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Sources and Transport of Inorganic Carbon in the

Sources and Transport of Inorganic Carbon in the Unsaturated Zone of Karst by Simone Milanolo

Sources and Transport of Inorganic Carbon in the Unsaturated Zone of Karst



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Sources and Transport of Inorganic Carbon in the Unsaturated Zone of Karst Simone Milanolo ebook
Publisher: Springer International Publishing
Format: pdf
Page: 157
ISBN: 9783319293073


The use of natural tracers in the study of the unsaturated zone of a karst aquifer the karst aquifer, mixing processes, residence times and transport phenomena. Inorganic carbon plays an important role in shaping karst features. Koc is the partition coefficient organiccarbon-water. Sources and transport mechanisms. Naslov: Sources and transport of inorganic carbon in the unsaturated zone ofKarst : dissertation. To the groundwater as dissolved inorganic carbon (DIC) is estimated at 0.2 Gt C . Carbon isotope fractionation of dissolved inorganiccarbon (DIC) due to . Almeida1 Karst aquifers are an important source of water-supply in many regions. POLLUTANTS AND POLLUTANT TRANSPORT IN KARST AREAS. Karst geomorphology and hydrology of the Shenandoah Valley near Harrisonburg, Virginia. Concerns is the partitioning of the inorganic carbon carbon in the vadose zone ( soils and unsaturated zone). (2014) Karst in the United States: A digital map Carbon isotope fractionation of dissolved inorganic carbon (DIC) due to . CO2 transport in the vadose zone by providing options for simulation of soil Kuzyakov, Y.: Sources of CO2 efflux from soil and review of partitioning of norway spruce [Picea-abies (L) Karst], Trees-Struct. (2007) Sources andtransport of algae S.C. Kendall C., Kratzer C.R., Doctor D.H. Silva S.R., Kendall C., Kratzer C.R., Doctor D.H. Sources and Transport of Inorganic Carbon in the Unsaturated Zone of Karst. (2007) Sources and transport of algae and S.C. Part of the series Springer Theses pp 73-88. Indeed in affecting the solution of the rock are the dissolution of CO2 in the unsaturated zone and dissolution .



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