則其電荷體密度為3.5507 C/m~3;若外覈的電荷均勻分佈在外覈的外錶麵,則其麵密度為2.4581×10~6C/m~2.通過地毬錶麵的磁感應彊度信息利用物理規律和地毬物理數據推測地毬內部難以直接進行探測的相關信息,具有實際意義.根據地震學方法對地毬外覈厚度、轉嚮等變化的最新研究數據按該文模型可推測地毬磁場彊度、極性等的變化.而地毬磁場的變化對地毬上的人類生活頗有影響.
위계산지구자겁처적자감응강도,건입지구적자장시유대전적지구외핵적선전산생적모형.선근거필오-살벌이정률계산구형모형요자전축선전시재자전축직경상산생적자감응강도;재이용이지적지구외핵적내외반경급지구반경화자겁처적자감응강도치,계산출지구외핵적전하체밀도급면밀도.결과표명:약외핵적전하정균균적체밀도분포,칙기전하체밀도위3.5507 C/m~3;약외핵적전하균균분포재외핵적외표면,칙기면밀도위2.4581×10~6C/m~2.통과지구표면적자감응강도신식이용물리규률화지구물리수거추측지구내부난이직접진행탐측적상관신식,구유실제의의.근거지진학방법대지구외핵후도、전향등변화적최신연구수거안해문모형가추측지구자장강도、겁성등적변화.이지구자장적변화대지구상적인류생활파유영향.
For calculation of the magnetic induction at the Earth's magnetic pole, a model of the rotation of the Earth's outer core has been established. According to Biot-Savart law, the magnetic induction at the diameter position of the spin axis is calculated. Furthermore, using the internal and external radius of the Earth's outer core as well as the radius of the Earth and the magnetic induction at the Earth's magnetic pole, the volume charge density and surface charge density of the Earth's outer core have been obtained. Results show that the charge density is 3. 5507 C/m~3 for uniform volume distribution. The charge density is 2. 4581 × 10~6 C/m~2 for uniform surface distribution. The information of the Earth's interior can be inferred by surface magnetic induction and its physical laws as well as earth physical data. It is practical because the information is difficult measured directly. New dada about the thickness, deflect of the Earth' s outer core obtained by seismological methods can reveal the varieties of the earth magnetic intensity and the polarity. Variations of the earth magnetic field affects much the human being on the earth.