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Undersökning Av Mindre Förkastningar För Vattenuttag I Sedimentärt Berg Kring Kingelstad Och Tjutebro

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Undersökning Av Mindre Förkastningar För Vattenuttag I Sedimentärt Berg Kring Kingelstad Och Tjutebro Undersökning av mindre förkastningar för vattenuttag i sedimentärt berg kring Kingelstad och Tjutebro Per Wahlquist Examensarbeten i geologi vid Lunds universitet, kandidatarbete, nr 577 (15 hp/ECTS credits) Geologiska institutionen Lunds universitet 2019 Undersökning av mindre förkastningar för vattenuttag i sedimentärt berg kring Kingelstad och Tjutebro Kandidatarbete Per Wahlquist Geologiska institutionen Lunds universitet 2019 Innehåll 1 Introduktion ...................................................................................................................................................... 7 1.1 Beskrivning av område 7 1.2 Geologin i området 7 1.2.1 Bergarter 7 1.2.2 Tektonik 9 1.2.3 Jordarter 10 2 Metod .............................................................................................................................................................. 12 2.1 Magnetometri 12 2.2 VLF 14 3 Resultat ............................................................................................................................................................. 15 3.1 Magnetometri 15 3.2 VLF 15 4 Diskussion ......................................................................................................................................................... 15 5 Slutsatser........................................................................................................................................................... 20 6 Tackord ............................................................................................................................................................. 20 7 Referenser ......................................................................................................................................................... 20 8 Bilaga ................................................................................................................................................................ 21 Omslagsbild: Översikt över sydöstra delen av undersökningsområdet. Foto: Per Wahlquist Undersökning av mindre förkastningar för vattenuttag i sediment- ärt berg kring Kingelstad och Tjutebro Per Wahlquist Wahlquist, P., 2019: Undersökning av mindre förkastningar för vattenuttag i sedimentärt berg kring Kingelstad och Tjutebro. Examensarbeten i geologi vid Lunds universitet, Nr. 577, 20 sid. 15 hp. Sammanfattning: På gränsen mellan Helsingborgs och Bjuvs kommun ligger ett område vars förutsättningar för grundvattenuttag bedöms vara dåliga. Av den anledning har en undersökning utförts över en förkastning, tolkad av SGU i just detta område, för att se om denna kan vara vattenförande eller om det kan finnas andra vattenförande strukturer i berget. Förkastningen och det omkringliggande området har undersökts med två olika geofysiska meto- der. Magnetometri har använts för att kartera diabasgångar i området och VLF (Very Low Frequency) har använts för att detektera elektriskt ledande strukturer samt dess egenskaper. Exempel på strukturer som detekterats är för- kastningen men även andra spricksystem kopplade till diabasgångarna och ett antal mänskliga strukturer som elled- ningar och vattenledningar har detekterats. Förkastningens egenskaper med avseende på vattenförande förmåga har ej kunnat bedömas utifrån mätningarna. Dock har ett par sprickor kopplade till diabasgångar uppvisat att de kan vara saltvattenförande medan andra uppvisat att de kan vara färskvattenförande. Antalet diabasgångar som karterats i området har varit stort, vilket kan tyda på att berggrunden allmänt är mer uppspräckt och troligen mer vattenfö- rande än annars kunnat väntas. Nyckelord: Kingelstad, Tjutebro, magnetometri, VLF, grundvatten, Handledare: Jesper Sjolte Geologiska institutionen, Peter Dahlqvist SGU, Mattias Gustafsson SGU, Virginie Le- roux SGU Ämnesinriktning: Berggrundsgeologi Per Wahlquist, Geologiska institutionen, Lunds universitet, Sölvegatan 12, 223 62 Lund, Sverige. E-post: [email protected] Survey of minor fault for water outtake in sedimentary rocks around Kingelstad and Tjutebro Per Wahlquist Wahlquist, P., 2019: Survey of minor fault for water outtake in sedimentary rocks around Kingelstad and Tjutebro. Dissertations in Geology at Lund University, No. 577, 20 pp. 15 hp (15 ECTS credits) . Abstract: In an area on the border between Helsingborg and Bjuv municipality a fault has been mapped by the Swedish Geological Survey (SGU) and since this area have poor prerequisites for groundwater outtake this is of big interest. This is also the reason why this survey have been carried out to try to identify if the fault is water-bearing and to find its position with a better accuracy then could be gathered during the SGU survey. To do this two geo- physical measurement methods was used. The first one being magnetometry to identify dolerite dikes known to cross the area so that these would not be mixed up with the fault in the second measurement method but also be- cause dolerite dikes are known to fracture surrounding bedrock and make it more water-bearing. The second meth- od to be used was VLF or “Very Low Frequency” which can detect conductive structures and their properties. This method detected the fault, fracture zones around some dolerite dikes but it also detected electric cabals from the power grid and a big water pipe. If the fault is water-bearing or not have not been able to be determined but some of the fracture zones have shown signs of saltwater will others shown signs of freshwater. Also the sheer amount of dolerite dikes could also be a sign that the older bedrock of the area is more water-bearing then would otherwise been expected. Keywords: Kingelstad, Tjutebro, magnetometry, VLF, groundwater Supervisors: Jesper Sjolte Department of Geology, Peter Dahlqvist SGU, Mattias Gustafsson SGU, Virginie Leroux SGU Subject: Bedrock Geology Per Wahlquist, Department of Geology, Lund University, Sölvegatan 12, SE-223 62 Lund, Sweden. E-mail: [email protected] 1 Introduktion ningen. Denna damm ligger söder om fäladsmarken I området nordöst om Kingelstad, på gränsen mellan och ut med Tjutebäcken. Någon vattenförande spricka Helsingborgs och Bjuvs kommun, finns en mindre eller förkastning noterades inte vid anläggningen av förkastning kopplad till Tornquistzonen (Fig. 1 & 2). denna damm (personlig kontakt). I sydligaste delen av Vid anläggning av vattenledningen mellan Ringsjöver- området finns två gamla stenbrott där det brutits diabas ket och Helsingborg påträffades ett mycket vattenfö- för användning som makadam. Idag är båda stenbrot- rande parti som sammanföll med var förkastningen ten vattenfyllda och det större av dessa, Rönnarps sten- hade karterats. Då området annars har dåliga eller brott, håller delvis på att återfyllas. mycket dåliga möjligheter för grundvattenuttag kan en Tvärs över området går två mycket stora kraftled- sådan förekomst vara mycket värdefull för vattenför- ningar som går i nordnordväst-sydsydöstlig riktning, sörjningen i området. nästan parallellt med förkastningen som undersöks, Projektets syfte är att ge en bättre bild av förutsätt- varav den ena halvvägs in på området viker av mot ningarna för grundvattenuttag i områden kring Tor- sydsydväst. Det finns även ett stort antal mindre elled- nquistzonens mindre förkastningar. Ett andra syfte ningar som förser fastigheterna inom området med med projektet är att utvärdera nyttan av SGU:s berg- ström. Dessa ledningar går antingen längs med vägar grundskartor, mineralsammansättning kontra bergart, eller sporadiskt över fält. Länsväg 110 korsar området samt på vilket sätt de kan användas med bästa resultat. i nord-sydlig riktning men även några större landsvä- Målet med projektet är att med hjälp av geofysiska gar går över området tillsammans med ett stort antal mätmetoder undersöka om förkastningen: mindre vägar. • går att detektera i de två olika typerna av 1.2 Geologin i området sedimentärt berg som denna löper genom. Geologin i undersökningsområdet präglas huvudsakli- gen av tre olika formationer/bergarter (Fig. 3). Dessa har också formats av det tektoniska spricksystem som • har tecken på lervittring eller vattenföre- den undersökta förkastningen härrör från (Fig. 4). Om- komst då detta är viktigt för eventuellt vat- rådets jordtäcke är tätt knutet till berggrunden då mäk- tenuttag. tigheten och variationer i sammansättning ofta kan kopplas till berggrundens överyta och dess samman- 1.1 Beskrivning av området sättning (Fig. 5). Området är karakteriserat av ett öppet jordbruksland- skap med märgelgravar och trädbeväxta stengärden 1.2.1 Bergarter (Fig. 2). Ett mindre skogsparti återfinns i centrala de- Den äldsta bergarten vi hittar i området är den siluriska len av området och utgörs huvudsakligen av bok och colonusskiffern som är avsatt i en marin miljö (Sivhed blandskog. Även ett fäladsområde finns i nordvästra delen av området. Denna fäladsmark ligger längs med en av de större bäckarna som rinner genom området, Tjutebäcken. Ett antal bevattningsdammar återfinns också i området varav två endast några hundra meter från förkastningen och en som ska skäras av förkast- Fig. 2. Undersökningen domineras av ett öppet jordbruks- Fig. 1. Röda fyrkanten markerar undersökningsområdets landskap. Förkastningen som den är tolkad i SGUs (Sveriges placering i västra Skåne. geologiska undersökning) kartor. 7 & Wikman 1986). Colonusskiffern är en lerskiffer bästa platserna för att se skiffern men även i den be- med en hög halt av grovsilt och finsand som ligger på vattningsdamm som finns centralt i undersökningsom- 20–40% medan
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