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By H. Şebnem Düzgün, Nuray Demirel

1 advent 1.1 Sustainability in mining 1.2 Environmental affects of mining 1.3 Environmental impression tracking in mining 1.4 Mine land tracking 1.5 function of distant sensing in mine tracking 1.6 Scope of the e-book References 2 ideas of distant sensing 2.1 Definition of distant sensing 2.2 rules of electromagnetic radiation 2.3 actual legislation of electromagnetic power 2.4 The electromagnetic spectrum 2.5 Read more...

summary: 1 creation 1.1 Sustainability in mining 1.2 Environmental affects of mining 1.3 Environmental influence tracking in mining 1.4 Mine land tracking 1.5 position of distant sensing in mine tracking 1.6 Scope of the e-book References 2 rules of distant sensing 2.1 Definition of distant sensing 2.2 ideas of electromagnetic radiation 2.3 actual legislation of electromagnetic power 2.4 The electromagnetic spectrum 2.5 The interplay of electromagnetic power with the ambience 2.6 The interplay of electromagnetic power with the thing surfaces in the world 2.7 function of spectral reflectance cu

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In perspective III, the classification of sensor systems are performed based on the spectral and spatial resolution of the sensors. 9 µm and the spatial resolution which is the smallest size of the object that can be detected by the sensor, is high. Multi-spectral sensors collect information in separate wavelength regions called bands. 16 Components of remote sensing four bands. Hyper-spectral sensors have ability to detect detailed spectral information by providing large number of bands with narrow spectral range.

G. deserts, have the lowest concentrations. As the electromagnetic energy is not directly transferred to the Earth’s surface and some of the wavelengths are blocked by the three gasses, remote sensing, especially passive remote sensing based on solar radiation, uses the wavelengths of the electromagnetic spectrum transferred without absorption. 6). The electromagnetic energy directly passing through atmospheric windows is called transmission. 5 µm coming from the Sun is absorbed by stratosphere due to reaction of oxygen with ultraviolet wavelengths to form ozone.

4. The microwave, infrared, and visible portion of the electromagnetic spectrum is mostly used by the remote sensing sensors in Earth observation. 4. As there is an inverse relation between the energy of the quanta and its wavelength (see Eq. 3) by the implication of Planck’s electromagnetic theory, the higher energy levels are obtained in shorter wavelengths. It is relatively more difficult to sense microwaves emitted from an object on the Earth due to low energy levels. On the other hand, it is easier to detect visible and infrared portion of the electromagnetic spectrum because of the associated higher energy levels.

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