a ™„„i„» Btream ; it only ™e. in .niEcient qn.ntity lo wet th, porous body When the hqma 

 JZZ:, » now supply rises np. But Ihis can only Lie place to a , cry Imnted height. If the 



''Th:t onTp'o^cTTnumcrated is a still n,orc feeble one. Tl,e author says that - it w, immerse 

 "xhe ,l!:drs«lT'lr,"dtl„s. I .in give you the word, of the author : " A certain space of 



the water. 



e water. causing cold, and a consequent condensation 



The fourth .the --7--^-;;? ^^fj'^^;^ ^ pU a y tubesr Th^-e are several objections to this 

 of the gases to be found near a^h^^^^^ no leaves being out at the time the sap 



co^r tf ::!• "rtht tJhatlstcad of drawing the sap up it would be more easy to draw 



air down describes the motion necessary to produce this 



The Mth B ceninfurja^^for e^ eornsti may bo placed one end in a basin of water, and the other 



phenomenon, and says that a coinsLUk may »« 1 „ ^j^ neighborhood of the 



Ind moved so rapidly as to cause the water to be ^J^fj^^. f ;^;^f ^;" ^i,,,. ^,,1, supernatural 



-^^ l;;;f iSiS." ThTl^bl-r :rtt!j :=,nenon, as ,aid down by the author, is be- 



-;t-ttr;:s:rs^^^^^^ 



1 nn The a X!- says that " portions of gases find their way into the capillary tub.s of he 

 elusions, ihe autiioi says iiKiL 1 t> , m,,- :„ „,jU„ erroneous ; no such thing 



s/^rt- ,;^:::^;sS-r-=;-- : i^::r ;:iTpres: 



TdLt::^rt,::;rrcf "Jn;:::^ h.ve „... thought «t to attribute the nsc „f .he ^p 

 . any of the cau-cs set out by the a„.t.^and -----::;: ^^Zd a. ,h. .oti.- 

 Not one of the P''«»°">"7'"'« " ^^7 fi^^;:°J3,,,,,ed „,at.er, e.leuUtcd only to fill up 

 power of the sap. The ->■»'«"»?:;' '^ ^ Jm«S .f"> nos.run,. Before attempting to assign 

 the pages of a journal principally devoted to tiic punuio 



