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101.
Ira H. Gilbert 《Astrophysics and Space Science》1971,14(1):3-10
The theory of collisional relaxation in stellar systems is discussed in terms of an expansion in powers of 1/N, the inverse of the total number of stars. The results are expressed in terms of the concept of gravitational polarization. 相似文献
102.
Activity levels of carbonic anhydrase (CA) were assessed in anemones Condylactis gigantea and Stichodactyla helianthus with laboratory exposures to copper, nickel, lead, and vanadium, and also in animals collected from polluted vs pristine field sites. CA activity was found to be decreased with increase in metal concentration and also in animals collected from the polluted field site. Preliminary assessments to adapt the CA assay for use in the widespread coral Montastraea cavernosa show decreased CA activity in specimens from the polluted field site and provide an avenue for future research aimed at more thoroughly describing coral CA activity for potential application in bioindication. 相似文献
103.
The offshore east African rift system: new insights from the Sakalaves seamounts (Davie Ridge,SW Indian Ocean)
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Simon Courgeon Patrick Bachèlery Gwénael Jouet Stephan J. Jorry Esther Bou Marcelle K. BouDagher‐Fadel Sidonie Révillon Gilbert Camoin Emmanuelle Poli 《地学学报》2018,30(5):380-388
The offshore branch of the East African Rift System (EARS) has developed during Late Cenozoic time along the eastern Africa continental margin. While Neogene–Pleistocene extensional tectonic deformation has been evidenced along the northern segment of the Davie Ridge, the spatial extent of deformation further south remains poorly documented. Based on recent and various oceanographic datasets (bathymetric surveys, dredge samples and seismic profiles), our study highlights active normal faulting, modern east–west extensional tectonic deformation and Late Cenozoic alkaline volcanism at the Sakalaves Seamounts (18°S, Davie Ridge) that seem tightly linked to the offshore EARS development. In parallel, rift‐related tectonic subsidence appears responsible for the drowning of the Sakalaves Miocene shallow‐water carbonate platform. Our findings bring new insights regarding the development of the EARS offshore branch and support recent kinematic models proposing the existence of a plate boundary across the Mozambique Channel. 相似文献
104.
Jonathan M. Malzone Ethan G. Sweet Addison C. Bell Gilbert L. Minzenberger 《水文研究》2020,34(4):1089-1100
Geographically isolated wetlands (GIWs) are commonly reported as having hardpan or low hydraulic conductivity units underneath that produce perched groundwater, which can sustain surface water levels independently of regional aquifer fluctuations. Despite the potential of GIW-perched aquifer systems to provide important hydrological and ecological functions such as groundwater storage and native amphibian habitat, little research has studied the hydrologic controls and dynamics of these systems. We compared several ridge-top depressional GIW-perched groundwater systems to investigate the role of watershed morphology on hydroregime and groundwater-surface water interaction. Ridge-top depressional wetlands in the Daniel Boone National Forest, Kentucky were chosen because they offer natural controls such as lack of apparent connection to surface water bodies, similar climate, and similar soils. Three wetlands with different topographic slopes and hillslope structures were mapped to distinguish key geomorphic parameters and monitored to characterize groundwater-surface water interaction. Wetlands with soil hummocks and low upland slopes transitioned from infiltration to groundwater discharge conditions in the spring and during storm events. The magnitude and duration of this transition fell along a continuum, where higher topographic slopes and steeper uplands produced comparably smaller and shorter head reversals. This demonstrates that ridge-top GIW-perched groundwater systems are largely sensitive to the runoff-recharge relationship in the upland area which can produce significant groundwater storage on a small-scale. 相似文献
105.
Xiaolan L. Wang Hui Wan Francis W. Zwiers Val R. Swail Gilbert P. Compo Robert J. Allan Russell S. Vose Sylvie Jourdain Xungang Yin 《Climate Dynamics》2011,37(11-12):2355-2371
This study analyzes extremes of geostrophic wind speeds derived from sub-daily surface pressure observations at 13 sites in the European region from the Iberian peninsula to Scandinavia for the period from 1878 or later to 2007. It extends previous studies on storminess conditions in the Northeast (NE) Atlantic-European region. It also briefly discusses the relationship between storminess and the North Atlantic Oscillation (NAO). The results show that storminess conditions in the region from the Northeast Atlantic to western Europe have undergone substantial decadal or longer time scale fluctuations, with considerable seasonal and regional differences (especially between winter and summer, and between the British Isles-North Sea area and other parts of the region). In the North Sea and the Alps areas, there has been a notable increase in the occurrence frequency of strong geostrophic winds from the mid to the late twentieth century. The results also show that, in the cold season (December–March), the NAO-storminess relationship is significantly positive in the north-central part of this region, but negative in the south-southeastern part. 相似文献
106.
We analyzed lake sediment deposits and local hydrometric records to assess the potential for developing a high-resolution
record of sediment delivery from the Rock Lake catchment, situated in the non-glacierized Front Ranges of the Rocky Mountains,
Canada. Rhythmic couplets of silt–clay characterized the clastic sediments recovered from the deep central basin of the lake.
Contemporary sediment yield to Rock Lake (10.7 ± 1.8 Mg km−2 year−1) is comparable to other studied Canadian Cordillera lakes that have sedimentary lithologies and absence of glacier cover,
but distinct rhythmic deposition is relatively unique to this basin. Spatial patterns of deposition within the lake were assessed
by correlating rhythmites between multiple sediment cores and by sub-bottom, acoustic profiling. Bracketed dates for a spatially
continuous sequence of eight thick rhythmites were established by correlating laminations between core samples collected more
than 30 years apart. We identified a consistent pattern between the rhythmite and hydrometric data series between 1975 and
2006 and determined that specific flooding events caused by summer rainstorms are associated with each of the eight thick
rhythmites. We observed a good relationship between rhythmite thickness and total flood volume that exceeded a threshold discharge.
Acoustic profiling showed that the lake could be a good candidate for longer-term proxy development. We discuss how some of
the methods used in this study could benefit ongoing paleoenvironmental assessments based on lacustrine rhythmite series. 相似文献
107.
108.
109.
Differential Kernels for Group Velocity 总被引:1,自引:1,他引:0
Freeman Gilbert 《Geophysical Journal International》1976,44(3):649-660
110.
David Gilbert Armin Freundt Steffen Kutterolf Cosima Burkert 《International Journal of Earth Sciences》2014,103(7):2043-2062
The Lonquimay volcanic complex (LVC) in the high Southern Andes comprises a stratocone and NE-trending flank-cone alignments. Numerous effusive and explosive volcanic eruptions characterize its post-glacial magmatic activity. Our tephrostratigraphic record, pre-dating the four historically documented eruptions, comprises 22 dated pyroclastic deposits that are used to constrain repose time distribution and eruption probability of the LVC magmatic system. Statistical examination of the stratigraphy-based eruption time series yields probabilities of 20–50 % for at least one explosive (VEI ≥ 3) eruption within the next 100 years as of 2011. The tephra deposits are subdivided into three petrographic groups: a felsic group (Lonquimay colored-pumice tephra, LCPT), an intermediate population (Lonquimay gray pumice tephra, LGPT), and a mafic member (Lonquimay dark scoria tephra, LDST). The distribution of these petrographic groups through the LVC tephrostratigraphy is linked to the observed changes in repose times. LDST-deposits as well as deposits compositionally zoned from LCPT to LGPT dominate the lower part of the stratigraphy for which recurrence times are short (RTmean = 417 ± 169a). Deposits younger than 6,000 b2k (years before 2000 AD) have dominantly LCPT and minor LDST compositions, no longer contain LGPT, and repose times are significantly longer (RTmean = 1,350 ± 310a). We interpret the change in eruption regime to result from a rearrangement in the magma storage and plumbing system. Thermobarometric calculations based on cpx–liquid equilibria and amphibole compositions reveal three distinct magma storage levels: the mafic LDST derive from mid crustal storage (P mean = 476 ± 95 MPa, T mean = 1,073 ± 24 °C), felsic LCPT mainly erupted from upper-crustal level (P mean = 86 ± 49 MPa, T mean = 936 ± 24 °C), whereas LGPT samples yield intermediate storage depths (P mean = 239 ± 100 MPa, T mean = 1,013 ± 17 °C). Magma contributions from this intermediate reservoir are restricted to >6,000 b2k when the Lonquimay plumbing system was in a regime of short repose times; disappearance of the intermediate reservoir coincides with the change to longer repose times between eruptions. 相似文献