REVISION OF ORDNANCE SURVEY 1:2500 SCALE MAPS     

J. P. Leonard 《The Photogrammetric Record》1982,10(60):681-685

With the completion of its programme to produce a national series of 1:2500 scale maps of rural areas, the Ordnance Survey is now faced with the major task of maintaining it up to date and making the revision information available to map users. The organisation and techniques for this are discussed, as are a number of innovations which are being considered.

Résumé

Avec l'achèvement du programme de réalisation de la série cartographique nationale à l'échelle du 1:2500 des régions rurales, l'Ordnance Survey doit maintenant faire face au maintien à jour de cette série et à la mise à disposition des usagers des données de révision, ce qui va constituer sa tâche principale. Une discussion sur l'organisation et les techniques correspondantes est fournie, prenant en compte l'examen de nombreuses innovations.

Zusammenfassung

Nach Fertigstellung der Kane 1:2500 von ländlichen Gebieten besteht für den Ordnance Survey jetzt die Aufgabe, diese Karte laufend zu halten und die Ergänzungen den Kartennutzern bereitzusteller. Diskussion der Organisation und Verfahren dafür sowie einiger Neuerungen, die in Erwägung gezogen werden.  相似文献   

Energy cost-accounting of Louisiana fishery production     

Leonard M. Bahr  John W. Day  James H. Stone 《Estuaries and Coasts》1982,5(3):209-215

A quantitative relationship between gross primary production and secondary production of aquatic upper level consumers was derived for the inshore portion of the Louisiana coastal zone. We estimate that 1,700 units of gross primary production are required to produce one unit of upper level consumers. Lower and mid-level consumers are estimated to require lesser amounts, 300 and 600 units, respectively. Harvested fishery groups in the inshore ecosystem represent a total average of about 23,000 metric tons (dry wt) or about 1.2×10¹¹ Kcal (5.0×10¹¹ KJ) annually. This harvest “costs” the system about 7×10¹³ Kcal (3.3×10¹⁴ KJ) of gross primary production, or an equivalent of 4×10¹⁴ Kcal (1.7×10¹⁵KJ) of fossil fuel.  相似文献   

The sea floor morphology seaward of Terre Adélie (Antarctica)     

Prof. Jean-René Vanney  Dr. G. Leonard Johnson 《Ocean Dynamics》1979,32(2):77-87

  相似文献   

Geological environment of a methane-rich Recent sedimentary basin in the Gulf of St. Lawrence     

M.A. Rashid  G. Vilks  J.D. Leonard 《Chemical Geology》1975,15(2):83-96

Two sediment cores collected in Chaleur Trough, Gulf of St. Lawrence are compared in terms of organic geochemistry, sediment texture and foraminifera. One of the cores was collected from a depression and contained methane in the range of 5,970–14,230 ppm, in comparison to 42–106 ppm in the core of open environment. The sediments of the methanerich core are finer, higher in organic carbon, extractable organic matter, plant pigments and contained more diverse foraminiferal assemblages. The results of these geological investigations tend to suggest a relatively fast rate of sedimentation in the depression. This results in the preservation of organic compounds and development of anaerobic subsurface conditions, consequently giving rise to high concentrations of methane through fermentative processes. No other gaseous hydrocarbons were detected hence the possibility of seepage of petroleum gases appears to be remote.  相似文献   

The “Delft” system for mineral identification, 1. Opaque minerals: R.A. Kühnel,J.J. Prins and H.J. Roorda. Delft University Press,Delft, 1980 [1982], ix + 204 pp., Dfl. 182.00 (for The Netherlands)/Dfl. 175.00 (for all other countries) (hardcover)     

B.F. Leonard 《International Journal of Mineral Processing》1983,11(3):235-237

  相似文献   

A finite-volume ELLAM for three-dimensional solute-transport modeling     

Russell TF  Heberton CI  Konikow LF  Hornberger GZ 《Ground water》2003,41(2):258-272

A three-dimensional finite-volume ELLAM method has been developed, tested, and successfully implemented as part of the U.S. Geological Survey (USGS) MODFLOW-2000 ground water modeling package. It is included as a solver option for the Ground Water Transport process. The FVELLAM uses space-time finite volumes oriented along the streamlines of the flow field to solve an integral form of the solute-transport equation, thus combining local and global mass conservation with the advantages of Eulerian-Lagrangian characteristic methods. The USGS FVELLAM code simulates solute transport in flowing ground water for a single dissolved solute constituent and represents the processes of advective transport, hydrodynamic dispersion, mixing from fluid sources, retardation, and decay. Implicit time discretization of the dispersive and source/sink terms is combined with a Lagrangian treatment of advection, in which forward tracking moves mass to the new time level, distributing mass among destination cells using approximate indicator functions. This allows the use of large transport time increments (large Courant numbers) with accurate results, even for advection-dominated systems (large Peclet numbers). Four test cases, including comparisons with analytical solutions and benchmarking against other numerical codes, are presented that indicate that the FVELLAM can usually yield excellent results, even if relatively few transport time steps are used, although the quality of the results is problem-dependent.  相似文献   

Residence of silver in mineral deposits of the Thunder Mountain caldera complex,Central Idaho,U.S.A.     

B. F. Leonard  R. P. Christian 《Mineralogy and Petrology》1987,36(3-4):151-168

Summary Silver is an accessory element in gold, antimony, and tungsten deposits of the caldera complex. Most of the deposits are economically of low grade and genetically of xenothermal or epithermal character. Their gold- and silver-bearing minerals are usually disseminated, fine grained, and difficult to study. Sparsely disseminated pyrite and arsenoprite are common associates.Identified silver minerals are: native silver and electrum; the sulfides acanthite, argentite (the latter always inverted to acanthite), and members of the Silberkies group; the sulfosalts matildite, miargyrite, pyrargyrite, argentian tetrahedrite, and unnamed Ag-Sb-S and Ag-Fe-Sb-S minerals; the telluride hessite and the selenide naumannite; halides of the cerargyrite group; and the antimonate stetefeldtite. Suspected silver minerals include the sulfide uytenbogaardtite and the sulfosalts andorite, diaphorite, and polybasite. Electrum, acanthite, and argentian tetrahedrite are common, though nowhere abundant. The other silver minerals are rare.Silver is present as a minor element in the structure of some varieties of other minerals. These include arsenopyrite, chalcopyrite, chalcostibite, covelline, digenite, galena, sphalerite, and stibnite. The search for adventitious Ag in most of these minerals has been cursory. The results merely indicate that elemental silver is not confined to discrete silver minerals and is, therefore, an additional complication for the recovery of silver-bearing material from some deposits.Silver occurs cryptically in some plants of the region. At Red Mountain, for example, the ashed sapwood of Douglas-fir (Pseudotsuga menziesii) contains 2 to 300 ppm Ag. Silver in the ashed wood is roughly 100 times as abundant as it is in soil. The phenomenon, useful in biogeochemical exploration, deserves the attention of mineralogists.

---

Das Vorkommen von Silber in den Erzlagerstätten des Thunder-Mountain-Caldera-Komplexes, Idaho, U.S.A.

Zusammenfassung Silber ist in den Gold-, Antimon- und Wolframlagerstätten des Caldera-Komplexes ein akzessorisches Element. Die Lagerstätten sind wirtschaftlich geringhaltig und genetisch als xeno- oder epithermal zu deuten. Gold- und silberführende Minerale sind meist feinkörnig und treten akzessorisch auf. Im einzelnen wurden folgende Minerale beobachtet: Gediegen Silber und Elektrum; die Sulfide Akanthit und Argentit (immer zu Akanthit umgewandelt) sowie Silberkiese; die Sulfosalze Matildit, Miargyrit, Pyrargyrit, silberhaltiger Tetraedrit und nicht näher identifizierte Ag-Sb-S- und Ag-FeSb-S-Verbindungen; das Tellurid Hessit und das Selenid Naumannit; Halogenide der Kerargyritgruppe; und das Antimonat Stetefeldit. Mögliche weitere Ag-Minerale schließen das Sulfid Uytenbogaardtit und die Sulfosalze Andorit, Diaphorit und Polybasit ein. Von diesen Mineralen kommen Elektrum, Akanthit und silberhaltiger Tetraedrit am häufigsten vor, während alle anderen selten sind. Die gewöhnlichen Nebengemengteile sind Pyrit und Arsenkies.Darüber hinaus wird vermutet, daß Spuren von Silber im Kristallgitter anderer Minerale eingebaut vorliegen; insbesondere in den Gittern von Arsenkies, Kupferkies, Chalcostibit, Covellin, Digenit, Bleiglanz, Zinkblende und Antimonit. Hierzu liegen noch keine umfassenden Untersuchungen vor, jedoch kann vermutet werden, daß Silber nicht ausschließlich auf Ag-Minerale sensu stricto beschränkt ist.Einige Pflanzen des Lagerstättenbezirkes enthalten beachtliche Mengen an Silber, so zum Beispiel die Asche der Douglas-FichtePseudotsuga menziesii. Der Silbergehalt beträgt 2 bis 300 g/t und ist damit gegenüber dem Boden etwa 100fach erhöht. Dieses Phänomen ist von Nutzen in der biogeochemischen Exploration und verdient das Interesse der Mineralogen.

---

---

With 10 Figures

---

Contribution to the Ore Mineralogy Symposium (IMA/COM) at the 14th General Meeting of the International Mineralogical Association, at Stanford, California, in July, 1986.  相似文献   

On experiments using an auto-regressive moving-average model for predicting the monthly 50–100 kPa thickness anomalies     

Leonard Steinberg 《Pure and Applied Geophysics》1985,123(5):757-775

A series of 75 auto-regressive integrated moving-average (ARIMA) forecasts of monthly mean 100–50 kPa thickness anomalies with lead time of one month are produced for 455 grid points over the northern hemisphere. The results are indistinguishable from persistence forecasts when the scores are averaged over the domain. A more detailed view indicates some differences which may merit closer investigation. Differences in the behaviour of positive and negative anomaly forecasts are also described.Some aspects of the methodology are discussed briefly in the introductory sections. The model used in the experiment is described in detail. A shortcoming of the method is that it does not lend itself to seasonal stratification.  相似文献   

Phytoplankton dynamics within Gulf Stream intrusions on the southeastern United States continental shelf during summer 1981     

James A. Yoder  Larry P. Atkinson  S. Stephen Bishop  Jackson O. Blanton  Thomas N. Lee  Leonard J. Pietrafesa 《Continental Shelf Research》1985,4(6):611-635

During July and August 1981 subsurface intrusion of upwelled nutrient-rich Gulf Stream water was the dominant process affecting temporal and spatial changes in phytoplankton biomass and productivity of the southeastern United States continental shelf between 29 and 32°N latitude. Intruded waters in the study area covered as much as 10¹ km including virtually all of the middle and outer shelf and approximately 50% of the inner shelf area.Within 2 weeks following a large intrusion event in late July, middle shelf primary production and Chl a reached 3 to 4 gC m⁻ d⁻¹ and 75 mg m⁻, respectively. At the peak of the bloom 80% of the water column primary production occurred below the surface mixed-layer, and new primary production (i.e., NO₃-supported) exceeded 90% of the total. Chl a-normalized photosynthetic rates were very high as evidenced by high mean assimilation number (15.5 mg C mg Chl a⁻¹ h⁻¹), high mean α (14 mg C mg Chl a⁻¹ Ein⁻¹ m), and no photoinhibition. As a result of the high photosynthetic rates, mean light-utilization index (Ψ) was 2 to 3 times higher than reported for temperature sub-arctic and arctic waters.The results imply a seasonal (June to August) middle shelf production of 150 g C m⁻¹, about 15% higher than previous estimates of annual production on the middle shelf. Intrusions of the scale we observed in 1981 may not occur every summer. However, when such events do occur, they are by far the most important processes controlling summer phytoplankton dynamics of the middle and outer shelf and of the inner shelf in the southern half of the study area.  相似文献   

The joint effect of rank and grain size on the flotation of Australian bituminous coals     

Heriberto Bustamante  Leonard J. Warren 《International Journal of Mineral Processing》1984,13(1):13-28

Laboratory batch flotation tests were carried out to determine the effect of grain size on the recovery of four Australian bituminous coals of high and low rank. The flotation concentrates, taken over successive time intervals, and the tailings, were sized and the recovery-size curves plotted. A method was developed for determining the proportions of liberated and composite grains in the various flotation products. Flotation tests were carried out in the presence of methylisobutylcarbinol (MIBC) and MIBC + kerosene. The shapes of the recovery-size curves depended on the rank of the coal and whether or not kerosene was present. The variation of the recovery with size was explained in terms of the joint effect of rank and size on the floatability of composite grains.  相似文献