Science. 1981 Apr 10;212(4491):211-7. doi: 10.1126/science.212.4491.211.
Magnetic field studies by Voyager 1 have confirmed and refined certain general features of the Saturnian magnetosphere and planetary magnetic field established by Pioneer 11 in 1979. The main field of Saturn is well represented by a dipole of moment 0.21 +/- 0.005 gauss-R(s)(3) (where 1 Saturn radius, R(s), is 60,330 kilometers), tilted 0.7 degrees +/- 0.35 degrees from the rotation axis and located within 0.02 R(s) of the center of the planet. The radius of the magnetopause at the subsolar point was observed to be 23 R(s) on the average, rather than 17 R(s). Voyager 1 discovered a magnetic tail of Saturn with a diameter of approximately 80 R(s). This tail extends away from the Sun and is similar to type II comet tails and the terrestrial and Jovian magnetic tails. Data from the very close flyby at Titan (located within the Saturnian magnetosphere) at a local time of 1330, showed an absence of any substantial intrinsic satellite magnetic field. However, the results did indicate a very well developed, induced magnetosphere with a bipolar magnetic tail. The upper limit to any possible internal satellite magnetic moment is 5 x 10(21) gauss-cubic centimeter, equivalent to a 30-nanotesla equatorial surface field.
旅行者 1 号的磁场研究证实并完善了先驱者 11 号在 1979 年建立的土星磁层和行星磁场的某些一般特征。土星的主要磁场由一个磁矩为 0.21 +/- 0.005 高斯-R(s)(3)(其中 1 个土星半径,R(s),为 60,330 公里)的偶极子很好地表示,相对于旋转轴倾斜 0.7 度 +/- 0.35 度,位于行星中心 0.02 R(s) 内。在太阳下点处,磁层顶的半径平均为 23 R(s),而不是 17 R(s)。旅行者 1 号发现了土星的磁尾,直径约为 80 R(s)。这条尾巴远离太阳,类似于 II 型彗星尾巴以及地球和木星的磁尾。在泰坦(位于土星磁层内)非常近的飞越时(当地时间 1330 时)的数据显示,没有任何实质性的内在卫星磁场。然而,结果确实表明存在一个非常发达的感应磁层,具有双极磁尾。任何可能的内部卫星磁矩的上限为 5 x 10(21) 高斯-立方厘米,相当于 30 纳特斯拉的赤道表面场。