Fracturing in Deep Boreholes: Stress, Structural and Lithology-controlled Fracture Initiation and Propagation in Deep Geothermal Boreholes in the Upper Jurassic Carbonate Rocks of the North Alpine Foreland Basin

Fracturing in Deep Boreholes: Stress, Structural and Lithology-controlled Fracture Initiation and Propagation in Deep Geothermal Boreholes in the Upper Jurassic Carbonate Rocks of the North Alpine Foreland Basin

by Georg Maximilian Stockinger
Fracturing in Deep Boreholes: Stress, Structural and Lithology-controlled Fracture Initiation and Propagation in Deep Geothermal Boreholes in the Upper Jurassic Carbonate Rocks of the North Alpine Foreland Basin

Fracturing in Deep Boreholes: Stress, Structural and Lithology-controlled Fracture Initiation and Propagation in Deep Geothermal Boreholes in the Upper Jurassic Carbonate Rocks of the North Alpine Foreland Basin

by Georg Maximilian Stockinger

Paperback(1st ed. 2022)

$169.99 
  • SHIP THIS ITEM
    Qualifies for Free Shipping
  • PICK UP IN STORE
    Check Availability at Nearby Stores

Related collections and offers


Overview

The development of the base-load capable, climate-friendly, and practically inexhaustible source of "geothermal energy" represents an important pillar of the energy supply of the future. If it were possible to expand geothermal energy production accordingly, Germany could generate 100% of its energy in a climate-neutral manner by 2050. The joint research project "Dolomitkluft," funded by the German Federal Ministry for Economic Affairs and Energy from 2016 to 2018, aims to establish a new and improved reservoir model for the Upper Jurassic carbonates of the Northern Alpine Foreland Basin for deep geothermal energy. Emerged from this project, the dissertation by Mr. Skinger geomechanically and numerically characterizes the deep geothermal reservoir in carbonate rocks—limestones and dolomites—of the Upper Jurassic in the Northern Alpine Foreland Basin in over 4000 m depth. This book specifically addresses fracture initiation, propagation, and hydraulic conductivity around a borehole and their controlling factors such as the in situ stress, the existing discontinuity network, and the geomechanical rock properties. Mr. Skinger has thus successfully addressed the most important aspects for the retrievability of deep geothermal energy at its point of origin—namely the (deep) borehole.


Product Details

ISBN-13: 9783030945718
Publisher: Springer International Publishing
Publication date: 02/18/2022
Series: Springer Theses
Edition description: 1st ed. 2022
Pages: 258
Product dimensions: 6.10(w) x 9.25(h) x (d)

About the Author

Georg Skinger is a Geologist with a Bachelor's degree in Geosciences and a Master's degree in Engineering Geology and Hydrogeology from the Technical University of Munich (TUM) and the Ludwig-Maximilians-Universität Munich (LMU). After a research fellowship at the University of British Columbia (Vancouver, Canada), he joined the Chair of Engineering Geology at TUM as research associate and lecturer in 2016. His research interests focus on various topics in engineering rock mechanics, such as parameterization of mechanical and petrophysical rock properties, landslide research and reservoir engineering. In 2021 he received his PhD from TUM for the dissertation on characterizing fracturing processes in geothermal reservoirs by applying combined field, laboratory, and advanced numerical FEM-DEM simulation methods.

Table of Contents

Introduction.- Rock Mechanical Basics.- The Bmwi Project “Dolomitkluft” and the Study Site.- Sampling and Methodology.- Results.- Discussion.- Conclusions, Implementation and Outlook.

From the B&N Reads Blog

Customer Reviews