FREE BOOKS

Author's List




PREV.   NEXT  
|<   113   114   115   116   117   118   119   120   121   122   123   124   125   126   127   128   129   130   131   132   133   134   135   136   137  
138   139   140   141   142   143   144   145   146   147   148   149   150   151   152   153   154   155   156   157   158   159   160   161   162   >>   >|  
to which the velocity of the planet varies. The adjoining figure (Fig. 39) shows a planetary orbit, with, of course, the sun at the focus S. We have taken two portions, A B and C D, round the ellipse, and joined their extremities to the focus. Kepler's second law may be stated in these words:-- "_Every planet moves round the sun with such a velocity at every point, that a straight line drawn from it to the sun passes over equal areas in equal times._" [Illustration: Fig. 39.--Equal Areas in Equal Times.] For example, if the two shaded portions, A B S and D C S, are equal in area, then the times occupied by the planet in travelling over the portions of the ellipse, A B and C D, are equal. If the one area be greater than the other, then the times required are in the proportion of the areas. This law being admitted, the reason of the increase in the planet's velocity when it approaches the sun is at once apparent. To accomplish a definite area when near the sun, a larger arc is obviously necessary than at other parts of the path. At the opposite extremity, a small arc suffices for a large area, and the velocity is accordingly less. These two laws completely prescribe the motion of a planet round the sun. The first defines the path which the planet pursues; the second describes how the velocity of the body varies at different points along its path. But Kepler added to these a third law, which enables us to compare the movements of two different planets revolving round the same sun. Before stating this law, it is necessary to explain exactly what is meant by the _mean_ distance of a planet. In its elliptic path the distance from the sun to the planet is constantly changing; but it is nevertheless easy to attach a distinct meaning to that distance which is an average of all the distances. This average is called the mean distance. The simplest way of finding the mean distance is to add the greatest of these quantities to the least, and take half the sum. We have already defined the periodic time of the planet; it is the number of days which the planet requires for the completion of a journey round its path. Kepler's third law establishes a relation between the mean distances and the periodic times of the various planets. That relation is stated in the following words:-- "_The squares of the periodic times are proportional to the cubes of the mean distances._" Kepler knew that the diffe
PREV.   NEXT  
|<   113   114   115   116   117   118   119   120   121   122   123   124   125   126   127   128   129   130   131   132   133   134   135   136   137  
138   139   140   141   142   143   144   145   146   147   148   149   150   151   152   153   154   155   156   157   158   159   160   161   162   >>   >|  



Top keywords:

planet

 

velocity

 

distance

 

Kepler

 

periodic

 

distances

 

portions

 

varies

 

planets

 

average


ellipse

 

stated

 

relation

 
elliptic
 

constantly

 

changing

 
enables
 
points
 

compare

 

stating


Before

 

movements

 
revolving
 

explain

 

quantities

 

greatest

 

requires

 

defined

 

number

 

completion


journey

 

meaning

 

distinct

 

attach

 

proportional

 

establishes

 

finding

 

simplest

 

called

 

squares


Illustration

 

passes

 

greater

 
travelling
 

shaded

 

occupied

 

straight

 

planetary

 
adjoining
 
figure