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排序方式: 共有137条查询结果,搜索用时 15 毫秒
61.
Ester Falgàs Juanjo Ledo Beatriz Benjumea Pilar Queralt Alex Marcuello Teresa Teixidó Anna Martí 《Surveys in Geophysics》2011,32(6):857-873
Groundwater management needs detailed aquifer characterization, especially in semiarid costal aquifer systems that are under
hydrological pressure. Our study area is in the Tordera delta, northeastern coast of Spain, where a detrital fluvio-deltaic
aquifer system has been developed above granitic basement. The main purpose of this study is to characterize the complex lithological
structure and the seawater intrusion state by combining hydrological information, audiomagnetotelluric (AMT) and seismic reflection
and refraction models. This allowed us to provide spatially continuous information about aquifer properties and processes.
Thus, we have determined the thickness and continuity of the aquifer units, as well as the morphology and depth to the basement.
The models revealed that the main seawater intrusion main path is found in the western deltaic area that coincides with an
existing buried paleochannel. This new result explains the anomalously high chlorine concentrations observed in the deep semiconfined
aquifer more than 1,500 m inland. 相似文献
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Dinophysis acuminata and Dinophysis acuta produce lipophilic toxins that cause most shellfish harvesting closures in the Atlantic coastal waters of Europe. Dinophysis often exhibit patchy distributions and sampling with conventional methods may fail to detect them. A 6-month calibration study in 2006, plus an additional sampling in 2010 were carried out in Galicia to compare Dinophysis counts obtained from weekly high vertical resolution bottle samples with depth-integrated hose samples. Counts with these two methods were comparable at some depth-ranges, but hose maxima were over one order of magnitude lower under thin-layer scenarios. Estimates from hose samplers should be used with caution in programmes using a "Dinophysis index", either to trigger shellfish sampling or to establish precautionary harvesting closures. In general, hose samplers provide reliable information on the occurrence of Dinophysis except under extreme site-specific hydrodynamic conditions. This study adds new information about the heterogeneous, specific vertical distributions of two Dinophysis spp. 相似文献
65.
Claudia Beatriz Quinteros Cartaya Fidencio Alejandro Nava Pichardo Ewa Glowacka José Duglas Frez Cárdenas 《Pure and Applied Geophysics》2014,171(7):1367-1383
In order to analyze observed seismicity in central Japan and Venezuela, we applied a new method to identify semi-periodic sequences in the occurrence times of large earthquakes, which allows for the presence of multiple periodic sequences and/or events not belonging to any sequence in the time series. We also explored a scheme for diminishing the effects of a sharp cutoff magnitude threshold in selecting the events to analyze. A main four-event sequence with probability P c = 0.991 of not having occurred by chance was identified for earthquakes with M ≥ 8.0 in central Japan. Venezuela is divided, from West to East, into four regions; for each of these, the magnitude ranges and identified sequences are as follows. Region 1: M ≥ 6.0, a six-event sequence with P c = 0.923, and a four-event sequence with P c = 0.706. Region 2: M ≥ 5.6, a five-event sequence with P c = 0.942. Region 3: M ≥ 5.6, a four-event sequence with P c = 0.882. Region 4: M ≥ 6.0, a five-event sequence with P c = 0.891. Forecasts are made and evaluated for all identified sequences having four or more events and probabilities ≥0.5. The last event of all these sequences was satisfactorily aftcast by previous events. Whether the identified sequences do, in fact, correspond to physical processes resulting in semi-periodic seismicity is, of course, an open question; but the forecasts, properly used, may be useful as a factor in seismic hazard estimation. 相似文献
66.
Fidencio Alejandro Nava Pichardo Claudia Beatriz Quinteros Cartaya Ewa Glowacka José Duglas Frez Cárdenas 《Pure and Applied Geophysics》2014,171(7):1355-1366
We present a new method to identify semi-periodic sequences in the occurrence times of large earthquakes, which allows for the presence of multiple semi-periodic sequences and/or events not belonging to any identifiable sequence in the time series. The method, based on the analytic Fourier transform, yields estimates of the departure from periodicity of an observed sequence, and of the probability that the sequence is not due to chance. These estimates are used to make and to evaluate forecasts of future events belonging to each sequence. Numerous tests with synthetic catalogs show that the method is surprisingly capable of correctly identifying sequences, unidentifiable by eye, in complicated time series. Correct identification of a given sequence depends on the number of events it contains, on the sequence’s departure from periodicity, and, in some cases, on the choice of starting and ending times of the analyzed time window; as well as on the total number of events in the time series. Some particular data combinations may result in spectra where significant periods are obscured by large amplitudes artifacts of the transform, but artifacts can be usually recognized because they lack harmonics; thus, in most of these cases, true semi-periodic sequences may not be identified, but no false identifications will be made. A first example of an application of the method to real seismicity data is the analysis of the Parkfield event series. The analysis correctly aftcasts the September 2004 earthquake. Further applications to real data from Japan and Venezuela are shown in a companion paper. 相似文献
67.
Isidro A. Pérez M. Luisa Sánchez M. Ángeles García Beatriz de Torre 《Theoretical and Applied Climatology》2009,98(3-4):269-277
CO2 in the rural atmosphere is related to respiration–photosynthesis processes, although the evolution of the low atmosphere is also a determinant factor. CO2 concentrations were measured at surface and meteorological variables obtained from a radio acoustic sounding system sodar at a flat rural site during a 3-year campaign. Yearly and daily cycles of CO2 were described. Maxima were observed in spring and autumn during the night. Wind speed and thermal structure of the lower atmosphere were analysed. Low level jets were observed during the night, their core proving lower in summer. Surface inversions observed with low winds reached up to 100 m. The turbulence layer which developed during the day extended up to 300–400 m and was capped by a stable layer. Median vertical wind speed reached 1 m s?1 in super-adiabatic conditions in summer. Determination of decoupled low level jets proved difficult with the device used and corresponding concentrations were slightly higher than medians calculated with all the observations. The bulk Richardson number was calculated in the lower atmosphere and four intervals were considered: drainage, transitional, shear flows and unstable conditions. Median CO2 concentrations were split according to these intervals. Higher values corresponded to drainage flow, which was associated to more stable conditions being less frequent and lower values to shear flow and unstable conditions, revealing a satisfactory link between the bulk Richardson number as a turbulence indicator in the low atmosphere and CO2 surface concentrations. 相似文献
68.
The upper Kimmeridgian outcrops in Jabaloyas (NE Spain) studied here have significant similarity in terms of carbonate ramp morphology and its facies architecture with Member D of the Upper Jurassic Arab Formation reservoirs in the Middle East. Geological models from analogue outcrops enhance or challenge the understanding of multi-scale sedimentological and diagenetic heterogeneities in the subsurface hydrocarbon reservoir models by providing morphometric parameters. For this purpose, conventional diagenetic studies (petrographic microscopy analysis and cathodoluminescence) have been performed to assess the impact of diagenetic modifications through burial. More than 50 thin sections have been used to define a full paragenetic sequence. Additional mineralogical mapping (Qemscan®) on a selection of thin sections serves as a calibration tool for semiquantitative analytic studies of every mineral phases and the proposed porosity evolution. This work unravels the whole paragenetic diagenetic processes and focused on those that occurred right after deposition to shallow burial (eogenesis). High-sequence stratigraphy allows linking these events to variations of the environmental domains that, in fact, respond most likely to sea-level fluctuations. In particular, it provides key parameters to frame the diagenetic overprint such as cementation processes plugging primary interparticle porosity and selective dissolution linked to master bounding surfaces: calcite meniscus cements in vadose zones and selective dissolution processes linked to firmgrounds. Ultimately, they offer valuable trends that would be potentially relevant to decipher and characterize reservoir parameters for the upscaling workflow of fabrics from microscopic to inter-well scale in carbonate hydrocarbon reservoirs. 相似文献
69.
Beatriz Melba Honnorez-Guerstein 《Mineralium Deposita》1971,6(2):111-121
The copper deposit La Leona consists of ore veins in a granite batholite which intruded into Permian sediments. In these veins the following minerals are observed: pyrite, sphalerite, chalcopyrite, galena, betekhtinite, two Bisulfosalts, electrum, bornite, chalcocite, enargite, tennantite, Zn-Fahlerz, cuprite, delafossite, molybdenite, hematite and iron hydroxides, and copper carbonates with quartz and iron carbonates as gangue. The betekhtinite, (CuFe)10Pb S6, found for the first time in Argentina, the Zn-Fahlerz and the sulfosalts (Cu3.2Bi1.2Pb1.2S8.5) and (Cu9.3Bi1.1S6.8) were studied in detail under the microscope, by X-rays and by microprobe. Specifically, the paragenesis of these three minerals with galena, chalcocite and bornite is discussed.
Résumé Le gisement de cuivre de la mine «La Leona» est formé de filons de minerais recoupant un batholite granitique qui a fait intrusion dans des sédiments permiens. Les minéraus suivants ont été observés: pyrite, blende, chalcopyrite, galène, bétekhtinite, deux sulfosels de Bi, électrum, bornite, chalcosine, énargite, tennantite, «Zn-Fahlerz», cuprite, delafossite, molybdénite, hématite et hydroxydes de fer, des carbonates de cuivre, dans une gangue de quartz et de carbonates de fer. La bétekhtinite (Cu Fe)10Pb S6, trouvée pour la première fois en Argentine, le «Zn-Fahlerz» et les sulfosels (Cu3.2Bi1.2Pb1.2S8.5) et (Cu9.3Bi1.1S6.8) ont été spécialement étudiés à l'aide de la microscopie, de la diffraction des rayons-X et de la microsonde. La paragénèse formée par ces trois mineraux associés à la galène, la chalcosine et la bornite est discutée.相似文献
70.