Resumen
It is well documented that aquatic sediments are sites of intensive microbial activity and that the majority of the processes which occur there involve the breakdown of organic matter and the subsequent transformations of the products of decomposition. Estuarine sediments typically have higher interstitial water concentrations of dissolved inorganic nitrogen (DIN) than in the overlying water column, suggesting that sediments are sites of active nitrogen cycling.
| Idioma original | English |
|---|---|
| Título de la publicación alojada | Transfer Processes in Cohesive Sediment Systems |
| Editores | W. R. Parker, D. J. J. Kinsman |
| Lugar de publicación | New York, USA |
| Editorial | Springer New York |
| Capítulo | 44 |
| Páginas | 215-229 |
| Número de páginas | 15 |
| ISBN (versión digital) | 978-1-4684-4763-7 |
| ISBN (versión impresa) | 978-1-4684-4765-1 |
| Estado | Published - 1984 |
Huella
Profundice en los temas de investigación de 'Nitrogen Cycling Bacteria and Dissolved Inorganic Nitrogen in Intertidal Estuarine Sediments'. En conjunto forman una huella única.Citar esto
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