Übersicht			Auf mobile öffnen

Lieferstatus:	Auf Bestellung (Lieferzeit unbekannt)
Veröffentlichung:	April 2017
Genre:	Naturwissensch., Medizin, Technik
	Analytical Chemistry / B / biochemistry / Earth and Environmental Science / Earth Sciences / Earth Sciences, general / Ecotoxicology / environmental science, engineering & technology / Environmental Sciences / Geotechnical engineering / Geotechnical Engineering & Applied Earth Sciences / Geotechnical Engineering and Applied Earth Sciences / Hydrogeology / Hydrology / Hydrology & the hydrosphere / Hydrology/Water Resources / Water
ISBN:	9783662517505
EAN-Code:	9783662517505
Verlag:	Springer Nature EN
Einband:	Kartoniert
Sprache:	English
Dimensionen:	H 235 mm / B 155 mm / D
Gewicht:	379 gr
Seiten:	230
Illustration:	XI, 230 p.
Zus. Info:	Previously published in hardcover
Bewertung:	Titel bewerten / Meinung schreiben

Inhalt:

To understand hydrochemistry and to analyze natural as well as man-made impacts on aquatic systems, hydrogeochemical models have been used since the 1960¿s and more frequently in recent times. Numerical groundwater flow, transport, and geochemical models are important tools besides classical deterministic and analytical approaches. Solving complex linear or non-linear systems of equations, commonly with hundreds of unknown parameters, is a routine task for a PC. Modeling hydrogeochemical processes requires a detailed and accurate water analysis, as well as thermodynamic and kinetic data as input. Thermodynamic data, such as complex formation constants and solubility-products, are often provided as databases within the respective programs. However, the description of surface-controlled reactions (sorption, cation exchange, surface complexation) and kinetically controlled reactions requires additional input data. Unlike groundwater flow and transport models, thermodynamic models, in principal, do not need any calibration. However, considering surface-controlled or kinetically controlled reaction models might be subject to calibration. Typical problems for the application of geochemical models are: ¿ speciation ¿ determination of saturation indices ¿ adjustment of equilibria/disequilibria for minerals or gases ¿ mixing of different waters ¿ modeling the effects of temperature ¿ stoichiometric reactions (e.g. titration) ¿ reactions with solids, fluids, and gaseous phases (in open and closed systems) ¿ sorption (cation exchange, surface complexation) ¿ inverse modeling ¿ kinetically controlled reactions ¿ reactive transport Hydrogeochemical models depend on the quality of the chemical analysis, the boundary conditions presumed by the program, theoretical concepts (e.g.