2 edition of Spectral reflectance characteristics of rock varnish in arid areas. found in the catalog.
Spectral reflectance characteristics of rock varnish in arid areas.
Kevin White
Published
1990
by University of Oxford School of Geography in Oxford
.
Written in
Edition Notes
| Series | Research papers / University of Oxford School of Geography -- 46 |
| Contributions | University of Oxford. School of Geography. |
| The Physical Object | |
|---|---|
| Pagination | 38p. : |
| Number of Pages | 38 |
| ID Numbers | |
| Open Library | OL13921179M |
Mainguet, M. Conséquences géomorphologiques de l'action du vent dans les régions de dunes en zones arides et semi-arides (Geomorphological consequences of aeolian action in dune areas in arid and semi-arid regions). Geneva: World Meteorological Organization (WMO), WCP , WMO-TD 49, pp. (in French) Mainguet, M. Implications of a sandblasting model for dust production by wind erosion in arid areas. In: Skidmore, E.L. and Tatarko, J. (eds), Wind Erosion - Proceedings of an International Symposium/Workshop, June , Manhattan, Kansas.
Fig. V-I characteristics of p-n junction diode. (i) Circuit diagram (ii) Characteristics The V-I characteristics of a semiconductor diode can be obtained with the help of the circuit shown in fig. (i) The supply voltage V is a regulated power supply, the diode is forward biased in the circuit shown. The resistor R is a current limiting. identification of the environmental characteristics of urban areas as a factor of formation of real estate prices; prospects of implementation of the practice of "green office" or "sustainable office" in russia. indications of megalithic culture on the island of bali in indonesia; interactive visualization tool – invito for sustainable planning.
correlations and regression mathematical to etablish the geomechanical characteristics of magmatic rock in south apuseni CREATION AND PROTECTION OVER INCRUSTATION AND RUSTING ON THE HOT-WATER PIPELINE DURING USING OF GEOTHERMAL WATER FROM DURKOV AT THE GTD-1, 2, 3 DRILL HOLES. unique characteristics of the land we are managing. unrepresentative high disturbance areas); (2) no plots on rock outcrops or slopes greater than 50 percent (these areas are unlikely to be In most arid and semi-arid areas, ft2 is the best size. As production and plant density.
Ellen Tebbits
Stamp collecting
ZR rifle
Canadian/American sport, fitness, and the law
Steam in Northern Ontario
Research on the institutional contexts of wildlife utilization in communal areas of eastern and southern Africa
Sprout It
Wheel throwing
Truman
The holy earth
Partial Differential Equations
Prophets without honour
Dissident Democrats
Regional development in north-western New South Wales.
Additional Physical Format: Online version: White, Kevin. Spectral reflectance characteristics of rock varnish in arid areas. Oxford [England]: School of Geography, University of Oxford, These weathering processes alter the shape, overall reflectance values, and certain absorption characteristics of different rock types in arid and semi-arid environments.
Weathering processes result in the formation of new materials that differ both chemically and mechanically from the original parent rock [ 13, 42 ].Cited by: 2. Abstract. Alluvial fans are semi-conical landforms composed of stream deposits and debris flow materials where a canyon exits a mountain range.
Alluvial fans are built in semi-arid, humid-temperate, and proglacial regions (RachockiNilsen and Moore ), but they have been studied more in deserts than in any other environment (BullGraf ).Cited by: The effects of grain size variations on rock and mineral reflectance spectra and of solid surfaces versus powders have been the topic of numerous studies.
Other spectral characteristics (such. The steeper profiles of the reflectance curves observed for weathered surfaces may be attributed to the formation of rock coatings and varnish, which are commonly encountered in semiarid to arid.
The 12 geologic end members can be grouped into (1) peridotites, (2) iron oxide and/or hydroxide weathering, (3) clastic metasediments, (4) carbonate rocks, (5) lichen-rock mixtures, and (6) varnish, based on spectral features (e.g.
Fe2+, Fe3+, Fe-OH, Mg-OH, Al-OH, CO3) and comparisons with field and laboratory spectra. Spectral measurements.
Proc. SPIEGeology from Space, pg 2 (30 December ); doi: / For the purposes of this chapter, the transect across the roof of the world illustrates a serious flaw in attempts to map geographical variability in rock coatings.
Asymmetry in Rock Coatings and Landscape Aesthetics Rock coatings are ubiquitous in both the cool and wet Khumbu of Nepal and the cold and dry West Kunlun Mountains of Tibet.
The varnish coating, which can mask the spectral response of the rock's mineral assemblages, strongly depends on weathering and erosion characteristics modulated by rock mineralogy and texture (Rivard et al., ).
The foliated metaturbidites are generally covered by a surface regolith composed of varnished platy-like slabs, detached from the Cited by: For each spectral sample location, three spectral measurements were collected over a 1 m 2 target area.
Each spectral measurement was the average of 50 sampled spectra, acquired under clear skies between two hours before and two hours after local noon. The field of view was set at 8° and the sensor head located 1 m above the by: 6.
Ogawa, K., S. Rokugawa, T. Matsunaga and Y. Ninomiya. Evaluation of thickness of desert varnish coatings on rock using thermal infrared remote sensing.
Measurements of thermal infrared spectral reflectance of frost, snow, and ice. Journal of Geophysical Research, 99(B12): Remote Sensing of Urban Areas, Regensburger. Simone De Angelis, Paola Manzari, Maria Cristina De Sanctis, Francesca Altieri, Cristian Carli and Giovanna Agrosì, Application of spectral linear mixing to rock slabs analyses at various scales using Ma_Miss BreadBoard instrument, Planetary and Space Science, /,(), ().Cited by: White, K.,Spectral reflectance characteristics of rock varnish in arid areas, School of Geography University of Oxford Research Paper 1– Google Scholar White, K., a, Image processing of Thematic Mapper data for discriminating piedmont surficial materials in the Tunisian Southern Atlas, International Journal of Remote Sensing Cited by: The spectroscopy of minerals is based on decades of published research [3,4,5,6,7,8,9,10,11,12,13,14,15,16,17,18,19,20], which have highlighted those wavelength regions where specific minerals and mineral groups possess diagnostic features, including: (i) the Visible and Near-InfraRed (VNIR, to nm)—transition element-bearing Cited by: 9.
Full text of "Imaging spectrometry [electronic resource]: basic principles and prospective applications" See other formats. AVIRIS spectral trajectories for forested areas of Gifford Pinchot National Forest, Proc.
5th Airborne Visible/Infrared Imaging Spectrometer (AVIRIS) Workshop, Vol. 1., Jet Propulsion Laboratory PublicationJet Propulsion Laboratory, Pasadena, CA., Spectral mixing is a problem inherent to remote sensing data and results in fewimage pixel spectra representing "pure" targets.
Linear spectral mixture analysis isdesigned to address this problem and it assumes that the pixel-to-pixel variability in ascene results from varying proportions of spectral endmembers. In this paper we present adifferent endmember-search algorithm Cited by: Ogawa, K., S. Rokugawa, T.
Matsunaga, and Y. Ninomiya () Evaluation of thickness of desert varnish coatings on rock using thermal infrared remote sensing, Remote Sensing Society of Japan, 19(1): Full text of "Nature and origin of secondary mineral coatings on volcanic rocks of the Black Mountain, Stonewall Mountain, and Kane Springs Wash.
16 book catalog arid zone irrigation s6i3.y3 yakon bruno a danfors e ed ecological studies v 5 irrigation arid regions agrlicultxjre 03b 06b springer verlao art lessons that teach children about their natu- ral environment np37 parker peck ruth l art study & teaching human ecology 03b art of administration hdt38 tead.
The lowland between the rivers supports rich pasturage. It features arid to sub-arid savanna, open woodland, and thickets that include frequently abundant underlying grasses. There are areas of grassland, and in the far southwest, near the .Lunar Earth PBr 11 I Lunar Red Rock PR I Lunar Violet PV 15, PBk 11 I Manganese Blue Hue PB 15 II Mars Yellow PY 42 I Mayan Dark Blue PB 82 II Mayan Orange PO N/A II Mayan Red PR II Mayan.Though that's not the focus of this book, I should just touch on it briefly, in a few pages, because if I don't many of you will have this as one of the top questions on your mind.
I want this book to have a positive message, and to do what I can to help us to find the way to a future that is inspiring and worthwhile.
