Ness N F, Acuña M H, Burlaga L F, Connerney J E, Lepping R P, Neubauer F M
Science. 1989 Dec 15;246(4936):1473-8. doi: 10.1126/science.246.4936.1473.
The National Aeronautics and Space Administration Goddard Space Flight Center-University of Delaware Bartol Research Institute magnetic field experiment on the Voyager 2 spacecraft discovered a strong and complex intrinsic magnetic field of Neptune and an associated magnetosphere and magnetic tail. The detached bow shock wave in the supersonic solar wind flow was detected upstream at 34.9 Neptune radii (R(N)), and the magnetopause boundary was tentatively identified at 26.5 R(N) near the planet-sun line (1 R(N) = 24,765 kilometers). A maximum magnetic field of nearly 10,000 nanoteslas (1 nanotesla = 10(-5) gauss) was observed near closest approach, at a distance of 1.18 R(N). The planetary magnetic field between 4 and 15 R(N) can be well represented by an offset tilted magnetic dipole (OTD), displaced from the center of Neptune by the surprisingly large amount of 0.55 R(N) and inclined by 47 degrees with respect to the rotation axis. The OTD dipole moment is 0.133 gauss-R(N)(3). Within 4 R(N), the magnetic field representation must include localized sources or higher order magnetic multipoles, or both, which are not yet well determined. The obliquity of Neptune and the phase of its rotation at encounter combined serendipitously so that the spacecraft entered the magnetosphere at a time when the polar cusp region was directed almost precisely sunward. As the spacecraft exited the magnetosphere, the magnetic tail appeared to be monopolar, and no crossings of an imbedded magnetic field reversal or plasma neutral sheet were observed. The auroral zones are most likely located far from the rotation poles and may have a complicated geometry. The rings and all the known moons of Neptune are imbedded deep inside the magnetosphere, except for Nereid, which is outside when sunward of the planet. The radiation belts will have a complex structure owing to the absorption of energetic particles by the moons and rings of Neptune and losses associated with the significant changes in the diurnally varying magnetosphere configuration. In an astrophysical context, the magnetic field of Neptune, like that of Uranus, may be described as that of an "oblique" rotator.
美国国家航空航天局戈达德太空飞行中心与特拉华大学巴托尔研究所合作,在“旅行者2号”航天器上进行的磁场实验发现,海王星存在强大而复杂的固有磁场以及相关的磁层和磁尾。在超声速太阳风气流中,在距离海王星34.9个海王星半径(R(N))处上游探测到分离的弓形激波,在行星 - 太阳连线附近26.5 R(N)处初步确定了磁层顶边界(1 R(N) = 24,765千米)。在最接近时,即距离为1.18 R(N)处,观测到最大磁场近10,000纳特斯拉(1纳特斯拉 = 10^(-5)高斯)。在4至15 R(N)之间的行星磁场可以用一个偏移倾斜磁偶极子(OTD)很好地表示,该磁偶极子从海王星中心偏移了惊人的0.55 R(N),并相对于自转轴倾斜47度。OTD偶极矩为0.133高斯 - R(N)^3。在4 R(N)范围内,磁场表示必须包括局部源或高阶磁多极子,或两者都有,目前尚未完全确定。海王星的倾角及其在交会时的自转相位偶然地结合在一起,使得航天器在极尖区几乎正好指向太阳时进入磁层。当航天器离开磁层时,磁尾似乎是单极的,未观测到嵌入磁场反转或等离子体中性片的穿越。极光区很可能远离自转轴,并且可能具有复杂的几何形状。海王星的环和所有已知卫星都深深嵌入磁层内部,除了海卫二,当它位于行星向太阳一侧时在磁层外部。由于海王星的卫星和环对高能粒子的吸收以及与日变化磁层构型的显著变化相关的损失,辐射带将具有复杂的结构。在天体物理学背景下,海王星的磁场与天王星的磁场一样,可被描述为“倾斜”旋转体的磁场。