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Nature of light rain during presence and absence of bright band 总被引：1，自引：0，他引：1
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B. S. MAZUMDER S. K. DAS S. N. DAS 《国际泥沙研究》2006,21(4):249-260
1 INTRODUCTION Movement of navigation traffic in restricted waterway can generate various hydrodynamic phenomena including return flow (RF), surge wave, drawdown and sediment re-suspension which are absent in open water conditions (Schofield and Martin, 1… 相似文献
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Durbar RAY Dalayya KOTA Pranab DAS L. Surya PRAKASH V.D. KHEDEKAR Anil L. PAROPKARI Abhay V. MUDHOLKAR 《《地质学报》英文版》2014,88(1):213-225
An extinct hydrothermal barite-silica chimney from the Franklin Seamount of the Woodlark Basin, in the southwestern Pacific Ocean, was investigated for mineral distribution and geochemical composition. Six layers on either side of the orifice of a chimney show significant disparity in color, mineral assemblage and major element composition. Electron microscope(SEM) images reveal that the peripheral wall of the chimney is composed of colloform silica, suggesting that incipient precipitation of silica-saturated hydrothermal fluid initiated the development of the chimney wall. Intermediate layers, between the exterior wall and the inner fluid-orifice, dominate with barite and sulfides. Low Sr-to-Ba ratios(SrO/BaO = 0.015–0.017) indicate restricted fluid-seawater mixing, which causes relatively high-temperature formation of the intermediate layers. Whereas the innermost layer bordering the chimney orifice is characterized by more silica and a higher Sr-to-Ba ratio(SrO/BaO = 0.023), could have formed due to a paragenetic shift from a high-temperature active phase to a cooler waning stage of formation. A paragenetic shift is also probably responsible for the change in mineral formation mechanism that resulted in the textural variation of barite and colloform silica developed during different growth phases of this barite-silica chimney. 相似文献
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V S PRASAD SAJI MOHANDAS SURYA KANTI DUTTA M DAS GUPTA G R IYENGAR E N RAJAGOPAL SWATI BASU 《Journal of Earth System Science》2014,123(2):247-258
Medium range weather forecasts are being generated in real time using Global Data Assimilation Forecasting System (GDAFS) at NCMRWF since 1994. The system has been continuously upgraded in terms of data usage, assimilation and forecasting system. Recently this system was upgraded to a horizontal resolution of T574 (about 22 km) with 64 levels in vertical. The assimilation scheme of this upgraded system is based on the latest Grid Statistical Interpolation (GSI) scheme and it has the provision to use most of available meteorological and oceanographic satellite datasets besides conventional meteorological observations. The new system has an improved procedure for relocating tropical cyclone to its observed position with the correct intensity. All these modifications have resulted in improvement of skill of medium range forecasts by about 1 day. 相似文献
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Characterizing spatial and seasonal variability of carbon dioxide and water vapour fluxes above a tropical mixed mangrove forest canopy, India 总被引：1，自引：0，他引：1
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The Central Indian Ocean Basin (CIOB) basalts are plagioclase-rich, while olivine and pyroxene are very few. The analyses of 41 samples reveal high FeOT (~10–18 wt%) and TiO2 (~1.4–2.7 wt%) indicating a ferrobasaltic composition. The basalts have high incompatible elements (Zr 63–228 ppm; Nb ~1–5 ppm; Ba ~15–78 ppm; La ~3–16 ppm), a similar U/Pb (0.02–0.4) ratio as the normal mid-oceanic basalt (0.16±0.07) but the Ba/Nb (12.5–53) ratio is much larger than that of the normal mid-oceanic ridge basalt (~5.7) and Primitive Mantle (9.56). Interestingly almost all of the basalts have a significant negative Eu anomaly (Eu/Eu*=0.78–1.00) that may have been a result of the removal of feldspar and pyroxene during crystal fractionation. These compositional variations suggest that the basalts were derived through fractional crystallization together with low partial melting of a shallow seated magma. 相似文献
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The delayed fission neutron counting method has been used for the analysis of thirty-three international geochemical reference samples for their uranium contents in the range of 0.2 to 1500 ppm. These include three from the Canada Centre for Mineral and Energy Technology, three from Atomic Energy Commission, USA, New Brunswick Laboratory, two from Bhabha Atomic Research Centre, India, fourteen from Centre de Recherches Pétrographiques et Géochimiques and eleven from US Geological Survey. The experimental set up has a detection limit of 0.08 μg and a determination limit of 0.15 μg U. At the lower limit the precision of determination is about 20 percent while at concentrations higher than 1 ppm it is better than 10 percent. 相似文献