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  • Isizathu sokuba inkxaso ye-seismic ingamelana namandla e-seismic

    Inkxaso ye-seismiczizinto ezahlukeneyo okanye izixhobo ezinciphisa umda wokususwa kwezixhobo zobunjineli bobulumko boMzantsi Afrika, zilawule ukuntywila kwezixhobo, kwaye zidlulise umthwalo kwisakhiwo sokuthwala. Iindawo zobunjineli bobuzwe ze-electromachican, ezinjengokunikezelwa kwamanzi kunye nokukhuselwa komlilo, ukufudumeza, ukunciphisa umoya, unxibelelwano, unxibelelwano, njl njl, njl njl.

     

    Kutheni le ntoInkxaso ye-seismicI-qinkai ichasa amandla e-seismic?

    Iinyikima zinyikima zibangelwa kukukhululwa kwamandla avela emhlabeni, nto leyo echaphazela okanye ukutshabalalisa ubomi bomntu ngamaza e-seismic. Amaza eSpiicic anokwahlulwa kwiifom ezintathu: i-waveritudinal wave (p wave), i-shear wave

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    I-wave yexesha elide yeyomza, obangela umhlaba ukuba utshazelele uye ezantsi, kwaye iyonakalisa iyonakalisa. Amaqhekeza esichonga lowo, makatshangatshangise, makanyikima umhlaba, aqine umphumo otshabalalisayo. Umphezulu wawo wedwa owawuveliswayo emva kwe-wave yase-cheitudinal kunye ne-shear wave wadibana emhlabeni, kwaye esona siphumo somelele.

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    NangonaInkxaso ye-striphic ravicNgaba unokumelana kwaye unciphise amandla e-vemic ethe nkqo (okt, i-wave yexesha elide), inkxaso ye-seanger kunye ne-hanger inokumelana kakhulu kwaye inciphise amandla athe tyando

    Oku kungasentla sisishwankathelo somhleli omncinci wokukhusela indalo esingqongileyo, umenzi weFinkaiInkxaso ye-seismic. Yintoni esifanele siyiqwalasele xa sisebenzisa inkxaso ye-wimicic ekhethiweyo? Ukuba kukho nantoni na ongazaziyo, unganxibelelana nenkonzo yethu yabathengi. Siza kukunceda ngentliziyo iphela. Okanye ulandele iwebhusayithi yethu esemthethweni ngolwazi oluthe kratya.

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    Ixesha lasemva: ngoFebruwari-15 ukuya ku-523