FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1999835521> ?p ?o ?g. }

• W1999835521 endingPage "174" @default.
• W1999835521 startingPage "164" @default.
• W1999835521 abstract "Contaminant sources have been attributed to shoe manufacturers in an alluvial aquifer located along 26 km2 in the Chienti River Valley, Central Italy. During the 1980s and 1990s, the main chlorinated compound used in the study area was 1,1,1-Trichloroethane (1,1,1-TCA), which was substituted by Perchloroethene (PCE) in the last 15 years. A hydrogeological conceptual model has been developed for the alluvial aquifer taking into account the presence of low permeability lenses, forming a multilayer semi-confined aquifer. Hydrodynamic tests (pumping and flowmeter heat-pulse tests) coupled with standard and multilevel hydrochemical and isotopic samplings were performed. Flowmeter tests showed the existence of vertical flow between aquifer levels having different permeability. Physical–chemical parameter logs agreed with the existence of a multilayer aquifer. Concentration data collected in 21 wells located downgradient of the different sources revealed VOC (Volatile Organic Compound) levels lower than 100 μg/L in the upper part of the valley and levels reaching about 200 μg/L in the near shore areas. PCE is the main compound present in the aquifer. No evidence of the presence of TCA was found in the upper areas of the Chienti Valley, but in the areas near the shore, TCA and its degradation products are predominant. Data collected at multilevels located at two sites (upper and near shore areas) to refine the results obtained in the regional survey show a stratification of the VOC concentrations; values of each compound are higher than those measured in the conventional wells during the standard sampling (e.g. PCE: 150 μg/L instead of 2 μg/L). In addition, the vertical distribution of the contaminant reflects the vertical flow pattern inferred from hydrogeological data. The hydrogeological, VOC and isotope data showed that dilution is the main process controlling VOCs concentration in the aquifer. Degradation also played a role in the attenuation of the parent compounds in some localized areas of the aquifer. The role of the low permeability layers on VOC degradation was documented by the presence of cis-1,2-DCE, a main daughter product of PCE, in some zones of the upper area, and 1,1-Dichloroethene (1,1-DCE) and 1,1-Dichloroethane (1,1-DCA), byproducts of 1,1,1-TCA degradation, in the near shore areas." @default.
• W1999835521 created "2016-06-24" @default.
• W1999835521 creator A5026169070 @default.
• W1999835521 creator A5034994294 @default.
• W1999835521 creator A5052280883 @default.
• W1999835521 creator A5067009387 @default.
• W1999835521 creator A5079439419 @default.
• W1999835521 creator A5085387940 @default.
• W1999835521 date "2013-05-01" @default.
• W1999835521 modified "2023-10-17" @default.
• W1999835521 title "Hydrodynamic and isotopic characterization of a site contaminated by chlorinated solvents: Chienti River Valley, Central Italy" @default.
• W1999835521 cites W1608294965 @default.
• W1999835521 cites W1974757881 @default.
• W1999835521 cites W1981817411 @default.
• W1999835521 cites W1982151458 @default.
• W1999835521 cites W1984671858 @default.
• W1999835521 cites W1986618888 @default.
• W1999835521 cites W1999591901 @default.
• W1999835521 cites W2010987775 @default.
• W1999835521 cites W2014528722 @default.
• W1999835521 cites W2017546439 @default.
• W1999835521 cites W2017676831 @default.
• W1999835521 cites W2018235058 @default.
• W1999835521 cites W2021179993 @default.
• W1999835521 cites W2023167417 @default.
• W1999835521 cites W2044142535 @default.
• W1999835521 cites W2045332781 @default.
• W1999835521 cites W2045526667 @default.
• W1999835521 cites W2062658116 @default.
• W1999835521 cites W2074219695 @default.
• W1999835521 cites W2080170139 @default.
• W1999835521 cites W2085849971 @default.
• W1999835521 cites W2087606790 @default.
• W1999835521 cites W2091706041 @default.
• W1999835521 cites W2092506983 @default.
• W1999835521 cites W2094427369 @default.
• W1999835521 cites W2121294658 @default.
• W1999835521 cites W2127162710 @default.
• W1999835521 cites W2134713290 @default.
• W1999835521 cites W2135589852 @default.
• W1999835521 cites W2333324465 @default.
• W1999835521 cites W2503176929 @default.
• W1999835521 cites W3045927976 @default.
• W1999835521 doi "https://doi.org/10.1016/j.apgeochem.2012.09.012" @default.
• W1999835521 hasPublicationYear "2013" @default.
• W1999835521 type Work @default.
• W1999835521 sameAs 1999835521 @default.
• W1999835521 citedByCount "13" @default.
• W1999835521 countsByYear W19998355212014 @default.
• W1999835521 countsByYear W19998355212015 @default.
• W1999835521 countsByYear W19998355212016 @default.
• W1999835521 countsByYear W19998355212017 @default.
• W1999835521 countsByYear W19998355212018 @default.
• W1999835521 countsByYear W19998355212019 @default.
• W1999835521 countsByYear W19998355212020 @default.
• W1999835521 crossrefType "journal-article" @default.
• W1999835521 hasAuthorship W1999835521A5026169070 @default.
• W1999835521 hasAuthorship W1999835521A5034994294 @default.
• W1999835521 hasAuthorship W1999835521A5052280883 @default.
• W1999835521 hasAuthorship W1999835521A5067009387 @default.
• W1999835521 hasAuthorship W1999835521A5079439419 @default.
• W1999835521 hasAuthorship W1999835521A5085387940 @default.
• W1999835521 hasConcept C111368507 @default.
• W1999835521 hasConcept C112570922 @default.
• W1999835521 hasConcept C114793014 @default.
• W1999835521 hasConcept C120882062 @default.
• W1999835521 hasConcept C127313418 @default.
• W1999835521 hasConcept C152382732 @default.
• W1999835521 hasConcept C185592680 @default.
• W1999835521 hasConcept C187320778 @default.
• W1999835521 hasConcept C18903297 @default.
• W1999835521 hasConcept C33556824 @default.
• W1999835521 hasConcept C41625074 @default.
• W1999835521 hasConcept C55493867 @default.
• W1999835521 hasConcept C69823785 @default.
• W1999835521 hasConcept C75622301 @default.
• W1999835521 hasConcept C76177295 @default.
• W1999835521 hasConcept C76886044 @default.
• W1999835521 hasConcept C86803240 @default.
• W1999835521 hasConceptScore W1999835521C111368507 @default.
• W1999835521 hasConceptScore W1999835521C112570922 @default.
• W1999835521 hasConceptScore W1999835521C114793014 @default.
• W1999835521 hasConceptScore W1999835521C120882062 @default.
• W1999835521 hasConceptScore W1999835521C127313418 @default.
• W1999835521 hasConceptScore W1999835521C152382732 @default.
• W1999835521 hasConceptScore W1999835521C185592680 @default.
• W1999835521 hasConceptScore W1999835521C187320778 @default.
• W1999835521 hasConceptScore W1999835521C18903297 @default.
• W1999835521 hasConceptScore W1999835521C33556824 @default.
• W1999835521 hasConceptScore W1999835521C41625074 @default.
• W1999835521 hasConceptScore W1999835521C55493867 @default.
• W1999835521 hasConceptScore W1999835521C69823785 @default.
• W1999835521 hasConceptScore W1999835521C75622301 @default.
• W1999835521 hasConceptScore W1999835521C76177295 @default.
• W1999835521 hasConceptScore W1999835521C76886044 @default.
• W1999835521 hasConceptScore W1999835521C86803240 @default.
• W1999835521 hasLocation W19998355211 @default.
• W1999835521 hasOpenAccess W1999835521 @default.

• next