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Texture strengthening and fracture toughness of titanium alloy sheets biaxial stress fields at room and cryogenic temperatures
Detection and scaling of statistical differences between visual texture
Texture strengthening and fracture toughness of titanium alloy sheet at room and cryogenic temperatures
Texture strengthening and fracture toughness of titanium alloy sheets biaxial stress fields at room and cryogenic temperatures
Results from studies of highway grooving and texturing at NASA Wallops Station
Results from studies of highway grooving and texturing by several state highway department
Relict diagenetic textures and structures in regional metamorphic rocks, northern Michigan
Subjects sensitivity to differences in statistical distributions of locally defined element density and shape, using stochastically textured visual patterns
Characterizing ancient tephra units on Surtsey by textural analysis of modern pyroclastic and hydroclastic deposits
Discriminator algorithm for computer pattern generation and texture recognition
Mesosiderites silicate textures and compositions and metal-silicate relationships from mineralogical, petrographical and chemical data
Lunar rocks 12063,9 and 12004,11 opaque mineralogy and textural feature, comparing to apollo 11 samples
Lunar anorthosite 15415 consists almost entirely of anorthite (homogeneous anorthite 96.6 molecule percent), with accessory diopsidic augite and traces of hypersthene, ilmenite, and a silica mineral. The rock has had a complex metamorphic history. The texture reflects at least two episodes of shearing (followed by intense and partial recrystallization, respectively), one episode of cataclastic deformation, and one or more episodes of shattering and fragmentation.
We report the production of (111) epitaxial Pb films on mica and (111) textured Pb films on mica and glass. Film structure is studied by reflection electron diffraction and by etching and optical microscopy. Thin (about 1000 A) epitaxial films are found to be doubly positioned. Reorientation during growth of thicker films leads to single positioning in areas several tenths of a millimeter across.
An experiment was performed in an attempt to evaluate autocorrelation as an indicator of texture using five small patches representing varying distances on each of four lunar photos. Each patch was scanned at 50 micron increments on a 64-level gray scale. Several problems were involved in using the ordinary autocorrelation value but a rougher autocorrelation measure, the percentage of neighboring pairs (at a given lag distance) which fell within one graylevel of one another, yielded very encouraging results. As the distance to the feature decreased, initial slope of the graph of percentage against lag increased, and the general level of the graph decreased. When a crestline was present, the graph tended to continue to decrease at higher lags as well, rather than leveling off after the initial steep slope.
The author has identified the following significant results. The land use category of subimage regions over Kansas within an MSS image can be identified with an accuracy of about 70% using the textural-spectral features of the multi-images from the four MSS bands.
Experiments seem to indicate that at the low pressures characteristic of an ejecta blanket, sintering or sintering/devitrification could have lithified boulder 1 matrix materials and produced the textural types observed in 72255 and 72275. This very preliminary conclusion is consistent with other observations that granitic clasts have undergone a slight degree of partial melting (and have therefore experienced temperatures on the order of 1000 C). It is concluded that maskelynite in the boulder is completely devitrified.
Review was made of past models for describing the reflectance and/or emittance properties of agricultural/forestry and geological targets in an effort to select the best theoretical models. An extension of the six parameter Allen-Gayle-Richardson model was chosen as the agricultural plant canopy model. The model is used to predict the bidirectional reflectance of a field crop from known laboratory spectra of crop components and approximate plant geometry. The selected geological model is based on Mie theory and radiative transfer equations, and will assess the effect of textural variations of the spectral emittance of natural rock surfaces.