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Environmental impact of uncontrolled waste disposal in mining and industrial areas in Central Germany 总被引：7，自引：0，他引：7
P. Schreck 《Environmental Geology》1998,35(1):66-72
The present-day landscape in Central Germany, in particular the region of Leipzig, Halle and Bitterfeld, is characterized
by the scars of former industrial activities. Vast districts have been devastated by lignite strip mining. Industrial and
domestic waste, residues from ore smelting, and highly toxic waste products from petrochemical plants and pesticide production
were deposited in abandoned pits near population centers. The chief effects of waste on the environment are the contamination
of groundwater by dissolved pollutants, the acidification of soil and water by the oxidation of pyrite-containing mining waste,
and the salinization of shallow aquifers by rising brines from adjacent confined groundwater affected by mining. The consequences
for the region are serious: mining lakes used for recreational purposes are contaminated by leachates from adjacent waste
dumps. Pyrite-containing refuse from lignite mining under oxidation gives rise to the acidification of surface and groundwater,
a basic condition for pollutant mobilization. In former metal mining districts, metalliferous and radioactive residues from
smelting jeopardize public health. These effects are described in detail using three case studies.
Received: 30 July 1996 · Accepted: 24 February 1997 相似文献
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Vassilios C. Kelessidis Cassiani Papanicolaou Antonios Foscolos 《International Journal of Coal Geology》2009,77(3-4):394-400
This review paper presents the results of an extensive study investigating whether addition of 3% w/w Greek lignite to 6.42% w/w water–bentonite suspensions, after being exposed to high temperatures, can prevent gelation and control filtration characteristics. Two different bentonites and eight lignites from different Greek basins have been used while a commercial lignite product has been used as standard. The lignite-free bentonite suspensions heated to 177 °C for 16 h (thermal aging) thicken considerably, increasing the yield stress and the yield point. Fluid consistency and flow behavior indices also change while no significant change is observed for plastic viscosity. Thermal aging of the suspensions results in unacceptably high fluid loss values.Addition of Greek lignite to water–bentonite suspensions, followed by thermal aging, provided the rheological stability of the suspensions by maintaining the low yield stress/point regardless of the type of bentonite. Some of the lignites performed as well as their commercial counterpart. No specific trends for rheological improvement have been identified with respect to various characteristics of lignites such as contents of humic, fulvic acids, humins and other parameters such as specific surface area and cation exchange capacity.Furthermore, addition of lignite in most cases provided very good filtration control of the water–bentonite suspensions after exposure to 177 °C, with some Greek lignites being superior to the commercial product. The same lignite parameters examined for rheological control, were also examined to determine their effect on fluid loss of these suspensions for both bentonites. The content of humic and fulvic acids of two groups of lignites showed weak inverse correlations with the fluid loss volumes for both bentonites, while all other parameters did not seem to directly correlate with the effectiveness of the lignites. 相似文献
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The Cenozoic Krabi Basin in the southern part of peninsular Thailand contains about 112 million tons proven coal reserves. At present, coal is only produced from the Bang Mark mine located in the southern part of the basin, where the main lignite bed is 7-20 m thick. The lignite bed occurs in an overall paralic succession. The present paper investigates the depositional conditions of an approximately 8 m thick lignite bed (main seam) in the Bang Mark mine using organic petrography, including maceral ratios, and geochemistry. The results are further interpreted in a sequence stratigraphic context. The lignite is of low rank and is completely dominated by huminite indicating generally oxygen-deficient conditions in the precursor mire. Very low inertinite contents suggest rare occurrences of wildfires. The lower part of the lignite bed represents a topogenous fresh water peat mire with open water areas that in few cases may have experienced influx of saline water. The peat mire was subjected to periodic inundations and deposition of siliciclastics. Tissue preservation was relatively poor. The upper part of the lignite bed represents a slightly domed fresh water ombrogenous peat mire with a stable watertable and a balance between peat accumulation and accommodation space creation that favoured preservation of plant tissues. In general, the mire vegetation changed from less woody in the topogenous mire to more arborescent in the ombrogenous mire, where plants with suberinised wood cell walls also were more frequent. Decompacted, the lignite bed corresponds to a minimum ~ 11 m thick peat deposit that records from ~ 22,000 to 55,000 years of peat accumulation. Watertable rise in the peat mire was controlled overall by relative sea-level rise. In a sequence stratigraphic context, the lignite bed overlies a terrestrialisation surface (TeS; sensu Diessel, 2007) and the lowermost part records peat formation during a falling watertable and a decreasing accommodation/peat accumulation ratio (terrestrialisation). An accommodation reversal surface (ARS; sensu Diessel, 2007) indicates a change to paludification style of peat formation characterised by rising watertable and a high accommodation/peat accumulation ratio. Another ARS marks a gradual change to a situation with a balanced accommodation/peat accumulation ratio. The overall watertable rise throughout peat formation, but at a gradually slower rate from base to top, suggests that the lignite bed could be located in the late transgressive systems tract (TST). 相似文献
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A. Schäfer T. Utescher M. Klett M. Valdivia-Manchego 《International Journal of Earth Sciences》2005,94(4):621-639
In the Cenozoic, the Lower Rhine Basin formed as a rift at the southeastern terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The study focusses on the marginal marine and fluvial fill of the Lower Rhine Basin. A basin model is developed. Support for this study was given by extensive industry outcrop and well data, by new stratigraphical and sedimentological observations. The ingression and subsequent regression of the Cenozoic North Sea is analysed using the concept of base level cyclicity. As the geohistory of the basin was complex, a subsidence curve is constructed. Furthermore, an attempt is made to trace the simultaneous uplift of the Rhenish Massif. 相似文献
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Lal C. Ram Nishant K. Srivastava Ramesh C. Tripathi Sanjay K. Thakur Awadhesh K. Sinha Sangeet K. Jha Reginald E. Masto Swapan Mitra 《Environmental Geology》2007,51(7):1119-1132
The maximum concentration of the majority of the trace metals in the leachates from shake and column test of lignite fly ash
(LFA) was within the prescribed limits; however, total dissolved solids, total hardness, cations and anions (except K+), being above the prescribed limits, may lead to the increase in the hardness and salinity in the soil on the disposal of
LFA. Present generation of huge amount of fly ash from thermal power plants (TPPs) is a big challenge concerning contamination
of soil, crop produce and surface and ground water bodies due to the presence of some of the toxic trace metals in it. The
leaching behavior of alkaline LFA (pH, 10.94), from TPP of Neyveli Lignite Corporation (NLC), India, was investigated by shake
and column tests using water and sodium acetate buffer. The leaching of trace metals from LFA was governed by their concentrations,
association with the ash particles, leaching duration and pH of the leachate (most influencing parameter). The leaching of
metals followed the order: buffer column > aqueous column > aqueous shake > buffer shake test. 相似文献
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E. Mavridou P. Antoniadis P. Khanaqa W. Riegel T. Gentzis 《International Journal of Coal Geology》2003,56(3-4):253-268
The objective of this study was to reconstruct the paleoenviromnent during formation of the deposit at Amynteon–Ptolemaida based mainly on its petrographic but also supported by its paleobotanic character and fossils found in the lignite beds themselves. The deposit of Amynteon occurs in the northern part of the elongated basin of Ptolemaida–Amynteon. The type of lignite formation is, in general terms, similar to the deposit of Ptolemaida, and the lignite is present in the Pleistocene strata of the basin. The alternating nature of lignite and interburden is an important characteristic of the deposit. In this study, we selected 20 samples of lignite from a representative drillhole, namely B-258 in order to discern its petrography. Optical microscopy showed that the huminite group macerals are dominant, ranging from 42.5% to 95.3%. Humotelinite is present in low to high quantities (12.0–79.5%), followed closely by humodetrinite. Humocollinite is present in very small amounts. In addition, macerals of the liptinite and inertinite groups are found in small concentrations, with a few exceptions.A number of indices, such as gelification index (GI), vegetation index (VI), groundwater index (GWI), tissue preservation index (TPI), and their ratios (e.g., VI/GWI, TPI/GI), were used to reconstruct the conditions prevailing during peat formation. The results indicate that the paleoenvironment was mainly limnic at the initial stages and transitioned to limnotelmatic with occasional rheotrophic conditions. The organic matter responsible for lignite formation developed mainly in a forested swamp environment with occasional transitions either towards a wet limnic (open water) or a drier telmatic environment. 相似文献