Moeck, Inga S.

[["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.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"]]