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Karst spring discharge

Model the carbonate precipitation in this carbonate channel by means of a Id transport with 40 cells of 10 m length each. Dispersivity is assumed with lm. Use the key words KINETICS and RATES and the BASIC program for calcite from the data set PHREEQC.dat describing the kinetics for both the calcite dissolution and the calcite precipitation. How much calcite precipitates each year within the channel s first 400 meter after the discharge How much C02 degasses at the same time  [Pg.137]

Fig. 44 Calcite ridge at a karst spring discharge near Weifienburg, Germany. Fig. 44 Calcite ridge at a karst spring discharge near Weifienburg, Germany.
CHARACTERISTICS OF SEDIMENT DISCHARGING FROM A KARST SPRING IN RESPONSE TO A STORM... [Pg.30]

Mahler, B. J., and Lynch, F. L., 1999, Muddy waters temporal variation in sediment discharging from a karst spring, J. Hydrol, 214 165-178. [Pg.46]

The study shows the utility of clay studies to karst hydrology. These data show that suspended sediment discharged from a karst aquifer can be derived from erosion of soil tens of kilometers away from the recharge zone of the aquifer. The data also show that other clearly allochthonous material, such as wood and (probably man-made) fibers travel through the aquifer and are discharged at the springs. [Pg.92]

See other pages where Karst spring discharge is mentioned: [Pg.137]    [Pg.176]    [Pg.137]    [Pg.176]    [Pg.137]    [Pg.4]    [Pg.24]    [Pg.30]    [Pg.111]    [Pg.27]    [Pg.4]    [Pg.83]    [Pg.84]    [Pg.308]    [Pg.54]   
See also in sourсe #XX -- [ Pg.137 , Pg.176 ]



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Karst

Springs

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