Namhlanje kukho uphando oluninzi kwiinkalo ezahlukeneyo, ezinye zinomdla ngakumbi kunenye, inyani, eqhutywa zizazinzulu ezivela kwihlabathi liphela ngeenjongo ezithile. Ngeli xesha ndifuna ukuba sithethe ngento enye enokwenzeka ukuthoba uqoqosho lwehlabathi ngenxa yobukhulu bayo. Ngokophando olusayinwe liqela elenziwe ngabaphandi abavela kwi I-Massachusetts Institute of Technology (MIT) ngokusebenzisana neeyunivesithi ezilishumi elinambini ezivela phantse kwihlabathi liphela, ngokucacileyo Umhlaba, ngaphakathi, ngokoqobo wenziwe ngedayimani.
Njengokuba uyifunda, uMhlaba ngaphakathi utyebile kakhulu kunendlela esinokucinga ngayo, ngokwedatha ephoswa sesi sifundo, sithetha ngento yokuba ngaphakathi kwiplanethi yethu kukho uvimba wedayimani onani lazo linyuswe laya kwiitoni ezili-10 yale nto, oko kukuthi, malunga neetoni ezingama-10.000, XNUMX zeedayimane. Inxalenye engathandekiyo yako konke oku, okanye mhlawumbi kulungile, kuxhomekeke kwiprism ojonga ngayo, kukuba, okwangoku, abantu abanayo itekhnoloji eyimfuneko yokufikelela kolu londolozo lukhulu.
Isifundo esenziwe yi-MIT ngokusebenzisana neeyunivesithi ezahlukeneyo sisixelela ukuba ngaphakathi eMhlabeni kukho iitoni zedayimani ezingaphezu kwe-10.000 yezigidi zezigidi
Nje ukuba upapasho lupapashwe ngokusemthethweni, uninzi belungamazwi athe afuna indlela yokufumana amanani afikelela kwindawo ekufumaneka kuyo le ndawo inkulu yedayimani efuna, kungenjalo kungenjalo, ukuzityebisa ngendlela ekunzima ukuyicinga. . Kuya kufuneka ucinge ukuba umntu othile ufumana itekhnoloji yoku, inokutshabalalisa uqoqosho lwehlabathi. Umzekelo ochaza le yokugqibela sinayo kwi Utshintsho ngequbuliso kwixabiso legolide kunye neoyile, inye enokuyenza lushiye uqoqosho lwehlabathiNgoku khawufane ucinge ukuba umntu othile uyavuma na ukugcina lo dayimani.
Nangona kunjalo… Kutheni ungafikeleli kuyo kwaye uqalise ukuzisa ezi dayimani kumphezulu wayo? Ngokwenyani ingxaki esinayo kukuba bangcwatyelwe ezingcanjini zeekreta, oko kukuthi, kanye emazantsi ezwekazi eliphakathi kwengqimba nengubo yoMhlaba. Ukukuqonda ngcono oku, sikuxelele ukuba kuya kufuneka siphuhlise itekhnoloji eyimfuneko ukusivumela yehla phakathi kwe-150 kunye neekhilomitha ezingama-300 ukusuka kumphezulu ukufikelela kolu londolozo lukhulu lwedayimane.
Iqela lezazinzulu lifumanisa njani ukuba kukho uvimba omkhulu wedayimani ongama-150 eekhilomitha ubunzulu?
Njengoko sele kupapashiwe kuxwebhu lwaseburhulumenteni olulungiselelwe liqela labaphandi abajongene nolu phononongo, kuye kwafuneka benze njalo Sebenzisa iisismographs ezihambele phambili. I-seismograph isetyenziselwa ukuthumela nokubamba amaza esandi embindini woMhlaba ukubona ukungafani okuhlukeneyo. Ngeli thuba bezisetyenziswa kuba isantya samaza siyatshintsha kuxhomekeka kuhlobo lwelitye elidlula kulo. Ngexesha lovavanyo lwabo, iqela lafumanisa ukuba amaza esandi ajikeleza kabini ngokukhawuleza kwiikhratons njengoko kufanelekile, ubunqabileyo obakhokelele kwisigqibo esimangalisayo.
Ukujongana nale anomaly isoftware ethile yenzelwe ukulinganisa isantya samaza kuzo zonke iintlobo zamatye kunye nezinto ezikhoyo ngaphakathi emhlabeni kude kube kufunyenwe ukwenziwa kweengcambu zecraton ezihambelana nesantya samaza esandi abanjwe ziisismografi. Emva kovavanyo oluninzi kuye kwagqitywa kwelokuba iingcambu zekhadibhodi kufuneka zenziwe phakathi kwe-1 kunye ne-2% yedayimane. Ukuthathela ingqalelo ubungakanani kunye noxinano lwee cratons, le pesenti iya kulingana ne-10.000 yezigidi zeetoni zedayimani.
Más información: phys.org