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Neben Messungen an der Erdoberfläche können mit speziellen Messsonden physikalische Parameter in Bohrlöchern beobachtet werden. Am HLNUG gibt es hierfür eine Multisonde mit drei Aufnehmern in einem Gehäuse, die an einem Messkabel mit einer elektrischen Winde bis zu 500 m tief kontinuierlich Messwerte aufzeichnen kann. Beobachtet werden mit dieser Apparatur die natürliche Gammastrahlung, die Temperatur und die elektrische Leitfähigkeit, bzw. ihr Kehrwert, der elektrische Widerstand.<\/SPAN>Die Gammastrahlung zeigt vornehmlich den Tongehalt des Untergrunds an, weil Ton einen besonders hohen Anteil des radioaktiven Kaliumisotops K40 enthält. So können häufig Schichtgrenzen erkannt werden.<\/SPAN>Die elektrische Leitfähigkeit reagiert empfindlich auf Inhaltsstoffe im Grundwasser und kann somit z.B. bei der Entdeckung auch schwacher Versalzungen helfen.<\/SPAN>Die Temperatur ist ein wichtiger Parameter bei der Beurteilung des geothermischen Potenzials. 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Geoelektrische Messungen ermitteln die Verteilung des spezifischen elektrischen Widerstands im Untergrund. Seismische Verfahren eignen sich für die Strukturerkundung und reagieren besonders sensitiv auf Dichtevariationen und Änderungen elastischer Parameter von Bodenmaterialien. Als geomagnetische Messungen werden jene Verfahren der Geophysik verstanden, die sich mit dem natürlichen Erdmagnetfeld und dessen Wirkung auf die Erdkruste befassen. 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Geologische Strukturen und Gesteine unterscheiden sich in ihren physikalischen Eigenschaften wie zum Beispiel die natürliche Gammastrahlung, der spezifische elektrische Widerstand oder die Magnetisierbarkeit. 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Die Bohrlochabweichungsmessungen (ABW-Daten) beschreiben den Bohrlochverlauf im Untergrund. Diese Geometrie wird durch die folgenden Messgrößen beschrieben: Messteufe, Azimut und Neigung. 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Darstellung der 2D-seismischen Profilverläufe (Nachweisdaten nach GeolDG) und Angaben zu damit verbundenen Fachdaten im Bereich des Bundesland Hessen. Die Reflexionsseismik ist ein Verfahren der Seismik, das zur Bestimmung von Schichtgrenzen im Erdinneren eingesetzt wird. Reflexionsseismische Messungen zielen darauf ab, aus reflektierten seismischen Wellen Erkenntnisse über die Untergrundstruktur zu gewinnen und geologische oder geophysikalische Grenzflächen zu rekonstruieren. Bei der refraktionsseismischen Methode wird die Verteilung der seismischen Geschwindigkeiten im Untergrund ermittelt. Bei den üblichen Verfahren werden dabei die durch eine Erschütterungsquelle (Fallgewicht, Explosion, Vibrator) erzeugten Kompressionswellen verwendet. Die Ausbreitungsgeschwindigkeit der seismischen Wellen ist durch die elastischen Eigenschaften und die Dichte des Gesteins bestimmt und erlaubt so in begrenztem Umfang Rückschlüsse auf das Material. <\/SPAN><\/P>

Die Beobachtung seismischer Wellen erfolgt mit erschütterungsempfindlichen Seismometern (Geophonen) auf Profilen. Sie werden mit einer Messapparatur aufgezeichnet und anhand der Laufzeiten von der Erschütterungsquelle zu den Geophonstandorten wird auf die Tiefenlage von Refraktoren und die zugehörigen Ausbreitungsgeschwindigkeiten geschlossen. 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Darstellung der 3D-seismischen Profilverläufe (Nachweisdaten nach GeolDG) und Angaben zu damit verbundenen Fachdaten im Bereich des Bundesland Hessen. Die Reflexionsseismik ist ein Verfahren der Seismik, das zur Bestimmung von Schichtgrenzen im Erdinneren eingesetzt wird. Reflexionsseismische Messungen zielen darauf ab, aus reflektierten seismischen Wellen Erkenntnisse über die Untergrundstruktur zu gewinnen und geologische oder geophysikalische Grenzflächen zu rekonstruieren. Bei der refraktionsseismischen Methode wird die Verteilung der seismischen Geschwindigkeiten im Untergrund ermittelt. Bei den üblichen Verfahren werden dabei die durch eine Erschütterungsquelle (Fallgewicht, Explosion, Vibrator) erzeugten Kompressionswellen verwendet. Die Ausbreitungsgeschwindigkeit der seismischen Wellen ist durch die elastischen Eigenschaften und die Dichte des Gesteins bestimmt und erlaubt so in begrenztem Umfang Rückschlüsse auf das Material. <\/SPAN><\/P>

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