Merger-Induced Starbursts     

Nicole Homeier  J.S. Gallagher 《Astrophysics and Space Science》2002,281(1-2):417-418

Starburst galaxies are extremely luminous objects with an abundance of young massive stars and a disturbed optical morphology. Famous examples such as the Antennae, involve major mergers, but the starburst phenomenon can also be triggered in a more gentle, minor merger. Such an event disturbs but does not disrupt the primary galaxy (i.e. the primary will recover from the interaction without a drastic jump along the Hubble sequence). In such an interaction a significant number of super-star clusters (SSCs) are formed,which may be the progenitors of present-day globular clusters. The ubiquity of globular cluster systems among a wide range of galaxy types suggests that these interactions play a significant role in the evolution of ‘normal’ galaxies. Therefore to understand the formation and evolution of galaxies, it is essential to understand such processes. Here we present a HST WFPC2 broad-band study of three starburst galaxies with different merger histories. This revised version was published online in September 2006 with corrections to the Cover Date.  相似文献   

Magnetic changes observed in the formation of two filaments in a complex active region: TRACE and MSDP observations     

Brigitte Schmieder  Nicole Mein  Yuanyong Deng  Cristiana Dumitrache  Jean-Marie Malherbe  Joachim Staiger  E. E. Deluca 《Solar physics》2004,223(1):119-141

This paper is focused on the formation of two filaments in a complex center of decaying active regions (AR 8329 and AR 8326), located in the northern hemisphere. The observations were obtained in Hα by the Multi-channel Subtractive Double Pass spectrograph (MSDP mounted on the German telescope VTT in Tenerife) and EUV lines with TRACE (Transition Region And Corona Explorer). High Doppler shifts are found to be related to the ends of filament segments where canceling magnetic fields are also located (as seen on magnetograms from Big Bear Solar Observatory). At these locations, velocities along the line of sight, derived by using a cloud model method reach −20 km s⁻¹, the segments of filaments merge and frequently a time-related sub-flare is observed by TRACE. The chirality of the filament segments has been determined by different methods: the segments of dextral chirality join together and form a long dextral filament, and a single filament of sinistral chirality forms end to end with the dextral filament but does not merge with it. Assuming a model of twisted flux tube for filament material, we suggest that the dextral filament has negative helicity and a relationship between its formation and the close by sunspot with the same sign of helicity.  相似文献   

On the formation and evolution of black hole binaries   总被引：1，自引：0，他引：1  

Ph. Podsiadlowski  S. Rappaport  Z. Han 《Monthly notices of the Royal Astronomical Society》2003,341(2):385-404

We present the results of a systematic study of the formation and evolution of binaries containing black holes and normal-star companions with a wide range of masses. We first reexamine the standard formation scenario for close black hole binaries, where the progenitor system, a binary with at least one massive component, experienced a common-envelope phase and where the spiral-in of the companion in the envelope of the massive star caused the ejection of the envelope. We estimate the formation rates for different companion masses and different assumptions about the common-envelope structure and other model parameters. We find that black hole binaries with intermediate- and high-mass secondaries can form for a wide range of assumptions, while black hole binaries with low-mass secondaries can only form with apparently unrealistic assumptions (in agreement with previous studies).
We then present detailed binary evolution sequences for black hole binaries with secondaries of 2 to 17 M_⊙ and demonstrate that in these systems the black hole can accrete appreciably even if accretion is Eddington-limited (up to 7 M_⊙ for an initial black hole mass of 10 M_⊙) and that the black holes can be spun up significantly in the process. We discuss the implications of these calculations for well-studied black hole binaries (in particular GRS 1915+105) and ultraluminous X-ray sources of which GRS 1915+105 appears to represent a typical Galactic counterpart. We also present a detailed evolutionary model for Cygnus X-1, a massive black hole binary, which suggests that at present the system is most likely in a wind mass-transfer phase following an earlier Roche-lobe overflow phase. Finally, we discuss how some of the assumptions in the standard model could be relaxed to allow the formation of low-mass, short-period black hole binaries, which appear to be very abundant in nature.  相似文献   

Type I and Type II chlorophyll-a transformation products associated with algal senescence     

Nicole J. Bale  Ruth L. AirsCarole A. Llewellyn 《Organic Geochemistry》2011,42(5):451-464

Microalgal culture experiments to track chlorophyll-a (chl-a) transformation during senescence were characterised by the production of demetallated Type I chl-a transformation products in Pavlova gyrans and by the production of oxidative Type I transformation products in Isochrysis galbana. Dark-induced senescence in I. galbana produced a different distribution of Type I products from nutrient depletion induced senescence. Several novel Type I compounds were detected, including a chl-d like compound in I. galbana and a chl-a precursor like compound in P. gyrans. Type II chl-a transformation products were detected in the dissolved phase of I. galbana cultures; this is the first report of such compounds associated with marine algae.  相似文献   

Preliminary estimates of regolith generation and mobility in the Susquehanna Shale Hills Critical Zone Observatory,Pennsylvania, using meteoric 10Be     

Nicole West  Eric Kirby  Paul Bierman  Dylan Rood 《Applied Geochemistry》2011

This study seeks to quantify the rate and timing of regolith generation in the Critical Zone at the Susquehanna Shale Hills Critical Zone Observatory (SSHO). Meteoric ¹⁰Be depth profiles were determined using measurements from 30 hillslope soil and bedrock core samples in an effort to constrain ¹⁰Be inventories. The SSHO is located in the temperate climate zone of central Pennsylvania and comprises a first-order watershed developed entirely on a Fe-rich, organic-poor, Silurian-aged shale. Two major perturbations to the landscape have occurred at SSHO in the geologically recent past, including significant and sustained periglacial activity until after the retreat of the Laurentide ice sheet (～21 ka) and deforestation during early colonial land-use. Bulk soil samples (n = 16) were collected at three locations along a planar hillslope on the southern ridge of the catchment, representing the ridge top, mid-slope and valley floor. Rock chip samples (n = 14) were also collected from a 24 m deep core drilled into the northern ridge top. All meteoric ¹⁰Be concentration profiles show a declining trend with depth, with most of the ¹⁰Be retained in the uppermost decimeters of the soil. Meteoric ¹⁰Be inventories are higher at the mid-slope and valley floor sample sites, at 3.71 ± 0.02 × 10¹⁰ at/cm² and 3.69 ± 0.02 × 10¹⁰ at/cm², than at the ridge top site (1.90 ± 0.01 × 10¹⁰ at/cm²). The ¹⁰Be inventory at the convex ridge top site implies a minimum residence time of ～10.6 ka, or if erosion is steady, an erosion rate of 19.4 ± 0.2 m/My.  相似文献   

Arsenic in framboidal pyrite from recent sediments of a shallow water lagoon of the Baltic Sea     

Thomas Neumann  Florian Scholz  Utz Kramar  Michael Ostermaier  Nicole Rausch  Zsolt Berner 《Sedimentology》2013,60(6):1389-1404

Arsenic is a redox‐sensitive element of environmental relevance and often enriched in iron sulphides. Because sediments from the Achterwasser lagoon, a part of the estuarine system of the river Oder, south‐west Baltic Sea, show unexpectedly high pyrite concentrations of up to 7·5 wt% they were used to investigate the influence of authigenic pyrite on the mobility and burial of As in the coastal environment. Micro‐X‐ray‐fluorescence measurements of 106 micrometre‐sized pyrite framboids from the anoxic sediments show highly variable As concentrations ranging from 6 to 1142 μg g^?1. Even within a 1 cm thick layer, the As concentration of different framboids varies greatly and no clear depth trend is visible throughout the 50 cm long sediment core. Pyrite can account for 9 to 55% (average 22%) of the total As budget of the sediments and the degree of trace metalloid pyritization for As ranges from 26 to 61%, indicating that authigenic pyrite formation is an important process in the geochemical cycling of As in coastal sediments. High‐resolution micro‐X‐ray fluorescence mapping of single pyrite grains shows that As is distributed inhomogeneously within larger framboids, suggesting changing pore water composition during pyrite growth. X‐ray absorption near edge structure spectra indicate that As is usually present as As(‐I) substituting S in the pyrite lattice. However, in samples close to the sediment/water interface a considerable part of As is in higher valence states (+III/+V). This can be explained by frequent re‐suspension of the surficial sediments to the oxic water column due to wave action and subsequent re‐deposition, leading to the adsorption of As oxyanions onto pyrite. Although reduced As(‐I) becomes more important in the deeper samples, reflecting decreasing redox potential and a longer time since deposition, the occurrence of oxidized As species (AsIII/AsV) in pyrite in the anoxic part of the sediment suggests formation under dysoxic conditions.  相似文献   

Small-business demise and recovery after Katrina: rate of survival and demise     

Holly L. Schrank  Maria I. Marshall  Adrienne Hall-Phillips  Renee F. Wiatt  Nicole E. Jones 《Natural Hazards》2013,65(3):2353-2374

Post-disaster research is often plagued by displacement of subjects, loss of infrastructure, and the disruption of communication. Economic losses and business disruptions caused by a disaster tend to affect small businesses on a greater scale. With the majority of small businesses being operated out of a home, the inability to recover affects both economic and overall well-being of the business and the family. Specifically for small businesses, post-disaster research is important because it leads to increased preparedness and survival strategies for the sector and reduced economic vulnerabilities in owner-controlled areas. Historically, most of what is known about preparation, response, and recovery of small businesses from natural disasters is based on businesses that have recovered. However, there exists a need for understanding recovery also from the perspective of those that tried, but failed to recover. Grounded in a pragmatic approach, this study presents a methodology for tracking demised small businesses after Hurricane Katrina. Supported by empirical evidence, solutions to the problems of timing, generalizability, and access are presented, providing a systematic methodology for successfully studying small businesses after a disaster event. Rate of survival and demise data are presented, providing more useful numbers than prior estimates. Locating demised and recovered small businesses efficiently is the first step in understanding how business owners prepare, react, adjust, and strive to recover from disaster-driven events. A solution to this challenging issue of access makes the study of demised small businesses possible.  相似文献   

Is earthquake activity along the French Atlantic margin favoured by local rheological contrasts?     

Yves Mazabraud  Nicole Béthoux  Bertrand Delouis 《Comptes Rendus Geoscience》2013,345(9-10):373-382

The seismological study of recent seismic crises near Oleron Island confirms the coexistence of an extensional deformation and a transtensive regime in the Atlantic margin of France, which is different from the general western European stress field corresponding to a strike-slip regime. We argue that the switch of the principal stress axes σ₁/σ₂ in a NW–SE vertical plane is linked with the existence of crustal heterogeneities. Events of magnitude larger than 5 sometimes occur along the Atlantic margin of France, such as the 7 September 1972 (M_L = 5.2) earthquake near Oleron island and the 30 September 2002 (M_L = 5.7) Hennebont event in Brittany. To test the mechanism of local strain localization, we model the deformation of the hypocentral area of the Hennebont earthquake using a 3D thermo-mechanical finite element code. We conclude that the occurrence of moderate earthquakes located in limited parts of the Hercynian shear zones (as the often reactivated swarms near Oleron) could be due to local reactivation of pre-existing faults. These sporadic seismic ruptures are favoured by stress concentration due to rheological heterogeneities.  相似文献   

Influence of the circumglobal wave-train on European summer precipitation     

Sajjad Saeed  Nicole Van Lipzig  Wolfgang A. Müller  Fahad Saeed  Davide Zanchettin 《Climate Dynamics》2014,43(1-2):503-515

We investigate European summer (July–August) precipitation variability and its global teleconnections using the NCEP/NCAR reanalysis data (1950–2010) and a historical Coupled Model Intercomparison Project climate simulation (1901–2005) carried out using the ECHAM6/MPIOM climate model. A wavelike pattern is found in the upper tropospheric levels (200 hPa) similar to the summer circumglobal wave train (CGT) extending from the North Pacific to the Eurasian region. The positive phase of the CGT is associated with upper level anomalous low (high) pressure over western (eastern) Europe. It is further associated with a dipole-like precipitation pattern over Europe entailing significantly enhanced (reduced) precipitation over the western (eastern) region. The anomalous circulation features and associated summer precipitation pattern over Europe inverts for the negative CGT phase. Accordingly, the global teleconnection pattern of a precipitation index summarizing summer precipitation over Western Europe entails an upper level signature which consists of a CGT-like wave pattern extending from the North Pacific to Eurasia. The imprint of the CGT on European summer precipitation is distinct from that of the summer North Atlantic Oscillation, despite the two modes of variability bear strong similarities in their upper level atmospheric pattern over Western Europe. The analysis of simulated CGT features and of its climatic implications for the European region substantiates the existence of the CGT-European summer precipitation connection. The summer CGT in the mid-latitude therefore adds to the list of the modes of large-scale atmospheric variability significantly influencing European summer precipitation variability.  相似文献   

The Relationship of Place Re-Making and Watershed Group Participation in Appalachia     

Heather A. Lukacs  Nicole M. Ardoin 《社会与自然资源》2014,27(1):55-69

This article explores how participation in watershed groups creates a social space that mediates the relationship between biophysical places and place-protective action. We analyze qualitative data from a survey of more than 200 watershed group volunteers in the Appalachian region of the United States who were asked to describe experiences that encouraged or discouraged their participation. “Place” emerged as a key theme, with further delineations between made places (those highly affected by human activity, including coal extraction); natural places; and re-made places (those restored by the efforts of the watershed-group participants). Our findings suggest that the places themselves—and the natural, institutional, and social resources in these places—are more than a backdrop or setting for the volunteer activities; they also inspire, enhance, and are transformed by the act of volunteering.  相似文献