{"id":4999,"date":"2010-12-03T23:20:34","date_gmt":"2010-12-03T22:20:34","guid":{"rendered":"http:\/\/fjala.shkoder.net\/?p=4999"},"modified":"2010-12-03T23:20:34","modified_gmt":"2010-12-03T22:20:34","slug":"permbytjet-zgjidhjet-per-lumin-buna","status":"publish","type":"post","link":"https:\/\/fjala.info\/2009-2015\/permbytjet-zgjidhjet-per-lumin-buna\/","title":{"rendered":"P\u00ebrmbytjet, zgjidhjet p\u00ebr lumin Buna"},"content":{"rendered":"

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\nNga: XHEVAHIR NGJEQARI<\/strong>, 03 Dhjetor 2010<\/em><\/p>\n

Nivelet e vazhdueshme t\u00eb uj\u00ebrave p\u00ebrmbyt\u00ebse n\u00eb Ult\u00ebsir\u00ebn e Shkodr\u00ebs dhe Lezh\u00ebs, nga datat 27 dhjetor 2009 – 12-17 janar 2010, p\u00ebrmbytjet pjesore n\u00eb muajin shkurt dhe rip\u00ebrmbytjet…<\/p>\n

n\u00eb muajin dhjetor 2010 n\u00eb t\u00eb dyja an\u00ebt e shtratit t\u00eb Bun\u00ebs, v\u00ebrtetuan se marr\u00ebdh\u00ebniet hidroteknike midis gjirit t\u00eb Drinit (niveleve detare), shkarkuesit t\u00eb Bun\u00ebs e Vilunit – kuotave t\u00eb ult\u00ebsir\u00ebs s\u00eb Shkodr\u00ebs dhe prurjeve t\u00eb liqenit t\u00eb Shkodr\u00ebs, Drinit e Kirit, nuk funksionojn\u00eb. E p\u00ebr rrjedhoj\u00eb, ult\u00ebsira e Shkodr\u00ebs gjendet e penalizuar nga p\u00ebrmbytjet periodike dhe do t\u00eb<\/p>\n

p\u00ebrmbytet sa her\u00eb t\u00eb rriten nivelet detare, prurjet e Mora\u00e7\u00ebs (liqeni i Shkodr\u00ebs), shkarkesat e Drinit apo plotat e Kirit. N\u00eb mediat e shkruara dhe vizive, specialist\u00ebt shpjegojn\u00eb me holl\u00ebsi mbi kaskad\u00ebn e Drinit dhe bonifikimin e ult\u00ebsir\u00ebs s\u00eb Shkodr\u00ebs, nd\u00ebrsa tregohen shum\u00eb t\u00eb kufizuar n\u00eb aksionet p\u00ebrmbyt\u00ebse t\u00eb liqenit t\u00eb Shkodr\u00ebs, aft\u00ebsin\u00eb thith\u00ebse t\u00eb uj\u00ebrave nga pasqyra detare e gjirit t\u00eb Drinit, etj. Nga p\u00ebrmbytjet k\u00ebrkohen kat\u00ebr p\u00ebrgjigje kryesore: E para, ku u gjend\u00ebn prurjet e uj\u00ebrave p\u00ebrmbyt\u00ebse?<\/p>\n

E dyta, p\u00ebrse nuk shkarkojn\u00eb v\u00ebllimet e uj\u00ebrave n\u00eb pasqyr\u00ebn detare? E treta, a do t\u00eb p\u00ebrmbyten p\u00ebrs\u00ebri banor\u00ebt e ult\u00ebsir\u00ebs s\u00eb Shkodr\u00ebs? E kat\u00ebrta, kush \u00ebsht\u00eb fajtori, ose m\u00eb mir\u00eb, cil\u00ebt jan\u00eb bashk\u00ebfajtor\u00ebt? Pyetja e fundit p\u00ebrb\u00ebn dhe konstanten e sherrit, me q\u00ebllim q\u00eb qeveria aktuale t\u00eb vet\u00ebfirmos\u00eb hipotek\u00ebn e p\u00ebrmbytjes. Pa mohuar zullumet e qeveris\u00eb apo qeverive, duhet t\u00eb shtojm\u00eb se hidrografi i p\u00ebrmbytjeve t\u00eb ult\u00ebsir\u00ebs s\u00eb Shkodr\u00ebs ka disa lidhje organike.<\/p>\n

Nj\u00eb nga k\u00ebto \u00ebsht\u00eb marr\u00ebdh\u00ebnia me pasqyr\u00ebn detare t\u00eb Drinit, mbi t\u00eb cilin veprojn\u00eb nj\u00eb kompleks faktor\u00ebsh hidrologjik\u00eb, klimatologjik\u00eb, meteorologjik\u00eb, veprojn\u00eb vektor\u00ebt e er\u00ebrave dhe korrenteve detare, me t\u00eb gjith\u00eb ekstremitetet e potencialeve t\u00eb Adriatikut dhe Mesdheut. Duke krijuar disnivele detare, q\u00eb n\u00eb rastin e interferencave me prurjet e Bun\u00ebs shkaktojn\u00eb p\u00ebrmbytjet n\u00eb ult\u00ebsir\u00ebn e Shkodr\u00ebs. Kjo v\u00ebrtetohet dhe nga vektor\u00ebt dhe diagramat e korrenteve dhe er\u00ebrave detare, q\u00eb kan\u00eb p\u00ebrpunuar altimetrin\u00eb dhe relievin bregdetar t\u00eb gjirit t\u00eb Drinit, me ve\u00e7orit\u00eb e rralla t\u00eb morfologjis\u00eb mjedisore.<\/p>\n

Gjiri i Drinit dhe korrentet detare<\/strong><\/p>\n

Gjiri i Drinit n\u00ebnkupton bregdetin nga delta e Bun\u00ebs-Sh\u00ebngjin-Kune Vaini-Tale-delta e Matit-bregdeti i Patogut-delta e Ishmit-bregdeti verior i kepit t\u00eb Rodonit. N\u00eb t\u00eb gjith\u00eb nj\u00ebsit\u00eb mat\u00ebse, Gjiri i Drinit p\u00ebrb\u00ebn pa asnj\u00eb krahasim nj\u00eb nga gjiret m\u00eb t\u00eb m\u00ebdhenj t\u00eb Adriatikut, gjirin me relievin m\u00eb t\u00eb bukur, m\u00eb mjedisor turistik, m\u00eb cil\u00ebsor dhe gjirin m\u00eb t\u00eb thell\u00eb n\u00eb natyr\u00ebn e tij n\u00eb gjith\u00eb Mesdheun, gjirin me hidrologjin\u00eb dhe me gjeometrin\u00eb e korrenteve detare m\u00eb t\u00eb pasur t\u00eb gjith\u00eb Adriatikut dhe Jonit lindor.<\/p>\n

N\u00eb gjirin e Drinit derdhen lumenjt\u00eb e Bun\u00ebs, Kirit, Drinit, Matit dhe Ishmit. Baseni uj\u00ebmbledh\u00ebs i Shqip\u00ebris\u00eb llogaritet 43 305 km\u00b2, nga t\u00eb cilat 22696 km\u00b2 ose 52,4 % derdhen n\u00eb gjirin e Drinit. Nd\u00ebrsa si prurje mesatare vjetore, lumenjt\u00eb transportojn\u00eb n\u00eb det rreth 1308 m3\/sek, nga e cila 802.9 m3\/sek ose 61,3 % derdhet n\u00eb gjirin e Drinit. Nj\u00eb kuriozitet tjet\u00ebr \u00ebsht\u00eb se bregdeti i st\u00ebrzgjatur slloven, kroat, malazez, ka nj\u00eb gjat\u00ebsi bregdetare 6160 km dhe nj\u00eb basen t\u00eb kufizuar uj\u00ebmbledh\u00ebs 46 544 km\u00b2, i cili pothuaj \u00ebsht\u00eb i barabart\u00eb me basenin uj\u00ebmbledh\u00ebs shqiptar 43 305 km\u00b2, q\u00eb derdhet n\u00eb nj\u00eb gjat\u00ebsi bregdetare adriatike (Bun\u00eb\u2013Vlor\u00eb) rreth 270 km.<\/p>\n

Duke krahasuar shifrat, rezulton se n\u00eb gjirin e Drinit shkarkohet rreth 25 % e gjith\u00eb basenit uj\u00ebmbledh\u00ebs Vlor\u00eb\u2013Bun\u00eb\u2013Trieste. N\u00eb gjirin e Drinit derdhen edhe dy shkarkues natyral\u00eb t\u00eb prurjeve t\u00eb liqenit t\u00eb Shkodr\u00ebs dhe liqenit t\u00eb Ohrit. Sepse shtrati i lumit Buna dhe Drini i Zi sh\u00ebrbejn\u00eb n\u00eb gjuh\u00ebn e hidroteknik\u00ebs si shkarkues katastrofik\u00eb ose shkarkues natyral\u00eb t\u00eb uj\u00ebrave t\u00eb tep\u00ebrta t\u00eb dy liqeneve. Por n\u00eb gjirin e Drinit veprojn\u00eb t\u00eb gjitha korrentet detare q\u00eb fryjn\u00eb n\u00eb Adriatik dhe Mesdhe.<\/p>\n

Korrentet violente veri-lindore e lindore fryjn\u00eb n\u00eb Adriatikun Lindor vet\u00ebm n\u00eb 11 nyje bregdetare. Dhe nj\u00eb nga k\u00ebta vektor\u00eb ka drejtimin n\u00eb gjirin e Drinit. N\u00eb gjirin e Drinit veprojn\u00eb dhe korrentet e Shirok\u00ebs, Libe\u00e7ios, pjes\u00ebrisht Grekalit, korrentet jugper\u00ebndimore, korrentet e hap\u00ebsir\u00ebs detare per\u00ebndimore, flladet, etj.<\/p>\n

Si rezultat i fenomenit t\u00eb rrotullimit n\u00eb pozicionin e hemisfer\u00ebs veriore, tangjentja e korrenteve t\u00eb ngushtic\u00ebs s\u00eb Messin\u00ebs nd\u00ebshkon faqen per\u00ebndimore t\u00eb Karaburunit, ishullit t\u00eb Sazanit, maj\u00ebn e kepit t\u00eb Rodonit dhe godet direkt n\u00eb delt\u00ebn e Bun\u00ebs, bregun e Velipoj\u00ebs dhe delt\u00ebn e Vilunit. Sipas matjeve tona n\u00eb datat 12 dhe 17 janar, nivelet e larta t\u00eb pasqyr\u00ebs detare kan\u00eb zgjatur t\u00eb pakt\u00ebn 9 dit\u00eb nga ciklet 12, 24, 48, 72-or\u00ebshe q\u00eb zakonisht zgjasin trazimet detare.<\/p>\n

Nj\u00eb rritje e nivelit t\u00eb ujit n\u00eb delt\u00ebn e Vilunit 50 cm shtyn uj\u00ebrat deri n\u00eb 3 km thell\u00ebsi t\u00eb Vilunit dhe t\u00eb Bun\u00ebs. Duke qen\u00eb se masa detare \u00ebsht\u00eb m\u00eb e madhe se rrjedhja e Bun\u00ebs, at\u00ebher\u00eb bllokohen dhe vonohen kullimet e uj\u00ebrave t\u00eb ult\u00ebsir\u00ebs s\u00eb Shkodr\u00ebs. Ky fenomen shpjegohet me p\u00ebrplasjen e dy prurjeve: t\u00eb detit dhe ujit t\u00eb Bun\u00ebs. Nga sa kuptohet, ngritjet e niveleve detare n\u00eb delt\u00ebn e Bun\u00ebs dhe Vilunit ulin aft\u00ebsin\u00eb e shkarkimit t\u00eb uj\u00ebrave. Kjo n\u00ebnkupton se hap\u00ebsira detare e gjirit t\u00eb Drinit dhe delt\u00ebs s\u00eb Bun\u00ebs nuk \u00ebsht\u00eb e p\u00ebrpunuar nga ana hidroteknike q\u00eb t\u00eb t\u00ebrheq\u00eb sipas d\u00ebshir\u00ebs s\u00eb shqiptar\u00ebve, prurjet e uj\u00ebrave t\u00eb Bun\u00ebs, Drinit, Matit, etj.<\/p>\n

Nga ana jon\u00eb jan\u00eb kryer shum\u00eb matje n\u00eb periudh\u00ebn e ver\u00ebs mbi nivelet detare n\u00eb gjirin e Drinit. Dhe dilet n\u00eb p\u00ebrfundimin se bonifikimi i ult\u00ebsir\u00ebs s\u00eb Shkodr\u00ebs nuk mund t\u00eb arrihet pa bashk\u00ebllogaritur dhe hidrologjin\u00eb detare t\u00eb gjirit t\u00eb Drinit, duke njohur gjeografin\u00eb, gjeometrin\u00eb, batimetrin\u00eb dhe gjith\u00eb fenomenet meteorologjike n\u00eb bregdetin e Adriatikut shqiptar. Mbi k\u00ebto llogaritje mund t\u00eb ofrohen zgjidhje bashk\u00ebkohore p\u00ebr shkarkimet n\u00eb delt\u00ebn e Bun\u00ebs dhe Vilunit. Zgjidhjet q\u00eb jan\u00eb ofruar deri tani se do t\u00eb rregullohet delta e Bun\u00ebs me skoliera ose me ndarje t\u00eb delt\u00ebs dhe do t\u00eb mbrohet bregu me argjinatura, jan\u00eb t\u00eb pjesshme.<\/p>\n

Konxhestioni i Bun\u00ebs ose Suezi i hidrologjis\u00eb dhe p\u00ebrmbytjet<\/strong><\/p>\n

Fjala konxhestion \u00ebsht\u00eb me prejardhje nga mjek\u00ebsia dhe n\u00ebnkupton bllokimin n\u00eb nj\u00eb nyje t\u00eb caktuar t\u00eb nj\u00eb arterieje n\u00eb trupin e njeriut. Vena fryhet n\u00eb t\u00eb dyja an\u00ebt, qarkullon ngadal\u00eb dhe ose pastrohet, ose \u00e7ahet. Ky term, p\u00ebr her\u00eb t\u00eb par\u00eb \u00ebsht\u00eb p\u00ebrdorur n\u00eb infrastruktur\u00eb, kur n\u00eb kufirin polako\u2013gjerman, vargu i makinave arriti deri n\u00eb 50 km nga vonesat kufitare. Por edhe trungu i lumit Buna nuk \u00ebsht\u00eb gj\u00eb tjet\u00ebr ve\u00e7se nj\u00eb \u201cbypass\u201d i hapur natyral, ndryshe Suezi i hidrologjis\u00eb shqiptare ose Suezi i hidrologjis\u00eb s\u00eb Adriatikut Lindor (i cili p\u00ebr 15 dit\u00eb resht bllokoi shkarkimet e uj\u00ebrave t\u00eb Drinit, Kirit dhe liqenit t\u00eb Shkodr\u00ebs.<\/p>\n

N\u00eb nivelet m\u00eb kritike t\u00eb p\u00ebrmbytjeve n\u00eb datat 12 dhe 17 janar, shkurt dhe n\u00ebntor \u2013 dhjetor 2010, arrit\u00ebm t\u00eb kalojm\u00eb n\u00eb brend\u00ebsi t\u00eb Velipoj\u00ebs, delt\u00ebs s\u00eb Bun\u00ebs n\u00eb zon\u00ebn e Pulas dhe nga pamja e jashtme, pasqyra ujore pothuaj nuk l\u00ebvizte. E nj\u00ebjta pamje ishte dhe n\u00eb zon\u00ebn e Vilunit, sip\u00ebr ur\u00ebs s\u00eb drurit. N\u00eb zon\u00ebn e Pulas, zona ishte e braktisur. N\u00eb p\u00ebrmbytjet e muajit janar 2010, trazirat detare zgjat\u00ebn rreth 9 dit\u00eb.<\/p>\n

Nivelet detare ishin t\u00eb larta. Uji i Bun\u00ebs nuk l\u00ebvizte. Me t\u00eb drejt\u00eb, shtrohen pyetjet: \u00c7far\u00eb p\u00ebrfaq\u00ebson lumi Buna n\u00eb konceptin hidrologjik, cilat jan\u00eb funksionet dhe aft\u00ebsit\u00eb hidroteknike, cilat jan\u00eb marr\u00ebdh\u00ebniet me bregdetin dhe \u00e7far\u00eb k\u00ebrkojn\u00eb shqiptar\u00ebt nga Buna?<\/p>\n

Shtrati i lumit Buna, n\u00eb vij\u00eb ajrore, ruan nj\u00eb gjurm\u00eb me gjat\u00ebsi 25,4 km, nd\u00ebrsa gjat\u00ebsia e shtratit nga dalja e liqenit t\u00eb Shkodr\u00ebs n\u00eb det arrin 41 km. Shtrati i lumit Buna \u00ebsht\u00eb thell\u00ebsisht aluvional ose lymor dhe zot\u00ebron pjerr\u00ebsin\u00eb natyrale mes 02 % ose 20 cm p\u00ebr 1 km dhe m\u00eb pak. Pjerr\u00ebsis\u00eb s\u00eb vog\u00ebl t\u00eb lumit i shtohen dhe gjarp\u00ebrimet ose meandrimet, fushat e B\u00ebrdic\u00ebs, Daragjatit, Oblik\u00ebs, Obotit, Samrisht\u00ebs, Daj\u00e7it, Pentarit, etj. Lumi Buna sh\u00ebrben si shkarkues natyral i liqenit t\u00eb Shkodr\u00ebs.<\/p>\n

Por, liqeni i Shkodr\u00ebs p\u00ebrpunon uj\u00ebrat e lumit Mora\u00e7a, Cemit, t\u00eb Malit t\u00eb Zi dhe uj\u00ebrat e basenit t\u00eb Vrak\u00ebs, Rjollit, me nj\u00eb sip\u00ebrfaqe uj\u00ebmbledh\u00ebse q\u00eb arrinte 5187 km2 dhe Kirit. Si rrjedhoj\u00eb e plotave n\u00eb vitin 1846 \u2013 1858, lumi Drin nd\u00ebrron drejtimin dhe shkarkohet n\u00eb shtratin e lumit Buna rreth 1,4 km m\u00eb posht\u00eb se dalja e Bun\u00ebs nga liqeni i Shkodr\u00ebs. Aktualisht, shtrati i lumit Buna duhet t\u00eb p\u00ebrcjell\u00eb n\u00eb det uj\u00ebrat e liqenit t\u00eb Shkodr\u00ebs, uj\u00ebrat e Drinit, Kirit, etj.<\/p>\n

N\u00eb konceptin hidrologjik, lumi i Bun\u00ebs duhet t\u00eb p\u00ebrcjell\u00eb basenin uj\u00ebmbledh\u00ebs 19 582 km2 ose 45 % t\u00eb uj\u00ebrave t\u00eb gjith\u00eb basenit t\u00eb lumenjve t\u00eb Shqip\u00ebris\u00eb, nd\u00ebrsa si prurje mesatare duhet t\u00eb p\u00ebrcjell\u00eb 679 m3\/sek ose 52 % t\u00eb prurjeve mes t\u00eb gjith\u00eb lumenjve t\u00eb vendit. Lumi Buna n\u00eb dalje t\u00eb liqenit t\u00eb Shkodr\u00ebs ka kuot\u00ebn 9,2 m, n\u00eb takimin me lumin Drin ka kuot\u00ebn 8,2m – 8,5 m, n\u00eb fushat e B\u00ebrdic\u00ebs 6,2 m, Obotit 5,4 m, n\u00eb Pentar 3 m. N\u00eb takimin e Kirit me Drinin, kuota arrin 8,9 m, nd\u00ebrsa zona urbane e past\u00ebr e Shkodr\u00ebs fillon mbi kuot\u00ebn 10 m.<\/p>\n

Edhe kuotat e m\u00ebsip\u00ebrme kan\u00eb vite q\u00eb nuk jan\u00eb azhornuar dhe mund t\u00eb jen\u00eb mbushur. Nga sa kuptohet, uji i lumit Buna duhet t\u00eb udh\u00ebtoj\u00eb 41 km me nj\u00eb diferenc\u00eb kuote jo m\u00eb shum\u00eb se 8 m. Sipas nj\u00eb studimi hidroteknik, delta e Bun\u00ebs duhet t\u00eb jet\u00eb gjithmon\u00eb 4 m nga niveli i bregut t\u00eb detit. Nga ana jon\u00eb \u00ebsht\u00eb fotografuar delta e Bun\u00ebs n\u00eb muajin gusht 2007 \u2013 2008 dhe rezulton se rrjedha e Bun\u00ebs si nivel nuk \u00ebsht\u00eb m\u00eb i thell\u00eb se bregdeti.<\/p>\n

Si rezultat i aluvioneve, delta e Bun\u00ebs ka nj\u00eb zgjatim n\u00eb form\u00eb elipsi, e futur rreth 3 km n\u00eb det m\u00eb shum\u00eb se brigjet an\u00ebsore dhe nga ana detare gjithmon\u00eb mbetet n\u00ebn ndikimin e korrenteve jug\u2013per\u00ebndimore. Kur niveli i detit ngrihet 60 \u2013 100 cm (q\u00eb \u00ebsht\u00eb normale n\u00eb dim\u00ebr) uj\u00ebrat detare dep\u00ebrtojn\u00eb deri n\u00eb 5-6 km n\u00eb brend\u00ebsi t\u00eb Bun\u00ebs. Dhe kur ka prurje nga liqeni i Shkodr\u00ebs, nivelet detare bllokojn\u00eb uj\u00ebrat e \u00ebmbla t\u00eb Bun\u00ebs, shkarkimet ngadal\u00ebsohen, Buna fryhet, e p\u00ebr rrjedhoj\u00eb, p\u00ebrmbyten menj\u00ebher\u00eb fushat e Obotit, Samrishtit, Pentarit, etj.<\/p>\n

Kur n\u00eb t\u00eb nj\u00ebjt\u00ebn koh\u00eb ka ngritje t\u00eb nivelit t\u00eb detit, rriten prurjet nga liqeni i Shkodr\u00ebs dhe prurjet nga shkarkesat e kaskad\u00ebs s\u00eb Drinit, Kirit ose si\u00e7 shprehen specialist\u00ebt, prurjet interferohen n\u00eb nj\u00ebsit\u00eb kohore, p\u00ebrmbyten menj\u00ebher\u00eb edhe zonat e Asht\u00ebs, Kolgjinit, Daj\u00e7it, Trushit, Melgush\u00ebs, Lek\u00ebs, etj. Sipas llogaritjeve, n\u00eb shtratin e Bun\u00ebs ka mbi 25 vjet q\u00eb nuk ka v\u00ebn\u00eb dor\u00eb njeri. Kjo gjendje \u00ebsht\u00eb me rezerva edhe n\u00eb infrastruktur\u00ebn mbrojt\u00ebse t\u00eb argjinaturave, veprave t\u00eb artit dhe sistemit t\u00eb kullimit.<\/p>\n

N\u00eb k\u00ebto kushte, seksioni i shtratit t\u00eb Bun\u00ebs nuk p\u00ebrcjell as gjysm\u00ebn e plotave, me siguri 2 % vet\u00ebm t\u00eb liqenit t\u00eb Shkodr\u00ebs, t\u00eb cilat jan\u00eb t\u00eb panjohura dhe t\u00eb padisiplinuara. N\u00eb vazhdim, shtrohet pyetja: \u00c7far\u00eb k\u00ebrkojn\u00eb shqiptar\u00ebt nga shtrati i lumit t\u00eb Bun\u00ebs, i cili p\u00ebr nga funksioni duhet t\u00eb p\u00ebrcjell\u00eb 45 % t\u00eb v\u00ebllimit t\u00eb uj\u00ebrave t\u00eb vendit, nd\u00ebrsa p\u00ebr nga interesi ekonomik krahasohet me Kanalin e Suezit. P\u00ebrfitimi nga veprat e kaskad\u00ebs s\u00eb Drinit, p\u00ebrfitimet nga liqeni i Shkodr\u00ebs dhe p\u00ebrfitimet nga veprat e kullimit e ujitjes t\u00eb ult\u00ebsir\u00ebs s\u00eb Shkodr\u00ebs jan\u00eb minimalisht 3,5 milion\u00eb euro\/dit\u00eb.<\/p>\n

Kjo e ardhur ditore krahasohet me t\u00eb ardhurat q\u00eb siguron tranziti n\u00eb Kanalit t\u00eb Suezit, i cili p\u00ebrfiton mbi 5 milion\u00eb dollar\u00eb\/dit\u00eb. Por, kanali i Suezit, p\u00ebr t\u00eb mir\u00ebmbajtur thell\u00ebsin\u00eb dhe dimensionet, e mban t\u00eb angazhuar Drag\u00ebn, e cila ka kushtuar 100 milion\u00eb euro. Por, kanali i Suezit 52 km lidh detin Mesdhe me Detin e Kuq, duke i shkurtuar 11 700 km \u00e7do udh\u00ebtimi nga Europa p\u00ebr n\u00eb lindje dhe anasjelltas. Dhe me t\u00eb drejt\u00eb \u00ebsht\u00eb shpallur trash\u00ebgimi komb\u00ebtare dhe bot\u00ebrore, duke u ruajtur e mir\u00ebmbajtur me nj\u00eb status t\u00eb ve\u00e7ant\u00eb.<\/p>\n

Por n\u00eb kuptimin ekonomik, Suezi nuk ka ndonj\u00eb ndryshim nga shkarkuesi i Bun\u00ebs, i cili \u00ebsht\u00eb pjes\u00eb e nj\u00eb skeme ekonomike nga p\u00ebrfitohet mbi 30 % e t\u00eb ardhurave komb\u00ebtare. Por, duke qen\u00eb se shteti shqiptar historikisht nuk \u00ebsht\u00eb marr\u00eb me vlerat ekonomike t\u00eb pasurive komb\u00ebtare, nuk e ka konceptin e r\u00ebnd\u00ebsis\u00eb, kostos dhe funksionit t\u00eb Bun\u00ebs. Sikur 1\/1000 e t\u00eb ardhurave nga kaskada e Drinit t\u00eb investohej n\u00eb p\u00ebrmir\u00ebsimin e vazhduesh\u00ebm t\u00eb sistemimit Bun\u00eb\u2013bregdet\u2013ult\u00ebsir\u00eb, nuk do t\u00eb arrihej niveli i p\u00ebrmbytjeve t\u00eb fillimit dhe funditvitit.<\/p>\n

Si konkluzion, shtrati i Bun\u00ebs ka nevoj\u00eb p\u00ebr nj\u00eb studim dhe sistemim kompleks n\u00eb marr\u00ebdh\u00ebnie t\u00eb ngusht\u00eb me plotat e liqenit t\u00eb Shkodr\u00ebs, n\u00eb marr\u00ebdh\u00ebnie t\u00eb ngusht\u00eb me shkarkimet, devijimet, ndarjet e Drinit, n\u00eb lidhje t\u00eb ngusht\u00eb me aft\u00ebsin\u00eb p\u00ebrcjell\u00ebse t\u00eb Drinit t\u00eb vjet\u00ebr, n\u00eb marr\u00ebdh\u00ebnie t\u00eb ngusht\u00eb me nivelet detare dhe bregdetare, n\u00eb marr\u00ebdh\u00ebnie t\u00eb ngusht\u00eb me depresionet e relievit t\u00eb ult\u00ebsir\u00ebs s\u00eb Shkodr\u00ebs, etj. Nga ana jon\u00eb ofrohen zgjidhje q\u00eb mund t\u2019i sh\u00ebrbejn\u00eb multifunksionit t\u00eb bypass-it natyral t\u00eb Bun\u00ebs.<\/p>\n

P\u00ebrmbytjet<\/strong><\/p>\n

E gjith\u00eb ult\u00ebsira nga Buna n\u00eb gjurm\u00ebn e vjet\u00ebr t\u00eb Drinit formon ult\u00ebsir\u00ebn e Shkodr\u00ebs. Natyrisht, kjo dhurat\u00eb natyrore \u00ebsht\u00eb produkt i aluvioneve t\u00eb Drinit dhe Bun\u00ebs. N\u00eb konceptin fizik, ult\u00ebsira e Shkodr\u00ebs, s\u00eb bashku me kurrizin e zgjatur t\u00eb Torovic\u00ebs, \u201cballkonin\u201d e zgjatur natyral t\u00eb malit t\u00eb Rencit, kojkat e Bushatit, Melgush\u00ebs, Syk Daj\u00e7it, Gjymlit, Baks Rrjollit, Re\u00e7it, t\u00eb mbira n\u00eb mes t\u00eb luginave, formojn\u00eb n\u00eb lidhje edhe me bregdetin, formacionet bujq\u00ebsore m\u00eb t\u00eb arrira p\u00ebr t\u00eb prodhuar dhe jetuar n\u00eb lart\u00ebsi. Nuk ka asnj\u00eb vend tjet\u00ebr n\u00eb bot\u00eb ku fushat jan\u00eb sistemuar, kulluar dhe ujitur si n\u00eb Shqip\u00ebri.<\/p>\n

Por, t\u00eb v\u00ebshtrosh n\u00eb pranver\u00eb ult\u00ebsir\u00ebn e Shkodr\u00ebs nga lart\u00ebsit\u00eb e Torovecit, Rencit, Bushatit, Syk Daj\u00e7it e Re\u00e7it gjendesh para nj\u00eb vizatimi teknik natyral, ku vijat e kanaleve kullues, ngastrave, rrug\u00ebve, argjinaturave t\u00eb orientuara nga drejtimet e rrjedhjeve, me nj\u00eb sakt\u00ebsi inxhinierike jan\u00eb materializuar n\u00eb fush\u00eb, duke krijuar nj\u00eb vep\u00ebr arti n\u00eb mjesht\u00ebrin\u00eb e sistemimit t\u00eb tok\u00ebs. Por, ka ardhur koha q\u00eb ult\u00ebsira e Shkodr\u00ebs t\u00eb ristudiohet n\u00eb kuadrin e nj\u00eb sistemimi kompleks t\u00eb Bun\u00ebs e Vilunit dhe bregdetit.<\/p>\n

Natyrisht, sistemimi i tokave bujq\u00ebsore \u00ebsht\u00eb produkt i nivelit hidroteknik dhe agronomik. Por, sistemimi, kullimi dhe mbrojtja e ult\u00ebsir\u00ebs s\u00eb Shkodr\u00ebs \u00ebsht\u00eb realizuar me shum\u00eb v\u00ebshtir\u00ebsi n\u00eb 2-3 dekada, q\u00eb n\u00ebnkupton se funksionimi i rrjetit t\u00eb sistemimit nuk \u00ebsht\u00eb \u00e7\u00ebshtje thjesht e nj\u00eb qeverie. Kjo n\u00ebnkupton se studimi kompleks dhe rikonstruksioni i ult\u00ebsir\u00ebs s\u00eb Shkodr\u00ebs k\u00ebrkon 5-10 vite pun\u00eb.<\/p>\n

Duke lundruar n\u00eb pasqyr\u00ebn ujore t\u00eb pal\u00ebvizshme t\u00eb p\u00ebrmbytjeve n\u00eb ult\u00ebsir\u00ebn e Shkodr\u00ebs, kur nivelet ishin kritike dhe ca kilometra m\u00eb tej, nyjat e bllokuara t\u00eb shkarkimeve, ndien keqardhje q\u00eb pasurit\u00eb komb\u00ebtare mbysin nj\u00ebra-tjetr\u00ebn dhe shmanget eksperienca hidroteknike vendore p\u00ebr nj\u00eb ult\u00ebsir\u00eb q\u00eb prodhon deri n\u00eb 10 % t\u00eb prodhimeve bujq\u00ebsore shqiptare.<\/p>\n","protected":false},"excerpt":{"rendered":"

Nga: XHEVAHIR NGJEQARI, 03 Dhjetor 2010 Nivelet e vazhdueshme t\u00eb uj\u00ebrave p\u00ebrmbyt\u00ebse n\u00eb Ult\u00ebsir\u00ebn e Shkodr\u00ebs dhe Lezh\u00ebs, nga datat 27 dhjetor 2009 – 12-17 janar 2010, p\u00ebrmbytjet pjesore n\u00eb muajin shkurt dhe rip\u00ebrmbytjet… n\u00eb muajin dhjetor 2010 n\u00eb t\u00eb dyja an\u00ebt e shtratit t\u00eb Bun\u00ebs, v\u00ebrtetuan se marr\u00ebdh\u00ebniet hidroteknike midis gjirit t\u00eb Drinit (niveleve […]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[2],"tags":[],"class_list":{"0":"post-4999","1":"post","2":"type-post","3":"status-publish","4":"format-standard","6":"category-artikuj"},"yoast_head":"\nP\u00ebrmbytjet, zgjidhjet p\u00ebr lumin Buna - FjALA e LIR\u00cb - Arkivi<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/fjala.info\/2009-2015\/permbytjet-zgjidhjet-per-lumin-buna\/\" \/>\n<meta property=\"og:locale\" content=\"sq_AL\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"P\u00ebrmbytjet, zgjidhjet p\u00ebr lumin Buna - 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