Autoregressive estimation of complex eigenfrequencies in low frequency seismic spectra   总被引：5，自引：0，他引：5  

B. Feng Chao  Freeman Gilbert 《Geophysical Journal International》1980,63(3):641-657

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The fact that a seismogram can be represented as an autoregressive (AR) time series and the use of Prony's method enable us to obtain the complex frequencies from the poles of the corresponding AR process. A frequency-domain formulation which employs a time-domain tapering technique is devised so that spectral peaks can be analysed individually, or in small groups. Statistical analysis of the estimators and several examples from two recent earthquakes illustrate the method.  相似文献   

A photoautotrophic source for lycopane in marine water columns     

Wakeham SG  Freeman KH  Pease TK  Hayes JM 《Geochimica et cosmochimica acta》1993,57(1):159-165

Suspended particulate matter and recent sediments from diverse oceanic sites have been investigated for their contents of lycopane. Lycopane was present in all samples, including both oxic and anoxic water column and sediments. The highest concentrations in the water column were found in surface waters of the central Pacific gyre (1.5 ng/L) and in the anoxic waters of the Cariaco Trench (1.1 ng/L) and the Black Sea (0.3 ng/L). Vertical concentration profiles suggest that lycopane is probably algal in origin. Moreover, biogeochemical conditions in anoxic zones apparently result in a secondary production of lycopane from an as yet unidentified precursor. Compound-specific carbon isotopic analyses have been carried out on lycopane from water column and sediment samples. Isotopic compositions of lycopane range between -23.6% and -32.9% and are consistent with a photoautotrophic origin. We postulate that some lycopane is produced in surface waters of the ocean, while additional lycopane is produced in anoxic zones by anaerobic microbial action on an algal precursor.  相似文献   

Elastic waves in a transitional solid with arbitrarily small rigidity     

Freeman Gilbert 《Geophysical Journal International》1998,133(2):230-232

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The upper atmosphere of Neptune: An analysis of occultation observations     

Kathy Rages  Joseph Veverka  Lawrence Wasserman  K.C. Freeman 《Icarus》1974,23(1):59-65

An analysis of available observations of the April 7, 1968 occultation of BD ?17° 4388 by Neptune yields upper atmosphere temperatures of ～140°K near the 5 × 10¹⁴cm^?3 level. The temperature structure of the atmosphere at these levels is complicated and nonisothermal. Diurnal temperature variations are certainly less than 10°K and may be absent. The average temperature decreases by less than 15°K between 0° and 55° latitude.  相似文献   

Lunar electric fields,surface Potential and Associated Plasma Sheaths   总被引：1，自引：0，他引：1  

J. W. Freeman  M. Ibrahim 《Earth, Moon, and Planets》1975,14(1):103-114

This paper reviews the electric field environment of the Moon. Lunar surface electric potentials are reported as follows: Solar Wind - Dayside: ø_o + 10 to + 18 V Solar Wind - Terminator: ø_o ç ? 10 to ? 100 V Electron and ion densities in the plasma sheath adjacent to each surface potential regime are evaluated and the corresponding Debye length estimated. The electric fields are then approximated by the surface potential over the Debye length. The results are: Solar Wind - Dayside: E_o ? 10 V m^?1 outward Solar Wind - Terminator: E_o ç 1 to 10 V m^?1 inward These fields are all at least 3 orders of magnitude higher than the pervasive solar wind electric field; however they are confined to within a few tens of meters of the lunar surface.  相似文献   

The Resolving Power of Gross Earth Data   总被引：22，自引：0，他引：22  

George Backus  Freeman Gilbert 《Geophysical Journal International》1968,16(2):169-205

A gross Earth datum is a single measurable number describing some property of the whole Earth, such as mass, moment of interia, or the frequency of oscillation of some identified elastic-gravitational normal mode. We show how to determine whether a given finite set of gross Earth data can be used to specify an Earth structure uniquely except for fine-scale detail; and how to determine the shortest length scale which the given data can resolve at any particular depth. We apply the general theory to the linear problem of finding the depth-variation of a frequency-independent local Q from the observed quality factors Q of a finite number of normal modes. We also apply the theory to the non-linear problem of finding density vs depth from the total mass, moment, and normal-mode frequencies, in case the compressional and shear velocities are known.  相似文献   

Size-dependent distribution, abundance and diurnal rhythmicity patterns in the short-spined sea urchin Anthocidaris crassispina     

S. M. Freeman 《Estuarine, Coastal and Shelf Science》2003,58(4):703-713

Little is known about the ecology and behaviour of the sea urchin Anthocidaris crassispina, particularly in relation to changes in its surrounding environment. In Cape d'Aguilar Marine Reserve, Hong Kong Island, urchins ranged from a high abundance of 16 ind m⁻² on steeply inclined rocky outcrops, which were exposed to strong onshore waves surges, to a complete absence on gravel and sandy substrata. Using a generalized additive model (GAM) the abundance and spatial extent of A. crassispina was predicted within the Bay. Predictions were strongly associated with the surface complexity of the habitat. On steep rocky slopes A. crassispina exhibited a size-dependent gradient where the mean test diameter increased in a down-shore direction as water depth increased. Since the mechanisms for maintaining this size-dependent distribution are unknown, a translocation experiment was conducted on two different size-classes of urchins. Following translocation, both large and small size-classes of A. crassispina were able to re-establish their original size-gradient within 3–5 days. Size-dependent distribution in A. crassispina may indicate resource partitioning, although the influence of hydrodynamic conditions on test size may also mediate this segregation. Anthocidaris crassispina was predominately nocturnal with almost 100% of the population moving between dusk and dawn. Locomotory activity patterns of urchins were strongly correlated with changes in seawater depth and changes in the direction of water-flow during tidal cycles. Anthocidaris crassispina exhibited an endogenously controlled locomotory activity pattern that was synchronized with changes in the tidal cycle, and which remained free-running for 13 h under constant laboratory conditions.  相似文献   

Predictive isotopic biogeochemistry: hydrocarbons from anoxic marine basins   总被引：5，自引：0，他引：5  

Freeman KH  Wakeham SG  Hayes JM 《Organic Geochemistry》1994,21(6-7):629-644

Carbon isotopic compositions were determined for individual hydrocarbons in water column and sediment samples from the Cariaco Trench and Black Sea. In order to identify hydrocarbons derived from phytoplankton, the isotopic compositions expected for biomass of autotrophic organisms living in surface waters of both localities were calculated based on the concentrations of CO2(aq) and the isotopic compositions of dissolved inorganic carbon. These calculated values are compared to measured delta values for particulate organic carbon and for individual hydrocarbon compounds. Specifically, we find that lycopane is probably derived from phytoplankton and that diploptene is derived from the lipids of chemoautotrophs living above the oxic/anoxic boundary. Three acyclic isoprenoids that have been considered markers for methanogens, pentamethyleicosane and two hydrogenated squalenes, have different delta values and apparently do not derive from a common source. Based on the concentration profiles and isotopic compositions, the C31 and C33 n-alkanes and n-alkenes have a similar source, and both may have a planktonic origin. If so, previously assigned terrestrial origins of organic matter in some Black Sea sediments may be erroneous.  相似文献   

Machine Learning Can Assign Geologic Basin to Produced Water Samples Using Major Ion Geochemistry     

Shelton  Jenna L.  Jubb  Aaron M.  Saxe  Samuel W.  Attanasi  Emil D.  Milkov  Alexei V.  Engle  Mark  Freeman  Philip A.  Shaffer  Christopher A.  Blondes  Madalyn S. 《Natural Resources Research》2021,30(6):4147-4163

Natural Resources Research - Understanding the geochemistry of waters produced during petroleum extraction is essential to informing the best treatment and reuse options, which can potentially be...  相似文献   

Global trench migration velocities and slab migration induced upper mantle volume fluxes: Constraints to find an Earth reference frame based on minimizing viscous dissipation     

W.P. Schellart  D.R. Stegman  J. Freeman   《Earth》2008,88(1-2):118-144

Since the advent of plate tectonics different global reference frames have been used to describe the motion of plates and trenches. The difference in plate motion and trench migration between different reference frames can be substantial (up to 4 cm/yr). This study presents an overview of trench migration velocities for all the mature and incipient subduction zones on Earth as calculated in eight different global reference frames. Calculations show that, irrespective of the reference frame: (1) trench retreat always dominates over trench advance, with 62–78% of the 244 trench segments retreating; (2) the mean and median trench velocity are always positive (retreating) and within the range 1.3–1.5 cm/yr and 0.9–1.3 cm/yr, respectively; (3) rapid trench retreat is only observed close to lateral slab edges (< 1500 km); and (4) trench retreat is always slow far from slab edges (> 2000 km). These calculations are predicted by geodynamic models with a varying slab width, in which plate motion, trench motion and mantle flow result from subduction of dense slabs, suggesting that trench motion is indeed primarily driven by slab buoyancy forces and that proximity to a lateral slab edge exerts a dominant control on the trench migration velocity. Despite these four general conclusions, significant differences in velocities between such reference frames remain. It is therefore important to determine which reference frame most likely describes the true absolute velocities to get an understanding of the forces driving plate tectonics and mantle convection. It is here proposed that, based on fluid dynamic considerations and predictions from geodynamic modelling, the best candidate is the one, which optimises the number of trench segments that retreat, minimizes the trench–perpendicular trench migration velocity (v_T) in the centre of wide (> 4000 km) subduction zones, maximizes the number of retreating trench segments located within 2000 km of the closest lateral slab edge, minimizes the average of the absolute of the trench–perpendicular trench migration velocity (|v_T|) for all subduction zones on Earth, and minimizes the global upper mantle toroidal volume flux (_To) that results from trench migration and associated lateral slab migration (i.e. slab rollback or slab roll-forward). Calculations show that these conditions are best met in one particular Indo-Atlantic hotspot reference frame, where 75% of the subduction zones retreat, v_T in the centre of wide subduction zones ranges between − 3.5 and 1.8 cm/yr, 83% of the trench segments located within 2000 km of the closest lateral slab edge retreat, the average of |v_T| is 2.1 cm/yr, and _To = 456 km³/yr (lower limit) and 539 km³/yr (upper limit). Inclusion of all the incipient subduction zones on Earth results in slightly greater fluxes of 465 km³/yr (lower limit) and 569 km³/yr (upper limit). It is also found that this reference frame is close to minimizing the total sub-lithospheric upper mantle volume flux (_K) associated with motion of continental keels located below the major cratons. It is stressed, however, that _K is an order of magnitude smaller than _To, and thus of subordinate importance. In conclusion, the Indo-Atlantic hotspot reference frame appears preferable for calculating plate velocities and plate boundary velocities.  相似文献