Drilling Success in Geothermal Fields Utilized by Major District Heating Services in Iceland

Total Page:16

File Type:pdf, Size:1020Kb

Drilling Success in Geothermal Fields Utilized by Major District Heating Services in Iceland Drilling Success in Geothermal Fields Utilized by Major District Heating Services in Iceland Björn Már Sveinbjörnsson Prepared for Orkustofnun (National Energy Authority of Iceland, NEA) Í SOR-2018/043 ICELAND GEOSURVEY Reykjavík: Orkugardur, Grensásvegur 9, 108 Reykjavík, Iceland - Tel.: 528 1500 - Fax: 528 1699 Akureyri: Rangárvellir, P.O. Box 30, 602 Akureyri, Iceland - Tel.: 528 1500 - Fax: 528 1599 [email protected] - www.isor.is Report Project no.:15-0252 Drilling Success in Geothermal Fields Utilized by Major District Heating Services in Iceland Björn Már Sveinbjörnsson Prepared for Orkustofnun (National Energy Authority of Iceland, NEA) ÍSOR-2018/043 August 2018 Key page Report no. Date Distribution ÍSOR-2018/043 August 2018 Open Closed Report name / Main and subheadings Number of copies Drilling Success in Geothermal Fields Utilized by Major District 3 Heating Services in Iceland Number of pages 200 + Appendix Authors Project manager Björn Már Sveinbjörnsson Steinunn Hauksdóttir Classification of report Project no. 15-0252 Prepared for Orkustofnun (National Energy Authority of Iceland) Cooperators N/A Abstract The report describes success of 446 production wells drilled in the years 1928-2017 in 63 low- and medium enthalpy geothermal fields which are exploited by the 64 major district heating services in Iceland. The dataset on which the report is based has been collected from the National Well Registry of boreholes and available reports. To the extent verifiable data are available, the assembled dataset is presented in an Excel document accompanying the report on CD. About 93% of the drilled wells were productive, i.e. encountered feeders that could yield a flow from the well. Of the productive wells 164 are still in use, with an average production capacity of 31.7 l/s at 90.3°C. The main reasons for productive wells not in use are: a) drawdown of reservoir pressure, b) replaced by better wells or c) idle but could produce. About 49% of the main feeders are shallower than 500 m, 76% are shallower than 1,000 m and 95% are shallower than 1,600 m. About 88% of the 446 drilled production wells fulfilled the minimum criterion set for space heating of a discharge temperature of 60°C and 65% fulfilled the criterion of 80°C discharge temperature. The far largest low enthalpy geothermal field, Reykir in Mosfellsbær, has a present production capacity equivalent to 1.800 l/s of 85.4°C hot water or a thermal power potential of 367 MWth above 35°C. The largest well fields, Æsustaðir and Suður-Reykir, in the Reykir field have a thermal power potential above 35°C of 139.7 and 96.7 MWth respectively. The total thermal power potential of all the geothermal fields exploited by the 64 major district heating services is equivalent to 1,770 MWth above 35°C. Key words ISBN-number Low enthalpy geothermal fields, medium enthalpy geothermal fields, productivity of wells, drilling Project manager’s signature success, thermal power potential, Iceland Reviewed by BS, SThor, SvB Table of contents 1 Introduction ....................................................................................................................... 17 1.1 Potential for exploitation ............................................................................................ 18 1.1.1 Thermal power potential ................................................................................ 18 1.1.2 Geothermal utilization .................................................................................... 18 2 Definitions and Overview of the Dataset .................................................................... 19 2.1 Location of well ............................................................................................................ 20 2.2 Well status ..................................................................................................................... 20 2.3 Description of well ....................................................................................................... 21 2.4 Reservoir characteristics.............................................................................................. 21 2.5 Production characteristics ........................................................................................... 22 2.6 Thermal power potential of well field and geothermal field ................................. 22 3 Overview of the Major Geothermal District Heating Services in Iceland ............. 22 3.1 Largest operators of district heating services .......................................................... 22 3.2 Location of the major geothermal district heating services ................................... 23 4 Results of Drilling ............................................................................................................ 26 4.1 Seltjarnarnes .................................................................................................................. 26 4.1.1 Seltjarnarnes District Heating ........................................................................ 26 4.2 Reykjavík ....................................................................................................................... 28 4.2.1 Reykjavík District Heating (Veitur) ............................................................... 28 4.3 Mosfellsbær ................................................................................................................... 37 4.3.1 Mosfellsbær District Heating (Veitur) ........................................................... 37 The Suður-Reykir subfield ........................................................................................ 41 4.4 Kjósarhreppur ............................................................................................................... 50 4.4.1 Kjós District Heating (Kjósarveita) ................................................................ 50 4.4.2 Hvammsvík District Heating (Veitur) .......................................................... 51 4.5 Skorradalshreppur ....................................................................................................... 51 4.5.1 Skorradalur District Heating (Veitur) ........................................................... 51 4.6 Borgarbyggð ................................................................................................................. 52 4.6.1 Akranes/Borgarfjörður District Heating (Veitur) ........................................ 55 4.6.2 Húsafell District Heating ................................................................................ 58 4.6.3 Reykholt District Heating ............................................................................... 58 4.6.4 Kleppjárnsreykir District Heating ................................................................. 59 4.6.5 Brúarreykir District Heating ........................................................................... 60 4.6.6 Varmaland District Heating ........................................................................... 60 4.6.7 Stafholtstungur District Heating .................................................................... 61 4.6.8 Munaðarnes District Heating (Veitur) .......................................................... 61 4.6.9 Norðurárdalur District Heating (Veitur) ...................................................... 63 4.7 Helgafellssveit .............................................................................................................. 64 4.7.1 Stykkishólmur District Heating (Veitur) ...................................................... 64 - 5 - 4.8 Dalabyggð ..................................................................................................................... 67 4.8.1 Dalabyggð District Heating (RARIK) ............................................................ 67 4.9 Reykhólahreppur ......................................................................................................... 68 4.9.1 Reykhólar District Heating (OV) ................................................................... 68 4.9.2 Thorverk Seaweed Plant ................................................................................. 69 4.10 Ísafjarðarbær ............................................................................................................... 69 4.10.1 Suðureyri District Heating (OV) .................................................................. 69 4.11 Kaldrananeshreppur .................................................................................................. 70 4.11.1 Drangsnes District Heating .......................................................................... 70 4.12 Húnaþing Vestra ........................................................................................................ 71 4.12.1 Húnaþing Vestra District Heating ............................................................... 71 4.12.1 Hvammstangi/Laugarbakki District Heating ............................................ 73 4.13 Húnavatnshreppur .................................................................................................... 74 4.13.1 Blönduós District Heating (RARIK) ............................................................ 74 4.13.2 Skagaströnd District Heating (RARIK) ....................................................... 75 4.14 Skagafjörður ................................................................................................................ 75 4.14.1 Steinsstaðir District Heating (SKV) ............................................................
Recommended publications
  • ANDI SNÆFELLSNESS Auðlind Til Sóknar
    ANDI SNÆFELLSNESS auðlind til sóknar Svæðisskipulag Snæfellsness 2014-2026 2 Andi Snæfellsness - auðlind til sóknar Andi Snæfellsness - auðlind til sóknar Svæðisskipulag Snæfellsness 2014-2026 Eyja- og Miklaholtshreppur Helgafellssveit Grundarfjarðarbær Snæfellsbær Stykkishólmsbær Alta ehf www.alta.is 3 Efnisyfirlit Efnisyfirlit Áherslur .................................................................................................16 Skýr mynd af svæðinu sem heild ..................................................................... 16 Um svæðisskipulagsáætlunina Nýting sérkenna svæðisins innan atvinnugreina............................................ 16 Svæðisskipulagstillaga .............................................................................8 Atvinnugreinar tvinnaðar saman ..................................................................... 19 Kynning tillögunnar ............................................................................................ 8 Breið verðmætasköpun .................................................................................. 19 Auglýsing tillögunnar ......................................................................................... 8 Sjálfbær nýting auðlinda og efling sameiginlegra innviða ........................... 20 Afgreiðsla að aflokinni auglýsingu .................................................................... 9 Víðtækt samráð ............................................................................................... 20 Aðilar.....................................................................................................10
    [Show full text]
  • Nr. 15 24. Mars 2003 Um Breyting Á Lögum Um Kosningar Til Alþingis, Nr. 24/2000. Gjörir Kunnugt: Alþingi Hefur Fallist
    Nr. 15 24. mars 2003 LÖG um breyting á lögum um kosningar til Alþingis, nr. 24/2000. FORSETI ÍSLANDS gjörir kunnugt: Alþingi hefur fallist á lög þessi og ég staðfest þau með samþykki mínu: 1. gr. 1.–3. tölul. 1. mgr. 6. gr. laganna orðast svo: 1. Norðvesturkjördæmi. Til þess teljast eftirtalin sveitarfélög: Akraneskaupstaður, Hvalfjarðarstrandarhreppur, Skil- mannahreppur, Innri-Akraneshreppur, Leirár- og Melahreppur, Skorradalshreppur, Borgar- fjarðarsveit, Hvítársíðuhreppur, Borgarbyggð, Kolbeinsstaðahreppur, Eyja- og Miklaholts- hreppur, Snæfellsbær, Grundarfjarðarbær, Helgafellssveit, Stykkishólmsbær, Dalabyggð, Saur- bæjarhreppur, Reykhólahreppur, Vesturbyggð, Tálknafjarðarhreppur, Bolungarvíkurkaupstaður, Ísafjarðarbær, Súðavíkurhreppur, Árneshreppur, Kaldrananeshreppur, Hólmavíkurhreppur, Broddaneshreppur, Bæjarhreppur, Húnaþing vestra, Áshreppur, Sveinsstaðahreppur, Torfa- lækjarhreppur, Blönduósbær, Svínavatnshreppur, Bólstaðarhlíðarhreppur, Höfðahreppur, Skagabyggð, Sveitarfélagið Skagafjörður og Akrahreppur. 2. Norðausturkjördæmi. Til þess teljast eftirtalin sveitarfélög: Siglufjarðarkaupstaður, Ólafsfjarðarbær, Grímseyjar- hreppur, Dalvíkurbyggð, Hríseyjarhreppur, Arnarneshreppur, Hörgárbyggð, Akureyrar- kaupstaður, Eyjafjarðarsveit, Svalbarðsstrandarhreppur, Grýtubakkahreppur, Þingeyjarsveit, Skútustaðahreppur, Aðaldælahreppur, Húsavíkurbær, Tjörneshreppur, Kelduneshreppur, Öxar- fjarðarhreppur, Raufarhafnarhreppur, Svalbarðshreppur, Þórshafnarhreppur, Skeggjastaða- hreppur, Vopnafjarðarhreppur, Norður-Hérað, Fljótsdalshreppur,
    [Show full text]
  • Chemical Variety of Water in Icelandic Heating Systems
    Proceedings World Geothermal Congress 2010 Bali, Indonesia, 25-29 April 2010 Chemical Variety of Water in Icelandic Heating Systems Hrefna Kristmannsdóttir1, Stefán Arnórsson2, Árný Sveinbjörnsdóttir2 and Halldór Ármannsson3 1University of Akureyri, Borgir Nordurslod, 600 Akureyri, Iceland, 2Institute of Earth Sciences, University of Iceland, IS-107 Reykjavík, 3Ísor, Grensásvegur 9, 108 Reykjavík, Iceland [email protected] of oxygen, waters devoid of hydrogen sulfide and even Keywords: Heating systems, geochemistry, geothermal carbonated water. Waters with extreme high pH, 10-11, are waters, production properties also encountered. By time and increased utilization of ABSTRACT geothermal resources for heating there have been utilized geothermal waters with a very varied geochemical properties Icelandic heating systems are traditionally of very simple in the Icelandic heating systems. design; water is pumped up from the wells, distributed to the users who use the water directly for heating and as tap water without using heat exchangers. The spent water is mostly 1. INTRODUCTION disposed of into the sewer or possibly first used for melting Recently a comprehensive study of the geochemisty of snow in the driveway or for the domestic hot pool. This is Icelandic groundwaters with the emphases on trace elements based on the reality that commonly the geothermal water is has been conducted (Kristmannsdóttir et al., 2005a). Within slightly mineralized, typically with TDS 200-400 mg/l and the study the chemical characteristics of waters from most with a low corrosion and scaling potential. The pH is heating systems in the country have been anlysed and typically 9-10, devoid of oxygen and contains enough characterized and correlated to geological, geographical and hydrogen sulfide to act as an inbuilt corrosion inhibitor by meteorological conditions.
    [Show full text]
  • Demographic Trends in the Nordic Local Labour Markets
    Demographic trends in the Nordic local labour markets Appendix 2: Statistical tables Johanna Roto NORDREGIO WORKING PAPER 2012:13 Demographic trends in the Nordic local labour markets Annex of statistical tables List of tables Table 1: Nordic local labour markets and municipalities 3 Table 2: Nordic local labour markets with key demographic data 12 Table 1: Nordic local labour markets and municipalities 1. Nordic capitals Local Labour Including municipalities of: Market København Albertslund Frederikssund Herlev Køge Slagelse Allerød Furesø Hillerød Lejre Solrød Ballerup Gentofte Holbæk Lyngby-Taarbæk Sorø Brøndby Gladsaxe Hvidovre Næstved Stevns Dragør Glostrup Høje-Taastrup Odsherred Tårnby Egedal Greve Hørsholm Ringsted Vallensbæk Faxe Gribskov Ishøj Roskilde Vordingborg Fredensborg Halsnæs Kalundborg Rudersdal Frederiksberg Helsingør København Rødovre Helsinki Askola Järvenpää - Träskända Lapinjärvi - Lappträsk Nummi-Pusula Sipoo - Sibbo Espoo - Esbo Karjalohja - Karislojo Lohja - Lojo Nurmijärvi Siuntio - Sjundeå Hausjärvi Karkkila - Högfors Loppi Pornainen - Borgnäs Tuusula - Tusby Helsinki - Helsingfors Kauniainen - Grankulla Loviisa - Lovisa Porvoo - Borgå Vantaa - Vanda Hyvinkää - Hyvinge Kerava - Kervo Myrskylä - Mörskom Pukkila Vihti - Vichtis Ingå - Inkoo Kirkkonummi - Mäntsälä Riihimäki Kyrkslätt Höfuðbor- Akranes Garður Hvalfjarðarsveit Reykjanesbær Skorradalshreppur garsvæðið Álftanes Grímsnes- og Hveragerði Reykjavík Sveitarfélagið Árborg Grafningshreppur Bláskógabyggð Grindavík Kjósarhreppur Sandgerði Sveitarfélagið Vogar
    [Show full text]
  • Fylgiskjal4 Sérstakar Greiðslur
    Sérstakar greiðslur Fjársýslunnar til sveitarélaga Í mars og desember fengu sveitarfélögin greiðslu til að bæta þeim staðgreiðslu vegna frestun skattgreiðslna fyrirtækja. Úr hreyfingalista Sum of Upphæð í ISK Birgi Dagsetning Númer greiðslu Total Akrahreppur 18.3.2020 Brb-færsla v. Innh. -1.398.722 30.12.2020 Brb v.innheimtu -982.053 Akrahreppur Total -2.380.775 Akraneskaupstaður 18.3.2020 Brb-færsla v. Innh. -74.182.042 8.4.2020 Brb færsla v/innh. -4.252.311 30.12.2020 Brb v.innheimtu -55.069.359 Akraneskaupstaður Total -133.503.712 Akureyrarbær 18.3.2020 Brb-færsla v. Innh. -180.624.693 30.12.2020 Brb v.innheimtu -126.817.978 Akureyrarbær Total -307.442.671 Árneshreppur 18.3.2020 Brb-færsla v. Innh. -372.512 30.12.2020 Brb v.innheimtu -261.544 Árneshreppur Total -634.056 Ásahreppur 18.3.2020 Brb-færsla v. Innh. -1.781.987 30.12.2020 Brb v.innheimtu -1.251.147 Ásahreppur Total -3.033.134 Bláskógabyggð 18.3.2020 Brb-færsla v. Innh. -9.848.122 30.12.2020 Brb v.innheimtu -6.914.442 Bláskógabyggð Total -16.762.564 Blönduósbær 18.3.2020 Brb-færsla v. Innh. -8.351.541 16.4.2020 Brb færsla v/innh. -584.462 30.12.2020 Brb v.innheimtu -6.274.036 Blönduósbær Total -15.210.039 Bolungarvíkurkaupstaður 18.3.2020 Brb-færsla v. Innh. -9.353.516 31.3.2020 Brb færsla v/innh. -7.589.311 30.12.2020 Brb v.innheimtu -11.895.688 Bolungarvíkurkaupstaður Total -28.838.515 Borgarbyggð 18.3.2020 Brb-færsla v.
    [Show full text]
  • ICELAND 2006 Geodynamics Field Trip May 30 – June 8, 2006
    ICELAND 2006 Geodynamics Field Trip May 30 – June 8, 2006 Massachusetts Institute of Technology/ Woods Hole Oceanographic Institution Joint Program in Oceanography This field trip guide was compiled by Karen L. Bice using information from Bryndís Brandsdóttir, Richard S. Williams, Helgi Torfason, Helgi Bjornsson, Oddur Sigurðsson, the Iceland Tourist Board and World W. Web Maps from Thordarson and Hoskuldsson, 2002, Iceland (Classic Geology in Europe 3), Terra Publishing, UK. Logistical genius: Andrew T. Daly Field trip participants: Mark Behn, Karen Bice, Roger Buck, Andrew Daly, Henry Dick, Hans Schouten, Martha Buckley, James Elsenbeck, Pilar Estrada, Fern Gibbons, Trish Gregg, Sharon Hoffmann, Matt Jackson, Michael Krawczynski, Christopher Linder, Johan Lissenberg, Andrea Llenos, Rowena Lohman, Luc Mehl, Christian Miller, Ran Qin, Emily Roland, Casey Saenger, Rachel Stanley, Peter Sugimura, and Christopher Waters The Geodynamics Program is co-sponsored by Woods Hole Oceanographic Institution’s Academic Programs Office and Deep Ocean Exploration Institute. TUESDAY May 30 Estimated driving (km) Meet at Logan Airport, Icelandair ticket counter @ 7:00 PM (80 km ≈ 50 mi) Depart BOS 9:30 PM Icelandair flight Day 1 - WEDNESDAY May 31 Arrive Keflavík International Airport 6:30 AM (flight duration 5 hours) Pick up 2 vans, 2 trailers (Budget) Free day in Reykjavík Night @ Laugardalur campground, Reykjavík Dinner: on own in town Day 2 - THURSDAY June 1 270 Late start due to trailer problems (2 hrs @ AVIS) To Þingvellir N.P., then north to Hvalfjörður fjord, stop at Skorradalsvatn Night @ Sæberg Hostel (1 km. off Rte 1 in Hrútafjörður, west side of road) Tel. 354-4510015 Fax. 354-4510034 [email protected] Dinner: mexican-style chicken (Rachel, Trish, Chris) Day 3 - FRIDAY June 2 320 To Lake Myvatn Lunch stop in Akureyri, stop at Godafoss, stop at Skutustadir pseudocraters Night @ Ferdathjonustan Bjarg campsite, Reykjahlid, on shore of Lake Myvatn Tel.
    [Show full text]
  • Adobeps Tektronix Phaser 740, Job
    127. löggjafarþing 2001–2002. Þskj. 432 — 255. mál. Svar umhverfisráðherra við fyrirspurn Drífu Hjartardóttur um stuðning við framkvæmdir sveitar- félaga í fráveitumálum. 1. Hversu mörg sveitarfélög hafa lokið gerð heildaráætlana um úrbætur í fráveitumálum? Með umsókn sveitarfélaga um fjárstuðning vegna fráveituframkvæmda skal fylgja heildar- áætlun um fráveituframkvæmdir í sveitarfélaginu. Skilyrði fyrir fjárstuðningi er að fram- kvæmdin sé áfangi í heildarlausn á fráveitumálum. Öll sveitarfélög sem hafa fengið úthlutað styrkjum til fráveituframkvæmda hafa lokið gerð heildaráætlana fyrir þann hluta sveitar- félagsins sem hlutaðeigandi framkvæmdir ná yfir. Heimilt er að skipta heildaráætlun upp í einstaka hluta, svo sem fyrir einstaka þéttbýliskjarna og dreifbýlið, þar sem svo háttar til. Um 40 sveitarfélög í landinu hafi lokið gerð heildaráætlunar, sjá nánar svar við 3. spurningu. 2. Hvernig er stuðningi ríkisins háttað í þessum málum? Fjárhagslegur stuðningur ríkisins vegna fráveituframkvæmda sveitarfélaga getur sam- kvæmt 4. gr. laga nr. 53/1995, um stuðning við framkvæmdir sveitarfélaga í fráveitumálum, numið allt að 200 millj. kr. á ári, þó aldrei hærri upphæð en sem nemur 20% af staðfestum heildarraunkostnaði styrkhæfra framkvæmda næstliðins árs. Heimilt er að ráðstafa allt að fjórðungi styrkupphæðar á hverju ári í þeim tilgangi að jafna svo sem kostur er kostnað ein- stakra sveitarfélaga við fráveituframkvæmdir þegar miðað er við heildarkostnað á íbúa. Kostnaður sveitarfélaga vegna úrbóta er mjög breytilegur. Þegar jöfnunarákvæðum lag- anna var beitt í fyrsta sinn árið 1996 var við það miðað að meðaltalskostnaður sveitarfélaga vegna úrbóta í fráveitumálum í þéttbýli væri um 55.000 kr. á íbúa og byggðist það á reynslu- tölum. Kostnaður vegna sambærilegra framkvæmda í dreifbýli, þ.e.
    [Show full text]
  • Bú Með Greiðslumark Í Sauðfé 1.1.2019 Búsnúmer Heiti Bús
    Bú með greiðslumark í sauðfé 1.1.2019 Greiðslumark Búsnúmer Heiti bús Sveitarfélag ærgildi 1257127Krókur 0Reykjavík 76,7 1257461 Saurbær 0 Reykjavík 20,7 1169571 Vatnsendi 1000 Kópavogur 15,4 1179031 Garðav. Vestri Dysjar 1300Garðabær 15,2 1178971 Garðavegur Miðengi 1300 Garðabær 28,1 1178981Garðavegur Nýibær 1300Garðabær 18,1 1178992Garðavegur Pálshús 1300Garðabær 25,3 1232281Gesthús 1603Álftanes 6,3 1232411Sviðholt 1603Álftanes 24 1236361Helgadalur 1604Mosfellsbær 54,4 1236751Hraðastaðir 3 1604Mosfellsbær 61,9 1236771Hrísbrú 1604Mosfellsbær 9,5 1259871 Eyjar 2 1606 Kjósarhreppur 101,4 1260371Fell 1606Kjósarhreppur 252,1 1260381 Flekkudalur 1606 Kjósarhreppur 49,7 1260472Fremri Háls 1606Kjósarhreppur 33,8 1260521Grímsstaðir 1606Kjósarhreppur 129,4 1261071 Hvammur 1606 Kjósarhreppur 6,5 1261301Hækingsdalur 1606Kjósarhreppur 485,3 1261341Ingunnarstaðir 1606Kjósarhreppur 154,3 1261361Írafell 1606Kjósarhreppur 85,5 1261381 Káranes 1606 Kjósarhreppur 0,2 1261431Kiðafell 1606Kjósarhreppur 396,4 1261651Meðalfell 1606Kjósarhreppur 70,2 1263711 Miðdalur 1606 Kjósarhreppur 2,1 1264891þorláksstaðir 1606Kjósarhreppur 6,5 1291671 Bjarmaland 2300 Grindavík 5,5 1291681 Buðlunga 2300 Grindavík 42 1291751Hof 2300Grindavík 7,6 1291791Hraun 2300Grindavík 22,4 1291931 Járngerðarstaðir 2300 Grindavík 25,5 1291611Vík 2300Grindavík 30,9 1308341Efri Brunnastaðir 1 2506Vogar 17,7 1300101Hólkot 2510Suðurnesjabær 8,8 1300131Hólshús 2510Suðurnesjabær 10,9 1340421Grund 3506Skorradalshreppur 128,6 1340521Hálsar 3506Skorradalshreppur 10 1340871Mófellsstaðakot 3506Skorradalshreppur
    [Show full text]
  • 148. Löggjafarþing 2017–2018. Þingskjal 1344 — 401. Mál. Fjármála- Og Efnahagsráðherra Við Fyrirspurn Frá Óla B
    148. löggjafarþing 2017–2018. Þingskjal 1344 — 401. mál. Svar fjármála- og efnahagsráðherra við fyrirspurn frá Óla Birni Kárasyni um skatttekjur ríkissjóðs. 1. Hverjar voru heildartekjur ríkissjóðs af eftirtöldum skattstofnum árin 2009–2017, sundurgreindar eftir sveitarfélögum og árum: a. tekjuskatti einstaklinga, b. tekjuskatti lögaðila, c. tryggingagjaldi, d. eignarsköttum, e. veiðigjöldum? Fyrst skal tekið fram að nær ógerlegt er að sundurliða tekjur ríkissjóðs (samkvæmt árs- reikningi) eftir sveitarfélögum. Álagningu skatta á einstaklinga og lögaðila má hins vegar flokka eftir lögheimilissveitarfélagi gjaldanda. Töflur fyrir a–d-lið sýna álagða skatta og gjöld sem ríkisskattstjóri lagði á einstaklinga og lögaðila í hverju sveitarfélagi, fyrir árin 2010–2018 (vegna tekna áranna 2009–2017) í tilfelli einstaklinga, og fyrir árin 2010–2017 (vegna starfsemi 2009–2016) í tilfelli lögaðila, þar sem álagning lögaðila 2018 hefur ekki átt sér stað. Lög (og reglugerðir) um veiðigjald miðast við fiskveiðiár, fremur en almanaksár. Vegna þessa er nær ógerlegt að flokka álagningu veiðigjalds niður á almanaksár eftir sveitar- félögum. Auk þessa gæfi flokkun eftir sveitarfélagi gjaldanda veiðigjalds ekki mynd af því hvar starfsemin, sem gjaldið er lagt á, á sér stað – þar sem sveitarfélag gjaldanda og sveitar- félagið þar sem starfsemin á sér stað er mjög oft ekki hið sama. Vegna þessa liggja umbeðnar upplýsingar (e-liður) ekki fyrir. Aðra liði má sjá í meðfylgjandi töflum. Tekjuskattur einstak- linga er færður annars vegar sem brúttóupphæð álagningar, og hins vegar nettóupphæð álagn- ingar, þar sem búið er að draga frá þann persónuafslátt til útsvars sem greiddur er af ríkissjóði til sveitarfélaga fyrir hönd tekjulágra. Eignarskattar eru hér auðlegðarskattur og viðbótar- auðlegðarskattur, en álagning annarra tegunda eignarskatta, t.d.
    [Show full text]
  • Pálsson, Grétar Már. 2015
    Impact on households and critical infrastructures from electricity failure Two case studies and a survey on public preparedness Grétar Már Pálsson Faculty of Civil and Environmental Engineering University of Iceland 2015 Impact on households and critical infrastructures from electricity failure Two case studies and a survey on public preparedness Grétar Már Pálsson 30 ECTS thesis submitted in partial fulfillment of a Magister Scientiarum degree in Civil Engineering Advisors Dr. Björn Karlsson Böðvar Tómasson Faculty Representative Sveinn Júlíus Björnsson Faculty of Civil and Environmental Engineering School of Engineering and Natural Sciences University of Iceland Reykjavik, May 2015 Impact on households and critical infrastructures - Two case studies and a survey on public preparedness. 30 ECTS thesis submitted in partial fulfillment of a Magister Scientiarum degree in civil engineering Copyright © 2015 Grétar Már Pálsson All rights reserved Faculty of Civil and Environmental Engineering School of Engineering and Natural Sciences University of Iceland VR II, Hjarðarhaga 2-6 107, Reykjavik Iceland Telephone: 525 4600 Bibliographic information: Grétar Már Pálsson, 2015, Impact on households and critical infrastructures - Two case studies and a survey on public preparedness, Master’s thesis, Faculty of Civil and Environmental Engineering, University of Iceland, pp. 76. Printing: Háskólaprent, Fálkagata 2, 107 Reykjavík Reykjavik, Iceland, May 2015 Abstract This thesis studies the impact from electricity failure in Iceland on households and critical infrastructures. Households and critical infrastructures electricity dependence is discussed along with a theoretical identification of impacts towards these two subjects from electricity failure. Risk Assessment Plans for Iceland, Norway and Sweden are compared. The main focus of the comparison relates to how the countries focus on electricity, information and communication technologies and the role of the general public in these plans.
    [Show full text]
  • Direct Use of Geothermal Water for District Heating in Reykjavík And
    Proceedings World Geothermal Congress 2010 Bali, Indonesia, 25-29 April 2010 Direct Use of Geothermal Water for District Heating in Reykjavík and Other Towns and Communities in SW-Iceland Einar Gunnlaugsson, Gretar Ívarsson Reykjavík Energy, Bæjarháls 1, 110 Reykjavík, Iceland [email protected] Keywords: Direct use, District heating, Reykjavík, Iceland 3. GEOTHERMAL WATER FOR HOUSE HEATING In the Icelandic sagas, which were written in the 12th – ABSTRACT 13th century A.D., bathing in hot springs is often The geothermal district heating utility in Reykjavík is the mentioned. Commonly bath was taken in brocks where hot world´s largest geothermal district heating service. It started water from often boiling springs would be mixed with cold on a small scale in 1930 and today it serves the capital of water. The famous saga writer Snorri Sturluson lived at Reykjavík and surrounding communities, about 58 % of the Reykholt in west Iceland in the 13th century. At that time total population of Iceland. All houses in this area are there was a bath at his farm but no information about its heated with geothermal water. Three low-temperature age, size or structure. There are also implications that fields, Laugarnes, Elliðaaár and Reykir/Reykjahlíð are used geothermal water or steam was directed to the house for for this purpose along with geothermal water from the high- heating (Sveinbjarnardóttir 2005). temperature field at Nesjavellir. Reykjavík Energy is also operating district heating utilities in 7 other towns outside In a cold country like Iceland, home heating needs are the capital area with total 15.000 thousand inhabitants and 7 greater than in most countries.
    [Show full text]
  • Framhaldsskólasókn Vestlendinga: Hvetur Uppbygging Framhaldsskóla Á Vesturlandi Ungt Fólk Til Náms Strax Að Loknum Grunnskóla?
    ISSN 1670-5556 Vífill Karlsson Hagvísir Vesturlands Framhaldsskólasókn Vestlendinga: Hvetur uppbygging framhaldsskóla á Vesturlandi ungt fólk til náms strax að loknum grunnskóla? Skýrsla nr. 1 2006 Samtök sveitarfélaga á Vesturlandi Höfundur er atvinnuráðgjafi hjá SSV og dósent við Viðskiptaháskólann í Bifröst. Höfundarréttur © 2006 Vífill Karlsson og Samtök sveitarfélaga á Vesturlandi. SSV, þróun & ráðgjöf Framhaldsskólasókn Vestlendinga EFNISYFIRLIT 1 SAMANTEKT........................................................................................................................................3 2 INNGANGUR.........................................................................................................................................4 3 FYRRI RANNSÓKNIR.........................................................................................................................4 4 GREINING.............................................................................................................................................5 4.1 SUÐ -VESTURLAND ............................................................................................................................7 4.2 NORÐ -VESTURLAND .........................................................................................................................9 5 NIÐURSTÖÐUR..................................................................................................................................12 6 HEIMILDASKRÁ ...............................................................................................................................12
    [Show full text]