GPS geodetic infrastructure for natural hazards study in the Puerto Rico and Virgin Islands region     

Linqiang Yang  Guoquan Wang  Victor Huérfano  Christa G. von Hillebrandt-Andrade  Jose A. Martínez-Cruzado  Hanlin Liu 《Natural Hazards》2016,81(1):641-662

  相似文献   

Porosity and size gradation of saturated gravel with percolated fines          下载免费PDF全文

Francisco Núñez‐González  Juan Pedro Martín‐Vide  Maarten G. Kleinhans 《Sedimentology》2016,63(5):1209-1232

Fine particles may infiltrate through coarse alluvial beds and eventually saturate the subsurface pore space. It is essential to understand the conditions that lead to bed saturation, and to forecast the packing characteristics of saturated beds to assess the effect of excess fine sediment supply on a number of processes that occur in the stream–sediment boundary. To address this problem, in this study, a new method is introduced to predict the grain‐size distribution for the saturated condition, and the resulting porosity decrease, given the characteristics of the bed and the supplied sediments. The new method consists of the numerical aggregation of infilling fines in a finite bed volume, during which the bed properties change to affect further infilling. An existing semi‐empirical, particle packing model is implemented to identify these properties. It is shown that these types of models are adequate to describe regimes of natural sediment fabric quantitatively, and are thus useful tools in the analysis of sediment infiltration processes. Unlike previous developments to quantify saturated bed conditions, which assume that the supplied material is uniform and finer than the bed pore openings, the method developed herein considers poorly sorted fines, and can identify size fractions that are able to ingress into the bed due to being smaller than the particles that form the bed structure. Application of the new method to published experimental data showed that the final content of infiltrated fines is strongly sensitive to the initial bed packing density, highlighting the need to measure and understand open‐work gravel deposits. In addition, the new method was shown to be suitable for assessing the degree of bed saturation, when it was applied to a published data set of field samples.  相似文献   

Reconstruction of Recent Sedimentary Processes in a Carbonate Platform (Gulf of Batabano,Cuba) Using Environmental Radiotracers     

M. Díaz-Asencio  J. A. Corcho-Alvarado  J. A. Sánchez-Cabeza  A. C. Ruiz-Fernández  M. Eriksson 《Estuaries and Coasts》2016,39(4):1020-1034

Recent (past 100 years) sedimentary processes in the highly dynamic Gulf of Batabano (Cuba, Caribbean Sea) were investigated through the analyses of environmental radionuclides (e.g., ²¹⁰Pb, ²²⁶Ra, ¹³⁷Cs, ^239,240Pu, and ¹⁴C) in nine sediment cores. We evaluated the mean mass accumulation rates (MARs) and the surface mixed layers (SMLs) in each sediment core. Based on these results, three sedimentary environments were identified in the study region. In the central zone, the sediments were mainly composed of carbonate transported from the southern area and showed elevated mass accumulation rates (MAR, 0.11–0.23 g cm^?2 year^?1) and relatively deep surface mixed layers (SML, 14–16 cm). The southwestern zone was characterized by lower MAR (0.05–0.08 g cm^?2 year^?1) and thinner SML (7–8 cm). In both areas, the long sediment mixing times in the SMLs (of 45–61 years) smoothed out the sedimentary records. The coastline sedimentary environments were characterized by higher MAR (0.30–0.57 g cm^?2 year^?1) and the sedimentary records displayed clear signatures of extreme climatic events such as the intensive rains in 1999 reported for La Coloma and the hurricanes Lili and Isodore in 2002. Our study shows that the application of the ²¹⁰Pb sediment dating method in dynamic costal zones is a challenging task but still may provide important information regarding sedimentation and mixing processes in the ecosystem.  相似文献   

Nitrogen Uptake and Internal Recycling in <Emphasis Type="Italic">Zostera marina</Emphasis> Exposed to Oyster Farming: Eelgrass Potential as a Natural Biofilter     

Jose?Sandoval-Gil  Ana?Alexandre  Rui?Santos  Víctor?F.?Camacho-IbarEmail author 《Estuaries and Coasts》2016,39(6):1694-1708

  相似文献   

Application of ultrasound for degradation of benzophenone-3 in aqueous solutions     

H. Zúñiga-Benítez  J. Soltan  G. A. Peñuela 《International Journal of Environmental Science and Technology》2016,13(1):77-86

  相似文献   

Treatment of water-repellent petroleum-contaminated soil from Bemidji,Minnesota, by alkaline desorption     

R. H. Adams  R. A. Cerecedo-López  L. A. Alejandro-Álvarez  V. I. Domínguez-Rodríguez  J. L. Nieber 《International Journal of Environmental Science and Technology》2016,13(9):2249-2260

A pipeline right-of-way contaminated with light crude in 1979 and subsequently burned shows severe hydrophobicity, poor infiltration rates, and loss of vegetative cover. To evaluate alkaline desorption as a treatment method, surface soil samples were collected and analyzed pre- and post-treatment. Samples had total petroleum hydrocarbon concentrations of 2800–63,100 mg/kg, severe water repellency, critical moisture 2–5 times above the in situ moisture content, but no acute toxicity. Thus, water repellency, rather than toxicity, is causing the loss of vegetation. Samples were treated with 0.1 N NaOH in two doses (1:3; soil/solution), with complete drainage between doses. Finally, each soil sample was washed with an equal volume or water and allowed to drain completely. For more hydrophobic samples, repeated treatments, without rinsing between each treatment, were made. Post-treatment, the samples were re-analyzed for water repellency and critical moisture content. In samples with initial water repellency values in the range of 5.0–6.7 M, the repellency was reduced 94–100 % and below critical levels to avoid soil hydrophobicity in field conditions. The other samples with initial water repellency values in the range of 10–13 M could not be recovered with single treatment, but sequential treatments reduced the hydrocarbon content up to 87 % and reduced the hydrophobicity to levels low enough or nearly low enough to avoid severe water repellency in the field. Currently, field studies are being carried out to evaluate this treatment method at the site, as a stand-alone method and in combination with organic amendment.  相似文献   

Monitoring of mercury and other metals mobility by sequential fractionation in soils nearby an abandoned chlor-alkali plant in Managua (Nicaragua)     

Rodolfo Fernández-Martínez  Belén Gómez-Mancebo  Emilio J. Peña  Pilar Galán  Akito Matsuyama  Fernando García  Isabel Rucandio 《Environmental Earth Sciences》2016,75(6):538

  相似文献   

Hypothesis on the hydrogeological context of wetland areas and springs related to evaporitic karst aquifers (Málaga,Córdoba and Jaén provinces,Southern Spain)     

Bartolomé Andreo  José Manuel Gil-Márquez  Matías Mudarra  Luis Linares  Francisco Carrasco 《Environmental Earth Sciences》2016,75(9):759

  相似文献   

Arsenic from gold mining in marine and stream sediments in Baja California Sur,Mexico     

Ivonne H. Posada-Ayala  Janette M. Murillo-Jiménez  Evgeni Shumilin  Ana J. Marmolejo-Rodríguez  Enrique H. Nava-Sánchez 《Environmental Earth Sciences》2016,75(11):996

  相似文献   

Geochemical mobility of arsenic in the surficial waters from Argentina     

Alicia Daniela Robles  Paula Polizzi  María Belén Romero  Leila Natalia Chiodi Boudet  Sandra Medici  Agustín Costas  Marcela Gerpe 《Environmental Earth Sciences》2016,75(23):1479

The presence of arsenic (As) in surface water constitutes an important environmental risk, where mobility and adsorption processes are responsible for its behavior in the sediment–water interface. Therefore, the assessment of adsorption, mobility and water availability of arsenic in freshwater sediments, with agricultural, livestock and urban soil uses was performed. Arsenic concentrations in sediments ranged from 5.4 to 15.9 mg kg^?1 (total) and 2.8 to 6.5 mg kg^?1 (labile), and those of iron and manganese were 11,563–23,500 and 140.6–662.1 mg kg^?1, respectively. The As levels in water were significantly lower than those of sediments. Results would suggest that As co-precipitation and adsorption on Fe oxides are probably the major route of immobilization, determining its low lability. Manganese did not present an outstanding contribution to the retention, and cation-exchange capacity, pH and organic matter of sediments did not show an influence on the mobility of As.  相似文献