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Mineral-organic layers

A general relationship between the composition of the water and that of the soHd minerals with which the water has come into contact during infiltration and in the aquifer can be expected. Biological activity, especially in the organic layer above the mineral part, has a pronounced effect on the acquisition of solutes. Because of microbial respiration, the CO2 pressure is increased. CO2 pressure tends to increase the alkalinity and the concentration of and other solutes. [Pg.213]

Stream sediment (mineral sediment, <0.150 mm) Residual soil, upper horizon (topsoil) 0 - 25 cm with out the top organic layer (<2 mm)... [Pg.9]

Stream water Stream sediment (mineral sediment) Residual soil, upper horizon (topsoil) 0 - 25 cm without organic layer Residual soil, lower (C) horizon (subsoil) a 25 cm layer within a depth range of 50 cm - 200 cm Soil samples should represent the dominant soil type of the small catchment. W s T C... [Pg.15]

COEFFICIENT OF DISTRIBUTION OF DINITROTOLUENE BETWEEN THE MINERAL AND ORGANIC LAYERS... [Pg.315]

Fig. 70. Influence of the concentration of sulphuric acid on the distribution coefficient R of DNT between the mineral and organic layer (Orlova [2a]). Fig. 70. Influence of the concentration of sulphuric acid on the distribution coefficient R of DNT between the mineral and organic layer (Orlova [2a]).
See other pages where Mineral-organic layers is mentioned: [Pg.613]    [Pg.613]    [Pg.88]    [Pg.70]    [Pg.427]    [Pg.139]    [Pg.13]    [Pg.666]    [Pg.380]    [Pg.1]    [Pg.230]    [Pg.172]    [Pg.208]    [Pg.48]    [Pg.332]    [Pg.29]    [Pg.47]    [Pg.211]    [Pg.189]    [Pg.11]    [Pg.36]    [Pg.20]    [Pg.28]    [Pg.250]    [Pg.202]    [Pg.205]    [Pg.497]    [Pg.580]    [Pg.730]    [Pg.317]    [Pg.83]    [Pg.56]    [Pg.450]    [Pg.725]    [Pg.109]    [Pg.25]    [Pg.507]    [Pg.557]    [Pg.558]    [Pg.266]    [Pg.47]    [Pg.366]    [Pg.294]    [Pg.88]    [Pg.216]    [Pg.315]   
See also in sourсe #XX -- [ Pg.613 ]



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Layer minerals

Organic layer

Organic mineralization

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