C. E. Jacob's Study on the Prospective and Hypothetical Future of the Mining of the Ground Water Deposited Under the Southern High Plains of Texas and New Mexico     

W. Brutsaert  Gerardo Wolfgang Gross  Ralph M. McGehee 《Ground water》1975,13(6):492-505

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Magnitude and Frequency of Flooding in the Tagus Basin (Central Spain) over the Last Millennium     

Gerardo Benito  Andrés Díez-Herrero  María Fernández de Villalta 《Climatic change》2003,58(1-2):171-192

A relational database using Access, and an interface based on a Geographical Information System (GIS) with ArcView program, were created to allow spatial-temporal analysis of documentary flood data collected for the Tagus basin (Central Spain). High flood frequencies were registered in the periods: AD 1160–1210 (3%), 1540–1640 (11%; peak at 1590–1610), 1730–1760 (5%), 1780–1810 (4%), 1870–1900 (19%), 1930–1950 (17%) and 1960–1980 (12%). Flood magnitudes of those documentary events were estimated at four sites (Aranjuez, Toledo, Talavera and Alcántara) along the Tagus River using HEC-RAS Computer program, matching the calculated water surface profiles with historical references of flood stage. The largest floods took place during the periods AD 1168–1211 (Toledo and Talavera), AD 1658–1706 (Talavera), AD 1870–1900, and AD 1930–1950 (Aranjuez, Toledo, Talavera and Alcántara). The temporal distribution of flood magnitude and frequency is discussed within the context of climatic variability experienced by the Iberian Peninsula. Although flood producing mechanisms of Atlantic and Mediterranean basins of the Iberian Peninsula are related to different, independent atmospheric patterns, there is a clear coincidence between most periods showing high flood frequencies. These periods of high flooding seem to correspond to the initial and final decades of periods with climate deterioration described at the continental scale. This suggests that climatic variability over the last millennium has induced a response in hydrological extremes (positive or negative), irrespective of the flood-producing mechanism.  相似文献   

Mineralization of organic material and bacterial dynamics in Mississippi River plume water     

Wayne S. Gardner  James B. Cotner  Brian J. Eadie  Joann F. Cavaletto  Ronald Benner  Gerardo Chin-Leo 《Estuaries and Coasts》1994,17(4):816-828

Net remineralization rates of organic matter and bacterial growth rates were observed in dark-bottle incubation experiments conducted in July–August and February with water samples collected from sites in the Mississippi River plume of the Gulf of Mexico. Our objectives were to measure site-specific degradation rates of labile dissolved and particulate organic matter, quantify the potential importance of bacteria in these processes, and examine the kinetics of degradation over time. Unfiltered samples, and samples treated to remove (or dilute out) particles larger than bacteria, were enclosed in 9-1 bottles and incubated in the dark for 3–5 d. Respiration rates and inorganic compound accumulation rates were higher in summer than in winter and were highest in unfiltered surface samples at sites of intermediate salinities where phytoplankton were most abundant. The ratio of ammonium accumulation to oxygen removal in summer experiments suggested that the mineralized organic material resembled “Redfield” stoichiometry. Chemical fluxes were greater in bottles containing large (>1–3 μm) particles than in the bottles with these particles removed, but bacterial activities were generally similar in both treatments. These results suggest that particle consumers were an important component of total organic matter degradation. However, these experiments may have underestimated natural bacterial degradation rates because the absence of light could affect the production of labile organic substrates by phytoplankton. In agreement, with this hypothesis, bacterial growth rates tended to decrease over time in summer in surface plume waters where phytoplankton were abundant. In conjunction with other data, our results indicate that heterotrophic processes in the water column are spatially and temporally dependent on phytoplankton production.  相似文献   

Hydrogeochemical characterization and evolution of a regional karst aquifer in the Cuatrociénegas area,Mexico     

Antonio Cardona  Carlos Gutierrez-Ojeda  Manuel Martínez-Morales  Gerardo Ortiz-Flores  Luis González-Hita 《Environmental Earth Sciences》2018,77(23):785

The Cuatrociénegas area is useful for the investigation of the effect of groundwater extraction in the Chihuahuan freshwater xeric ecoregion. It has been investigated at this time using a selection of geochemical indicators (major, minor and trace elements) and δ³⁴S data, to characterize the origin of groundwater, the main geochemical processes and the mineral/groundwater interactions controlling the baseline geochemistry. The area is composed of limestones of Mesozoic age, with a composite thickness of about 500 m, overlaid by basin fill (poorly consolidated young sediments). Substantial water extraction and modification of natural discharges from the area along the last century have produced a detrimental impact on ecosystem structure and function. Water–rock interactions, mixing and evaporative processes dominate the baseline groundwater quality. Natural recharge is HCO₃–Ca type in equilibrium with calcite, low salinity (TDS?<?500 mg/L), Cl^? lower than 11 mg/L and average Li⁺ concentration of 0.005 mg/L. Along the groundwater flow systems, δ³⁴S evidence and mass transfer calculations indicate that Cretaceous gypsum dissolution and dedolomitization reactions adjust water composition to the SO₄–Ca type. The increase of water–rock interaction is reflected by Cl^? values increase (average 68 mg/L), TDS up to about 1500 mg/L and an average Li⁺ concentration of 0.063 mg/L. Calculations with chemical geothermometers indicate that temperature at depth could be at maximum of 15–20 °C higher than field-measured temperature for pozas. After groundwater is discharged to the surface, chemical evolution continues; water evaporation, CO₂ degassing and precipitation of minerals such as gypsum, calcite and kaolinite represent the final processes and reactions controlling water chemical composition.  相似文献   

Coastal lateral spreading in the world heritage site of the Tramuntana Range (Majorca,Spain). The use of PSInSAR monitoring to identify vulnerability     

Rosa María Mateos  Pablo Ezquerro  Jose Miguel Azañón  Bernadí Gelabert  Gerardo Herrera  Jose Antonio Fernández-Merodo  Daniele Spizzichino  Roberto Sarro  Inmaculada García-Moreno  Marta Béjar-Pizarro 《Landslides》2018,15(4):797-809

The Bàlitx area is located on the steep coastal side of the Tramuntana Range (Majorca), a mountainous region which was declared a World Heritage Site by UNESCO in 2011 in the cultural landscape category. The Bàlitx site was occupied by farming areas with dry stone constructions and water storing systems of both Roman and Islamic origin. The coastal landscape is characterised by a large fault escarpment of up to 260 m in height. Lateral spreading processes are favoured by local stratigraphy and tectonics in an energetic coastal dynamics scenario. Block spreading morphologies are identified along the escarpment, with large, rocky blocks of volumes up to 60?×?10³ m³ moving very slowly until their collapse. Consequently, a thick and highly karstified breccia deposit is accumulated at the base of the scarp. The lowest, oldest breccia outcrop has been dated (Th/U), and an age of 82.5?±?5.6 kyr was obtained, reflecting the time span this process has been active. Additionally, numerous geomorphological slope features are identified in the area: landslides, rockfalls, and, more specifically, long and deep cracks in the hanging wall block of the fault, which also reveal active lateral spreading processes. Coastal dynamics have been investigated by interpreting offshore geophysical studies, bathymetry data and borehole information to determine the role of wave energy in the stability of the slope. Additionally, 14 SAR images from the ALOS PALSAR satellite have been exploited for the present work, covering a period spanning from 2007 to 2010, an anomalous rainy period in the region. Images were processed using the Persistent Scattered Interferometry (PSI) technique. PSInSAR results reveal that the rate of movement for the Bàlitx lateral spreading is extremely low (??5.2 mm/year on average), but major activity has been detected in the NE sector, where velocity rates can reach values of up to ??16 mm/year Coastal dynamics in the area can explain this, as a small island generates wave refraction and reflection determining more intense erosive processes in the NE part, which lead to a greater destabilising effect on the slopes. A simple vulnerability approach has been developed to take the elements of cultural heritage into account. Vulnerability increases from SW to NE, in accordance with landslide activity. The Bàlitx case study could provide a testimony to the effects of mass movements and coastal dynamics in an exceptional example of Mediterranean agricultural landscape.  相似文献   

O,p'-DDT induction of vitellogenesis and its inhibition by tamoxifen in Nile tilapia (Oreochromis niloticus)     

Leaños-Castañeda O  Van Der Kraak G  Lister A  Simá-Alvarez R  Gold-Bouchot G 《Marine environmental research》2002,54(3-5):703-707

In order to investigate the mechanism by which o,p'-DDT disrupts endocrine functioning of Nile tilapia in vivo, the estrogenicity of o,p'-DDT was investigated in conjunction with 17beta-estradiol (E2) and tamoxifen. Mature, male tilapia were treated intraperitoneally with o,p'-DDT (60 mg/kg, one dose) or E2 (5 mg/kg, four doses) in the presence or absence of tamoxifen (5 mg/kg, six doses) for 12 days and then plasma vitellogenin (Vtg) (measured as alkaline-labile phosphorous), E2, and testosterone (T) were measured. Vtg levels were increased dramatically by E2 (1,744 +/- 171 microg/ml) and moderately by o,p'-DDT (82 +/- 15 microg/ml) compared with controls (23 +/- 3.5 microg/ml). Tamoxifen alone had no effect on Vtg production, but inhibited both E2 and o,p'-DDT stimulated vitellogenesis. T levels were reduced with E2 administration (1,688 +/- 383 pg/ml) and declined further with the combined treatment of E2 and tamoxifen (281 +/- 70 pg/ml), compared with controls (6,558 +/- 1,438 pg/ml). Tamoxifen or o,p'-DDT alone did not affect T levels, but their combined treatment did (2,069 +/- 647 pg/ml). The results of this study suggest that o,p'-DDT is weakly estrogenic in male tilapia, and that this activity may be mediated through the estrogen receptor.  相似文献   

An aromatase inhibitor and tamoxifen decrease plasma levels of o,p-DDT and its metabolites in Nile tilapia (Oreochromis niloticus)     

Olga Leaos-Castaeda  Gerardo Gold-Bouchot  Glen Van Der Kraak  Andrea Lister  Victor Ceja-Moreno  Raul Sim-Alvarez 《Marine environmental research》2004,58(2-5):337

The objective of this study was to determine if tamoxifen or an aromatase inhibitor (4-hydroxyandrostenedione; 4-OHA) affected plasma concentrations of o,p^′-DDT and its metabolites, o,p^′-DDD and o,p^′-DDE, in mature tilapia. Male and female tilapia were injected 6 times intraperitoneally with o,p^′-DDT (40 mg/kg) alone or in combination with 4-OHA (2 mg/kg) over a 12 day period. An additional group of male fish was injected with tamoxifen (5 mg/kg) plus o,p^′-DDT. At the end of the treatment period, plasma samples were extracted and analyzed by GC/ECD. Females injected only with o,p^′-DDT had significantly higher levels of o,p^′-DDT compared with males. Interestingly, females and males treated concomitantly with o,p^′-DDT and 4-OHA or tamoxifen had significantly lower concentrations of plasma o,p^′-DDT (about 50%) compared with fish treated with only o,p^′-DDT. These initial results suggest that an interaction between endocrine-active compounds occurs in vivo in tilapia and may involve alterations in metabolism of o,p^′-DDT.  相似文献   

Characterization of cholinesterase activity from different tissues of Nile tilapia (Oreochromis niloticus)     

Rodríguez-Fuentes G  Gold-Bouchot G 《Marine environmental research》2004,58(2-5):505-509

Cholinesterases (ChE) from brain, muscle and liver in Nile tilapia (Oreochromis niloticus) were characterized using three substrates: acetylthiocholine iodide, propionylthiocholine iodide, and butyrylthiocholine iodide. Eserine was used as a total ChE inhibitor; BW284c51 and iso-OMPA were used as selective inhibitors for acetylcholinesterase (AChE) and butyrylcholinesterase (BuChE), respectively. The results indicate that AChE is the enzyme present in brain, whereas in both liver and muscle, the presence of atypical ChEs are suggested. These findings indicate that characterization of ChE is necessary prior to use in monitoring programs.  相似文献   

Seismogenic basin and range and intra‐arc normal faulting in the central Mexican Volcanic Belt,Querétaro,México     

Gerardo J. Aguirre‐Díaz  Jorge Nieto‐Obregn  F. Ramn Zúiga 《Geological Journal》2005,40(2):215-243

North‐northwest normal faults intersect ENE normal faults in the vicinity of Querétaro City, in central México, affecting the Miocene–Pliocene northern‐central sector of the Mexican Volcanic Belt province. This intersection produced an orthogonal arrangement of grabens, half‐grabens and horsts that include the Querétaro graben. The NNW faults are part of the Taxco–San Miguel de Allende fault system, which is proposed here as part of the southernmost Basin and Range province in México. The ENE to E–W faults are part of the E–W oriented Chapala–Tula fault zone, which has been interpreted as an active intra‐arc fault system of the Mexican Volcanic Belt. Seventy‐four normal faults were mapped, of which the NNW faults are the largest and have the best morphological expression in the region. More numerous, although shorter, are the ENE faults. Total length of the ENE faults is greater than the total length of the NNW faults. Both sets are dominantly normal faults, indicating ENE extension for the NNW set and NNW extension for the ENE set. Field data indicate that displacement on the two fault sets has overlapped in time, as some NNW faults are younger than some ENE faults, which are supposed to be the younger ones. Seismicity in 1998 on a NNW fault indicates ENE active extension on the NNW faults. These observations support our interpretation that the northern Mexican Volcanic Belt lies on the boundary between the Basin and Range province, which is undergoing ENE extension, and the central Mexican Volcanic Belt province, which is undergoing northerly extension. The apparent overlap in space and time of displacements on the two fault sets reflects the difference in stress regime between the two provinces. Copyright © 2005 John Wiley & Sons, Ltd.  相似文献   

Evaluation of a wind erosion model in a desert area of northern Asia by eddy covariance     

Gerardo Fratini  Monia Santini  Paolo Ciccioli  Riccardo Valentini 《地球表面变化过程与地形》2009,34(13):1743-1757

For the first time, vertical fluxes of mineral dust measured by Eddy Covariance in two desert sites of Northern Asia have been used to test the performances of a wind erosion model in the field. Soil parameters required by the model were obtained through field and laboratory determinations. Model predictions and direct measurements have been compared. The main finding was that the direction of the horizontal wind relative to the orientation of nebkhas played a crucial role in determining the emission of particles in one of the investigated sites. Being unable to simulate such interaction, the model generally overestimated the actual emission. It provided, instead, reliable predictions (r² = 0·87) when the wind direction was suitable in detaching loose erodible elements placed on nebkhas thanks to their normal orientation. Copyright © 2009 John Wiley & Sons, Ltd.  相似文献