TY - JOUR A1 - Eibl, Eva P. S. A1 - Müller, Daniel A1 - Walter, Thomas R. A1 - Allahbakhshi, Masoud A1 - Jousset, Philippe A1 - Hersir, Gylfi Páll A1 - Dahm, Torsten T1 - Eruptive cycle and bubble trap of Strokkur Geyser, Iceland JF - Journal of geophysical research : JGR. B: Solid earth N2 - The eruption frequency of geysers can be studied easily on the surface. However, details of the internal structure including possible water and gas filled chambers feeding eruptions and the driving mechanisms often remain elusive. We used a multidisciplinary network of seismometers, video cameras, water pressure sensors and one tiltmeter to study the eruptive cycle, internal structure, and mechanisms driving the eruptive cycle of Strokkur geyser in June 2018. An eruptive cycle at Strokkur always consists of four phases: (1) Eruption, (2) post-eruptive conduit refilling, (3) gas filling of the bubble trap, and (4) regular bubble collapse at shallow depth in the conduit. For a typical single eruption 19 +/- 4 bubble collapses occur in Phase 3 and 8 +/- 2 collapses in Phase 4 at a mean spacing of 1.52 +/- 0.29 and 24.5 +/- 5.9 s, respectively. These collapses release latent heat to the fluid in the bubble trap (Phase 3) and later to the fluid in the conduit (Phase 4). The latter eventually reaches thermodynamic conditions for an eruption. Single to sextuple eruptions have similar spacings between bubble collapses and are likely fed from the same bubble trap at 23.7 +/- 4.4 m depth, 13-23 m west of the conduit. However, the duration of the eruption and recharging phase linearly increases likely due to a larger water, gas and heat loss from the system. Our tremor data provides documented evidence for a bubble trap beneath a pool geyser. KW - bubble trap KW - eruptive cycle KW - geyser KW - hydrothermal systems KW - source KW - location KW - tremor Y1 - 2021 U6 - https://doi.org/10.1029/2020JB020769 SN - 2169-9313 SN - 2169-9356 VL - 126 IS - 4 PB - Wiley CY - Hoboken, NJ ER - TY - JOUR A1 - Jänicke, Clemens A1 - Goddard, Adam A1 - Stein, Susanne A1 - Steinmann, Horst-Henning A1 - Lakes, Tobia A1 - Nendel, Claas A1 - Müller, Daniel T1 - Field-level land-use data reveal heterogeneous crop sequences with distinct regional differences in Germany JF - European journal of agronomy N2 - Crop cultivation intensifies globally, which can jeopardize biodiversity and the resilience of cropping systems. We investigate changes in crop rotations as one intensification metric for half of the croplands in Germany with annual field-level land-use data from 2005 to 2018. We proxy crop rotations with crop sequences and compare how these sequences changed among three seven-year periods. The results reveal an overall high diversity of crop sequences in Germany. Half of the cropland has crop sequences with four or more crops within a seven-year period, while continuous cultivation of the same crop is present on only 2% of the cropland. Larger farms tend to have more diverse crop sequences and organic farms have lower shares of cereal crops. In three federal states, crop rotations became less structurally diverse over time, i.e. the number of crops and the number of changes between crops decreased. In one state, structural diversity increased and the proportion of monocropping decreased. The functional diversity of the crop sequences, which measures the share of winter and spring crops as well as the share of leaf and cereal crops per sequence, remained largely stable. Trends towards cereal-or leaf -crop dominated sequences varied between the states, and no clear overall dynamic could be observed. However, the share of winter crops per sequence decreased in all four federal states. Quantifying the dynamics of crop sequences at the field level is an important metric of land-use intensity and can reveal the patterns of land-use intensification. KW - crop production KW - crop rotation KW - cropping diversity KW - IACS KW - intensification KW - land-use intensity Y1 - 2022 U6 - https://doi.org/10.1016/j.eja.2022.126632 SN - 1161-0301 SN - 1873-7331 VL - 141 PB - Elsevier CY - Amsterdam ER - TY - THES A1 - Müller, Daniel T1 - Identification and monitoring of structures, controls, and evolution dynamics of hydrothermal systems and associated alteration through high-resolution remote sensing and in situ analysis T1 - Identifizierung und Überwachung von Strukturen, Kontrollmechanismen und Entwicklungsdynamiken hydrothermaler Systeme und damit verbundener Alteration durch hochauflösende Fernerkundung und In-situ-Analyse N2 - Volcanic hydrothermal systems are an integral part of most volcanoes and typically involve a heat source, adequate fluid supply, and fracture or pore systems through which the fluids can circulate within the volcanic edifice. Associated with this are subtle but powerful processes that can significantly influence the evolution of volcanic activity or the stability of the near-surface volcanic system through mechanical weakening, permeability reduction, and sealing of the affected volcanic rock. These processes are well constrained for rock samples by laboratory analyses but are still difficult to extrapolate and evaluate at the scale of an entire volcano. Advances in unmanned aircraft systems (UAS), sensor technology, and photogrammetric processing routines now allow us to image volcanic surfaces at the centimeter scale and thus study volcanic hydrothermal systems in great detail. This thesis aims to explore the potential of UAS approaches for studying the structures, processes, and dynamics of volcanic hydrothermal systems but also to develop methodological approaches to uncover secondary information hidden in the data, capable of indicating spatiotemporal dynamics or potentially critical developments associated with hydrothermal alteration. To accomplish this, the thesis describes the investigation of two near-surface volcanic hydrothermal systems, the El Tatio geyser field in Chile and the fumarole field of La Fossa di Vulcano (Italy), both of which are among the best-studied sites of their kind. Through image analysis, statistical, and spatial analyses we have been able to provide the most detailed structural images of both study sites to date, with new insights into the driving forces of such systems but also revealing new potential controls, which are summarized in conceptual site-specific models. Furthermore, the thesis explores methodological remote sensing approaches to detect, classify and constrain hydrothermal alteration and surface degassing from UAS-derived data, evaluated them by mineralogical and chemical ground-truthing, and compares the alteration pattern with the present-day degassing activity. A significant contribution of the often neglected diffuse degassing activity to the total amount of degassing is revealed and constrains secondary processes and dynamics associated with hydrothermal alteration that lead to potentially critical developments like surface sealing. The results and methods used provide new approaches for alteration research, for the monitoring of degassing and alteration effects, and for thermal monitoring of fumarole fields, with the potential to be incorporated into volcano monitoring routines. N2 - Vulkanische Hydrothermalsysteme sind ein integraler Bestandteil vieler Vulkane und erfordern allgemein eine ausreichende Wärmequelle, eine ausreichende Flüssigkeitszufuhr und Kluft- oder Porensysteme, durch die Flüssigkeiten zirkulieren können. Damit verbunden sind subtile, aber wirksame Prozesse, welche die Entwicklung der vulkanischen Aktivität oder die Stabilität des oberflächennahen Vulkansystems durch mechanische Schwächung, Verringerung der Durchlässigkeit und Versiegelung des betroffenen vulkanischen Gesteins erheblich beeinflussen können. Solche Prozesse sind für Gesteinsproben durch Laboranalysen gut definiert, aber es ist immer noch schwierig sie auf der Skala eines ganzen Vulkans zu bewerten. Fortschritte bei unbemannten Flugsystemen (UAS), Sensortechnologie und photogrammetrischen Prozessierungs-routinen ermöglichen es uns heute, Vulkanoberflächen im Zentimeterbereich abzubilden und damit vulkanische Hydrothermalsysteme sehr detailliert zu untersuchen. Ziel dieser Arbeit ist es, deren Potenzial für die Untersuchung der Strukturen, Prozesse und Dynamik solcher Systeme zu erforschen, aber auch methodische Ansätze zu finden, um in den Daten verborgene Sekundärinformationen zu analysieren, die auf raum-zeitliche Dynamiken oder potenziell kritische Entwicklungen im Zusammenhang mit hydrothermaler Alteration hinweisen können. Wir haben zwei oberflächennahe vulkanische hydrothermale Systeme analysiert, das Geysirfeld von El Tatio in Chile und das Fumarolenfeld von La Fossa di Vulcano in Italien, die beide zu den am besten untersuchten Systemen ihrer Art gehören. Durch Bildanalyse, statistische und räumliche Analysen konnten wir das bisher detaillierteste Abbild des strukturellen Aufbaus beider Standorte erstellen, neue Einblicke in die oft faszinierende Systematik solcher Systeme geben, aber auch neue potenzielle Kontrollfaktoren aufzeigen. Die Ergebnisse werden in konzeptionellen Modellen zusammengefasst. Darüber hinaus haben wir methodische Ansätze der Fernerkundung zur Erkennung, Klassifizierung und räumlichen Eingrenzung hydrothermaler Alteration aus UAS-Daten untersucht, durch mineralogisches und chemisches „Ground-Truthing“ bewertet und die Alterationsmuster mit der aktuellen Entgasungsaktivität verglichen. Wir zeigen dass die oft nicht berücksichtigte diffuse Aktivität einen signifikanten Beitrag zur Gesamtaktivität liefert, aber auch Bereiche in denen sekundäre Prozesse hydrothermaler Alteration scheinbar zu potenziell kritischen Entwicklungen wie Oberflächenversiegelung führen. Die Ergebnisse und die verwendeten Methoden bieten neue Ansätze für die Alterationsforschung, für die Überwachung von Entgasungs- und Alterationseffekten und für die thermische Überwachung von Fumarolenfeldern, und haben Potential in Vulkanüberwachungsroutinen integriert zu werden. KW - volcano remote sensing KW - Fernerkundung an Vulkanen KW - volcanic hydrothermal systems KW - vulkanische Entgasungs-und Hydrothermalsysteme KW - Vulkanüberwachung KW - hydrothermale Alteration KW - vulkanische Entgasungssysteme KW - Drohnen-Fernerkundung Y1 - 2024 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-626683 ER - TY - JOUR A1 - Müller, Daniel A1 - Schröder-Esselbach, Boris A1 - Müller, Jörg T1 - Modelling habitat selection of the cryptic Hazel Grouse Bonasa bonasia in a montane forest N2 - The Hazel Grouse Bonasa bonasia is strongly affected by forest dynamics, and populations in many areas within Europe are declining. As a result of the 'wilding' concept implemented in the National Park Bavarian Forest, this area is one of the refuges for the species in Germany. Even though the effects of prevailing processes make the situation there particularly interesting, no recent investigation about habitat selection in the rapidly changing environment of the national park has been undertaken. We modelled the species-habitat relationship to derive the important habitat features in the national park as well as factors and critical threshold for monitoring, and to evaluate the predictive power of models based on field surveys compared to an analysis of infrared aerial photographs. We conducted our surveys on 49 plots of 25 ha each where Hazel Grouse was recorded and on an equally sized set of plots with no grouse occurrence, and used this dataset to build a predictive habitat-suitability model using logistic regression with backward stepwise variable selection. Habitat heterogeneity, stand structure, presence of mountain ash and willow, root plates, forest aisles, and young broadleaf stands proved to be predictive habitat variables. After internal validation via bootstrapping, our model shows an AUC value of 0.91 and a correct classification rate of 87%. Considering the methodological difficulties attached to backward selection, we applied Bayesian model averaging as an alternative. This multi-model approach also yielded similar results. To derive simple thresholds for important predictors as a basis for management decisions, we alternatively ran tree-based modelling, which also leads to a very similar selection of predictors. Performance of our different survey approaches was assessed by comparing two independent models with a model including both data resources: one constructed only from field survey data, the other based on data derived from aerial photographs. Models based on field data seem to perform slightly better than those based on aerial photography, but models using both predictor datasets provided the highest predictive accuracy. Y1 - 2009 UR - http://www.springerlink.com/content/110831 U6 - https://doi.org/10.1007/s10336-009-0390-6 SN - 0021-8375 ER -