The Vietnamese science and high education system plays a major role in the country’s social and economical development. Due to a mixed influence of international education systems, the contribution of the Vietnamese research to the international scientific landscape is still modest. Over the past decades, the most scientific programmes focused mostly on rather theoretical sciences and less on applied sciences. The results are reflected by a rather low rate of international publications on experimental science. Together with the country’s efforts on the efficient use of natural resources, there is an urgent demand for strengthening the scientific activity on environmental sciences. The new Journal of Vietnamese Environment was created to respond to the increasing interest in environmental research. The journal was founded as part of an academic network initiated by the Dresden University of Technology in the framework of Vietnamese-German cooperation programs on training and education. With multidisciplinary fields of interest and several types of manuscripts, the journal has a predominant academic character, the submission of manuscripts is open to students, graduates, researchers and staff members of research and academic institutions, as well as to any individual willing to disseminate the knowledge about the management of Vietnamese environment. / Hệ thống khoa học và giáo dục đại học Việt Nam đóng vai trò quan trọng trong sự phát triển kinh tế và xã hội của đất nước. Trong xu hướng giao thoa mạnh mẽ giữa các hệ thống giáo dục quốc tế, đóng góp của các nhà nghiên cứu ở Việt Nam cho cộng đồng khoa học quốc tế còn khiêm tốn. Trong những thập niên qua, hầu hết các hoạt động khoa học tập trung vào khoa học lý thuyết hơn là các lĩnh vực khoa học ứng dụng. Điều này đã được phản ánh qua tỷ lệ khá thấp các ấn phẩm quốc tế về khoa học thực nghiệm. Cùng với những nỗ lực của đất nước để sử dụng hiệu quả các nguồn tài nguyên thiên nhiên, một nhu cầu cấp bách đặt ra là tăng cường các hoạt động nghiên cứu về khoa học môi trường. Tạp chí Môi trường Việt Nam ra đời nhằm hưởng ứng sự quan tâm ngày một gia tăng trong nghiên cứu môi trường. Tạp chí được thành lập như một phần của mạng lưới học thuật được đề xuất bởi Trường Đại học Tổng hợp Kỹ Thuật Dresden trong khuôn khổ chương trình hợp tác Việt Nam - CHLB Đức về đào tạo và giáo dục. Với mối quan tâm đa ngành và đa dạng trong ấn phẩm, tạp chí chủ yếu mang tính học thuật, cơ hội gửi đăng bài viết mở rộng cho cả sinh viên, kỹ sư / cử nhân, nghiên cứu viên và các thành viên của Viện nghiên cứu và giáo dục, các cá nhân có mong muốn phổ biến kiến thức về quản lý môi trường ở Việt Nam.

Numerical analysis of multi-field problems in porous and fractured media is an important subject for various geotechnical engineering tasks such as the management of geo-resources (e.g. engineering of geothermal, oil and gas reservoirs) as well as waste management. For practical usage, e.g. for geothermal, simulation tools are required which take into account both coupled thermo-hydro-mechanical (THM) processes and the uncertainty of geological data, i.e. the model parametrization. For modeling fractured rocks, equivalent porous medium or multiple continuum model approaches are often only the way currently due to difficulty to handle geomechanical discontinuities. However, they are not applicable for prediction of flow and transport in subsurface systems where a few fractures dominates the system behavior. Thus modeling coupled problems in discretely fractured porous media is desirable for more precise analysis. The subject of this work is developing a framework of the finite element method (FEM) for modeling coupled THM problems in discretely fractured and non-fractured porous media including thermal water flow, advective-diffusive heat transport, and thermoporoelasticity. Pre-existing fractures are considered. Systems of discretely fractured porous media can be considered as a problem of interacted multiple domains, i.e. porous medium domain and discrete fracture domain, for hydraulic and transport processes, and a discontinuous problem for mechanical processes. The FEM is required to take into account both kinds of the problems. In addition, this work includes developing a methodology for the data uncertainty using the FEM model and investigating the uncertainty impacts on evaluating coupled THM processes. All the necessary code developments in this work has been carried out with a scientific open source project OpenGeoSys (OGS). In this work, fluid flow and heat transport problems in interactive multiple domains are solved assuming continuity of filed variables (pressure and temperature) over the two domains. The assumption is reasonable if there are no infill materials in fractures. The method has been successfully applied for several numerical examples, e.g. modeling three-dimensional coupled flow and heat transport processes in discretely fractured porous media at the Gross Schoenebck geothermal site (Germany), and three-dimensional coupled THM processes in porous media at the Urach Spa geothermal site (Germany). To solve the mechanically discontinuous problems, lower-dimensional interface elements (LIEs) with local enrichments have been developed for coupled problems in a domain including pre-existing fractures. The method permits the possibility of using existing flow simulators and having an identical mesh for both processes. It enables us to formulate the coupled problems in monolithic scheme for robust computation. Moreover, it gives an advantage in practice that one can use existing standard FEM codes for groundwater flow and easily make a coupling computation between mechanical and hydraulic processes. Example of a 2D fluid injection problem into a single fracture demonstrated that the proposed method can produce results in strong agreement with semi-analytical solutions. An uncertainty analysis of THM coupled processes has been studied for a typical geothermal reservoir in crystalline rock based on the Monte-Carlo method. Fracture and matrix are treated conceptually as an equivalent porous medium, and the model is applied to available data from the Urach Spa and Falkenberg sites (Germany). Reservoir parameters are considered as spatially random variables and their realizations are generated using conditional Gaussian simulation. Two reservoir modes (undisturbed and stimulated) are considered to construct a stochastic model for permeability distribution. We found that the most significant factors in the analysis are permeability and heat capacity. The study demonstrates the importance of taking parameter uncertainties into account for geothermal reservoir evaluation in order to assess the viability of numerical modeling.

This study investigates the aspects of resilience in the management strategies of the key stakeholders of flood risk management in the city of Accra, Ghana. The overall objective is to analyse the response capacity in the strategies of the key stakeholders in flood risk management for managing the unexpected course of flood disasters in addition to the expected features of flood risk. To achieve the set objective, the following research questions are addressed: Who are the key stakeholders of flood risk management in the city of Accra? How are these stakeholders dealing with the unexpected course of flood disasters in addition to the expected features of flood risk in their management strategies? How could the capacity of the strategies for responding to the unexpected course of flood disasters be advanced? The inductive case study design applies document analyses, semi-structured interviews as well as key stakeholder identification and validation methods. Scientific and policy documents about resilience and flood risk management were reviewed. The research participants were mainly directors and representatives of organisations in flood risk management of the study. Empirical findings include key stakeholders in flood risk management as well as aspects of resilience and anticipation in flood risk management strategies. The main finding on the key stakeholders of flood risk management are national, district, civil society, and private sector organisations as well as traditional authorities (local chiefs). Aspects of resilience in flood risk management strategies comprises omnivorousness, agile and timely flow of response resource, homoeostasis, flatness of the response structure and process, redundancy of the response resources and buffer capacity. Findings revealed resilience regarding diversity in sources of resource and responses for dealing with unexpected course of flood disasters. The aspects of anticipation are described as resistance to known risk, maintenance of boundary conditions of the management strategies and specialisation for dealing with specific flood risk within and among organisations. Regarding anticipation, results indicate that there are measures for resisting known flood risk but their implementation is ineffective. Based upon the findings, hypotheses are derived for advancement of resilience and anticipation in flood risk management strategies. Involvement of the local chiefs, Slum Union of Ghana, Local Development Associations of flood-prone communities and key private sector organisations in flood risk management strategies in the city of Accra would amend their response capacities in diversity of sources of response resources and allow for advanced resilience regarding their responses to the impacts of land-use changes and the waste disposal in watercourses. Recommendations refer to prospects to advance the response capacity of key stakeholders of flood risk management strategies by integrating traditional authorities and private organisations in flood risk management in the city of Accra. / Diese Arbeit untersucht Aspekte von Resilienz in den Strategien von Schlüsselakteuren des Hochwasserrisikomanagements in der Stadt Accra (Ghana). Das übergeordnete Ziel besteht darin, das Reaktionsvermögen dieser Akteure in ihren Management-Strategien nicht nur hinsichtlich des erwarteten, sondern vor allem hinsichtlich des unerwarteten Verlaufs von Hochwasserkatastrophen zu untersuchen. Die folgenden drei Forschungsfragen werden untersucht: Wer sind die Schlüsselakteure des Hochwasserrisikomanagements in der Stadt Accra? Wie berücksichtigen diese Akteure in ihren Management-Strategien den unerwarteten Verlauf von Hochwasserkatastrophen zusätzlich zu dem erwarteten Verlauf? Wie könnte das Reaktionsvermögen bezüglich des Umgangs mit dem unerwarteten Verlauf von Hochwasserkatastrophen in diesen Strategien ausgeweitet werden? Im Rahmen des induktiven Fallstudiendesigns werden Dokumentenanalysen, halbstandardisierte Interviews und Gruppendiskussionen eingesetzt. Die daraus resultierenden empirischen Befunde beziehen sich neben der Identifikation der Schlüsselakteure des Hochwasserrisikomanagements auch auf die Aspekte von Resilienz und Antizipation in ihren Management-Strategien. Zu den Schlüsselakteuren zählen nationale und lokale Organisationen, aber auch solche aus der Zivilgesellschaft, dem privaten Sektor und traditionelle Autoritäten. Bei den Aspekten von Resilienz in den Hochwasserrisikomanagement-Strategien handelt es sich um ganzheitliche Herangehensweisen, regen und zeitnahen Einsatz von Ressourcen zur Ereignisbewältigung sowie Pufferkapazitäten. Die Ergebnisse zeigten Widerstandsfähigkeit in Bezug auf die Vielfalt in den Quellen von Ressourcen und Antworten auf den unerwarteten Verlauf von Hochwasserkatastrophen. Die Ergebnisse hinsichtlich der Antizipation von Hochwasserrisikomanagement-Strategien umfassen den Widerstand gegen das bekannte Risiko, die Aufrechterhaltung von Rahmenbedingungen der Management-Strategien und die Spezialisierung auf bestimmte Hochwasserrisiken. Auf den Erkenntnissen über die Aspekte von Resilienz und Antizipation in den Hochwasserrisikomanagement-Strategien aufbauend werden Hypothesen abgeleitet. In den Handlungsempfehlungen werden die Chancen einer Integration traditioneller Autoritäten und anderer Interessensgruppen in das Hochwasserrisikomanagement der Stadt Accra aufgezeigt, wodurch eine Weiterentwicklung der Resilienz in den Hochwasserrisikomanagement-Strategien für die Zukunft erreicht werden kann.

The Western Mediterranean realm is considered as a region highly sensitive with regard to climate changes and landscape transformations. Within its semi arid and semi humid areas, even slight climatic changes but also human interventions may result in far-reaching consequences in respect of environment and ecological systems. Thus, research on landscape development has a high relevance in geosciences, especially in the light of current climate change research. It is a major concern to reveal regularities and patterns in past landscape evolution in order to provide a basis for the assessment of future developments. For the reconstruction of late Quaternary environmental conditions fluvial sediments play an important role as they almost uniquely reflect landscapes and landscape changes on a regional scale. This is due to the fact that fluvial dynamics and all enclosed processes are based on multi-causal relationships and a variety of factors like climatic conditions, vegetation development, human impact, or tectonic activity finds expression in fluvial dynamics. About 70 % of the Iberian Peninsula is influenced by moist Atlantic air masses, but in the whole area there is a considerable research gap concerning the exploration of fluvial archives. Taking this into account, this dissertation aims to systematically work out fluvial sediment successions of two river systems, namely the Jarama River in central Spain and the Guadalete River in southwestern Spain. For complementary considerations, first stratigraphic results from the middle to lower Guadalquivir River in southern Spain will be consulted. In a first step, the objective is to intensively study and document sediment profiles for the purpose of deriving a valuable composite profile for each river system. In a second step, the significance of these composite profiles regarding palaeoenvironmental conditions as well as changes will be examined. Beside the reaction of fluvial systems towards climatic changes, relationships with other influencing factors are a main issue. On the basis of a supra-regional comparison a possible coupling of fluvial geomorphic systems and large-scale climate fluctuations shall be analyzed. Furthermore, it is intended to address issues like system connectivity or varying response times and response durations. The bases for these considerations are abundant sedimentary profile records supported by electrical resistivity tomography and percussion drillings. Stratigraphic work includes the differentiation of sediment units, the identification of soil horizons, and the correlation of specific layers and horizons across different profile sections based on sedimentologic and pedogenetic characteristics. Subsequent soil-chemical and sedimentological laboratory analyses on certain key-profiles imply grain-size analyses, the measurement of organic carbon content, calcium carbonate content, pedogenic and total iron contents, as well as magnetic susceptibility. Laboratory analyses are used to strengthen results of field work and to differentiate between soils and soil sediments in ambiguous cases. The chronological resolution of the sediment successions will be provided by radiocarbon dating. The final aim is to work out a detailed fluvial sedimentation history for the late Quaternary. The precise characterization of the catchment areas, together with a comparison of the stratigraphic findings and secondary archive information from the literature, will enable the identification of relationships between fluvial dynamics and different influencing factors. In this dissertation, 36 profile sections have been worked out intensively. Furthermore, 13 percussion drillings were conducted in floodplain positions with insufficient exposure conditions. For the chronological frame 70 radiocarbon samples have been dated. The obtained results show a significant pattern of sedimentation periods and phases of stability associated with soil formation for each river system. The sedimentation history of the Guadalete and Guadalquivir Rivers could be reconstructed for the last 15 ka, while conclusions with regard to sedimentation dynamics of the Jarama River could be drawn for a period of 43 ka. Thanks to an abundance of available studies on other terrestrial archives with climatic or environmental relevance, it was possible to assess the influence of different parameters such as climate, vegetation, humankind, tectonics, and base-level changes on fluvial sedimentation dynamics. It emerged that, first and foremost, rapid climate changes had significant impact on the mobilization of sediments in the catchment area as well as their deposition in floodplain positions. On the other hand prolonged periods of climatic amelioration caused floodplain stability along with soil formation, as documented for the time spans between 13.3 and 12.7 ka, 7 and 5.1 ka, 2.8 and 2.3 ka, 1.4 and 1.2 ka, as well as 0.8 and 0.5 ka cal. BP in several river systems. Periods of increased sedimentation were initiated by phases of climatic aridification that affected fluvial systems through the weakening of the vegetation cover and the accentuation of the hydrological discharge regime. Corresponding patterns have been found for the time intervals between 8 and 7 ka, 5 and 3.8 ka, 2.2 and 1.5 ka, as well as around 1 ka and 0.4 ka cal. BP. The supra-regional effectiveness of the factor climate is contrasted by a strong regional individuality of the river catchments that is expressed by further, regionally limited phases of fluvial activity. Crucial to this development – apart from regional climate differences – are, inter alia, tectonic movements as evidenced for the Jarama River system in central Spain, or late Pleistocene and Holocene sea-level fluctuations that primarily affected fluvial dynamics along the lower course of the Guadalete River in southwestern Spain. Furthermore, it can be shown that variations in time and duration of fluvial system response are attributable to differing buffer capacities of river catchments towards external influences. The increase of human impact during the late Holocene apparently provoked a reinforcement of the effects of climatic impulses. There are clear evidences for the participation of humans in the mobilization of sediments; however, concerning the degree of influence it is hardly possible to differentiate between the factors humans and climate. / Der westliche Mediterranraum gilt als landschaftlich und klimatisch hochsensible Region, für deren semiaride bis semihumide Gebiete bereits kleinere klimatische Änderungen, aber auch Eingriffe des Menschen, mit weitreichenden Folgen für Umwelt und ökologische Systeme verbunden sein können. Forschungen zum Landschaftswandel nehmen hier vor allem vor dem Hintergrund des derzeitigen Klimawandels einen hohen Stellenwert in den Geowissenschaften ein. Ein wichtiges Anliegen ist dabei, in früheren Landschaftswandeln Muster zu entdecken, welche als Grundlage für Bewertungen zukünftiger Veränderungen dienen können. Für die Rekonstruktion spätquartärer Umweltbedingungen kommt fluvialen Sedimenten eine besondere Rolle zu. Wie kein anderes Archiv spiegeln fluviale Sedimentabfolgen Landschaftszustände und -entwicklung auf regionaler Ebene wieder. Dies ist dem Umstand geschuldet, dass fluviale Dynamik mit allen inbegriffenen Prozessen auf polykausalen Zusammenhängen beruht und somit eine Vielzahl an Faktoren, wie klimatische Verhältnisse und Vegetationsentwicklung, menschliche Einflussnahme oder tektonische Aktivität Ausdruck in fluvialer Dynamik finden. Von feuchten atlantischen Luftmassen geprägte Gebiete nehmen etwa 70 % der Fläche der Iberischen Halbinsel ein, allerdings besteht hier eine erhebliche Forschungslücke im Bereich der Analyse fluvialer Archive. Diesem Umstand soll in vorliegender Dissertation in Form einer systematischen Aufarbeitung der fluvialen Sedimentabfolgen zweier Flusssysteme in Zentralspanien (Rio Jarama), sowie in SW-Spanien (Rio Guadalete) Rechnung getragen werden. Für ergänzende Betrachtungen werden dabei erste Befunde zur stratigraphischen Gliederung des Guadalquivir-Mittellaufes in S-Spanien herangezogen. Ziel der Arbeiten ist es zunächst über umfangreiche Aufnahmen und Dokumentationen von Sedimentprofilen ein belastbares Standardprofil für jedes Flusssystem zu erarbeiten und dieses hinsichtlich der Aussagekraft in Bezug auf Paläoumweltbedingungen und vor allem -wandeln zu prüfen. Neben der möglichen Reaktion fluvialer Systeme auf klimatische Änderungen, stehen dabei vor allem auch Beziehungsgeflechte zu anderen Einflussfaktoren im Vordergrund. Anhand eines überregionalen Vergleichs soll eine mögliche Kopplung fluvialmorphologischer Systeme an großräumige Klimafluktuationen untersucht werden, zudem soll weiteren Themenkomplexen, wie der Konnektivität verschiedener Systeme oder unterschiedlichen Reaktionszeiten und -geschwindigkeiten nachgegangen werden. Grundlage für diese Betrachtungen bilden dabei aus zahlreichen Geländeaufnahmen resultierende Profilaufnahmen, sowie Ergebnisse geoelektrischer Messungen und Bohrsondierungen. Stratigraphische Arbeiten belaufen sich zunächst auf die Untergliederung verschiedener Sedimenteinheiten, die Ausweisung von Bodenhorizonten, sowie die Korrelation einzelner Schichten und Horizonte über unterschiedliche Profile hinweg anhand charakteristischer sedimentologischer und pedogenetischer Merkmale. Nachfolgende bodenchemische und sedimentologische Laboruntersuchungen an ausgewählten Profilen sollen über die Bestimmung von Korngrößenverhältnissen, Gehalten an organischem Kohlenstoff, Kalk- und Eisengehalten, sowie der magnetischen Suszeptibilität die Geländebefunde stützen und in unklaren Fällen eine Unterscheidung von Böden und Bodensedimenten erleichtern. Die zeitliche Auflösung der Sedimentabfolgen soll über Radiokarbondatierungen realisiert werden, mit dem letztendlichen Ziel, eine detaillierte fluviale Sedimentationsgeschichte für das Spätquartär zu erarbeiten. In einem weiteren Schritt werden begleitend zu einer detaillierten Einzugsgebietscharakteristik die chronostratigraphischen Befunde einem intensiven Vergleich mit in der Literatur verfügbaren Studien an Sekundärarchiven zugeführt, um Beziehungsgeflechte zwischen fluvialer Dynamik und verschiedenen Einflussfaktoren aufzudecken. Im Rahmen dieser Dissertation konnten zunächst 36 Profilaufschlüsse detailliert bearbeitet und zudem 13 Rammkernsondierungen in Flussauenpositionen abgeteuft werden. Für den chronologischen Rahmen wurden 70 Radiokohlenstoffproben datiert. Die Ergebnisse zeigen ein deutliches Muster von Sedimentationsphasen und Zeiten der Stabilität mit einhergehender Bodenbildung für jedes Flusseinzugsgebiet. Dabei konnte die Sedimentationsgeschichte der Flusssysteme Rio Guadalete und Rio Guadalquivir für die letzten 15.000 Jahre und des Rio Jarama für die letzten 43 ka rekonstruiert werden. Dank der Fülle an verfügbaren Studien an terrestrischen Vergleichsarchiven mit klima- und umweltrelevantem Bezug war es möglich, den Einfluss der unterschiedlichen Parameter Klima, Vegetation, Mensch und Tektonik, bzw. Erosionsbasis auf die fluviale Sedimentationsdynamik zu prüfen. So zeigte sich, dass vor allem rasche Klimaänderungen in der Lage waren die Mobilisierung von Sedimenten im Einzugsgebiet und deren Ablagerung in den Flussauen zu initiieren. Dahingegen bewirkten anhaltende klimatische Gunstphasen eine Stabilisierung mit einhergehender Bodenbildung, wie für die Zeiträume zwischen 13.3 und 12.7 ka, 7 und 5.1 ka, 2.8 und 2.3 ka, 1.4 und 1.2 ka, sowie 0.8 und 0.5 ka cal. BP für sämtliche Flusssysteme zu verzeichnen ist. Perioden verstärkter Sedimentation folgten in der Regel Phasen klimatischer Aridifizierung, welche über eine Schwächung der Vegetationsbedeckung und Akzentuierung des hydrologischen Abflussregimes in der Lage waren auf das fluviale System Einfluss zu nehmen. Entsprechende Muster konnten für die Zeiträume zwischen 8 und 7 ka, 5 und 3.8 ka, 2.2 und 1.5 ka, sowie um 1 ka als auch 0.4 ka cal. BP dokumentiert werden. Dem überregional wirksamen Einfluss des Faktors Klima steht jedoch eine starke landschaftsgeschichtliche Individualität der verschiedenen Regionen gegenüber, welche in weiteren, regional begrenzten Phasen fluvialer Aktivität zum Ausdruck kommt. Ausschlaggebend sind hier neben der Ausbildung regionaler Klimaunterschiede unter Anderem tektonische Verstellungen, welche für das in Zentralspanien gelegene System des Rio Jarama belegt werden konnten, oder spätpleistozäne und holozäne Meeresspiegelschwankungen, welche sich vor allem auf die fluviale Dynamik im Unterlauf des in SW-Spanien gelegenen Rio Guadalete auswirkten. Desweiteren können Unterschiede in Reaktionsdauer und -geschwindigkeit fluvialer Systeme mit variierendem Puffervermögen der Flusseinzugsgebiete gegenüber äußeren Einflüssen erklärt werden. Das intensivierte Wirken des Menschen im Spätholozän führte allem Anschein nach zu einer Verstärkung der Wirkung klimatischer Impulse, wobei sich klare Evidenzen für eine Beteiligung des Menschen an der Sedimentmobilisierung erkennen lassen, der Umfang des Einflusses des Menschen aber in der Regel nicht klar von dem des Klimas zu trennen ist.