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来自维基百科,自由的百科全书
基本频率(或简称 基频、fundamental frequency),当发声体由于振动而发出声音时,声音一般可以分解为许多单纯的正弦波,也就是说所有的自然声音基本都是由许多频率不同的正弦波组成的,其中频率最低的正弦波即为基音,而其他频率较高的正弦波则为泛音。[1][2][3]
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