a$* TENTJMEN THEORIAE 



H-C(t-aD)£cof^+D;cofH(i-aB)(i-aC)(i-aD)^ 

 -4-aB(i-aC)(i— aD)^r-HaC(i— -aDJ-^-HaD.-^— ■* 



39. Ponatur porro ad abbreuiandum : 



/~7~:z:i-aA=z3{ ; <?~zz 1 -aBzz$& 



* "zzi-aCzzC. * ' zzi-aDzz® 

 tum vero : 



p- f ; j* _ $ ; 6* zz J); et ,♦ =r t ent 



A% ■£ S/j-_B£9g C0 Al_±_C ® *> co/. Yj ; + D i co/. 1 ~ ? ^. 5?«!5-£ 25 j 



V — 1 — *£2)f — aBC2)8— aCSJ -eDi 



vbi ^-f-^cof.^-h^cof. -v)4-^cofJ eft altitudo aquae 

 fupremae AA fupia orificium EE. 



40. Si omnes poteftates ipfius a praeter primam 

 negligamus , reperiemus .: 



-,a^cof.^( 2 ^+4^ 

 -*dcdM.(£ j 



ct fi nulla plane eflet fri&io, ieu azzo, foret; 



— ° -*- & co/. £ -4- «9)^4- d co/. 



*? — - T=Z1 " 



vnde pofita tota altitudine A\ — q, erit y—f-/—-r-*- 4 



41. In tranfitu hic obfemo , f_ ampiitudo vafis 

 fupremi fit maxima prae amplitudine orificii , forc v~q t 

 feu celeritatem effluxus in EE debitam cfTe altitudini 

 Alzz^, Yti per confueta principia conitat. Sin autem 



ampli. 



