# Appendix A: Exercise

Series | Geophysical References Series |
---|---|

Title | Digital Imaging and Deconvolution: The ABCs of Seismic Exploration and Processing |

Author | Enders A. Robinson and Sven Treitel |

Chapter | 1 |

DOI | http://dx.doi.org/10.1190/1.9781560801610 |

ISBN | 9781560801481 |

Store | SEG Online Store |

**1. Find the equal-time curve for reflection and the one for refraction.**

To illustrate the elegance of Huygens’ principle (Huygens, 1690^{[1]}, second, third, and fourth paragraphs of Chapter 6), we repeat his demonstration verbatim:

“To proceed then to these figures [Figure A-1 for reflection and Figure A-2 for refraction], let us suppose first that it is desired to find a surface *CDE* which shall reassemble at a point *B* rays coming from another point *A*; and that the summit of the surface shall be the given point *D* in the straight line *AB*. I say that, whether by reflection or by refraction, it is only necessary to make this surface such that the path of the light from the point *A* to all points of the curved line *CDE*, and from these to the point of concurrence (as here the path along the straight lines *AC*, *CB*, along *AL*, *LB*, and along *AD*, *DB*), shall be everywhere traversed in equal times, by which principle the finding of these curves becomes very easy.

“So far as relates to the reflecting surface, since the sum of the lines *AC*, *CB* ought to be equal to that of *AD*, *DB*, it appears that *DCE* ought to be an ellipse; and for refraction, the ratio of the velocities of waves of light in the media *A* and *B* being supposed to be known, for example that of 3 to 2 (which is the same, as we have shown, as the ratio of the sines in the refraction), it is only necessary to make *DH* equal to 3/2 of* DB*; and having after that described from the center *A*, some arc *FC*, cutting *DB* at *F*, then describe another from center *B* with its semi-diameter *BX* equal to 2/3 of *FH*; and the point of intersection of the two arcs will be one of the points required, through which the curve should pass. For this point, having been found in this fashion, it is easy forthwith to demonstrate that the time along *AC*, *CB*, will be equal to the time along *AD*, *DB*.

“For assuming that the line *AD* represents the time which the light takes to traverse this same distance *AD* in air, it is evident that *DH*, equal to 3/2 of *DB*, will represent the time of the light along *DB* in the medium, because it needs here more time in proportion as its speed is slower. Therefore the whole line *AH* will represent the time along *AD*, *DB*. Similarly the line *AC* or *AF* will represent the time along *AC*; and *FH* being by construction equal to 3/2 of *CB*, it will represent the time along *CB* in the medium; and in consequence the whole line *AH* will represent also the time along *AC*, *CB*. Hence it appears that the time along *AC*, *CB*, is equal to the time along *AD*, *DB*. And similarly it can be shown if *L* is another point in the curve *CDE*, that the times along *AL*, *LB* are always represented by the line *AH*, and therefore equal to the said time along *AD*, *DB*.”

## References

- ↑ Huygens, C., 1690, Traité de la Lumière [Treatise on Light, in which are explained the causes of that which occurs in reflection and in refraction, and particularly in the strange refraction of Iceland Crystal]: The Hague. Republished by Macmillan and Company, London, 1912.

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## Also in this chapter

- Introduction
- Wavefronts and raypaths
- d’Alembert’s solution
- One-dimensional waves
- Sinusoidal waves
- Phase velocity
- Wave pulses
- Geometric seismology
- The speed of light
- Huygens’ principle
- Reflection and refraction
- Ray theory
- Fermat’s principle
- Fermat’s principle and reflection and refraction
- Diffraction
- Analogy