对“土壤磁性剖面”的分异作了若干解释和讨论。
Some explanations and discussions about the differentiation of the "soil magnetic profile" were given.
色彩也可能是由一种被称作“磁扫”(magneticsweeping)的现象引起的，磁性粒子在土星磁场的作用下扫过土卫五，嵌入到土壤中。
The colors could also be caused by an effect called magnetic sweeping, in which charged particles in Saturn's magnetic field sweep over Rhea and become implanted in the soil.
本文利用土壤剩余磁性作为确定烃类渗漏带的参考系。
Remanent magnetism of soil layer is taken as a reference frame for locating hydrocarbon seepage zone.
层土壤的磁性与烃含量之间呈明显的相关特征。
Magnetism and hydrocarbon content of shallow soil show interrelated characteristics.
土壤磁化率剖面受纬度、土壤母质磁性本底、气候条件、土壤熟化度，及发育度、土壤颗粒等因子的影响。
It was observed that the magnetic susceptibility profile in soils related to the latitude, magnetic base of the parent materials, climatic condition, soil pedogenesis and ripening.
磁化率空间分布机理如下：首先，强烈的人为影响使土壤中磁性矿物人为来源占有重要地位。
The distribution mechanism of magnetic susceptibility as follows: first, magnetic minerals from human activity in soils play an important role;
微米级磁性矿物在黄土-古土壤序列中含量不足1%，为了满足多种测试的需要，要尽可能地富集磁性矿物。
Micron grade magnetic minerals are less than 1%of total minerals in the loess paleosol sequences. To satisfy requirements of a lot of kind of measurement, it needs to enrich the magnetic minerals.
微米级磁性矿物在黄土-古土壤序列中含量不足1%，为了满足多种测试的需要，要尽可能地富集磁性矿物。
Micron grade magnetic minerals are less than 1%of total minerals in the loess paleosol sequences. To satisfy requirements of a lot of kind of measurement, it needs to enrich the magnetic minerals.
应用推荐