427 



greement may perhaps be due to the changes elsewhere, inci- 

 dent to rising winter floods. 



SUMMARY. 



Phelps Lake is the richest in plankton of all the localities 

 examined by us, averaging 19.65 cm.'' per m.^ the mean of all 

 collections, or 22.35 cm.^ the mean of the monthly averages. 

 This is 8- fold the production in the river and more than twice 

 that in any other impounding area examined. We find, how- 

 ever, that the lake does not contribute to the river at levels be- 

 low 8 ft., and is therefore cut off for a considerable part of the 

 time. In the years 1894-1899 inclusive, the days of run-off 

 were 14, 0, 71, 139, 145, and 86 days respectively, or an average 

 of 76 days. As a rule the plankton content of the lake waters 

 during periods of run-off exceeds that in the channel in varying 

 degrees, and the lake by virtue of the impounding function 

 serves to increase the plankton content of channel waters. The 

 exceptions fall mainly at levels above 10 ft., when the diluent 

 action of Spoon River floods affects the production in the lake. 

 The high records of production which indicate the great rela- 

 tive and absolute fertility of this body of water are in the main 

 found during summer and autumn months, when there is no 

 discharge and the impounding function is at its maximum. 

 This is conflrmatory evidence of the effect of impounding when 

 the disturbing factor of tributary water is absent and coarse 

 vegetation is of little extent. Owing to its small area, its early 

 separation from the channel, and its relation to Spoon River at 

 high levels, the total contributions from this area are relatively 

 small as compared with those from Thompson's and Flag lakes, 

 and at times from Quiver Lake, and its relative fertility during 

 nioitJis of ynn-off, as compared with these localities, is wont to 

 rise above their level of production, especially at stages be- 

 tween 8 and 10 ft., when run-off' is slight and impounding 

 function dominant. Illustrations of this will be found in the 

 monthly averages of 1897 and 1898 in April-June, the sea- 

 son of greatest run-off, when 4 of the 6 monthly averages 



