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31323334 1651 - 1652 of 1652
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  • 1651.
    Österlin, Calle
    Stockholms universitet, Naturvetenskapliga fakulteten, Institutionen för naturgeografi och kvartärgeologi (INK).
    A systems approach to biogasplanning in Stockholm, Sweden2012Independent thesis Advanced level (degree of Master (Two Years)), 20 poäng / 30 hpOppgave
    Abstract [en]

    The Swedish capital Stockholm is at the forefront of biogas gas use, especially when it comesto biogas used for vehicle gas. This technology has the potential of being a fuel with veryhigh environmental performance, but in order to realize the full potential publicenvironmental management must be optimized. Environmental objectives are anenvironmental management is one tool that is used to strive for the desired development. Theaim of this study is to explain the dynamics within the biogas system in Stockholm, with aparticular emphasis on which factors that affects the amount of biogas available for vehiclegas upgrading on the market in Stockholm. The study has been conducted using modelingsessions with key stakeholders involved in the biogas system. The study concludes that theformulation of environmental objectives has a profound impact on how the variousstakeholders act, and thus how the system behaves. The trade off of how much fossil naturalgas that can be mixed into the renewable biogas based vehicle gas is at the very pinnacle ofcomplex matter. A conclusion that is of vital importance for the local planning process andwhen the experiences of Stockholm’s environmental planning are communicated out to therest of the world.

  • 1652.
    Österlin, Carl
    Stockholms universitet, Naturvetenskapliga fakulteten, Institutionen för naturgeografi och kvartärgeologi (INK).
    STABLE CARBON ISOTOPES IN SPELEOTHEMS FROM TEMPERATE AREAS2010Independent thesis Basic level (degree of Bachelor), 10 poäng / 15 hpOppgave
    Abstract [en]

    Speleothems are considered a reliable proxy for paleoclimatic reconstructions and analysis of stable carbon isotopes in speleothems is used for paleoclimatic reconstructions. However, in temperate areas that lacks C4 vegetation there are uncertainties in how to interpret changes in the δ13C signal. The aim of this study is toincrease the understanding of how the δ13C signal in speleothems from temperateareas can be interpreted. The study was divided in two parts, first a literature studythat focused on interpretations of the δ13C signal in speleothems from temperate areasand a case study in which a comparison of seven 13C records from similarenvironments in the Scandes Mountains and the Alps are made. The results from the literature study were used in the case study to draw conclusions on tree line and vegetation changes during Holocene in central northern Scandinavia. The study showed that trends in interpretation of the δ13C signal in speleothems from temperateareas are that low δ13C values are interpreted as wetter, warmer conditions with higherbio productivity, and high δ13C values are interpreted as colder, drier conditions withlower bio productivity. Further it was found in the study that vegetation changes seen in Holocene pollen data are also seen in δ13C records from Scandinavia. The δ13Csignal in temperate speleothems therefore appears to be related to changes invegetation density and to tree-line changes.

31323334 1651 - 1652 of 1652
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