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Sources and transport of inorganic carbon in the unsaturated zone of Karst[electronic resource] /

Record Type:	Language materials, printed : Monograph/item
[NT 15000414]:	551.9
Title/Author:	Sources and transport of inorganic carbon in the unsaturated zone of Karst/ by Simone Milanolo.
Author:	Milanolo, Simone.
Published:	Cham : : Springer International Publishing :, 2016.
Description:	xiv, 157 p. : : ill., digital ;; 24 cm.
Contained By:	Springer eBooks
Subject:	Geochemistry.
Subject:	Karst.
Subject:	Earth Sciences.
Subject:	Earth Sciences, general.
ISBN:	9783319293080
ISBN:	9783319293073
[NT 15000228]:	Introduction -- Site Description -- Materials and Methods -- A Conceptual Model -- Cave Climate -- Carbon Dioxide Sources, Storage and Transport in cave Atmosphere -- Cave Atmosphere Response to Artificial input of Carbon Dioxide -- From Soil to Cave: The Inorganic carbon in Drip water -- Calcite Deposition -- The Isotopic Imprint -- General Conclusions.
[NT 15000229]:	This book combines field, laboratory and modelling methods to identify, characterize and quantify sources and fluxes within and between the different compartments: water, rock and air. Inorganic carbon plays an important role in shaping karst features. In the unsaturated zone, the percolating water consumes soil-derived carbon dioxide while dissolving carbonate bedrock and then releases it again while degassing and precipitating calcite in caves. A portion of the released CO2 is returned to the atmosphere through the natural ventilation of caves. This book is an important reference source for all those interested in the global carbon budget, karst geochemistry, cave climate and paleoclimate studies using cave speleothem as proxies.
Online resource:	http://dx.doi.org/10.1007/978-3-319-29308-0

Sources and transport of inorganic carbon in the unsaturated zone of Karst[electronic resource] /
Milanolo, Simone.

Sources and transport of inorganic carbon in the unsaturated zone of Karst[electronic resource] /by Simone Milanolo. - Cham :Springer International Publishing :2016. - xiv, 157 p. :ill., digital ;24 cm. - Springer theses,2190-5053. - Springer theses..

Introduction -- Site Description -- Materials and Methods -- A Conceptual Model -- Cave Climate -- Carbon Dioxide Sources, Storage and Transport in cave Atmosphere -- Cave Atmosphere Response to Artificial input of Carbon Dioxide -- From Soil to Cave: The Inorganic carbon in Drip water -- Calcite Deposition -- The Isotopic Imprint -- General Conclusions.

This book combines field, laboratory and modelling methods to identify, characterize and quantify sources and fluxes within and between the different compartments: water, rock and air. Inorganic carbon plays an important role in shaping karst features. In the unsaturated zone, the percolating water consumes soil-derived carbon dioxide while dissolving carbonate bedrock and then releases it again while degassing and precipitating calcite in caves. A portion of the released CO2 is returned to the atmosphere through the natural ventilation of caves. This book is an important reference source for all those interested in the global carbon budget, karst geochemistry, cave climate and paleoclimate studies using cave speleothem as proxies.

ISBN: 9783319293080

Standard No.: 10.1007/978-3-319-29308-0doiSubjects--Topical Terms:

463825
Geochemistry.

LC Class. No.: QE515

Dewey Class. No.: 551.9

Sources and transport of inorganic carbon in the unsaturated zone of Karst[electronic resource] /
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505 0 $a Introduction -- Site Description -- Materials and Methods -- A Conceptual Model -- Cave Climate -- Carbon Dioxide Sources, Storage and Transport in cave Atmosphere -- Cave Atmosphere Response to Artificial input of Carbon Dioxide -- From Soil to Cave: The Inorganic carbon in Drip water -- Calcite Deposition -- The Isotopic Imprint -- General Conclusions.
520 $a This book combines field, laboratory and modelling methods to identify, characterize and quantify sources and fluxes within and between the different compartments: water, rock and air. Inorganic carbon plays an important role in shaping karst features. In the unsaturated zone, the percolating water consumes soil-derived carbon dioxide while dissolving carbonate bedrock and then releases it again while degassing and precipitating calcite in caves. A portion of the released CO2 is returned to the atmosphere through the natural ventilation of caves. This book is an important reference source for all those interested in the global carbon budget, karst geochemistry, cave climate and paleoclimate studies using cave speleothem as proxies.
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