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1.
The hydraulic behaviour of the karst aquifer in the Hubelj spring catchment area (SW Slovenia) was studied by using an indirect
research method based on natural tracers. The variations of natural tracers (in precipitation and in groundwater) during the
storm event made possible the separation of the Hubelj spring storm hydrograph by the three-component separation technique.
The results produced information on the aquifer recharge, storage and discharge processes, as well as on the mechanisms that
affected them. They verified the so-called epikarst hypothesis presuming that an important part of a karst aquifer recharge
reaches rapidly and intensively from the epikarst zone. It was demonstrated that epikarst water could occupy up to 50% of
the spring discharge during precipitation events. This phenomenon could have important consequences on protection and management
of the problems of karst aquifers, including engineering problems in karst areas. With this respect the results could give
way to new engineering ideas. 相似文献
2.
Structures in bedrock and sediments suggest that the Fennoscandian Shield was subjected to a higher seismicity at the end of the last glaciation than it is today. We suggest that the annual varves of the glacial clays document this seismicity. In the Stockholm area, three paleoseismic events have so far been recorded in the varved clay chronology. Liquefaction structures have also been documented. The occurrence of heaps of ‘sharp-edged blocks’ (large caves in crystalline bedrock) might be another sign of this seismicity. 相似文献
3.
Informal networks and resilience to climate change impacts: A collective approach to index insurance
Sara L.M. Trærup 《Global Environmental Change》2012,22(1):255-267
This article contributes to the understanding of how to proceed with the development of index-insurance in order to reach extended population coverage with the insurance. The approach is applied to an example from a region in Tanzania. One of the main coping strategies that resource-poor households rely on to manage risks related to fluctuations in income flows is risk-sharing in informal networks. An informal network is an ideal way of managing idiosyncratic shocks, but once such shocks become covariate and affect whole communities, as is the case with most climate change impacts, informal networks become insufficient since the majority of risk-sharers will be affected by the shock at the same time. This paper proposes a collective approach to index-insurance in which the members of an informal network will be insured as one insurance taker. The paper raises a conceptual argument that targeting households through existing informal networks will remove a number of prevailing barriers to the take-up of insurance and consequently the approach has the potential to increase households’ resilience to climate change impacts. The policy implications of the conclusions are significant since the number of covariate shocks is predicted to increase with climate change. 相似文献
4.
The role of technology in combatting climate change through mitigation and adaptation to its inevitable impacts has been acknowledged and highlighted by the Parties to the United Nations Framework Convention on Climate Change (UNFCCC). In the developing world, this has received particular attention through the technology needs assessment (TNA) process. As Parties put forward their national pledges to combat climate change, the scarcity of resources makes it important to assess (i) whether national processes designed to tackle climate change are working together and (ii) whether existing national processes should be terminated with the initiation of new ones. This study presents an assessment of the existing TNA process and its linkages to the nationally determined contributions (NDCs) under the Paris Agreement. The conclusions stem from an assessment of the TNAs completed to date, as well as 71 NDCs from developing countries at various stages of the TNA process. The analyses show that further developing the TNAs could play a vital role in filling gaps in the existing NDCs, specifically those relating to identifying appropriate technologies, their required enabling framework conditions and preparing implementation plans for their transfer and diffusion.
Key policy insights
The full potential of the TNAs has still to be rolled out in many countries.
Developing countries can maximize the potential of their TNAs by further developing them to explicitly analyse what is needed to implement existing NDCs, including by better aligning their focus, scope and up-to-dateness with the priority sectors included in the NDCs.
Requests of developing countries for international assistance, through technology transfer, will be better guided by the completion of the TNA process.
Policies for strengthening the NDCs will benefit from the results of completed, ongoing and future TNA processes.
5.
6.
Branka Trček 《Environmental Geology》2007,51(5):761-765
The role of an epikarst zone in the karst aquifer hydraulic behaviour was brought into focus in our studies referring to the
catchment area of the Hubelj spring (SW Slovenia). This study points out the significance of effects of the fast preferential
flow—epiflow, which is the main factor controlling solute/contaminant transport towards the aquifer saturated zone. The so-called
epikarstic hypothesis is verified on the basis of the most significant research results that are supported by the most important
findings from the literature. 相似文献
7.
Why plate tectonics was not invented in the Alps 总被引:1,自引:0,他引:1
R. Trümpy 《International Journal of Earth Sciences》2001,90(3):477-483
8.
9.
Zusammenfassung In der geosynklinalen Vorgeschichte mancher Kettengebirge gibt es zwei Phasen mit verschiedener paläogeographischer Konfiguration: 1. mit Dehnungstektonik, 2. mit Kompressionstektonik. Der Höhepunkt der vororogenen magmatischen Tätigkeit fällt in eine Zwischenphase mit geringerem submarinem Relief.Kurzfassung eines am 12. März 1960 vor der Geologischen Vereinigung gehaltenen Vortrages. Eine ausführliche Arbeit über die Geosynklinalentwicklung der Westalpen (mit umfangreichem Literaturverzeichnis) erschien im Bull. Geol. Soc. America, Juni 1960, unter dem Titel Paleotectonic Evolution of the Central and Western Alps. 相似文献
10.
Prof. Dr. Rudolf Trümpy 《International Journal of Earth Sciences》1972,61(3):961-964
Zusammenfassung Die alpine Krustenverkürzung (300–400 km oder mehr im Profil der Westschweiz, 400–500 km oder mehr im Profil der Ostschweiz) erfolgte in diskreten orogenen Phasen, welche durch Zeiten langsamerer Bewegung oder eigentlicher Remission getrennt waren. Während der wichtigsten Phase, an der Eozän-Oligozän-Wende, betrug die Relativgeschwindigkeit der nördlichen Platte und der südlichen Kleinplatte einige cm/a.
Crustal shortening in the Central Alps (300–400 km or more in western Switzerland, 400–500 km or more in eastern Switzerland) occurrend in discrete orogenic phases, separated by times of slower movement or of complete stop. During the most important phase, at the turn from the Eocene to the Oligocene, the rate of relative movement of the northern plate and the southern microplate was of the order of several cm/y.
Résumé Le raccourissement de la croûte dans les Alpes Centrales (300–400 km ou davantage en Suisse occidentale, 400–500 km ou davantage en Suisse orientale) se fit par phases orogéniques défines, séparées par des intervalles à mouvement plus lent ou même à arrêt total. Pendant la phase principale, à la fin de l'Eocène ou au début de l'Oligocène, la vitesse relative de la plaque septentrionale et de la microplaque méridionale était de l'ordre de plusieurs cm/a.
(300–400 , , 400–500 , ) , , . , - , /.相似文献