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791.
Eric C. J. Oliver Jinyu Sheng Keith R. Thompson Jorge R. Urrego Blanco 《Natural Hazards》2012,64(2):1425-1446
This study presents a methodology for estimating extreme current speeds from numerical model results using extremal analysis techniques. This method is used to estimate the extreme near-surface and near-bottom current speeds of the northwest Atlantic Ocean with 50-year return periods from 17?years of model output. The non-tidal currents produced by a three-dimensional ocean circulation model for the 1988?C2004 period were first used to estimate and map the 17-year return period extreme current speeds at the surface and near the bottom. Extremal analysis techniques (i.e., fitting the annual maxima to the Type I probability distribution) are used to estimate and map the 50-year extreme current speeds. Tidal currents are dominant in some parts of the northwest Atlantic, and a Monte Carlo-based methodology is developed to take into account the fact that large non-tidal extrema may occur at different tidal phases. The inclusion of tidal currents in this way modifies the estimated 50-year extreme current speeds, and this is illustrated along several representative transects and depth profiles. Seasonal variations are examined by calculating the extreme current speeds for fall-winter and spring?Csummer. Finally, the distribution of extreme currents is interpreted taking into account (1) variability about the time-mean current speeds, (2) wind-driven Ekman currents, and (3) flow along isobaths. 相似文献
792.
Miguel Tupinambá Monica Heilbron Claudio Valeriano Rubem Porto Júnior Fátima Blanco de Dios Nuno Machado Luiz Guilherme do Eirado Silva Júlio Cesar Horta de Almeida 《Gondwana Research》2012,21(2-3):422-438
The ca. 790–600 Ma Rio Negro Complex (RNC) of the Ribeira belt (Brazil) consists of a plutonic portion of a magmatic arc built by the E-vergent subduction of the ESE border of the São Francisco paleoplate during the amalgamation of Western Gondwana.The plutonic series comprises low- to medium-K granitoids (ca. 790–620 Ma) and high-K granitoids and shoshonite rocks (ca. 610–605). The age span of 185 m.y. is suggestive of a long history of arc-related magmatism, continuously or not in time. The Nd isotopic signatures of the RNC consist of εNd(t) ratios from ? 3 to + 5 for the medium-K series shoshonite series and from ? 14 to ? 3 for the younger high-K group. This time-dependent trend of Nd isotopes is indicative of progressive maturity of the arc over time. The same evolution is indicated by Sr data, as the medium-K rocks have 87Sr/86Sr initial ratios < 0.705 while the high-K rocks yield values between 0.705 and 0.710. The predominance of intermediate rocks over mafic ones suggests an initial intra-oceanic to transitional stage, possibly developed in a distal portion of a passive margin, such as the Japanese arc, evolving to a more developed, differentiated felsic rock associations.The role of transform fault zones, such as the Luanda shear zone, is emphasized in order to explain the consumption of a wide oceanic plate in the inner portion of Western Gondwana. 相似文献
793.
Sedimentary geochemical record of historical anthropogenic activities affecting Guanabara Bay (Brazil) environmental quality 总被引:3,自引:2,他引:1
Fábio F. Monteiro Renato C. Cordeiro Ricardo E. Santelli Wilson Machado Heitor Evangelista Leonardo S. Villar Luis C. A. Viana Edison D. Bidone 《Environmental Earth Sciences》2012,65(6):1661-1669
A sediment core from Guanabara Bay (Brazil) was analyzed for 210Pb dating, grain size, total organic carbon (TOC) and total nitrogen, carbon stable isotope ratio (δ13C), nitrogen stable isotope ratio (δ15N) and the metals Fe, Mn, Ni, Co, Cu, Pb, V and Zn, to assess the influence of land use changes on the aquatic system in a
region for which large industrial and urban development is expected in the next few decades. To obtain baseline data for improving
the monitoring of the expected increase in anthropogenic impacts from surrounding drainage basins, a multivariate analysis
of data from different sediment layers was carried out to evaluate the dated sediment record. The geochemical data suggested
three different sedimentary phases along the last 200 years. Before the 1880s, the highest clay and TOC contents were observed,
where the C/N ratios and the δ13C values suggested a mixture of algal and terrestrial organic matter and the lowest concentrations of Co, Cu, Pb, V and Zn,
for which background levels were estimated (4.6, 2.7, 14.9, 24.3 and 70.2 mg kg−1, respectively). From the 1880s to the 1950s, the metal concentrations and sand particles increased, but no change in organic
matter quality was observed, reflecting a period of land use change, still without significant sewage input. After the 1950s,
the sedimentation rate increased from 0.42 to 0.77 cm year−1 and increasing urban sewage input was evidenced by lower C/N ratios, higher δ15N, decrease of Fe and Mn concentrations and increased fluxes of metals and TOC, which showed a good relationship with population
growth data. 相似文献
794.
Marbles and carbonate rocks from central Morocco: a petrographic,mineralogical and geochemical study
Francesca Origlia Elisabetta Gliozzo Anna Gandin Marco Meccheri Jorge E. Spangenberg Isabella Turbanti Memmi 《Environmental Earth Sciences》2012,66(1):209-222
Petrographic, mineralogical, and stable isotopes (δ13C, δ18O values) compositions were used to characterise marbles and sedimentary carbonate rocks from central Morocco, which are considered
to be a likely source of ornamental and building material from Roman time to the present day. This new data set was used in
the frame of an archaeometric provenance study on Roman artefacts from the town of Thamusida (Kenitra, north Morocco), to assess the potential employment of these rocks for the manufacture of the archaeological materials.
A representative set of samples from marbles and other carbonate rocks (limestone, dolostone) were collected in several quarries
and outcrops in the Moroccan Meseta, in a region extending from the Meknes–Khenifra alignment to the Atlantic Ocean. All the
samples were studied using a petrographic, mineralogical and geochemical methods. The petrographic and minerological investigations
(optical microscopy, electron microscopy, X-ray diffraction) allowed to group the carbonate rocks in limestones, foliated
limestone, diagenetic breccias and dolostone. The limestones could be further grouped as mudstones, wackestones–packstones,
crinoid grainstones, oolitic grainstone and floatstones. Textural differences allowed to define marbles varieties. The stable
carbon and oxygen isotope composition proved to be quite useful in the discrimination of marble sources, with apparently less
discriminatory potential for carbonate rocks. 相似文献
795.
796.
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799.
A. L. Rodrigues A. V. Machado J. M. Nóbrega A. Albuquerque A. G. Brito R. Nogueira 《International Journal of Environmental Science and Technology》2014,11(2):263-268
Nitrate removal from water has been accomplished by heterotrophic biofilms using organic carbon as a source of reducing power. To overcome the natural limitation in organic carbon in water, a poly-ε-caprolactone based biofilm carrier that serves simultaneously as a biofilm carrier and as a source of organic carbon was developed and tested in the present work. The feasibility of the new biofilm carrier for nitrate removal from water was evaluated in a packed bed reactor. The combination of size and structure provided a carrier element having high surface area and void volume, 1,170 m2/m3 and 67 %, respectively. A maximum denitrification rate of 4.4 mg N–NO3 ?/(L.h) (9.2 mg N–NO3 ?/(m2.h)) was achieved in the packed bed reactor at 20 °C and pH 7.0. Main advantages of the biofilm carrier developed in the present work are its mechanical stability in water even after biofilm formation and controlled release of organic carbon by enzymatic reactions. The proposed biotechnology to remove nitrate from groundwater is robust and easy to operate. 相似文献
800.
Rodrigo Augusto Bellezoni Cristiano Kenji Iwai Vagner Roberto Elis Wanderley da Silva Paganini Jorge Hamada 《Environmental Earth Sciences》2014,71(5):2429-2439
In Brazil, the large quantities of solid waste produced are out of step with public policies, technological developments, and government budgets for the division. In small municipalities, the common lack of technological knowledge and financial conditions for suitable waste disposal has resulted in a large number of illegal dumps. Therefore, small sanitary landfill facilities are working with simplified operations focusing on cost reduction and meeting the economic and technological standards of the city without endangering the environment or public health. Currently, this activity is regulated at a federal level although there is some uncertainty regarding the risk of soil and aquifer contamination as theses facilities do not employ liners. Thus, this work evaluates a small landfill to identify changes in soil and groundwater using geotechnical parameters, monitoring wells, and geophysical tests performed by electrical profiling. It is verified that based on current conditions, no contaminants have migrated via underground water aquifers, and overall no significant changes have occurred in the soil. It is concluded that, despite its simplicity, the method investigated is a viable alternative for the final disposal of municipal solid waste from small cities, especially in developing countries. 相似文献