Moeck, Inga S.

[["dc.bibliographiccitation.journal","Netherlands Journal of Geosciences"],["dc.bibliographiccitation.volume","98"],["dc.contributor.author","Moeck, Inga S."],["dc.contributor.author","Dussel, Michael"],["dc.contributor.author","Weber, Josef"],["dc.contributor.author","Schintgen, Tom"],["dc.contributor.author","Wolfgramm, Markus"],["dc.date.accessioned","2020-12-10T15:22:11Z"],["dc.date.available","2020-12-10T15:22:11Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1017/njg.2019.12"],["dc.identifier.eissn","1573-9708"],["dc.identifier.issn","0016-7746"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/17209"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/73298"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.notes.intern","Merged from goescholar"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.title","Geothermal play typing in Germany, case study Molasse Basin: a modern concept to categorise geothermal resources related to crustal permeability"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","228"],["dc.bibliographiccitation.journal","Geothermics"],["dc.bibliographiccitation.lastpage","239"],["dc.bibliographiccitation.volume","51"],["dc.contributor.author","Brehme, Maren"],["dc.contributor.author","Moeck, Inga"],["dc.contributor.author","Kamah, Yustin"],["dc.contributor.author","Zimmermann, Guenter"],["dc.contributor.author","Sauter, Martin"],["dc.date.accessioned","2018-11-07T09:38:41Z"],["dc.date.available","2018-11-07T09:38:41Z"],["dc.date.issued","2014"],["dc.description.abstract","In this study tectonic structural features and their hydraulic characteristics of fault zones were integrated into a consistent hydrotectonic model of the Lahendong geothermal reservoir, Indonesia. Moreover, these elements were analysed with respect to their relevance for the operation of the geothermal power plant at initial conditions, i.e. before the start of operation. The complex tectonic setting with volcanic activity provides evidence for relevant structural and hydrogeological elements, such as fault zones, surface spring discharge and joints at different spatial scales. The study area is highly variable with respect to hydraulic properties and chemical composition of the fluids. It consists of two types of fluids. Acid brine water with a pH of around 3 and an electrical conductivity ranging between 462011 mu S/cm and 9700 p,S/cm is characteristic for the reservoir in the North with temperatures up to 274 C. A moderate pH between 4 and 7, an electrical conductivity in the range of 400-1730 mu S/cm and temperatures of up to 340 C characterise the southern study area. The Lahendong geothermal field is subdivided into two sub-reservoirs. Faults are less permeable perpendicular to the strike of the faults than parallel to the strike. The characteristics of the complex reservoir system could be explained by the combination of hydrotectonics and hydrogeological parameters. Understanding the permeability distribution along fault zones is crucial to investigate subsurface fluid pathways as well as to sustainably use the reservoir. A compartmentalisation of the reservoir was derived from a stress field analysis of the tectonic elements and from hydrogeological observations. The information on underground fluid flow is essential to understand the subsurface flow of geothermal fluids. Here, the permeability of structures is identified as the limiting factor. (C) 2014 Elsevier Ltd. All rights reserved."],["dc.description.sponsorship","German Federal Ministry for Education and Research (BMBF) [03G0753A]"],["dc.identifier.doi","10.1016/j.geothermics.2014.01.010"],["dc.identifier.isi","000336778700019"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/33121"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.relation.issn","1879-3576"],["dc.relation.issn","0375-6505"],["dc.title","A hydrotectonic model of a geothermal reservoir - A study in Lahendong, Indonesia"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","2097"],["dc.bibliographiccitation.issue","6"],["dc.bibliographiccitation.journal","Solid Earth"],["dc.bibliographiccitation.lastpage","2117"],["dc.bibliographiccitation.volume","11"],["dc.contributor.author","Shipilin, Vladimir"],["dc.contributor.author","Tanner, David C."],["dc.contributor.author","von Hartmann, Hartwig"],["dc.contributor.author","Moeck, Inga"],["dc.date.accessioned","2021-04-14T08:22:51Z"],["dc.date.available","2021-04-14T08:22:51Z"],["dc.date.issued","2020"],["dc.identifier.doi","10.5194/se-11-2097-2020"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/80720"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-399"],["dc.relation.eissn","1869-9529"],["dc.title","Multiphase, decoupled faulting in the southern German Molasse Basin – evidence from 3-D seismic data"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","102523"],["dc.bibliographiccitation.journal","Geothermics"],["dc.bibliographiccitation.volume","105"],["dc.contributor.author","Fadel, Mohamed"],["dc.contributor.author","Reinecker, John"],["dc.contributor.author","Bruss, Dietfried"],["dc.contributor.author","Moeck, Inga"],["dc.date.accessioned","2022-09-01T09:49:36Z"],["dc.date.available","2022-09-01T09:49:36Z"],["dc.date.issued","2022"],["dc.identifier.doi","10.1016/j.geothermics.2022.102523"],["dc.identifier.pii","S0375650522001699"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/113476"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-597"],["dc.relation.issn","0375-6505"],["dc.rights.uri","https://www.elsevier.com/tdm/userlicense/1.0/"],["dc.title","Causes of a premature thermal breakthrough of a hydrothermal project in Germany"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","25"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Geothermal Energy"],["dc.bibliographiccitation.volume","9"],["dc.contributor.author","Schintgen, Tom V."],["dc.contributor.author","Moeck, Inga S."],["dc.date.accessioned","2021-11-25T11:24:58Z"],["dc.date.accessioned","2022-08-16T12:46:16Z"],["dc.date.available","2021-11-25T11:24:58Z"],["dc.date.available","2022-08-16T12:46:16Z"],["dc.date.issued","2021-10-28"],["dc.date.updated","2022-07-29T12:18:42Z"],["dc.description.abstract","Abstract\r\n The Molasse Basin in Southern Germany is part of the North Alpine Foreland Basin and hosts the largest accumulation of deep geothermal production fields in Central Europe. Despite the vast development of geothermal energy utilization projects especially in the Munich metropolitan region, the evolution of and control factors on the natural geothermal field, more specifically the time-varying recharge and discharge governing groundwater and heat flow, are still debated. Within the Upper Jurassic (Malm) carbonate aquifer as the main geothermal reservoir in the Molasse Basin, temperature anomalies such as the Wasserburg Trough anomaly to the east of Munich and their underlying fluid and heat transport processes are yet poorly understood. We delineate the two end members of thermal–hydraulic regimes in the Molasse Basin by calculating two contrasting permeability scenarios of the heterogeneously karstified Malm carbonate aquifer along a model section through the Wasserburg Trough anomaly by means of two-dimensional numerical thermal-hydraulic modelling. We test the sensitivity of the thermal-hydraulic regime with regard to paleoclimate by computing the two Malm permeability scenarios both with a constant surface temperature of 9 °C and with the impact of paleo-temperature changes during the last 130 ka including the Würm Glaciation. Accordingly, we consider the hydraulic and thermal effects of periglacial conditions like permafrost formation and the impact of the numerous glacial advances onto the Molasse Basin. Thermal-hydraulic modelling reveals the effect of recurrent glacial periods on the subsurface targets of geothermal interest, which is minor compared to the effect of permeability-related, continuous gravity-driven groundwater flow as a major heat transport mechanism."],["dc.identifier.citation","Geothermal Energy. 2021 Oct 28;9(1):25"],["dc.identifier.doi","10.1186/s40517-021-00207-x"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/93552"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/112744"],["dc.language.iso","en"],["dc.rights","CC BY 4.0"],["dc.rights.holder","The Author(s)"],["dc.subject","Würm Glaciation"],["dc.subject","Permafrost"],["dc.subject","North Alpine Foreland Basin"],["dc.subject","Molasse Basin"],["dc.subject","Upper Jurassic"],["dc.subject","Malm"],["dc.subject","Carbonate aquifer"],["dc.subject","Coupled heat and fluid flow"],["dc.subject","Gravity-driven groundwater flow"],["dc.subject","Permeability"],["dc.title","The interplay of Malm carbonate permeability, gravity-driven groundwater flow, and paleoclimate – implications for the geothermal field and potential in the Molasse Basin (southern Germany), a foreland-basin play"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Geothermal Energy"],["dc.bibliographiccitation.volume","3"],["dc.contributor.author","Deon, Fiorenza"],["dc.contributor.author","Förster, Hans-Jürgen"],["dc.contributor.author","Brehme, Maren"],["dc.contributor.author","Wiegand, Bettina"],["dc.contributor.author","Scheytt, Traugott"],["dc.contributor.author","Moeck, Inga"],["dc.contributor.author","Jaya, Makky S."],["dc.contributor.author","Putriatni, Dewi J."],["dc.date.accessioned","2019-07-09T11:41:55Z"],["dc.date.available","2019-07-09T11:41:55Z"],["dc.date.issued","2015"],["dc.description.abstract","Magmatic settings involving active volcanism are potential locations for economic geothermal systems due to the occurrence of high temperature and steam pressures. Indonesia, located along active plate margins, hosts more than 100 volcanoes and, therefore, belongs to the regions with the greatest geothermal potential worldwide. However, tropical conditions and steep terrain reduce the spectrum of applicable exploration methods, in particular in remote areas. In a case study from the Lamongan volcanic field in East Java, we combine field-based data on the regional structural geology, elemental and isotopic composition of thermal waters, and the mineralogical and geochemical signatures of volcanic rocks in exploring hidden geothermal systems. Results suggest infiltration of groundwater at the volcanoes and faults. After infiltration, water is heated and reacts with rocks before rising to the surface. The existence of a potential heat source is petrologically and geophysically constrained to be an active shallow mafic-magma chamber, but its occurrence is not properly reflected in the composition of the collected warmed spring waters that are predominantly meteoric in origin. In conclusion, spring temperature and hydrochemistry alone may not always correctly reflect the deep geothermal potential of an area."],["dc.identifier.doi","10.1186/s40517-015-0040-6"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/12588"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/58549"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.relation.issn","2195-9706"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Geochemical/hydrochemical evaluation of the geothermal potential of the Lamongan volcanic field (Eastern Java, Indonesia)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","332"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","Energies"],["dc.bibliographiccitation.volume","11"],["dc.contributor.author","Agemar, Thorsten"],["dc.contributor.author","Weber, Josef"],["dc.contributor.author","Moeck, Inga S."],["dc.date.accessioned","2018-11-13T11:19:44Z"],["dc.date.available","2018-11-13T11:19:44Z"],["dc.date.issued","2018"],["dc.description.abstract","Any geothermal resource assessment requires consistent and widely accepted terminology, methods, and reporting schemes that facilitate the comparison of geothermal resource estimates. This paper reviews common resource assessment methods, as well as reporting codes and terminology. Based on a rigorous analysis of the portrayed concepts and methods, it discusses the appropriateness of the existing reporting codes for sustainable utilization of geothermal resources in Germany. Since the last quantitative geothermal resource assessment in Germany was done 15 years ago, a revised report is overdue. Unlike fossil energy commodities, geothermal energy replenishes naturally and heat recuperation increases in created heat sinks. This replenishment process offers the opportunity for sustainable reservoir management in the case of moderate production rates or cyclic operation. Existing reporting codes, however, regard geothermal resources in a similar way to fossil resources or focus too much on field development rather than on the whole assessment process. In order to emphasize the renewability of geothermal energy, we propose the reporting of geothermal capacities (per doublet or per km2) instead of recoverable heat energy which depends very much on project lifetime and other factors. As a first step, a new classification scheme for geothermal resources and reserves is outlined."],["dc.identifier.doi","10.3390/en11020332"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/56788"],["dc.language.iso","en"],["dc.notes.status","zu prüfen"],["dc.title","Assessment and Public Reporting of Geothermal Resources in Germany: Review and Outlook"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dspace.entity.type","Publication"]]