133,816 research outputs found

    World War I record of service survey for Whittier B. Gates, signed 26 April 1926.

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    Questionnaire about Whittier Bullard Gates' service in World War I, 1917-1919, signed by Gates on 26 April 1926.Questionnaire originally part of a survey of Norwich University alumni conducted by a “Norwich in the World War” committee consisting of Charles N. Barber (chairman), Carl V. Woodbury, K.R.B. Flint, and Gustaf A. Nelson. Data from these questionnaires may have been used in a chapter of "Vermont in the world war, 1917-1919" by Harold P. Sheldon (1928). Two responses to this questionnaire by Whittier B. Gates exist; the other response is dated 2 September 1922

    World War I record of service survey for Whittier B. Gates, signed 2 September 1922.

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    Questionnaire about Whittier Bullard Gates' service in World War I, 1917-1919, signed by Gates on 2 September 1922.Questionnaire originally part of a survey of Norwich University alumni conducted by a “Norwich in the World War” committee consisting of Charles N. Barber (chairman), Carl V. Woodbury, K.R.B. Flint, and Gustaf A. Nelson. Data from these questionnaires may have been used in a chapter of "Vermont in the world war, 1917-1919" by Harold P. Sheldon (1928). Two responses to this questionnaire by Whittier B. Gates exist; the other response is dated 26 April 1926

    Radiocarbon and stable isotope evidence of dietary change from the Mesolithic to the Middle Ages in the iron gates: New results from Lepenski Vir

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    A previous radiocarbon dating and stable isotope study of directly associated ungulate and human bone samples from Late Mesolithic burials at Schela Cladovei in Romania established that there is a freshwater reservoir effect of approximately 500 yr in the Iron Gates reach of the Danube River valley in southeast Europe. Using the delta(15)N values as an indicator of the percentage of freshwater protein in the human diet, the C-14 data for 24 skeletons from the site of Lepenski Vir were corrected for this reservoir effect. The results of the paired C-14 and stable isotope measurements provide evidence of substantial dietary change over the period from about 9000 BP to about 300 BR The data from the Early Mesolithic to the Chalcolithic are consistent with a 2-component dietary system, where the linear plot of isotopic values reflects mixing between the 2 end-members to differing degrees. Typically, the individuals of Mesolithic age have much heavier delta(15)N signals and slightly heavier delta(13)C, while individuals of Early Neolithic and Chalcolithic age have lighter delta(15)N and delta(13)C values. Contrary to our earlier suggestion, there is no evidence of a substantial population that had a transitional diet midway between those that were characteristic of the Mesolithic and Neolithic. However, several individuals with "Final Mesolithic" C-14 ages show delta(15)N and delta(13)C values that are similar to the Neolithic dietary pattern. Provisionally, these are interpreted either as incomers who originated in early farming communities outside the Iron Gates region or as indigenous individuals representing the earliest Neolithic of the Iron Gates. The results from Roman and Medieval age burials show a deviation from the linear function, suggesting the presence of a new major dietary component containing isotopically heavier carbon. This is interpreted as a consequence of the introduction of millet into the human food chain

    Experimental and Numerical Investigation of Flow under Sluice Gates

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    The flow characteristics upstream and downstream of sluice gates are studied experimentally and numerically using Reynolds averaged Navier-Stokes two-dimensional simulations with a volume of fluid method. Special attention was brought to large opening and submergence, a frequent situation in distribution canals that is little seldom addressed in the literature. Experimental results obtained by ADV measurements provide mean velocity distributions and turbulence characteristics. The flow is shown to be mostly two-dimensional. Velocity fields were simulated using renormalization group k-epsilon and Reynolds stress model turbulence models, leading to an estimation of energy and momentum correction coefficients, head loss, and bed friction. The contraction coefficient is also shown to increase with gate opening at large submergence, which is consistent with the energy-momentum balance. This result can be used to derive accurate discharge equation

    Calculation of Contraction Coefficient under Sluice Gates and Application to Discharge Measurement

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    The contraction coefficient under sluice gates on flat beds is studied for both free flow and submerged conditions based on the principle of momentum conservation, relying on an analytical determination of the pressure force exerted on the upstream face of the gate together with the energy equation. The contraction coefficient varies with the relative gate opening and the relative submergence, especially at large gate openings. The contraction coefficient may be similar in submerged flow and free flow at small openings but not at large openings, as shown by some experimental results. An application to discharge measurement is also presented

    Recovery at Morvin: SERPENT final report

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    Recovery from disturbance is poorly understood in deep water, but the extent of anthropogenic impacts is becoming increasingly well documented. We used Remotely Operated Vehicles (ROV) to visually assess the change in benthic habitat after exploratory hydrocarbon drilling disturbance around the Morvin well located at 380m depth in the Norwegian Sea.An ROV, launched directly from the rig drilling the well in 2006 was used to carry out video transects around the well before drilling and immediately after. On a return to the site three years after disturbance a larger survey was conducted with a ship-launched ROV in 2009. Transects were repeated at the disturbed area and random background transects were taken. Visible drill cuttings were mapped for each survey, and positions and counts of epibenthic invertebrate megafauna were determined, revealing a fauna dominated by Cnidaria (45% of total observations) and Porifera (33%).Immediately after disturbance a visible cuttings pile extended to over 100m from the well and megafaunal density was significantly reduced (0.07 individuals m-2) in comparison to pre-drill data (0.23 ind. m-2). Three years later the visible extent of the cuttings pile had reduced in size, reaching 60m from the well and considerably less in some headings. In comparison to background transects (0.21 ind. m-2), megafaunal density was significantly reduced on the remaining cuttings (0.04m-2), but beyond the visible disturbance there was no significant difference (0.15m-2). The investigation at this site shows a return to background densities of megafaunal organisms over a large extent of the area previously disturbed. However a central area, where the initial cuttings pile was deepest, demonstrated reduced sessile megafaunal density which persisted three years after disturbance. Elevated Barium concentration and reduced sediment grain size suggests persistence of disturbance beyond the remaining visibly impacted area which may result in changes to the infaunal communities undetectable by ROV video survey

    Khamul Gates 2008

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    Key to species of Khamul 1 Tegula golden or brownish..........................................................................................................................2 1' Tegula black (Fig. 65) ............................................................................................ Khamul gothmogi, n. sp. 2 Mandible with lower tooth as an equilateral triangle, curved (Fig. 19).......................................................3 2' Mandible with lower tooth as an isosceles triangle, linear (Fig. 20) ................. Khamul lanceolatus, n. sp. 3 Preorbital carina produced as blunt, triangular process between lateral ocellus and eye (Fig. 54); distinct reniform subocular fovea present (Fig. 54); hind tibia black (Fig. 55).................... Khamul tolkeini, n. sp. 3' Preorbital carina not produced (Figs. 38, 44); subocular fovea absent (Fig. 43); hind tibia yellow to pale brown (Fig. 1) ............................................................................................................. Khamul erwini, n. sp.Published as part of Gates, M. W., 2008, Description of Khamul, gen. n. (Hymenoptera: Chalcidoidea: Eurytomidae), with a hypothesis of its phylogenetic placement, pp. 1-33 in Zootaxa 1898 (1) on page 27, DOI: 10.11646/zootaxa.1898.1.1, http://zenodo.org/record/513397

    Aximopsis hippolytis Gates, n. sp.

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    Aximopsis hippolytis Gates, n. sp. (Figs. 27, 56, 66–67) Etymology hippolyta (Greek, noun, feminine) = the Amazon queen of Greek myth; a feminized adjective attributing the exotic, fantastical Brazilian locality. Diagnosis and identification Aximopsis hippolytis lacks distinct preorbital horns on the vertex, being represented by only a slight angulation of the preorbital carina (Fig. 27, 66). It is unique among the known species in lacking distinct paired spinelike processes anteromedially on the dorsal pronotum, which are present as low alveolate bosses (Fig. 56). Female. Length 2.9–3.3 mm. Prepectus with only a shallow weakly striate concavity in middle, alveolate ventrally. Metacoxa posterolateral carina weak. Gaster effaced reticulation occurring dorsally on some segments; Gt 1 lacking sculpture anteriorly. Antenna dark brown. Legs brown, except extreme apices of femora, bases and apices of tibiae, and tarsomeres pale yellow, apical tarsomere and pretarsus brown. Head. 1.2 X wider than high; 1.1 X width of pronotum; HTE:msp 2.14. Preorbital carina horn at vertex greatly reduced. POL 0.83 X longer than OOL. Width of oral fossa 0.36 X width of head. Scape 4 X longer than broad. Antennal segment ratios 20: 5: 1: 11: 10: 10: 9: 9: 17. Clava 3 X longer than broad. Mesosoma. Dorsal pronotum 2 X wider than long, paired pronotal processes absent. Mesoscutum 2 X broader than long. Scutellum 1.3 X longer than wide at its widest. Dorsellum disc composed sublateral shaped structures with lateral arms descending into space between scutellum and propodeum (Fig. 67). Propodeum (Fig. 67) central depression scarcely recognizable. Postmarginal vein subequal in length to stigma, ratio of mv:pmv 0.83. Metasoma. Petiole 1.9 X longer than wide; dorsal lateral carinae formed by discontinuous anterior and posterior portions; ventral surface with weak sublateral carinae. Male. Unknown Va r i a t i o n One female (USNM ENT 00480026) has slightly more distinct paired, differential sculpturing on the dorsal pronotum that correlate with the spinelike pronotal processes of other species. Type material (2 Ψ ) Holotype Ψ (USNM ENTO 00480028) (USNM); Brazil; Rio Grande do Sul; Ilha do Pavao; ii. 1962; G.B. Vogt; Vogt coll. # 62­269; reared from Taphrocerus (Coleoptera: Buprestidae) ex. Cyperus (giant flatsedge). Paratype 1 Ψ (USNM ENTO 00480026) (USNM) same locality as holotype; ii. 22 ­23.1962; Vogt coll. # 62­229; reared from Taphrocerus (Coleoptera: Buprestidae) ex. Scirpus (bullrush).Published as part of Gates, M. W., Metz, M. A. & Schauff, M. E., 2006, The circumscription of the generic concept of Aximopsis Ashmead (Hymenoptera: Chalcidoidea: Eurytomidae) with the description of seven new species, pp. 9-54 in Zootaxa 1273 on pages 42-43, DOI: 10.5281/zenodo.17328

    Aximopsis anubis Gates, n. sp.

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    Aximopsis anubis Gates, n. sp. (Figs. 59–62) Etymology anubis (Latin, noun, feminine) = a noun in apposition recalling the dark god of the chase or hunt of Egyptian myth. Diagnosis and identification Aximopsis anubis is the only known species occurring in the Caribbean islands. This species possesses the diagnostic features of the genus and is most similar to A. vogti in having prominent vertex horns; dense, dirty blonde, vertex setae; a shorter lower face; setae of the lower face filiform, not lanceolate; prominent pronotal processes; and a deeply punctate median channel of the propodeum. It differs from A. vogti by the female having a petiole that is 3 X longer than it is wide while the length and width of the female petiole in A. vogti are nearly subequal. Female. Length 2.9 –3.0 mm. Prepectus with a shallow finely alveolate concavity (Fig. 59). Metacoxa posterolateral carina weak (Fig. 60). Gaster with effaced reticulation occurring dorsally on posterior segments; Gt 1 coarsely alveolate anteriorly just above petiolar insertion. Antenna dark brown, base of scape yellow. Legs brown, except extreme bases and apices of femora, bases and apices of tibiae, and tarsomeres pale yellow, pretarsus brown. Head. 1.4 X wider than high; 1.4 X wider than pronotum; HTE:msp 2.65. POL 2.0X longer than OOL. Width of oral fossa 0.37 X width of head. Scape 5 X longer than broad. Antennal segment ratios 30: 6: 1: 12: 11: 11: 11: 11: 23. Clava 3 X longer than broad. Mesosoma. Dorsal pronotum 2.8 X wider than long, with paired pronotal processes. Mesoscutum 3 X broader than long. Scutellum length subequal to its width at its widest; broadly convex dorsally. Dorsellum disc composed of a central ­shaped structure with lateral arms broadening laterally into paddle­shapes (Fig. 62). Propodeum deeply punctate in central depression with interstices alveolate. Postmarginal vein subequal in length to stigma, ratio of mv:pmv 2.4. Metasoma. Petiole 3.0X longer than wide; dorsal lateral carinae weak; median carina discontinuous subapically; lateral surface with strong carina; ventral surface with medial and lateral carinae. Male. Unknown. Va r i a t i o n The type series exhibits very little variation. Type material (3 Ψ ) Holotype Ψ (USNM ENTO 00481367) (USNM); West Indies: Tobago: Goldsborough: Ex. neglected citrus orchard bordering on primary forest, 5–12.v. 1994, M.J. Sommeijer, Malaise trap. Paratypes 2 Ψ (USNM ENTO 0 0 481327, 0 0 481328, 004800041) (USNM), same data as holotype.Published as part of Gates, M. W., Metz, M. A. & Schauff, M. E., 2006, The circumscription of the generic concept of Aximopsis Ashmead (Hymenoptera: Chalcidoidea: Eurytomidae) with the description of seven new species, pp. 9-54 in Zootaxa 1273 on pages 38-40, DOI: 10.5281/zenodo.17328

    The Gates of Europe

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    The Gates of Europe is a proposal for the city of Brussels to balance out the differences in the city and to improve the representation of the presence of Europe in the city. One of the buildings, the Gate of Culture, is worked out into detail. It is a Centre for Performing Arts and functions on a regional and on a local scale. It contains a large music hall (4000 standing places), a theatre and dance hall (1000 seats) and a small stage (300 seats). Further, there are rehearsal studios for music, dance and theatre. The first levels are related to the metro- and the Euroline station. This last one is a raised monorail, running through the Gates of Europe.Public Realm: studio BrusselsPublic BuildingArchitectur
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