Encyclopædia Britannica: Or, A Dictionary of Arts, Sciences, and Miscellaneous Literature, Volume 18, Part 1Colin Macfarquhar, George Gleig A. Bell and C. Macfarquhar, 1797 - Encyclopedias and dictionaries |
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Page 15
... fore this hypothefis agrees with the Galilean ; but it affigus to every beam a fmaller proportion of the abfolute cohelion of the fection of fracture , in the proportion of 3 to 2. In the Galilean hypothesis this fection has a momentun ...
... fore this hypothefis agrees with the Galilean ; but it affigus to every beam a fmaller proportion of the abfolute cohelion of the fection of fracture , in the proportion of 3 to 2. In the Galilean hypothesis this fection has a momentun ...
Page 16
... fore the momentum of actual cohesion is } ƒs × 4 d , = ƒs } d ; that is , it is the fame as if the full cohefon of all the fibres were accumulated at a point I whose distance from A is th of AD or d ; or ( that we may fee its value in ...
... fore the momentum of actual cohesion is } ƒs × 4 d , = ƒs } d ; that is , it is the fame as if the full cohefon of all the fibres were accumulated at a point I whose distance from A is th of AD or d ; or ( that we may fee its value in ...
Page 17
... fore fuppofe that it has been established by experiment on by any o- any kind of folid matter , that the forces actually exerted in the internal equilibrium between the particles render it high- ther hypo- the inftant of fracture by the ...
... fore fuppofe that it has been established by experiment on by any o- any kind of folid matter , that the forces actually exerted in the internal equilibrium between the particles render it high- ther hypo- the inftant of fracture by the ...
Page 21
... fore let S reprefent the furface of fracture from A to D , and ƒ represent the absolute cohesion of a fibre at D in the in- ftant of fracture . We shall have ƒ Sx I + i = pl , or / : I ƒS + ifS : p ; that is , the length AB is to the ...
... fore let S reprefent the furface of fracture from A to D , and ƒ represent the absolute cohesion of a fibre at D in the in- ftant of fracture . We shall have ƒ Sx I + i = pl , or / : I ƒS + ifS : p ; that is , the length AB is to the ...
Page 24
... fore greateft in the middle . 93 Let us now confider the ftrain on any point C arifing The rain from a load uniformly diftributed along the beam . Let arifing from a load AP be reprefented by x , and Pp by x , and the whole weight ...
... fore greateft in the middle . 93 Let us now confider the ftrain on any point C arifing The rain from a load uniformly diftributed along the beam . Let arifing from a load AP be reprefented by x , and Pp by x , and the whole weight ...
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Common terms and phrases
affiftance againſt alfo almoſt alſo arifes artery becauſe blood body bone cafe caſe caufe cauſe coheſion compreffion confequence confiderable confifts courſe cure difeafe diſcharge diſeaſe diſtance divifion dreffings eafily emollient enemy eſpecially faid fame fays fecond fection fecured feems feparated feven feveral fhall fhips fhould fide filk firft firſt fituation fize fleet fmall fome fometimes foon force fore fpecies fracture frequently ftate ftill ftrain ftrength ftrong fubftance fubject fuch fufficient fugar fuppofed fupport furface fwelling fymptoms Guftavus hernia himſelf hydrocele incifion increaſe inflammation inftances inftrument itſelf king laft lefs ligature meaſure moft moſt muft muſcles muſt neceffary obferved occafion operation paffed patient perfon pledget poffible preffed preffure prevent purpoſe raiſed reafon refpect reft Ruffia ſhips ſkin ſmall ſome ſtate ſuch Sweden tack thefe themſelves theſe thofe thoſe tion trepan tumor ufual urethra uſed veffels weft whole windward wound