Edhe n\u00ebse nj\u00eb tavolin\u00eb graniti ose nj\u00eb dysheme ose lavaman i b\u00ebr\u00eb nga ky gur konsiderohet natyrsh\u00ebm si i fort\u00eb, ky gur natyror gjithashtu ka nevoj\u00eb p\u00ebr mir\u00ebmbajtje t\u00eb rregullt – n\u00eb fund t\u00eb fundit, ai duhet t\u00eb duket p\u00ebrgjithmon\u00eb i bukur dhe me shk\u00eblqim. Graniti i shtrenjt\u00eb dhe fisnik, i cili konsumohet n\u00eb afat t\u00eb gjat\u00eb dhe n\u00eb k\u00ebt\u00eb m\u00ebnyr\u00eb b\u00ebhet i shurdh\u00ebr dhe i sh\u00ebmtuar, shpesh k\u00ebrkon nj\u00eb prerje dhe vulosje t\u00eb re. Fshirja e rregullt me agjent\u00eb t\u00eb ve\u00e7ant\u00eb pastrimi do t\u00eb ruaj\u00eb dhe p\u00ebrmir\u00ebsoj\u00eb n\u00eb m\u00ebnyr\u00eb t\u00eb q\u00ebndrueshme bukurin\u00eb natyrore t\u00eb granitit. P\u00ebr mir\u00ebmbajtje, dyshemeja mund t\u00eb f\u00ebrkohet me amoniak dhe m\u00eb pas me dyll dyshemeje. Jasht\u00eb, alkale t\u00eb forta (p.sh. pluhur dhe tabela p\u00ebr lavastoviljen) mund t\u00eb b\u00ebjn\u00eb mrekulli me ndotje t\u00eb leht\u00eb nga pluhuri dhe myshku. Kripa e njom\u00eb mund t\u00eb ndihmoj\u00eb me njollat e fresk\u00ebta. Muchsht\u00eb shum\u00eb m\u00eb e v\u00ebshtir\u00eb t\u00eb heq\u00ebsh njollat e yndyrshme me dyll ose vaj. N\u00eb k\u00ebt\u00eb rast, pluhurat thith\u00ebs t\u00eb lag\u00ebshtir\u00ebs ose pastat speciale jan\u00eb provuar efektive. Ato duhet t\u00eb veprojn\u00eb sipas udh\u00ebzimeve t\u00eb prodhuesit, t’i fshijn\u00eb dhe t’i p\u00ebrs\u00ebrisin disa her\u00eb. K\u00ebtu mund t\u00eb p\u00ebrdoret koncentrati yn\u00eb pastrues BIOSATIVA\u00ae<\/a> . Kjo \u00ebsht\u00eb e p\u00ebrshtatshme sepse \u00ebsht\u00eb plot\u00ebsisht e biodegradueshme. Nuk ka humbje t\u00eb fuqis\u00eb s\u00eb pastrimit.<\/p>\n\n Granit\u00ebt jan\u00eb shk\u00ebmbinj ndez\u00ebs q\u00eb formohen nga shk\u00ebmbinj t\u00eb shkrir\u00eb. Shk\u00ebmbi i zjarrt\u00eb masiv dhe relativisht i trash\u00eb kristalor \u00ebsht\u00eb i pasur me feldspars, kuarc dhe minerale t\u00eb err\u00ebta si mika. Graniti formohet nga ngurt\u00ebsimi i magm\u00ebs (shkrirja e shk\u00ebmbit) brenda kores s\u00eb tok\u00ebs, kryesisht n\u00eb thell\u00ebsi m\u00eb shum\u00eb se dy kilometra n\u00ebn sip\u00ebrfaqen e tok\u00ebs. P\u00ebr k\u00ebt\u00eb arsye, graniti \u00ebsht\u00eb nj\u00eb nga shk\u00ebmbinjt\u00eb e thell\u00eb. P\u00ebrmbajtja e k\u00ebrkuar e kuarcit t\u00eb mineraleve t\u00eb lehta p\u00ebr granitin duhet t\u00eb jet\u00eb s\u00eb paku 20 p\u00ebr qind deri n\u00eb nj\u00eb maksimum prej 60 p\u00ebr qind. N\u00eb shumic\u00ebn e rasteve, granit\u00ebt jan\u00eb shk\u00ebmbinj me ngjyr\u00eb t\u00eb hapur. P\u00ebrve\u00e7 ngjyrave t\u00eb bardha, t\u00eb kuq\u00ebrremta ose t\u00eb verdha, ka edhe variante me shum\u00eb ngjyra – megjithat\u00eb, graniti nuk \u00ebsht\u00eb kurr\u00eb plot\u00ebsisht i zi. Pik\u00ebrisht k\u00ebtu dallon graniti nga gabrot\u00eb apo bazaltet, ve\u00e7an\u00ebrisht pasi ato nuk p\u00ebrmbajn\u00eb asnj\u00eb kuarc. Ky aspekt duhet t\u00eb merret parasysh n\u00eb tregtin\u00eb e gurit natyror, pasi k\u00ebta gur\u00eb nuk kan\u00eb asnj\u00eb lidhje me granitin dhe shpesh jan\u00eb m\u00eb pak t\u00eb fort\u00eb.<\/p>\n<\/div>\n\n\n\n Nj\u00eb nga avantazhet e m\u00ebdha t\u00eb granitit mund t\u00eb shihet n\u00eb q\u00ebndrueshm\u00ebrin\u00eb e tij. Nuk \u00ebsht\u00eb p\u00ebr asgj\u00eb q\u00eb jan\u00eb vendosur shprehje t\u00eb tilla si “t\u00eb forta si graniti” ose “kafshoni granitin”, duke iu referuar elasticitetit t\u00eb shk\u00ebmbit. Granit\u00ebt mund t\u00eb duken shum\u00eb t\u00eb ndrysh\u00ebm edhe me t\u00eb nj\u00ebjt\u00ebn p\u00ebrb\u00ebrje kimike. Ngjyra e mineraleve dhe madh\u00ebsia e kokrr\u00ebs s\u00eb tyre jan\u00eb kryesisht p\u00ebrgjegj\u00ebse p\u00ebr variantet e shumta t\u00eb ndryshme. Graniti \u00ebsht\u00eb p\u00ebrgjith\u00ebsisht me kok\u00ebrr t\u00eb mesme ose t\u00eb trash\u00eb. Ka nj\u00eb pamje relativisht t\u00eb nj\u00ebtrajtshme, e cila rezulton nga shp\u00ebrndarja homogjene e mineraleve me cil\u00ebsi kryesisht pa drejtim. Struktura e tij karakterizohet nga nj\u00eb lidhje e drejtp\u00ebrdrejt\u00eb e grurit, me madh\u00ebsin\u00eb e kristalit q\u00eb zakonisht luhatet midis nj\u00eb dhe disa centimetra. P\u00ebrve\u00e7 graniteve me t\u00eb nj\u00ebjt\u00ebn madh\u00ebsi, n\u00eb t\u00eb cilat pothuajse t\u00eb gjith\u00eb kristalet jan\u00eb t\u00eb s\u00eb nj\u00ebjt\u00ebs madh\u00ebsi, nuk \u00ebsht\u00eb e pazakont\u00eb t\u00eb ndodhin granit\u00eb me kok\u00ebrr t\u00eb parregullt ose porfir. N\u00eb k\u00ebt\u00eb rast, kristalet individuale – kryesisht t\u00eb ashtuquajturat feldspars – jan\u00eb disa her\u00eb m\u00eb t\u00eb m\u00ebdha se mineralet e tjera.<\/p>\n<\/div>\n<\/div>\n\n Vulosja jon\u00eb e granitit arrin nj\u00eb efekt unik afatgjat\u00eb p\u00ebr shkak t\u00eb efektit t\u00eb tij t\u00eb thell\u00eb, i cili e b\u00ebn gurin t\u00eb duket i mir\u00eb n\u00eb afat t\u00eb gjat\u00eb dhe mbron n\u00eb m\u00ebnyr\u00eb efektive dhe t\u00eb p\u00ebrhershme kund\u00ebr t\u00eb gjitha ndikimeve t\u00eb jashtme. P\u00ebr shkak t\u00eb efektit t\u00eb zambakut, uji thjesht do t\u00eb dal\u00eb nga sip\u00ebrfaqja n\u00eb t\u00eb ardhmen.<\/p>\n\nP\u00ebrkufizimi dhe p\u00ebrb\u00ebrja<\/h2>\n\n\n\n
Vetit\u00eb dhe klasifikimi<\/h2>\n\n\n\n
Video e produktit: Mbyllja e pllakave t\u00eb granitit brenda dhe jasht\u00eb<\/h2>\n\n