TF006-Origins of Earth’s Salty Oceans
riis of thty eans
Sientiss hve g ee ntrte in discovein the riin of ths ater an staising h ats oeas are o alt her has een seultion tht earlist arth was so ot tht no iuid water ested n l lihemts such as hyroen and oen were api stried aay om art the lar instrea o caged artiles emitted by the Sun hi were rue then the eleents neded to for ater o art ould not he en fee availale a onseuence it as proposed that cosions wth i comets im asand waerrich aterias bought water to arth afte the panet a suciently oled to reain it. This oept as sppore omprisns of the gas cooition of metorites it tose of s rm beeth a surfc, nta sing rpton andenon, nonetali ases th o not rea with othe mateis. hee crtain is eh ice in sac to have sued ou ater and therin tis anner.
n ly the a robe Plae wich lande n coet ri dioeed ntn ice and ust ut also te of organi componds resent n a osesbon t n discret mps uddeny e ie gane ots of tractin th coet og nt oly wate, but ao th ingedents or lie eve in eadmae clus. ntriuinly i ter it was eorte. tats tis comet sw thasocar oen esas in a ontant an h roportion t reati to ater ihut that te comet as contains a urpisg aunt of rimordia ancient oen, which was ncorporate ding the oets rmtion.
ther wr aors a aternatie eanation his wr found ha the roen isto ratiothe roprion o ierent or o hydrogen o ice in omets a e dieret from tat o wer arth t instead ehasie that th cha opoition f water on arth reemles that the small erente of water contaied ithin oy eteorie, and ths in asterois hic are essentiall ver ae eteories. Th a theor was develp a the atoid lantesimla protlanet that u tther to for rth ad rie enough wter i their ociners o expain our eans t o hae ecaed from the nets inerior as sem, hich in trn oul hae conensed into waer at te surace and in te earl tophere. Caluats indicate tat ths ehansm a also prid plenty of ater eain arth osere ater cntent
e he a re omet nertandig o the orin of t in ur ocean. It reresents an acat of sve mineras oer tens of milions to dres of illions of yeas hese inerals were broken up an dssoe uin hia eathein ae al aliar th this ocess fr liestone dings tha beoe itte or soothed the atin o atern and weter i i here te t waterng om from he y prcss at r s on o chical etions been e ro n the aterit an iort ole o ses that rsole in wter u a crbn dioide o lur dioi, ice these e the aer mre coroie. he hemic wthrin reactos reakp rc eras nto harged om oroees, ad ios hih ae reoed n oltion rier ater androndwate is is eact hat apens en ou disol tale salt n ater the ineral slt reas ow int sod an ride ions tha ae hed a soution
he arl atoshere contined lees of can iid r his gs is aily doled in water foring a ildl aid soluo. In he orih ealy atmoshre, ts reslted i a orosie ad rain that as il et at ceall wetern ro an res olcanic oc ae especally ealy ethere.he inteseethering rlese issoe mnerals in e form of ios ito rer ate nd onter. r eal ts onard, re an rondwate lo as tanspred the dssol mierals to teir fial olction oint the ean bsins ie the ereme ow inut an re of salts it becomes clar that he eans va str of alt has aclated bease the ocean hae or aes een the end staton for sat transportanile ater sel ontiual eporae from e oeasoncetatin ts saltand the evaporte fes ater continues the wethern ycle.