Book Review     

Scott E. Drummond Jr. 《Marine Geodesy》2013,36(2):143-144

Electronic Surveying and Navigation by Simon H. Laurila (New York: John Wiley &; Sons, 1976), 545 pages, hardcover, $25.00.  相似文献   

Submarine Sand Resources,Southeastern Virginia-Contributions from Year 9 and Year 10 of Virginia's Continental Margins Program     

Carl H. Hobbs  C. Scott Hardaway  C. R. Berquist 《Marine Georesources & Geotechnology》2013,31(2-3):155-163

Virginia's year 9 and year 10 funds from the Continental Shelf Program were used to supplement other work funded by the Minerals Management Service in an ongoing Cooperative Agreement focused on the area offshore of southeastern Virginia. Year 9 and year 10 funds facilitated interpretation of subbottom profiles and the analysis of sediment samples from cores and grabs. On Virginia's sediment-starved continental shelf, deposits of material potentially suitable for use as beach nourishment or, perhaps, as construction aggregate occur in three stratigraphic settings, each with specific characteristics of morphology, grain-size gradients, likelihood of discovery, and physical ease of exploitation. All must be verified with a careful program of coring. Modern shoals generally are easier to identify, prove, and access than either filled channels or lenticular facies. Shoals usually are identifiable on nautical charts and characteristically have a definite lower boundarythat can be seen in subbottom profiles. In most cases, the base of the shoal coincides with the level of the surrounding sea floor. Filled channels are readily identifiable on subbottom profiles but may have a narrow, sinuous form and steep lateral gradients in sediment properties. Buried lenticular facies of good-quality sand usually are found only fortuitously. As the lateral and often vertical gradients in geotechnical properties usually are low, the lenticular facies can be mined with a lesser concern for the consequences of violating the deposit's limits than with the other two types of deposit. There are three types of filled paleochannels in the study area. (1) Relatively near-surface, generally small, roughly shore normal channels most likely mark the migration of tidal inlets across the shelf during the most recent transgression. (2) Small, relatively wide and relatively shallow generally shore parallel channels may be filled back-barrier or lagoonal channels. (3) Larger channels trending across the shelf probably result from riverine flow. The complexity of the seismostratigraphy of the Quaternary deposits on south eastern Virginia's inner continental shelf is a result of series of high-frequency (fifth-order, 10-20,000 y), low-amplitude (20-30 m) variations in sea level that occurred during the last highstand, roughly 80,000 to 130,000 BP. The evidence of the small oscillations in sea level is best seen in the regions that were between the shoreline and wave base, today's inner shelf; however, the very low rates of deposition on the shelf make it difficult to correlate specific reflectors or beds or, at times, to distinguish between fifth-and fourth-order changes. Results for the continuing studies already have been used in the determination to mine several hundred thousand cubic meters of sand from Sandbridge Shoal for use on a Navy-owned facility and in consideration of mining greater quantities of sand from Sandbridge and other shoals for use in local beach nourishment and hurricane protection efforts.  相似文献   

Estimating the Random Error in Eddy-Covariance Based Fluxes and Other Turbulence Statistics: The Filtering Method   总被引：1，自引：1，他引：0  

Scott T. Salesky  Marcelo Chamecki  Nelson L. Dias 《Boundary-Layer Meteorology》2012,144(1):113-135

A spatially local decomposition of turbulent fluxes based on properties of spatial filters is used to develop a new method of estimating random error in turbulent moments of any order. The proposed error estimation method does not require an estimate of the integral time scale, which can be highly sensitive to the method used to calculate it. The error estimation method is validated using synthetic flux data with a known ensemble mean and intercompared with existing methods using data from the Advection Horizontal Array Turbulence Study (AHATS). Typical errors for a 27.3-min block of data collected at a height of 8 m are found to be approximately 10% for the heat flux and 7–15% for variances. The error in the momentum flux increases rapidly with increasing atmospheric instability, reaching values of 40% or greater for unstable conditions. A new method based on filtering is also proposed to estimate integral time scales of turbulent quantities.  相似文献   

Estimated changes in wind speed and wind power density over the western High Plains, 1971–2000     

J. Scott Greene  Matthew Chatelain  Mark Morrissey  Steve Stadler 《Theoretical and Applied Climatology》2012,109(3-4):507-518

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The paleoenvironmental distribution of Phanerozoic wrinkle structures   总被引：4，自引：0，他引：4  

Scott A. Mata  David J. Bottjer 《Earth》2009,96(3):181-178

Wrinkle structures are microbially induced sedimentary structures that are known to have formed in ancient marine siliciclastic environments. This study reviews the sedimentary context and paleoenvironmental distribution of these sedimentary structures throughout three distinct intervals of the Phanerozoic: the Cambrian, the post-Cambrian Paleozoic, and the Lower Triassic. During these times, wrinkle structures are found primarily within two sedimentary environments, storm-dominated subtidal environments and the intertidal zone. Subtidal occurrences of wrinkle structures during the post-Ordovician Phanerozoic only appear to occur during intervals of environmental stress, while earlier examples from the Cambrian and lowermost Ordovician likely formed prior to significant increases in extent and depth of bioturbation that hallmark most of the Phanerozoic. Intertidal examples occur regardless of severe environmental stress, and may have formed under low levels of bioturbation due to inherent vagaries of a marginal marine setting. These environmental preferences appear to be conservative throughout the Phanerozoic, and may very well extend throughout Earth's history.  相似文献   

Granoblastic olivine aggregates as precursors of Type I chondrules: An experimental test     

Scott A. Whattam  Roger H. Hewins 《Geochimica et cosmochimica acta》2009,73(18):5460-5482

Chondrule formation models involving precursors of granoblastic olivine aggregates (GOA) of either planetesimal or nebular origin have recently been proposed. We have therefore conducted chondrule simulation experiments using mixtures of 100 h-thermally annealed GOA and An + En to test the viability of GOA as predecessors of porphyritic olivine (PO) chondrules. Isothermal runs of less than 5 min at 1350–1550 °C result in GOA disaggregation and Fe–Mg exchange; runs of 0.5–4 h show textures superficially similar to granular and PO chondrules, but with reversely zoned olivine. Charges isothermally heated at 1550 °C for 1 and 4 h before being cooled at 10 and 100 °C/h undergo olivine crystallization and yield classical PO textures. Although most evidence of origin from GOA is erased, the cores of normally zoned euhedral crystals are relict. As ‘phenocrysts’ in Type I chondrules can be relict such chondrules could have experienced similar peak temperatures to those of Type II chondrules.Chondrules containing GOA with olivine triple junctions resemble experimental charges heated for minutes at temperatures between 1350 and 1450 °C and Type I chondrules with subhedral to anhedral olivine plus GOA relicts resemble charges heated at the same temperatures but for longer duration. Type I chondrules with a mass of granular olivine or irregular, anhedral olivine grains in the center, and much glass nearer the margin, on the other hand, require limited heating at high temperature (1550 °C) while Type I chondrules with euhedral olivines, resemble charges heated at 1550 °C for 4 h. The majority of Type I chondrules in CV chondrites display evidence of derivation from GOA. Many finer-grained chondrules in CR and UOC on the other hand, could not have been derived from such coarse-grained precursors, but could have formed from fine-grained dustballs as stipulated in the standard paradigm. Thus, both GOA and dustballs represent viable chondrule precursors of coarser and finer-grained Type I PO chondrules, respectively.  相似文献   

Numerical modeling of the development of a preferentially leached layer on feldspar surfaces     

Changbing Yang  Javier Samper  Chen Zhu  Scott B. Jones 《Environmental Geology》2009,57(7):1639-1647

Compositional depth profiles in the leached layer of feldspar surfaces are usually interpreted by using analytical solutions which introduce oversimplifying assumptions. Here we present a general multicomponent interdiffusion numerical model for simulating cation release from a preferentially leached layer on feldspar surfaces in acid solutions. The numerical model takes into account interdiffusion, dissolution of the solid phase (represented by a moving boundary problem), and adsorption in the leached layer. Effective diffusion coefficients of ions vary with concentration along the leached layer. Governing equations of ions diffusion in the leached layer are solved numerically with a finite element method implemented in a multicomponent reactive transport code, CORE^3D, previously verified against analytical solutions of compositional depth profiles. The numerical model is tested with published X-ray photoelectron spectroscopy (XPS) data on early development of compositional profiles of labradorite leached in pH 2 HCl solutions. Model parameters are estimated by fitting depth profiles of Ca and Al measured at 12, 26, 48, 72, and 143 h. The best fit is achieved with tracer diffusion coefficients of 4 × 10⁻¹⁸, 8 × 10⁻¹⁷, 3.4 × 10⁻¹⁷, and 7 × 10⁻¹⁸ cm²/s for H, Na, Ca, and Al, respectively, which fall within the range of values reported in the literature. Our estimate of the retreat velocity corresponding to the dissolution rate is 3 × 10⁻¹³ cm/s. Results of sensitivity runs show that computed compositional profiles are sensitive to most model parameters.  相似文献   

Square Kilometre Array: The radio telescope of the XXI century     

K. Grainge  B. Alachkar  Shaun Amy  D. Barbosa  M. Bommineni  P. Boven  R. Braddock  J. Davis  P. Diwakar  V. Francis  R. Gabrielczyk  R. Gamatham  S. Garrington  T. Gibbon  D. Gozzard  S. Gregory  Y. Guo  Y. Gupta  J. Hammond  D. Hindley  U. Horn  R. Hughes-Jones  M. Hussey  S. Lloyd  S. Mammen  S. Miteff  V. Mohile  J. Muller  S. Natarajan  J. Nicholls  R. Oberland  M. Pearson  T. Rayner  S. Schediwy  R. Schilizzi  S. Sharma  S. Stobie  M. Tearle  B. Wang  B. Wallace  L. Wang  R. Warange  R. Whitaker  A. Wilkinson  N. Wingfield 《Astronomy Reports》2017,61(4):288-296

The Square Kilometre Array (SKA) will be the world’s largest and most sensitive radio telescope. It will address fundamental unanswered questions about our Universe including how the first stars and galaxies formed after the Big Bang, how dark energy is accelerating the expansion of theUniverse, the role of magnetism in the cosmos, the nature of gravity, and the search for life beyond Earth. This project envisages the construction of 133 15-m antennas in South Africa and 131072 log-periodic antennas in Australia, together with the associated infrastructure in the two desert sites. In addition, the SKA is an exemplar Big Data project, with data rates of over 10 Tbps being transported from the telescope to HPC/HTC facilities.  相似文献   

Future research needs involving pathogens in groundwater     

Scott A. Bradford  Ronald W. Harvey 《Hydrogeology Journal》2017,25(4):931-938

Contamination of groundwater by enteric pathogens has commonly been associated with disease outbreaks. Proper management and treatment of pathogen sources are important prerequisites for preventing groundwater contamination. However, non-point sources of pathogen contamination are frequently difficult to identify, and existing approaches for pathogen detection are costly and only provide semi-quantitative information. Microbial indicators that are readily quantified often do not correlate with the presence of pathogens. Pathogens of emerging concern and increasing detections of antibiotic resistance among bacterial pathogens in groundwater are topics of growing concern. Adequate removal of pathogens during soil passage is therefore critical for safe groundwater extraction. Processes that enhance pathogen transport (e.g., high velocity zones and preferential flow) and diminish pathogen removal (e.g., reversible retention and enhanced survival) are of special concern because they increase the risk of groundwater contamination, but are still incompletely understood. Improved theory and modeling tools are needed to analyze experimental data, test hypotheses, understand coupled processes and controlling mechanisms, predict spatial and/or temporal variability in model parameters and uncertainty in pathogen concentrations, assess risk, and develop mitigation and best management approaches to protect groundwater.  相似文献   

Sun-induced variations in time in the global positioning system     

Scott R. Chubb 《Astrophysics and Space Science》1994,213(1):63-73

Sun-induced effects on the measurement and transfer of time information reported by orbiting satellites are reexamined. The problem of transforming the frequency of coherent radio signals to the Geocentric Inertial Coordinate frame (as required during the transfer of time information) involves an implicit, dependence on earth-sun-clock orientation that has been omitted, except in Very-Long-Baseline Interferometry (VLBI) studies. This known VLBI effect leads to an important second order Doppler effect. The effect explains systematic deviations between the time reported by satellites in the Global Positioning System (GPS) relative to Universal Time (UT) and can be used to improve existing bounds for the validity of the equivalence principle.  相似文献