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K R I S T A L I

               Autori: Darja Nikolid, učenica VIII4 razreda, OŠ “Vuk Karadžid”, Isidora Todosid

                Mentor: Ljiljana Grkovid, predmetni nastavnik, OŠ “Vuk Karadžid”, Beograd




                                                        REZIME


                      Kristali  (najverovatnije  od  grčke  reči  koja  znači  "led")  su  minerali  pravilnog
               geometrijskog oblika određeni ravnim površima. Stvaranje kristala je posledica pravilnog ređanja
               čestica (molekula, atoma, jona) u kristalnoj rešetki, koja se pruţa u sve tri prostorne dimenzije.
               Formiraju  se  kada  podlegnu  procesu  očvršćavanja.  Pod  idealnim  uslovima,  rezultat  moţe  biti
               poseban monokristal, gde su svi atomi smešteni u istu  kristalnu  strukturu. Mnogi kristali se
               formiraju istovremeno za vreme očvršćavanja, pa nastaju polikristali. Kristali simetrično srastaju
               u  udvojene  kristale.  Prostori  između  ćelija  kristala  nazivaju  se  kristalna  rešetka.  Simetrija
               kristala  razotkriva  se    u  njegovoj  prostornoj  dimenziji.  U  idealnim  aranţmanima  kristali
               pokazuju značajne nedostatke, da bi upravo ovi nedostaci  kristala presudno uticali na mnoge
               elektične i mehaničke osobine prirodnih materijala.

               Ključne reči: kristali – kristalna struktura – udvojeni kristali – kristalna rešetka – kristalna
               simetrija – kristalni nedostaci.


                                                      ABSTRACT


               A crystal (most likely from a Greek word which means "ice") is a solid in which the constituent
               atoms, molecules or ions  are packed in  a regularly ordered,  repeating pattern extending in  all
               three spatial dimensions. Generally, crystals form when they undergo a process of solidification.
               Under ideal conditions, the result may be a single crystal, where all of the atoms in the solid fit
               into the same crystal structure. However, generally, many crystals form simultaneously during
               solidification,  leading  to  a  polycrystalline  solid.  For  example,  most  metals  encountered  in
               everyday life are polycrystals. Crystals are often symmetrically intergrown to form crystal twins.
               The  spacing  between  unit  cells  in  various  directions  are  called  crystal  lattice.  The
               symmetryproperties  of  the  crystal  are  embodied  in  its  space  group.  Real  crystals  feature
               defectsor irregularities in the ideal arrangements and it is these defects that critically determine
               many of the electrical and mechanical properties of real materials.

               Key words: crystal – crystal structure - crystal twins - crystal lattice - crystal symmetry –
               crystal defects.
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