Access the full text.
Sign up today, get DeepDyve free for 14 days.
The Physical Basis of Pitch and Loudness.—In general, our auditory sensations are due to the occurrence of sound waves in the external air. These waves vary in length, in amplitude, and in form. Other things being equal, the shorter the wave length (i.e. the greater the vibration frequency) the higher in pitch will be the auditory sensation ; and the greater the amplitude (i.e. the more distant the crest or trough of a wave from the position of equilibrium) the louder or more intense will be the auditory sensation. But these relations are only broadly true. For, as we shall see, the pitch and the loudness of our sensations do not always correspond to the wave length and the amplitude of the objective stimuli. The Conduction of Sounds to the Inner Ear.—Sounds which are of moderate pitch and loudness are led to the inner ear by the membranes and ossicles of the middle ear. It has been experimentally shown that the ossicles vibrate with a frequency dependent on the vibration frequency of the sound stimulus, and that they must consequently be regarded, not as a fixed conducting rod, but as a jointed, freely vibrating chain. The Conduction of Sounds from Ear to Ear.—Direct bone conduction also occurs when a sounding instrument, e.g. a tuning-fork, is brought in contact with the head or teeth (exp. 15). It is likewise a factor of considerable psychological importance when a sound is led to one ear only (exp. 16); for unless the sound be low in pitch and intensity, it travels to the opposite ear, partly perhaps by way of the two Eustachian tubes across the pharynx, but chiefly over the bony vault and across the base of the skull. (PsycInfo Database Record (c) 2023 APA, all rights reserved)
Published: Feb 13, 2012
Keywords: sound conduction; auditory sensations; vibration frequency; wave length; frequencies; inner ear; sound perception; pitch; loudness; hearing ability; ear mechanisms; bone conduction
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.