FREE BOOKS

Author's List




PREV.   NEXT  
|<   167   168   169   170   171   172   173   174   175   176   177   178   179   180   181   182   183   184   185   186   187   188   189   190   191  
192   193   194   195   >>  
chiefly used there, the ice is frequently renewed by flooding with water at the close of the day. It thus never gets so very cold as on the lakes. I have been on ice in North France, which, in the early morning, was too hard to afford sufficient bite for comfort. The cause of this is easily understood from what we have been considering. We may now return to the experimental results which we obtained early in the lecture. The heavy weights slip off the ice at a low angle because just at the points of contact with the ice the latter melts, and they, in fact, slip not on ice but on water. The light weights on cold, dry ice do not lower the melting point below the temperature of the ice, _i.e._ below -10 deg. C., and so they slip on dry ice. They therefore give us the true coefficient of friction of metal on ice. This subject has, more recently been investigated by H. Morphy, of Trinity College, Dublin. The refinement of a closed vessel at uniform temperature, in which the ice is formed and the experiment carried out, is introduced. Thermocouples give the temperatures, not only of the ice but of the aluminium sleigh which slips upon it under various loads. In this way we may be certain that the metal runners are truly at the temperature of the ice. I now quote from Morphy's paper 281 "The angle of friction was found to remain constant until a certain stage of the loading, when it suddenly fell to about half of its original value. It then remained constant for further increases in the load. "These results, which confirmed those obtained previously with less satisfactory apparatus, are shown in the table below. In the first column is shown the load, _i.e._ the weight of sleigh + weight of shot added. In the second and third columns are shown, respectively, the coefficient and angle of friction, whilst the fourth gives the temperature of the ice as determined from the galvanometer deflexions. Load. Tan y. y. Temp. 5.68 grams. 0.36+-.01 20 deg.+-30' -5.65 deg. C. 10.39 -5.65 deg. 11.96 -5.75 deg. 12.74 -5.60 deg. 13.53 -5.65 deg. 14.31 -5.65 deg. 15.10 grams. 0.17+-.01 9 deg..30'+-30' -5.60 deg. 16.67 -5.55 deg. 19.81 -5.60 deg. 24.52
PREV.   NEXT  
|<   167   168   169   170   171   172   173   174   175   176   177   178   179   180   181   182   183   184   185   186   187   188   189   190   191  
192   193   194   195   >>  



Top keywords:

temperature

 

friction

 

weights

 

results

 
obtained
 
weight
 

coefficient

 

Morphy

 

constant

 

sleigh


loading

 

confirmed

 

apparatus

 

satisfactory

 

previously

 

original

 

suddenly

 
remained
 

increases

 

remain


column
 
columns
 

determined

 

galvanometer

 

deflexions

 

fourth

 

whilst

 
Trinity
 

return

 

experimental


understood

 
comfort
 

easily

 
lecture
 

contact

 

points

 
sufficient
 
flooding
 

renewed

 

frequently


chiefly

 

afford

 

morning

 

France

 

introduced

 

Thermocouples

 
temperatures
 

carried

 
experiment
 

vessel