{"id":739,"date":"2020-03-10T14:54:33","date_gmt":"2020-03-10T14:54:33","guid":{"rendered":"http:\/\/localhost\/sydney\/?page_id=739"},"modified":"2025-11-10T13:42:06","modified_gmt":"2025-11-10T13:42:06","slug":"rrjeti-shteteror-gravimetrik","status":"publish","type":"page","link":"https:\/\/krgjsh.asig.gov.al\/?page_id=739","title":{"rendered":"Rrjeti Shtet\u00ebror Gravimetrik"},"content":{"rendered":"\t\t
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Rrjeti Shtet\u00ebror Gravimetrik<\/h1>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
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1.Rrjeti <\/b>Shtet\u00ebror<\/b> Gravimetrik<\/b> ka si q\u00ebllim kryesor t\u00eb mund\u00ebsoj\u00eb nj\u00eb baz\u00eb cil\u00ebsore t\u00eb dh\u00ebnash gravimetrike t\u00eb nevojshme p\u00ebr p\u00ebrcaktimin e Gjeoidit Gravimetrik t\u00eb sakt\u00ebsis\u00eb s\u00eb lart\u00eb p\u00ebr territorin e Shqip\u00ebris\u00eb i cili do t\u00eb sh\u00ebrbej\u00eb p\u00ebr nd\u00ebrtimin e nj\u00eb sistemi t\u00eb ri lart\u00ebsish fizike n\u00eb p\u00ebrputhje me standardet evropiane.<\/p>

Rrjeti Shtet\u00ebror Gravimetrik \u00ebsht\u00eb pjes\u00eb e KRGJSH-s\u00eb dhe ka n\u00eb p\u00ebrb\u00ebrjen e tij:<\/p>

a) Rrjetin Shtet\u00ebror Gravimetrik t\u00eb Rendit Zero (3 pika);<\/p>

b) Rrjetin Shtet\u00ebror Gravimetrik t\u00eb Rendit t\u00eb Par\u00eb (42 pika);<\/p>

c) Rrjetin Shtet\u00ebror Gravimetrik t\u00eb Rendit t\u00eb Dyt\u00eb (338 pika);<\/p>

d) Rrjetin Shtet\u00ebror Gravimetrik t\u00eb Rendit t\u00eb Tret\u00eb (772 pika);<\/p>

Pikat gravimetrike absolute t\u00eb rendit zero (Shkod\u00ebr, Tiran\u00eb, Sarand\u00eb) dhe 42 pikat e rrjetit gravimetrik relativ t\u00eb rendit t\u00eb par\u00eb p\u00ebrb\u00ebjn\u00eb Datumin Gravimetrik Shqiptar.<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t

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Rrjeti Shtet\u00ebror Gravimetrik i Rendit Zero<\/strong><\/h3>

Rrjeti Shtet\u00ebror Gravimetrik i Rendit Zero p\u00ebrb\u00ebhet nga tre<\/b> pika<\/b> absolute<\/b>, n\u00eb t\u00eb cilat \u00ebsht\u00eb matur vlera absolute e nxitimit<\/b> gravitacional<\/b> t\u00eb<\/b> forc\u00ebs<\/b> s\u00eb<\/b> r\u00ebndes\u00ebs<\/b>, duke p\u00ebrdorur gravimetra<\/b> absolute me <\/b>sakt\u00ebsi<\/b> t\u00eb<\/b> lart\u00eb<\/b>.
Stacionet absolute n\u00eb territorin e vendit ndodhen n\u00eb: Shkod\u00ebr<\/b>, Tiran\u00eb<\/b>, Sarand\u00eb<\/b>.<\/b><\/p>

Ky rrjet sh\u00ebrben si baz\u00eb<\/b> referimi<\/b> p\u00ebr mb\u00ebshtetjen e rrjeteve gravimetrike t\u00eb rendeve m\u00eb t\u00eb ul\u00ebta dhe siguron ruajtjen<\/b> e <\/b>Datumit<\/b> Gravimetrik<\/b> Shqiptar<\/b> p\u00ebrmes matjeve absolute.<\/p>

Pikat absolute gravimetrike jan\u00eb stabilizuar<\/b> n\u00eb<\/b> blloqe<\/b> masive<\/b> betoni<\/b>, t\u00eb nd\u00ebrtuara mbi struktura<\/b> gjeologjike<\/b> t\u00eb<\/b> q\u00ebndrueshme<\/b>, n\u00eb p\u00ebrputhje me rekomandimet<\/b> nd\u00ebrkomb\u00ebtare<\/b>.<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t

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\"Shkod\u00ebr\"
Shkod\u00ebr<\/figcaption><\/figure><\/a><\/div>
\"Tiran\u00eb\"
Tiran\u00eb<\/figcaption><\/figure><\/a><\/div>
\"Sarand\u00eb\"
Sarand\u00eb<\/figcaption><\/figure><\/a><\/div>\t\t\t<\/div>\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
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Rrjeti <\/strong>Shtet\u00ebror\u00a0<\/strong>Gravimetrik i Rendit t\u00eb Par\u00eb<\/strong><\/h3>

Rrjeti Gravimetrik Shtet\u00ebror i Rendit t\u00eb Par\u00eb \u00ebsht\u00eb pjes\u00eb e t\u00eb<\/b> Dh\u00ebnave<\/b> Gravimetrike<\/b> Shqiptare<\/b> dhe sh\u00ebrben p\u00ebr t\u00eb dend\u00ebsuar<\/b> Rrjetin<\/b> Gravimetrik<\/b> Shtet\u00ebror<\/b> t\u00eb<\/b> Rendit<\/b> Zero<\/b>.<\/p>

Ky rrjet p\u00ebrb\u00ebhet nga 42 <\/b>pika<\/b>, t\u00eb shp\u00ebrndara n\u00eb m\u00ebnyr\u00eb uniforme<\/b> n\u00eb<\/b> territorin<\/b> e <\/b>vendit<\/b>, n\u00eb distanca q\u00eb variojn\u00eb nga 35 <\/b>deri<\/b> n\u00eb<\/b> 50 km<\/b>. T\u00eb gjitha pikat jan\u00eb t\u00eb<\/b> stabilizuara<\/b> n\u00eb<\/b> blloqe<\/b> betoni<\/b>, t\u00eb nd\u00ebrtuara mbi struktura<\/b> gjeologjike<\/b> t\u00eb<\/b> q\u00ebndrueshme<\/b>, n\u00eb p\u00ebrputhje me rekomandimet<\/b> nd\u00ebrkomb\u00ebtare<\/b>.<\/p>

N\u00eb k\u00ebto pika \u00ebsht\u00eb matur nxitimi<\/b> gravitacional<\/b> i<\/b> forc\u00ebs<\/b> s\u00eb<\/b> r\u00ebndes\u00ebs<\/b>, duke p\u00ebrdorur dy<\/b> gravimetra<\/b> relativ\u00eb<\/b> t\u00eb<\/b> kalibruar<\/b>, t\u00eb cil\u00ebt ofrojn\u00eb sakt\u00ebsi<\/b> t\u00eb<\/b> lart\u00eb<\/b> n\u00eb<\/b> matjet<\/b> gravimetrike<\/b> relative<\/b>, n\u00eb p\u00ebrputhje me metodat<\/b> gravimetrike<\/b> standarde<\/b>.<\/p>

Devijimi<\/b> standard<\/b> n\u00eb p\u00ebrcaktimin e nxitimit absolut t\u00eb gravitetit n\u00eb pikat e k\u00ebtij rrjeti nuk<\/b> kalon<\/b> vler\u00ebn<\/b> 10 \u00d7 10\u207b\u2078 m\/s\u00b2<\/b>.<\/p>

Rrjeti Shtet\u00ebror <\/strong>Gravimetrik i Rendit t\u00eb Dyt\u00eb<\/h3>

Rrjeti Gravimetrik i Rendit t\u00eb Dyt\u00eb sh\u00ebrben p\u00ebr dend\u00ebsimin<\/b> e <\/b>m\u00ebtejsh\u00ebm<\/b> t\u00eb<\/b> Rrjetit<\/b> Gravimetrik<\/b> Shtet\u00ebror<\/b> t\u00eb<\/b> Rendit<\/b> t\u00eb<\/b> Par\u00eb<\/b> dhe p\u00ebrb\u00ebhet nga 338 <\/b>pika<\/b>, t\u00eb shp\u00ebrndara n\u00eb territorin e vendit, t\u00eb cilat jan\u00eb t\u00eb<\/b> stabilizuara<\/b> n\u00eb<\/b> blloqe<\/b> betoni<\/b>.<\/p>

Pikave t\u00eb k\u00ebtij rrjeti u jan\u00eb p\u00ebrcaktuar vlerat<\/b> e <\/b>nxitimit<\/b> gravitacional<\/b> t\u00eb<\/b> forc\u00ebs<\/b> s\u00eb<\/b> r\u00ebndes\u00ebs<\/b>, duke p\u00ebrdorur gravimetra<\/b> relativ\u00eb<\/b> t\u00eb<\/b> kalibruar<\/b>, t\u00eb cil\u00ebt ofrojn\u00eb sakt\u00ebsi<\/b> t\u00eb<\/b> lart\u00eb<\/b> n\u00eb<\/b> matjet<\/b> gravimetrike<\/b> relative<\/b>, n\u00eb p\u00ebrputhje me metodat<\/b> standarde<\/b> t\u00eb<\/b> matjeve<\/b> gravimetrike<\/b> relative<\/b>.<\/p>

Devijimi<\/b> standard<\/b> n\u00eb p\u00ebrcaktimin e nxitimit absolut t\u00eb gravitetit n\u00eb pikat e Rrjetit t\u00eb Rendit t\u00eb Dyt\u00eb nuk<\/b> kalon<\/b> vler\u00ebn<\/b> 20 \u00d7 10\u207b\u2078 m\/s\u00b2<\/b>.<\/p>

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Rrjeti\u00a0<\/strong>Shtet\u00ebror\u00a0<\/strong>Gravimetrik i Rendit t\u00eb Tret\u00eb<\/strong><\/h3>

Rrjeti Gravimetrik i Rendit t\u00eb Tret\u00eb p\u00ebrfaq\u00ebson faz\u00ebn p\u00ebrfundimtare t\u00eb densifikimit t\u00eb Rrjetit Gravimetrik Shtet\u00ebror. Ky rrjet luan nj\u00eb rol ky\u00e7 n\u00eb sigurimin e t\u00eb dh\u00ebnave gravimetrike tok\u00ebsore t\u00eb nevojshme p\u00ebr p\u00ebrllogaritjen e nj\u00eb modeli t\u00eb sakt\u00eb dhe t\u00eb detajuar t\u00eb gjeoidit p\u00ebr territorin e Shqip\u00ebris\u00eb.<\/p>

Deri n\u00eb vitin 2024 jan\u00eb matur gjithsej 772 pika t\u00eb k\u00ebtij rrjeti, t\u00eb shp\u00ebrndara n\u00eb m\u00ebnyr\u00eb t\u00eb uniforme n\u00eb t\u00eb gjith\u00eb vendin. Objektivi yn\u00eb p\u00ebr t\u00eb ardhmen \u00ebsht\u00eb rritja e dend\u00ebsis\u00eb s\u00eb k\u00ebtij rrjeti, sipas standardeve teknike gravimetrike nd\u00ebrkomb\u00ebtare:<\/p>

1 pik\u00eb \u00e7do 2 km\u00b2 n\u00eb zonat fushore<\/p>

1 pik\u00eb \u00e7do 4 km\u00b2 n\u00eb zonat malore<\/p>

Sh\u00ebnim<\/b>:<\/b> Pikat e Rrjetit t\u00eb Rendit t\u00eb Tret\u00eb nuk jan\u00eb t\u00eb materializuara fizikisht n\u00eb terren. Sakt\u00ebsia e matjes s\u00eb gravitetit n\u00eb k\u00ebto pika \u00ebsht\u00eb shum\u00eb e lart\u00eb, me devijimin standard q\u00eb nuk kalon vler\u00ebn 30 \u00d7 10\u207b\u2078 m\/s\u00b2.<\/p>

K\u00ebto t\u00eb dh\u00ebna do t\u00eb kontribuojn\u00eb n\u00eb nd\u00ebrtimin e nj\u00eb gjeoidi gravimetrik me sakt\u00ebsi dhe rezolucion t\u00eb lart\u00eb, i cili \u00ebsht\u00eb thelb\u00ebsor p\u00ebr aplikime t\u00eb ndryshme n\u00eb fushat e gjeodezis\u00eb, hartografis\u00eb, inxhinieris\u00eb dhe planifikimit hap\u00ebsinor.<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t

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Rrjeti Shtet\u00ebror Gravimetrik (Gjeoidi Gravimetrik Shqiptar)<\/strong><\/h4>

Modelimi i gjeoidit gravimetrik p\u00ebrfshin nj\u00eb hap\u00ebsir\u00eb gjeografike midis koordinatave 38.5\u00b0\u201343.5\u00b0 N<\/b> dhe 18.0\u00b0\u201322.0\u00b0 E<\/b>, duke mbuluar t\u00eb gjith\u00eb territorin shqiptar dhe zonat p\u00ebrreth. N\u00eb k\u00ebt\u00eb projekt jan\u00eb p\u00ebrdorur metoda<\/b> t\u00eb<\/b> avancuara<\/b> si Katror\u00ebt<\/b> m\u00eb<\/b> t\u00eb<\/b> Vegj\u00ebl<\/b> t\u00eb<\/b> Kolokacionit<\/b> (LSC)<\/b> dhe Transformimi<\/b> i<\/b> Shpejt\u00eb<\/b> Furier<\/b> (FFT)<\/b> p\u00ebr t\u00eb nd\u00ebrtuar modele t\u00eb sakta t\u00eb gjeoidit.<\/p>

T\u00eb dh\u00ebnat p\u00ebrb\u00ebhen nga m\u00eb shum\u00eb se 63,000 <\/b>pika<\/b> gravimetrike<\/b>, t\u00eb mbledhura nga Shqip\u00ebria, Greqia dhe rajonet p\u00ebrreth, duke p\u00ebrfshir\u00eb edhe t\u00eb<\/b> dh\u00ebna<\/b> detare<\/b> nga<\/b> altimetria<\/b> satelitore<\/b>.<\/p>

P\u00ebr analiz\u00ebn jan\u00eb p\u00ebrdorur dy<\/b> modele<\/b> globale<\/b> t\u00eb<\/b> fush\u00ebs<\/b> s\u00eb<\/b> gravitetit<\/b>, EIGEN6c4<\/b> dhe XGM2019e<\/b>. Efektet topografike dhe batimetrike jan\u00eb llogaritur p\u00ebrmes Modelit<\/b> t\u00eb<\/b> Terrenit<\/b> t\u00eb<\/b> Mbetur<\/b> (RTM)<\/b>, duke u aplikuar si me qasje klasike<\/b>, ashtu edhe me qasje spektrale<\/b>, p\u00ebr t\u00eb garantuar kontroll dhe sakt\u00ebsi t\u00eb lart\u00eb.<\/p>

Gjeoidet e p\u00ebrftuar nga metodat e ndryshme (1D FFT<\/b>, 2D FFT<\/b>, LSC<\/b>) jan\u00eb validuar kundrejt 225 <\/b>pikave<\/b> GNSS\/<\/b>Nivelim<\/b>, t\u00eb ofruara nga ASIG<\/b>, duke u krahasuar me datumet<\/b> vertikale<\/b> ekzistuese<\/b> si<\/b> ALB86<\/b>, si dhe kundrejt 50 <\/b>pikave<\/b> t\u00eb<\/b> reja<\/b> GNSS\/<\/b>Nivelim<\/b> t\u00eb bazuara n\u00eb MSL <\/b>t\u00eb<\/b> Durr\u00ebsit<\/b>.<\/p>

Si p\u00ebrfundim, jan\u00eb p\u00ebrftuar disa modele gjeoidesh, ku m\u00eb i sakti ka rezultuar gjeoidi<\/b> gravimetrik<\/b> i<\/b> llogaritur<\/b> sipas<\/b> metod\u00ebs<\/b> 2D FFT<\/b>, bazuar n\u00eb modelin global EIGEN6c4<\/b> dhe n\u00eb reduktimin<\/b> e <\/b>mbetjeve<\/b> t\u00eb<\/b> terrenit<\/b> (RTM)<\/b> sipas metod\u00ebs<\/b> spektrale<\/b>, i cili ka arritur:<\/p>

Sakt\u00ebsin\u00eb<\/b> standarde<\/b> prej<\/b> 11.5 cm<\/b> referuar pikave t\u00eb rrjetit klasik ALB86<\/b><\/p>

Sakt\u00ebsin\u00eb<\/b> 6 cm<\/b> referuar 50 <\/b>pikave<\/b> t\u00eb<\/b> reja<\/b> t\u00eb<\/b> nivelimit<\/b>, t\u00eb bazuara n\u00eb MSL <\/b>t\u00eb<\/b> stacionit<\/b> mareografik<\/b> t\u00eb<\/b> Durr\u00ebsit<\/b><\/p>

Me q\u00ebllim llogaritjen e gjeoidit<\/b> gravimetrik<\/b> me <\/b>rezolucion<\/b> dhe<\/b> sakt\u00ebsi<\/b> t\u00eb<\/b> lart\u00eb<\/b> (synim: 2\u20133 cm<\/b>), i cili do t\u00eb p\u00ebrfaq\u00ebsoj\u00eb n\u00eb t\u00eb ardhmen referenc\u00ebn<\/b> gjeodezike<\/b> vertikale<\/b> moderne<\/b> n\u00eb Republik\u00ebn e Shqip\u00ebris\u00eb, dhe p\u00ebr t\u00eb p\u00ebrmbushur t\u00eb gjitha nevojat e p\u00ebrdoruesve, ASIG <\/b>\u00ebsht\u00eb<\/b> n\u00eb<\/b> zhvillim<\/b> t\u00eb<\/b> m\u00ebtejsh\u00ebm<\/b> t\u00eb<\/b> k\u00ebtij<\/b> projekti<\/b> si nj\u00eb nga pikat m\u00eb t\u00eb r\u00ebnd\u00ebsishme t\u00eb tij.<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t

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\n\t\t\t\t\t\t\t\t\t\t\"\"\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"

Rrjeti Shtet\u00ebror Gravimetrik 1.Rrjeti Shtet\u00ebror Gravimetrik ka si q\u00ebllim kryesor t\u00eb mund\u00ebsoj\u00eb nj\u00eb baz\u00eb cil\u00ebsore t\u00eb dh\u00ebnash gravimetrike t\u00eb nevojshme p\u00ebr p\u00ebrcaktimin e Gjeoidit Gravimetrik t\u00eb sakt\u00ebsis\u00eb s\u00eb lart\u00eb p\u00ebr territorin e Shqip\u00ebris\u00eb i cili do t\u00eb sh\u00ebrbej\u00eb p\u00ebr nd\u00ebrtimin e nj\u00eb sistemi t\u00eb ri lart\u00ebsish fizike n\u00eb p\u00ebrputhje me standardet evropiane. Rrjeti Shtet\u00ebror Gravimetrik […]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-templates\/page_front-page.php","meta":[],"_links":{"self":[{"href":"https:\/\/krgjsh.asig.gov.al\/index.php?rest_route=\/wp\/v2\/pages\/739"}],"collection":[{"href":"https:\/\/krgjsh.asig.gov.al\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/krgjsh.asig.gov.al\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/krgjsh.asig.gov.al\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/krgjsh.asig.gov.al\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=739"}],"version-history":[{"count":35,"href":"https:\/\/krgjsh.asig.gov.al\/index.php?rest_route=\/wp\/v2\/pages\/739\/revisions"}],"predecessor-version":[{"id":1788,"href":"https:\/\/krgjsh.asig.gov.al\/index.php?rest_route=\/wp\/v2\/pages\/739\/revisions\/1788"}],"wp:attachment":[{"href":"https:\/\/krgjsh.asig.gov.al\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=739"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}