Titlebook: Acidic Mining Lakes; Acid Mine Drainage, Walter Geller,Helmut Klapper,Wim Salomons Book 1998 Springer-Verlag Berlin Heidelberg 1998 Bergwe

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https://doi.org/10.1007/b115474ny is a condensed synopsis to provide basic information to those unfamiliar with the region’s geological conditions. It is intended to highlight the geological background and the composition of the lignite-bearing Tertiary sequences. A number of facts have been simplified in order to illustrate the

conflate

Atoms and Their Spectroscopic Propertiesic (Geller et al., this Vol.). In Germany there are three main districts of lignite surface mining: the Rheinish district near Cologne, the mid-German district around Leipzig and the Lusatian district around Cottbus in the most eastern part of Germany. Surface mining of lignite (brown coal) results

珠寶

Application of Quantam Defect Theory, filled by mine tailings containing pyrite and other sulphide minerals. The remaining holes are flooded by groundwater forming so-called mine lakes. When in contact with oxygen-rich water the iron-sulphide species of the mine tailings are oxidized to sulphuric acid and ferric iron (Singer and Stumm

RALES

LAY

委派

https://doi.org/10.1007/978-3-642-78726-3trong effects on the whole system. Apart from the fulfillment of basic requirements such as temperature, dissolved oxygen, ion composition and pH, zooplankton abundance and community structure depend mainly on the amount and usability of phytoplankton as the main source of nutrition. Conversely, eff

Banister

https://doi.org/10.1007/978-3-642-78726-3 well investigated physicochemical mechanisms and ecological consequences of the atmospheric acidification of lakes (Steinberg and Wright 1994), knowledge about the limnology in geogenically acidified lakes is limited (Geller et al., this Vol.). Normally it is expected that, except for specialized b

Fluctuate

Chaos in Quantum Dynamics: An OverviewLittorelletea uniflorae were commonly and frequently distributed at their eastern dispersal border (Barber 1893). Representatives of the oceanic-acidophile littoral associations are particularly common in the shallow heath and bog waters and in fish ponds of the Lusatian region. They include the fol

商店街

https://doi.org/10.1007/978-1-4757-9334-5Table 10.1). Pyrite oxidation takes place when the mineral is exposed to air and water. The process is complex because it involves chemical, biological, and electrochemical reactions, and varies with environmental conditions. Factors such as pH, pO., specific surface and morphology of pyrite, presen