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Nicol prism

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133: 36: 141: 304:-ray, is the more commonly used for further experimentation because it is again traveling in the original horizontal direction, assuming that the calcite prism angles have been properly cut. The direction of the upper ray, or 144:
Schematic representation of the propagation of light in a Nicol prism showing the splitting of unpolarized light into ordinary and extraordinary polarized rays
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Unpolarized light ray enters through the side face of the crystal, and is split into two orthogonally polarized, differently directed rays by the
132: 280:= 1.486) in the calcite crystal and is not totally reflected at the interface because it strikes the interface at a sub-critical angle. The 119: 57: 404: 100: 414: 361: 72: 53: 296:, undergoing another refraction, as it exits the opposite side of the prism. The two exiting rays have polarizations 250: 399: 79: 46: 309: 246: 165: 409: 389: 184: 340: 136:
Nicol prism at the Mineralogical Collection "Luigi Bombicci Museum" of the University of Bologna, in Bologna
86: 258: 293: 161: 68: 332:) is still used to refer to the observing of a sample placed between orthogonally oriented polarizers. 336: 394: 335:
In most instruments, however, Nicol prisms have been replaced by other types of polarizers such as
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at the glue interface, as well as a final refraction on exit from the upper side of the prism.
212: 173: 235: 93: 289: 261:
for the interface. It passes out the top side of the upper half of the prism with some
177: 383: 297: 223: 216: 169: 204: 200: 325: 35: 321: 308:-ray, is quite different from its original direction because it alone suffers 285: 262: 288:, or bending, as it passes through the interface into the lower half of the 188: 153: 17: 215:, cut again diagonally, and then rejoined, using a layer of transparent 140: 208: 157: 139: 131: 164:. It is made in such a way that it eliminates one of the rays by 183:
It was the first type of polarizing prism, invented in 1828 by
29: 211:) that has been cut at an angle of 68° with respect to the 27:
Optical polarizer made of two birefrengent calcite crystals
328:, and the term "using crossed Nicols" (abbreviated as 320:
Nicol prisms were once widely used in mineralogical
300:(at right angles) to each other, but the lower, or 60:. Unsourced material may be challenged and removed. 249:at the calcite–glue interface because of its 8: 273:-ray, experiences a lower refractive index ( 160:crystal used to convert ordinary light into 292:. It finally leaves the prism as a ray of 120:Learn how and when to remove this message 352: 245:= 1.658 in the calcite and undergoes a 7: 253:at the glue layer (refractive index 156:. It is an optical device made from 58:adding citations to reliable sources 25: 34: 284:-ray merely undergoes a slight 45:needs additional citations for 199:The Nicol prism consists of a 1: 176:is transmitted through the 172:is eliminated and only the 431: 360:Greenslade, Thomas B. Jr. 310:total internal reflection 247:total internal reflection 226:property of calcite. The 166:total internal reflection 145: 137: 294:plane-polarized light 257:= 1.550) exceeds the 162:plane polarized light 143: 135: 405:Polarization (waves) 341:Glan–Thompson prisms 234:-ray, experiences a 54:improve this article 415:Scottish inventions 251:angle of incidence 146: 138: 400:Optical materials 174:extraordinary ray 130: 129: 122: 104: 16:(Redirected from 422: 374: 373: 371: 369: 364:. Kenyon College 357: 236:refractive index 125: 118: 114: 111: 105: 103: 62: 38: 30: 21: 430: 429: 425: 424: 423: 421: 420: 419: 410:Prisms (optics) 390:1828 in science 380: 379: 378: 377: 367: 365: 359: 358: 354: 349: 318: 279: 244: 197: 187:(1770–1851) of 126: 115: 109: 106: 63: 61: 51: 39: 28: 23: 22: 15: 12: 11: 5: 428: 426: 418: 417: 412: 407: 402: 397: 392: 382: 381: 376: 375: 351: 350: 348: 345: 317: 314: 277: 259:critical angle 242: 207:(a variety of 196: 193: 128: 127: 42: 40: 33: 26: 24: 14: 13: 10: 9: 6: 4: 3: 2: 427: 416: 413: 411: 408: 406: 403: 401: 398: 396: 393: 391: 388: 387: 385: 363: 362:"Nicol Prism" 356: 353: 346: 344: 342: 338: 333: 331: 327: 323: 315: 313: 311: 307: 303: 299: 295: 291: 287: 283: 276: 272: 268: 267:extraordinary 264: 260: 256: 252: 248: 241: 237: 233: 229: 225: 224:birefringence 220: 218: 217:Canada balsam 214: 210: 206: 202: 194: 192: 190: 186: 185:William Nicol 181: 179: 175: 171: 167: 163: 159: 155: 152:is a type of 151: 142: 134: 124: 121: 113: 110:November 2018 102: 99: 95: 92: 88: 85: 81: 78: 74: 71: â€“  70: 69:"Nicol prism" 66: 65:Find sources: 59: 55: 49: 48: 43:This article 41: 37: 32: 31: 19: 366:. Retrieved 355: 334: 329: 319: 305: 301: 281: 274: 270: 266: 254: 239: 231: 227: 221: 213:crystal axis 205:Iceland spar 201:rhombohedral 198: 182: 170:ordinary ray 149: 147: 116: 107: 97: 90: 83: 76: 64: 52:Please help 47:verification 44: 339:sheets and 326:polarimetry 219:as a glue. 203:crystal of 168:, i.e. the 150:Nicol prism 18:Nicol Prism 395:Microscopy 384:Categories 368:23 January 347:References 322:microscopy 298:orthogonal 286:refraction 263:refraction 80:newspapers 195:Mechanism 189:Edinburgh 154:polarizer 337:polaroid 269:ray, or 230:ray, or 228:ordinary 209:calcite 158:calcite 94:scholar 265:. The 96:  89:  82:  75:  67:  290:prism 178:prism 101:JSTOR 87:books 370:2014 324:and 316:Uses 73:news 238:of 56:by 386:: 343:. 330:XN 191:. 180:. 148:A 372:. 306:o 302:e 282:e 278:e 275:n 271:e 255:n 243:o 240:n 232:o 123:) 117:( 112:) 108:( 98:· 91:· 84:· 77:· 50:. 20:)

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Nicol Prism

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polarizer
calcite
plane polarized light
total internal reflection
ordinary ray
extraordinary ray
prism
William Nicol
Edinburgh
rhombohedral
Iceland spar
calcite
crystal axis
Canada balsam
birefringence
refractive index

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