Detail publikace

Reflection of underlying rocks in chemistry of underground and surface waters

ŠKODA, S. VÁCHAL, J. TESAŘ, M. VÁCHALOVÁ, R. DUMBROVSKÝ, M. SOBOTKOVÁ, V.

Originální název

Reflection of underlying rocks in chemistry of underground and surface waters

Anglický název

Reflection of underlying rocks in chemistry of underground and surface waters

Jazyk

en

Originální abstrakt

More then 20 years the chemistry of surface water has been observed within GEOMON project in the Zdíkov region in the Šumava Mts. The knowledge of composition and chemistry of geological environment is very important for assessment of input and output of matter toúfrom this catchment. Soils, represented by oligotrophic and oligomezotrophic cambisoils, are very acid, sorption unsaturated. Their silicate buffering system significantly contributes to decrease leaching of calcium, manganese, chlorine and total aluminium, and so to reduction of intensity weathering of rocks.

Anglický abstrakt

More then 20 years the chemistry of surface water has been observed within GEOMON project in the Zdíkov region in the Šumava Mts. The knowledge of composition and chemistry of geological environment is very important for assessment of input and output of matter toúfrom this catchment. Soils, represented by oligotrophic and oligomezotrophic cambisoils, are very acid, sorption unsaturated. Their silicate buffering system significantly contributes to decrease leaching of calcium, manganese, chlorine and total aluminium, and so to reduction of intensity weathering of rocks.

Dokumenty

BibTex


@misc{BUT89343,
  author="Stanislav {Škoda} and Jan {Váchal} and Miroslav {Tesař} and Radka {Váchalová} and Miroslav {Dumbrovský} and Veronika {Sobotková}",
  title="Reflection of underlying rocks in chemistry of underground and surface waters",
  annote="More then 20 years the chemistry of surface water has been observed within GEOMON project in the Zdíkov region in the Šumava Mts. The knowledge of composition and chemistry of geological environment is very important for assessment of input and output of matter toúfrom this catchment. Soils, represented by oligotrophic and oligomezotrophic cambisoils, are very acid, sorption unsaturated. Their silicate buffering system significantly contributes to decrease leaching of calcium, manganese, chlorine and total aluminium, and so to reduction of intensity weathering of rocks.",
  address="Česká společnost chemická",
  chapter="89343",
  institution="Česká společnost chemická",
  number="s871-s1072",
  year="2011",
  month="september",
  pages="951--951",
  publisher="Česká společnost chemická",
  type="abstract"
}