依据这个新标度，原先的化学原子量数值只需作很小的变动。
The new scale required only minimal changes to the values that had been used for chemical atomic weights.
相应地，用R型因子分析法、单变量因子克立格法和多标度分形谱便能有效地实现地球化学场的分解。
And so, the methods of R-mode factor analysis, single-variate factor Krig-ing and multifractals are used in the present paper, to disperse the compounding geochemical field.
最后，指出了标度不变性原理在地球化学研究中的应用前景。
Finally, since geochemical laws can apply to various scales, and are scale-invariant, they should be treated with the modern concept of scale-invariance.
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