Bytheway, there's also a Rhpressure, rightairpressurepushingonthewaterinthecontainer, andifthisstrawwasempty, thatwouldthatwouldcausethewatertogointothestraw.
Sotheyalsocanceloutallwe'releftwith R H twoand H three, thedepthofwaterabovethewaterinthecontaineronboththeinsideandtheoutsideofthetube.
If H twoisequalto H three, thatmeanswehavethesamepressureoutofthestrawintothecontainer, aswedooutofthestrawintotheenvironment, andsonothingwillmove.
However, if I pourmorewaterintothecontainerandsay, raisethelevelofwaterinituptohere.
Sothisisnowallwaterwill.
Nowthereis a greaterpressureoutofthecontainerbecause H twohasbecomemuchsmaller.
H twoisnowonlythislarge, andif H twoissmallerthan a TSHthree, ifthedepthofwaterontheinsideabovethecontainerslevelissmallerthanthedepthofwaterontheoutside, there's morepressureheremovingout, andsothewaterwillflowoutuntilthewaterlevelinthecontainerhasdroppedbackdowntothesamelevelastheexit, atwhichpointwe'llbebackinequilibrium.
Therewillbethissituation H twoand H threeequaldepthsontheinsideandtheoutside, andthewaterwillstopmoving.
However, afterallofthis, itmayhavereached, wehope, if I putthestrawinfastenough, a velocitysufficienttocontinueonaroundthisthirdbendbeforebeingstoppedandreverseduntilitislowenough, maybe, likesayherethatit's belowthewaterlevelinthecontainer.
Whenthathappens, itwillcontinueflowing.
Andwe'vegotourselves a selfstartedsiphon.
Tomakeyourownselfstartingsiphon, youwillneed a fullglassofwater, threebendystrawsandsomescissors.