Quelbi Bel Hob Sar Mefni ; Quelbi Bel Hob Sar Mefni (suite) / Laazar Sliman, chant [acc. instr.]

[Traditions. Afrique du Nord. Algérie]

Imaging the ultrasmall-angle x-ray scattering distribution with grating interferometry.

X-ray imaging with grating interferometry has previously been regarded as a technique providing information only in direct space. It delivers absorption, phase, and dark-field contrast, which can be viewed as parameters of the underlying but unresolved scattering distribution. Here, we present a method that provides the ultrasmall-angle x-ray scattering distribution and, thus, allows simultaneous access to direct and reciprocal space information.

Optimized back-focal-plane interferometry directly measures forces of optically trapped particles

Back-focal-plane interferometry is used to measure displacements of optically trapped samples with very high spatial and temporal resolution. However, the technique is closely related to a method that measures the rate of change in light momentum. It has long been known that displacements of the interference pattern at the back focal plane may be used to track the optical force directly, provided that a considerable fraction of the light is effectively monitored. Nonetheless, the practical application of this idea has been limited to counter-propagating, low-aperture beams where the accurate momentum measurements are possible. Here, we experimentally show that the connection can be extended to single-beam optical traps. In particular, we show that, in a gradient trap, the calibration product κ·β (where κ is the trap stiffness and 1/β is the position sensitivity) corresponds to the factor that converts detector signals into momentum changes; this factor is uniquely determined by three construction features of the detection instrument and does not depend, therefore, on the specific conditions of the experiment. Then, we find that force measurements obtained from back-focal-plane displacements are in practice not restricted to a linear relationship with position and hence they can be extended outside that regime. Finally, and more importantly, we show that these properties are still recognizable even when the system is not fully optimized for light collection. These results should enable a more general use of back-focal-plane interferometry whenever the ultimate goal is the measurement of the forces exerted by an optical trap.

Optimized back-focal-plane interferometry directly measures forces of optically trapped particles

Back-focal-plane interferometry is used to measure displacements of optically trapped samples with very high spatial and temporal resolution. However, the technique is closely related to a method that measures the rate of change in light momentum. It has long been known that displacements of the interference pattern at the back focal plane may be used to track the optical force directly, provided that a considerable fraction of the light is effectively monitored. Nonetheless, the practical application of this idea has been limited to counter-propagating, low-aperture beams where the accurate momentum measurements are possible. Here, we experimentally show that the connection can be extended to single-beam optical traps. In particular, we show that, in a gradient trap, the calibration product κ·β (where κ is the trap stiffness and 1/β is the position sensitivity) corresponds to the factor that converts detector signals into momentum changes; this factor is uniquely determined by three construction features of the detection instrument and does not depend, therefore, on the specific conditions of the experiment. Then, we find that force measurements obtained from back-focal-plane displacements are in practice not restricted to a linear relationship with position and hence they can be extended outside that regime. Finally, and more importantly, we show that these properties are still recognizable even when the system is not fully optimized for light collection. These results should enable a more general use of back-focal-plane interferometry whenever the ultimate goal is the measurement of the forces exerted by an optical trap.

Off-axis low-coherence interferometry for surface topology measurement.

In this communication we introduce a low or reduced coherence interferometry technique that can be used to retrieve surface topology on samples with high roughness. Moreover, we will show that the approach enables surface topology measurement also at the interface of so-called turbid media, where multiple scattering inside tissues can be a major issue, preventing accurate measurements.

A two-dimensional doppler-radiometer for earth observation

Compared to synthetic aperture radars (SARs), the angular resolution of microwave radiometers is quite poor. Traditionally, it has been limited by the physical size of the antenna. However, the angular resolution can be improved by means of aperture synthesis interferometric techniques. A narrow beam is synthesized during the image formation processing of the cross-correlations measured at zero-lag between pairs of signals collected by an array of antennas. The angular resolution is then determined by the maximum antenna spacing normalized to the wavelength (baseline). The next step in improving the angular resolution is the Doppler-Radiometer, somehow related to the super-synthesis radiometers and the Radiometer-SAR. This paper presents the concept of a three-antenna Doppler-Radiometer for 2D imaging. The performance of this instrument is evaluated in terms of angular/spatial resolution and radiometric sensitivity, and an L-band illustrative example is presented.

Polarimetric radar interferometry for improved mine detection and surface clutter rejection

A recently developed technique, polarimetric radar interferometry, is applied to tackle the problem of the detection of buried objects embedded in surface clutter. An experiment with a fully polarimetric radar in an anechoic chamber has been carried out using different frequency bands and baselines. The processed results show the ability of this technique to detect buried plastic mines and to measure their depth. This technique enables the detection of plastic mines even if their backscatter response is much lower than that of the surface clutter.

SAR-satelliittien hyödyntäminen merivalvonnassa

Yhteiskunnan eri toimijoiden riippuvuus avaruustoiminnasta on kasvamassa. Satelliittien paikka- ja aikatietojen lisäksi satelliittien valvontakyvyn hyödyntäminen on lisääntymässä. Merivoimat on mukana kansainvälisissä merivalvontahankkeissa, muun muassa Euroopan puolustusviraston johtamassa Maritime Surveillance -hankkeessa, jossa hyödynnetään satelliittien valvontakykyä merialueiden valvonnassa. Tämä tutkimuksen tavoitteena on selvittää miten SAR (Synthetic Aperature Radar) -satelliitteja voidaan hyödyntää merivalvonnassa ja mitkä ovat merivalvonnan tietotarpeet sekä SAR-aineistojen saatavuus.

Länsimaisten SAR/GMTI-tutkien suorituskyky

SAR/GMTI-tutka (Synthetic Aperture Radar/Ground Moving Target Indicator) tuottaa tiedustelutietoa johtamisen, tiedustelun, valvonnan ja maalinosoituksen tueksi. SAR/GMTI -tutka on luotettava tiedusteluväline tutkataajuusalueella tapahtuvan tiedustelutiedon tuottamisen ansiosta, jolloin tutkan käyttö ja tiedustelutiedon tuottaminen onnistuvat huonoissakin sääolosuhteissa. SAR/GMTI-tutkien käyttö on yleistynyt sotilaskäytössä viimeisen kahdenkymmenen vuoden aikana ja niillä on ollut suuri merkitys kaikissa suuremmissa konflikteissa kylmän sodan loppumisen jälkeen. SAR-tutka käyttää lavettina liikkuvaa alustaa, useimmiten lentokonetta, muodostaakseen virtuaalisen antenniryhmän ja signaaliprosessoinnin avulla, jolloin vastaanottimeen palautuvat kaiut sijoitetaan kohdilleen ja muodostetaan SAR-kuvaa. Tarkimmillaan nykyisten SARtutkien resoluutio on muutaman kymmenen senttimetrin luokkaa ja mittausetäisyydet suurimmillaan satoja kilometrejä. GMTI-tutka havaitsee liikkuvat kohteet, kun liikkuvista kohteista palautuvat kaiuilla on eri taajuus kuin ympäröivästä maastosta palautuvilla kaiuilla ja kohteet pystytään erottelemaan välkkeen seasta. GMTI-tutkan toiminta perustuu doppler-ilmiöön. SAR-tutkaa pystytään useimmiten käyttämään GMTI-moodissa. Sotilaskäytössä olevat GMTI-tutkat pystyvät havaitsemaan keskimäärin noin henkilöauton kokoisen maalin, joka liikkuu noin 5 km/h nopeudella. SAR/GMTI-tutkia on käytetty menestyksellisesti molemmissa Irakin sodissa Yhdysvaltojen toimesta, kun tasainen aavikko ei aiheuttanut juurikaan ongelmia alueen valvontaan ilmasta käsin. Sen sijaan haasteita SAR/GMTI-tutkille ovat aiheuttaneet operaatiot Balkanilla ja Afganistanissa korkean vuoriston, peitteisen maaston ja kohteiden hankalan tunnistettavuuden takia. Suoraan taistelun tukemiseen liittyen GMTI-tutkat ovat olleet hyödyllisiä, kun valvontakoneilta saadut tiedot liikkuvista vihollisosastoista on voitu lähettää datalinkkien kautta lähestulkoon reaaliajassa. SAR-tutkat ovat olleet hyödyllisiä ennen taisteluiden alkua tiedustelutiedon keräämisessä ja vaikeakulkuisessa maastossa SAR-tutkia on käytetty esimerkiksi taisteluvaikutuksen jälkiarviointiin. SAR/GMTI-tutkien suorituskyky kehittyy jatkuvasti laitteiden resoluution ja koon pienentyessä. Datalinkeillä voidaan välittää tietoa alajohtoportaille ja SAR/GMTI-tutkia on voitu sijoittaa esimerkiksi UAV-lennokkeihin (Unmanned Aerial Vehicle), joilla on voitu suorittaa tarkempaa aluevalvontaa kuin mitä isomman kokoluokan valvontakoneilla voitaisiin toteuttaa.

Development of hypogene and supergene alteration and copper mineralization patterns, Sar Cheshmeh porphyry copper deposits, Iran /

The formation of the Sar Cheshmeh porphyry Cu-Mo deposit is related to the culmination of calc-alkaline igneous activity in the Kerman region. The deposit comprises a suite of Late Cenozoic intrusive sub-volcanic and extrusive rocks emplaced into a folded series of Eocene andesitic lavas and pyroclastic sediments. The earliest stage of magmatism was emplacement of a large granodiorite stock about 29 m.y.b.p. This was followed by intrusion of two separate porphyritic bodies at 15 (Sar Cheshrneh porphyry) and 12 m.y.b.p. (Late porphyry) and a series of sub-volcanic dikes between 12 and 9 m.y.b.p. Magmatic activity terminated with multi-phase extrusion of a Pelean dacitic dome complex between 10 and 2.8 m.y.b.p. The country rocks and the earlier porphyritic intrusions are pervasively altered to biotite-rich potassium silicate (metasomatic and hydrothermal) sericite-clay, phyllic and chlorite-clay, argillic assemblages. These grade outwards to an extensive propylitic zone. Within the ore body, the later intra-. and post-mineral dikes only reach the propylitic grade. At least three different sets of quartz veins are present, including a sericite-chlorite-quartz set which locally retrogrades pervasive secondary biotite to sericite. In the hypogene zone, metasomatic and hydrothermal alteration is related to all stages of magmatism but copper mineralization and veining are restricted to a period of 15 to 9 m.y.b.p.related to the early intrusive phases. The copper mineralization and silicate alteration do not fit a simple annular ring model but have been greatly modified by, 1. The existence of an ititial, outer ring, of metasomatic alteration overprinted by an inner.ring of hydrothermal alteration and, 2. later extensive dilating effects of intra- and post-mineral dikes. The hydrothermal clay mineral assemblage in the hypogene zone is illite-chlorite-kaolinite-smectite (beidellite). Preliminary studies indicate that the amount of each of these clays varies vertically and that hydrothermal zonation of clay minerals is possible. However, these minerals alter to illite-kaolinite assemblages in the supergene sulfide zone and to more kaolinite-rich assemblages in the supergene leached zone. Hydrothermal biotite breaks down readily in the supergene zone and is not well preserved in surface outcrops. The distribution of copper minerals in the supergene sulfide enrichment zone is only partly related to rock type being more dependent on topography and the availability of fractures.

Femtosecond wavepacket interferometry using the rotational dynamics of a trapped cold molecular ion

A Ramsey-type interferometer is suggested, employing a cold trapped ion and two time-delayed offresonant femtosecond laser pulses. The laser light couples to the molecular polarization anisotropy, inducing rotational wavepacket dynamics. An interferogram is obtained from the delay dependent populations of the final field-free rotational states. Current experimental capabilities for cooling and preparation of the initial state are found to yield an interferogram visibility of more than 80%. The interferograms can be used to determine the polarizability anisotropy with an accuracy of about ±2%, respectively ±5%, provided the uncertainty in the initial populations and measurement errors are confined to within the same limits.

Educación y compromiso : el IES de Sar responde ante la catástrofe del Prestige y la guerra contra Irak.

El artículo forma parte de un monográfico de la revista dedicado a educación ambiental en tiempos de catástrofes

Using airborne laser altimetry to improve river flood extents delineated from SAR data

Flood extent maps derived from SAR images are a useful source of data for validating hydraulic models of river flood flow. The accuracy of such maps is reduced by a number of factors, including changes in returns from the water surface caused by different meteorological conditions and the presence of emergent vegetation. The paper describes how improved accuracy can be achieved by modifying an existing flood extent delineation algorithm to use airborne laser altimetry (LiDAR) as well as SAR data. The LiDAR data provide an additional constraint that waterline (land-water boundary) heights should vary smoothly along the flooded reach. The method was tested on a SAR image of a flood for which contemporaneous aerial photography existed, together with LiDAR data of the un-flooded reach. Waterline heights of the SAR flood extent conditioned on both SAR and LiDAR data matched the corresponding heights from the aerial photo waterline significantly more closely than those from the SAR flood extent conditioned only on SAR data.