Impact of erosion-transported overburden dump materials on water quality in Lake Cospuden evolved from a former open cast lignite mine south of leipzig, Germany

2002 ◽  
Vol 43 (1) ◽  
pp. 70
2001 ◽  
Vol 73 (2) ◽  
pp. 97-111 ◽  
Author(s):  
Wolfgang Rolland ◽  
Hella Wagner ◽  
Robert Chmielewski ◽  
Uwe Grünewald

2018 ◽  
Vol 29 ◽  
pp. 00023
Author(s):  
Jaroslaw Wajs

The paper presents satellite imagery from active SENTINEL-1A and passive SENTINEL-2A/2B sensors for their application in the monitoring of mining areas focused on detecting land changes. Multispectral scenes of SENTINEL-2A/2B have allowed for detecting changes in land-cover near the region of interest (ROI), i.e. the Szczercow dumping site in the Belchatow open cast lignite mine, central Poland, Europe. Scenes from SENTINEL-1A/1B satellite have also been used in the research. Processing of the SLC signal enabled creating a return intensity map in VV polarization. The obtained SAR scene was reclassified and shows a strong return signal from the dumping site and the open pit. This fact may be used in detection and monitoring of changes occurring within the analysed engineering objects.


Solid Earth ◽  
2016 ◽  
Vol 7 (3) ◽  
pp. 789-815 ◽  
Author(s):  
Michael Kettermann ◽  
Sebastian Thronberens ◽  
Oscar Juarez ◽  
Janos Lajos Urai ◽  
Martin Ziegler ◽  
...  

Abstract. Clay smears in normal faults can form seals for hydrocarbons and groundwater, and their prediction in the subsurface is an important problem in applied and basic geoscience. However, neither their complex 3-D structure, nor their processes of formation or destruction are well understood, and outcrop studies to date are mainly 2-D. We present a 3-D study of an excavated normal fault with clay smear, together with both source layers, in unlithified sand and clay of the Hambach open-cast lignite mine in Germany. The faults formed at a depth of 150 m, and have shale gouge ratios between 0.1 and 0.3. The fault zones are layered, with sheared sand, sheared clay and tectonically mixed sand–clay gouge. The thickness of clay smears in two excavated fault zones of 1.8 and 3.8 m2 is approximately log-normal, with values between 5 mm and 5 cm, without holes. The 3-D thickness distribution is heterogeneous. We show that clay smears are strongly affected by R and R' shears, mostly at the footwall side. These shears can locally cross and offset clay smears, forming holes in the clay smear, while thinning of the clay smear by shearing in the fault core is less important. The thinnest parts of the clay smears are often located close to source layer cut-offs. Locally, the clay smear consists of overlapping patches of sheared clay, separated by sheared sand. More commonly, it is one amalgamated zone of sheared sand and clay. A microscopic study of fault-zone samples shows that grain-scale mixing can lead to thickening of the low permeability smears, which may lead to resealing of holes.


2002 ◽  
Vol 81 (2) ◽  
pp. 193-199 ◽  
Author(s):  
G. Heumann ◽  
Th. Litt

AbstractMore than 400 samples for paleobotanical and sedimentological investigations were collected from Late Pliocene and earliest Pleistocene beds in the open-cast lignite mine Hambach. They were analysed to obtain information about the paleoecology and paleoclimate of this time interval. The sedimentation type changed from a high-energy meandering fluvial system to floodplain, swamp and oxbow lake sedimentation. The typical Tertiary floral elements decreased with the onset of increasingly cooler climatic conditions and disappeared at the beginning of the Pleistocene to be substituted by a impoverished and coldadapted flora. These combined litho- and biostratigraphic investigations led to an improved and reproducible separation of Late Pliocene from Early Pleistocene deposits.


IARJSET ◽  
2017 ◽  
Vol 4 (5) ◽  
pp. 42-47
Author(s):  
Srivastav S K ◽  
Yadav H L ◽  
Seervi V ◽  
Jamal A
Keyword(s):  

Boreas ◽  
1999 ◽  
Vol 28 (3) ◽  
pp. 363-374 ◽  
Author(s):  
Jan A. Piotrowski ◽  
Jörn Geletneky ◽  
Ralf Vater

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