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81.
Roberto Carniel Marta Tárraga Fausto Barazza Alicia García 《Bulletin of Volcanology》2008,70(9):1113-1121
Continuous seismic noise is recorded in the volcanic island of Tenerife (Canary Islands, Spain). The origin of this noise,
strongly augmented by anthropogenic contamination, is still under debate. In this paper, we discuss the relationship between
this noise and the occurrence of local tectonic events in the same area. In particular, transitions are sought in the time
evolution of dynamic parameters computed on the seismic noise, and examples are shown where abrupt transitions may be associated
with the occurrence of tectonic events. These transitions provide further evidence of the existence of a natural origin for
at least part of the seismic noise, which is strongly contaminated—if not dominated—by anthropogenic sources. 相似文献
82.
83.
E. Davesne K. Dideriksen B.C. Christiansen K.B. Ayala-Luis H.C.B. Hansen 《Geochimica et cosmochimica acta》2010,74(22):6451-6467
In a recent study, sulphate-bearing green rust (GRSO4) was shown to incorporate Na+ in its structure (NaFeII6FeIII3(OH)18(SO4)2(s); GRNa,SO4). The compound was synthesised by aerial oxidation of Fe(OH)2(s) in the presence of NaOH. This paper reports on its free energy of formation .Freshly synthesised GRNa,SO4 was titrated with 0.5 M H2SO4 in an inert atmosphere at 25 °C, producing dissolved Fe2+ and magnetite or goethite. Solution concentrations, PHREEQC and the MINTEQ database were used to calculate reaction constants for the reactions:
84.
85.
A detailed study of the lipids of selected zooplankton species and scavenging amphipods in the near-bottom water layer (15–100 m above bottom, mab) was carried out at the BENGAL site in late summer 1998. Copepoda were the main contributors to the zooplankton, comprising 75% of the total abundance, followed by Ostracoda and Chaetognatha. Calanoid copepods of the family Metridinidae were predominant and accounted for more than 50% of all copepods.Two types of storage lipids were distinguished: triacylglycerols and wax esters. Ostracoda and the polychaete Vanadis sp. stored exclusively triacylglycerols whilst the bulk of the Copepoda accumulated wax esters, with the exception of the family Aetideidae. In the amphipods both lipid classes were found: Eurythenes gryllus stored wax esters and Paralicella spp. and Orchomene sp. triacylglycerols.The fatty acid composition was characterized by a high level of monounsaturated 18:1 (n—9), which is described as characteristic for animals living in the deeper layers of the water column, and to a lesser degree by 16:1 (n—7) and 20:5 (n—3), which are typical components of diatom lipids, and 22:6 (n—3), typical of dinoflagellates. The ratio of 18:1 (n—9):18:1 (n—7) fatty acids was between 5 and 10 in the copepods and indicates a carnivorous/omnivorous feeding behaviour in this group, whereas the higher ratios of 8–18 in the amphipods confirm their necrophagy. The fatty alcohols of the animals storing wax esters were dominated by the monounsaturated isomers 18:1 (n—9) and 18:1 (n—7).The predominance of wax esters as storage lipids in the deep-sea copepods indicates a strong seasonality in the availability of food. This is supported by the high levels of 16:1 (n—7), 20:5 (n—3) and 22:6 (n—3) fatty acids, which point to there being a direct link between the surface primary production and deep-sea copepods, probably via the rapid deposition of phytodetritus. 相似文献
86.
87.
Javier Arístegui Eric D. Barton Paul Tett María F. Montero Mercedes García-Muoz Gotzon Basterretxea Anne-Sophie Cussatlegras Alicia Ojeda Demetrio de Armas 《Progress in Oceanography》2004,62(2-4):95
The variability in dissolved and particulate organic matter, plankton biomass, community structure and metabolism, and vertical carbon fluxes were studied at four stations (D1–D4), placed along a coastal-offshore gradient of an upwelling filament developed near Cape Juby (NW Africa). The filament was revealed as a complex and variable system in terms of its hydrological structure and distribution of biological properties. An offshore shift from large to small phytoplankton cells, as well as from higher to lower autotrophic biomass, was not paralleled by a similar gradient in particulate (POC) or dissolved (DOC) organic carbon. Rather, stations in the central part of the filament (D2 and D3) presented the highest organic matter concentrations. Autotrophic carbon (POCChl) accounted for 53% (onshore station, D1) to 27% (offshore station, D4) of total POC (assuming a carbon to chlorophyll ratio of 50), from which nano- and pico-phytoplankton biomasses (POCA < 10 μm) represented 14% (D1) to 79% (D4) of POCChl. The biomass of small hetrotrophs (POCH < 10 μm) was equivalent to POCA < 10 μm, except at D1, where small autotrophs were less abundant. Dark community respiration (Rd) in the euphotic zone was in general high, almost equivalent to gross production (Pg), but decreasing offshore (D1–D4, from 108 to 41 mmol C m−2 d−1). POC sedimentation rates (POCsed) below the euphotic zone ranged from 17 to 6 mmol C m−2 d−1. Only at D4 was a positive carbon balance observed: Pg−(Rd + POCsed) = 42 mmol C m−2 d−1. Compared to other filament studies from the NE Atlantic coast, the Cape Juby filament presented lower sedimentation rates and higher respiration rates with respect to gross production. We suggest that this is caused by the recirculation of the filament water, induced by the presence of an associated cyclonic eddy, acting as a trapping mechanism for organic matter. The export capacity of the Cape Juby filament therefore would be constrained to the frequency of the interactions of the filament with island-induced eddies. 相似文献
88.
89.
P. L. Christoffersen C. Christiansen J. B. Jensen T. Leipe S. Hille 《Geo-Marine Letters》2007,27(5):325-338
Information on grain-size distribution and total organic carbon (TOC) content of surface sediment and cores from the Bornholm
Basin, together with dating of cores using the 210Pb method and shallow seismic chirp profiling, has been analysed to elucidate long-term accumulation patterns. The presence
of non-depositional areas with lag sediments and low TOC content below the wave base indicates that inflows of dense bottom
water originating in the North Sea and associated near-bottom currents have strong influence on the depositional patterns
of bulk sediment and organic matter in this deep basin. The general fining in mean grain size towards the northeast corresponds
to the direction of inflow currents and prevailing winds. Recent and previously found 210Pb-based mean accumulation rates vary greatly within the basin, between 129 and 1,144 g m−2 year−1. The accumulation rate may vary by a factor of three even between stations located only 3–4 km apart. Rates recorded close
to a seismic profile are consistent with the variation in Holocene sediment thickness. This variation reflects a depositional
system controlled by near-bottom inflow currents, consisting of a large-scale channel and a wedge-formed sediment package.
The spatial variation in TOC content depends partly on water depth, presumably due to generally poorer degradation in the
deepest part of the basin because of less frequent oxygen supply by inflow water. Moreover, there is a tendency of higher
TOC contents in the southern part of the basin, which may be due to the input of sediments originating from the Oder River.
Compared to values for the central, deep Baltic Sea, TOC contents show lower values of 4–6% and insignificant temporal variations.
This may be due to the Bornholm Basin being located much closer to the source of the more oxic inflow water, resulting in
more favourable degradation conditions. 相似文献
90.
Erik O. D. Sevre Monica D. Christiansen Matt Broten Shuo M. Wang David A. Yuen 《Visual Geosciences》2008,13(1):125-132
The Sony PlayStation 3 (PS3) offers the computational power of a parallel processor at low cost, which makes it a great starter
unit for development in parallel programming. To explore the capabilities of the unit, we took a simple ray tracing program
and extended it to render triangulated height field data across the PS3’s 6 synergistic processing units (SPUs). We also implemented
the heat averaging equation as a precursor to CFD analysis on the PS3. In our studies, we found the Cell engine in the PS3
to be a powerful machine, however great care must be taken while developing because its unique platform calls for many levels
of optimization to ensure efficiency.
For insight on early work done on modern stream computing and GPU processing look up the Merrimac project and Pat Hanrahan. 相似文献