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Titlebook: Environmental Geology; Handbook of Field Me Klaus Knödel,Gerhard Lange,Hans-Jürgen Voigt Book 2007 Springer-Verlag Berlin Heidelberg 2007 B

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https://doi.org/10.1007/978-3-658-27383-5r, middle, and thermal infrared (Table 3.1-1). MSS can work in rather narrow spectral bands of a few nanometers. Thus, such remote sensing can focus on specific spectral features to identify detailed physical and chemical characteristics of the land surface objects of interest.
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row and the detrimental aftereffects of industrialization and environmental negligence become more apparent, society has become more aware of, and concerned about, stewardship of the natural environment – water, soil, and air. Sustainable development has become more widely received and promoted in m
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https://doi.org/10.1007/978-3-658-41574-7d spatial patterns and associations. Hence, such observations can be interpreted and analyzed with regard to their geoscientific information (Chapter 3.1) and with regard to their geometric structures (Chapter 3.2).
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https://doi.org/10.1007/978-3-540-88647-1 the Earth’s magnetic field ranging from 10. seconds to several hours to study the distribution of the conductivities with depth (Cagniard, 1953). The electromagnetic exploration methods described in this Chapter are based on the use of electromagnetic fields generated by controlled sources.
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Nonphotographic Imaging from Aircraft and Space-borne Platformsr, middle, and thermal infrared (Table 3.1-1). MSS can work in rather narrow spectral bands of a few nanometers. Thus, such remote sensing can focus on specific spectral features to identify detailed physical and chemical characteristics of the land surface objects of interest.
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Gravity Methodsocal gravity field differences due to density variations in the subsurface. The effects of smallscale masses are very small compared with the effects of the global part of the Earth’s gravity field (often on the order of 1 part in 10. to 10.).
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