A Treatise On Optics
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XXXII. POLARISING STRUCTURE OP ANALCIME. 2?7 dulation from d, the interval of retardation within the plate, to have the real difference of the intervals of re- tardation. Hence the two intervals of retardation will differ by a whole undulation; and consequently the colour produced when the plate B has been turned round 90, will be complementary to that which is produced when the plate B has the position shown in^. 135.
If we suppose the rays E and O to be received upon, and analysed by, a prism... of Iceland spar, we shall have two ordinary rays interfering to form the colours in one image, and two extraordinary rays interfering to produce the complementary colours in the other image.
CHAP. XXXIL ON THE POLARISING STRUCTURE OP ANALCIME.
(137. ) IN a preceding chapter I have mentioned the very remarkable double refraction which is possessed by anal- cime. This mineral, which is also called Cubizitf, has been regarded by mineralogists as having the cube for its primitive form ; but if this were correct, it should have exhibited no double refraction.
What to read after A Treatise On Optics?
You can find similar books in the "Read Also" column, or choose other free books by David Brewster to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
XXXII. POLARISING STRUCTURE OP ANALCIME. 2?7 dulation from d, the interval of retardation within the plate, to have the real difference of the intervals of re- tardation. Hence the two intervals of retardation will differ by a whole undulation; and consequently the colour produced when the plate B has been turned round 90, will be complementary to that which is produced when the plate B has the position shown in^. 135.
If we suppose the rays E and O to be received upon, and analysed by, a prism... of Iceland spar, we shall have two ordinary rays interfering to form the colours in one image, and two extraordinary rays interfering to produce the complementary colours in the other image.
CHAP. XXXIL ON THE POLARISING STRUCTURE OP ANALCIME.
(137. ) IN a preceding chapter I have mentioned the very remarkable double refraction which is possessed by anal- cime. This mineral, which is also called Cubizitf, has been regarded by mineralogists as having the cube for its primitive form ; but if this were correct, it should have exhibited no double refraction.
What to read after A Treatise On Optics?
You can find similar books in the "Read Also" column, or choose other free books by David Brewster to read onlineMoreLess
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