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Signature du carbone organique dissous dans un aquifère côtier stratifié

Signature du carbone organique dissous dans un aquifère côtier stratifié

          
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About the Book

Les pénuries d'eau sont devenues un problème de plus en plus grave dans la région de Pondichéry. Les eaux souterraines sont devenues la principale source d'approvisionnement en eau pour les secteurs domestique, industriel et agricole de cette région. Cet aquifère côtier partage avec les aquifères continentaux de nombreuses caractéristiques hydrogéologiques et il existe un risque de détérioration de la qualité de l'eau. La région de Pondichéry est un terrain sédimentaire séquentiel composé de grès, de sable et d'argile avec des occurrences de lignite dans les formations de la période Mio-Pliocène, ce qui indique la présence de carbone organique dans ces aquifères. La formation de Cuddalore est également considérée comme un environnement réducteur en raison de la présence de Marcasite, de tourbe et de lignite. La formation du Crétacé supérieur se compose de calcaires, d'argiles sableuses et de grès déposés dans un environnement marin et sert de source naturelle de carbone organique qui est ensuite lessivé des sédiments vers les eaux souterraines. Les sources anthropiques sont principalement représentées par les produits agrochimiques, les effluents industriels, les lixiviats de remblais et les pratiques agricoles.


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Product Details
  • ISBN-13: 9786206425946
  • Publisher: KS Omniscriptum Publishing
  • Publisher Imprint: Editions Notre Savoir
  • Height: 229 mm
  • No of Pages: 100
  • Spine Width: 6 mm
  • Width: 152 mm
  • ISBN-10: 6206425940
  • Publisher Date: 06 Sep 2023
  • Binding: Paperback
  • Language: French
  • Returnable: N
  • Weight: 159 gr


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