Academic literature on the topic 'Optically Stimulated Luminescence (OSL)'

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Journal articles on the topic "Optically Stimulated Luminescence (OSL)"

1

West, William Geoffrey, and Kimberlee Jane Kearfott. "Optically Stimulated Luminescence Dosimetry: An Introduction." Solid State Phenomena 238 (August 2015): 161–73. http://dx.doi.org/10.4028/www.scientific.net/ssp.238.161.

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A subset of solid state materials have long been used as integrating dosimeters because they store energy deposited as a result of their interactions with ionizing radiation and then, when stimulated appropriately, release a proportionate amount of visible or near-visible light. During the 1960s, thermoluminescent dosimeters (TLDs), for which heat is used to extract the stored dosimetric signal, began to replace the photographic film as occupational dosimeters of record and for medical dosimetry. At the end of the twentieth century, a viable optically stimulated luminescent (OSL) material was developed which is now gaining in popularity as both an occupational and medical dosimeter. This paper reviews the related stored luminescence processes, presenting a simple conceptual model for optical absorption transitions in OSL materials along with a basic mathematical model for delayed luminescence. The approaches for extracting signal from the OSLs are enumerated.
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Tamura, Toru. "Optically Stimulated Luminescence (OSL) Dating." RADIOISOTOPES 70, no. 3 (March 15, 2021): 107–16. http://dx.doi.org/10.3769/radioisotopes.70.107.

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Nakagawa, Kohei, Hiroaki Hayashi, Hiroki Okino, Kazuki Takegami, Tohru Okazaki, and Ikuo Kobayashi. "Fabrication of Annealing Equipment for Optically Stimulated Luminescence (OSL) Dosimeter." Japanese Journal of Radiological Technology 70, no. 10 (2014): 1135–42. http://dx.doi.org/10.6009/jjrt.2014_jsrt_70.10.1135.

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Yukihara, E. G., and S. W. S. McKeever. "Optically stimulated luminescence (OSL) dosimetry in medicine." Physics in Medicine and Biology 53, no. 20 (September 17, 2008): R351—R379. http://dx.doi.org/10.1088/0031-9155/53/20/r01.

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Ito, Kazumi. "Optically Stimulated Luminescence (OSL) Dating of Sediments." RADIOISOTOPES 70, no. 3 (March 15, 2021): 147–57. http://dx.doi.org/10.3769/radioisotopes.70.147.

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6

Yukihara, Eduardo G. "Luminescence properties of BeO optically stimulated luminescence (OSL) detectors." Radiation Measurements 46, no. 6-7 (June 2011): 580–87. http://dx.doi.org/10.1016/j.radmeas.2011.04.013.

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7

KITIS, G., C. FURETTA, and V. PAGONIS. "MIXED-ORDER KINETICS MODEL FOR OPTICALLY STIMULATED LUMINESCENCE." Modern Physics Letters B 23, no. 27 (October 30, 2009): 3191–207. http://dx.doi.org/10.1142/s0217984909021351.

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The theory of mixed-order kinetics is well-established for the description of single thermoluminescence (TL) glow-peaks. The main advantage of mixed-order kinetics relative to the more widely used general-order kinetic theory is that the former is physically meaningful whereas the latter is entirely empirical. In the case of optically stimulated luminescence (OSL) either non-first-order or second-order kinetics are studied using the empirical general-order kinetics theory. In the present work, expressions for mixed-order kinetics are derived for OSL curves. A peak shape parameter for linear modulation OSL is developed and special mixed-order expressions are derived for use in the computerized OSL curve deconvolution analysis.
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8

Gaikwad, S. U., R. R. Patil, M. S. Kulkarni, C. M. Dudhe, and S. V. Moharil. "DEVELOPMENT OF NACL-BASED OPTICALLY STIMULATED LUMINESCENT PHOSPHORS FOR THE POSSIBLE APPLICATIONS IN DOSIMETRY." Radiation Protection Dosimetry 192, no. 1 (October 2020): 27–35. http://dx.doi.org/10.1093/rpd/ncaa184.

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Abstract New highly sensitive optically stimulated luminescent phosphors with NaCl moiety and dopants Ca,Cu,P/Mg,Cu,P are developed. These phosphors show very high optically stimulated luminescence (OSL) sensitivity. The dose response for NaCl:Ca,Cu,P is linear up to 1.2 Gy and for NaCl:Mg,Cu,P is slightly sub linear from 0.2 Gy. These phosphors show 30% fading during first 4 and later signal gets stabilised with no further signal loss. These sensitive phosphors will find applications in radiation dosimetry using OSL.
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9

Sawakuchi, André Oliveira, Fernanda Costa Gonçalves Rodrigues, Thays Desiree Mineli, Vinícius Ribau Mendes, Dayane Batista Melo, Cristiano Mazur Chiessi, and Paulo César Fonseca Giannini. "Optically Stimulated Luminescence Sensitivity of Quartz for Provenance Analysis." Methods and Protocols 3, no. 1 (January 13, 2020): 6. http://dx.doi.org/10.3390/mps3010006.

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Finding the source or provenance of quartz grains occurring in a specific location allows us to constrain their transport pathway, which is crucial information to solve diverse problems in geosciences and related fields. The optically stimulated luminescence (OSL) sensitivity (light intensity per unit mass per unit radiation dose) has a high capacity for discrimination of quartz sediment grains and represents a promising technique for provenance analysis. In this study, we tested the use of quartz OSL sensitivity (ultraviolet emission) measured under different preheating temperatures and with blue light stimulation at room temperature (~20 °C) for sediment provenance analysis. Quartz OSL sensitivity measured at 20 °C is positively correlated with the sensitivity of an OSL signal measured using procedures (preheat at 190 °C for 10 s, blue stimulation at 125 °C and initial 1 s of light emission) to increase the contribution of the fast OSL component, which has been successfully applied for sediment provenance analysis. The higher OSL signal intensity measured without preheating and with light stimulation at room temperature allows the use of lower given doses, thus reducing measurement time. Additionally, the OSL sensitivity measured at 20 °C in polymineral silt samples of a marine sediment core is also suitable for provenance analysis, as demonstrated by comparison with other independent proxies. OSL signals obtained through light stimulation at room temperature have thus the potential to considerably expand measurement possibilities, including in situ measurements using portable OSL readers.
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Tani, A., C. Yamanaka, M. Ikeya, O. Ohtaka, M. Takada, and T. Katsura. "Optically stimulated luminescence (OSL) study of synthetic stishovite." Radiation Measurements 32, no. 5-6 (December 2000): 473–77. http://dx.doi.org/10.1016/s1350-4487(00)00116-5.

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Dissertations / Theses on the topic "Optically Stimulated Luminescence (OSL)"

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Kusoglu, Sarikaya Cemre. "Optically Stimulated Luminescence Studies On Natural Fluorites." Master's thesis, METU, 2011. http://etd.lib.metu.edu.tr/upload/12612962/index.pdf.

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Optically Stimulated Luminescence (OSL) is the luminescence emitted from a previously irradiated insulator (or a wide band gap semiconductor) upon exposure to light. The OSL signal intensity is a function of the radiation dose absorbed by the sample and thus can be used as the basis of a radiation dosimetry method. In the literature, OSL studies on natural fluorites are rather limited. In order to promote the material for radiation dosimetry, OSL properties of natural fluorites of different origin were examined in this study. For this purpose, dose-response, reproducibility, thermal stability and fading of the OSL signals were analyzed. In order to find a relation between OSL and TL signals, TL signals and the effect of OSL measurements on TL signals were examined. Thermal activation energies of the light sensitive TL peaks and the OSL signals were also calculated using different methods and the results were compared. Also, absence of the thermal quenching was shown. Finally, TR-OSL signals were measured to have an opinion about the recombination centers. As a result of these studies, it is possible to conclude that natural fluorites show promising features to be used as an environmental dosimeter with regard to a suitable OSL signal, range of linearity, repeatability in response, as well as being readily available at a low cost.
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Yeltik, Aydan. "Time-resolved Optically Stimulated Luminescence (osl) Studies On Samples Containing Quartz And Feldspar." Master's thesis, METU, 2009. http://etd.lib.metu.edu.tr/upload/3/12611103/index.pdf.

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Time Resolved OSL (TR-OSL) is a technique to record the luminescence decay curve data after a brief stimulation pulse and can possibly be used for the separation of luminescence signals from quartz and feldspars. In this study luminescence emission from quartz and feldspar samples was investigated. TR-OSL signals of these samples were studied for the variations with preheating and annealing temperature, stimulation pulse width and total stimulation time, optical bleaching, radiation dose and measurement temperature. TR-OSL decay lifetime of quartz samples was found as ~40 µ
s. Na-feldspar and K-feldspar luminescence signals were deconvoluted using a linear sum of three exponential decays with lifetimes about 45 µ
s, 8 µ
s and 1 µ
s and about 35 µ
s, 7 µ
s and 0.6 µ
s, respectively. Since feldspars signals have a component with lifetime similar to that of quartz (~40 µ
s), luminescence signal separation with TR-OSL seems to be not straightforward.
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Demirturk, Tayfun. "Dating Of Laodikeia (denizli) Building Ceramics Using Optically Stimulated Luminescence (osl) Techniques." Phd thesis, METU, 2006. http://etd.lib.metu.edu.tr/upload/12607746/index.pdf.

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The objective of this study is to perform Optically Stimulated Luminescence (OSL) dating on the ceramic samples from different parts of the Laodikeia by using Infra Red Stimulated Luminescence (IRSL) on polyminerals. As a first step, a literature survey has been done about the dating system and the methodology of dating. The calibration of the system was done before carrying out the experiments. The six ceramic samples were collected from the site and dated. The mineral compositions of the samples were examined by X-ray Diffraction Analysis, which showed that all samples contain quartz, feldspars, calcites and together with other minerals. The equivalent dose was found by using Multiple Aliquot Additive Dose (MAAD) and Multiple Aliquot Regenerative Dose (MARD) techniques using Infra Red diode array of the system that gave the IRSL ages for samples. Alpha counter measured the dose components of uranium and thorium contributions to the annual dose. The potassium concentration was determined by Atomic Emission Spectrometry. The cosmic ray component of annual dose was evaluated by the Al2O3:C Thermoluminescence Dosimeter (TLD) discs which have been placed and kept for 8 and 11 months in the site. From the data the IRSL ages were calculated for six ceramic samples LDKY-1, LDKY-2, LDKY-3, LDKY-4, LDKY-5 and LDKY-6 with the help of the OSL system software. The IRSL ages for these samples, in the given order, are 737 ±
60, 1563 ±
120, 1445 ±
110, 1602 ±
120, 1034 ±
80 and 1034 ±
80 years by using MAAD technique. The IRSL ages for the same samples are 870 ±
60, 1550 ±
120, 1440 ±
110, 1600 ±
120, 1030 ±
80 and 1030 ±
70 years by using MARD technique.
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余耀良 and Yiu-leung Yieu. "OSL dating of sediment and climate change of late quaternary." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2013. http://hdl.handle.net/10722/192989.

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The objective of this project is to apply the Optical Stimulated Luminescence (OSL) technique to date the palaeo sediment from Mu Us Desert, part of the Inner Mongolia in northern China and reconstruct the palaeo environment. Five OSL samples were collected from Dagouwan, Salawusu River Valley at Inner Mongolia by Dr S. H. Li and his team in 2009. Extraction of 150μm to 180μm silt-size feldspar from collected dune sand, lacustrine facies and fluvial facies samples and running of luminescence dating therefore to obtain the age from 50ka to 90ka. Climate proxies - magnetic susceptibility, grain size, fossil vertebrates and fossil pollens have been analyzed and it is concluded that significant climate change occurred within this period, which change from domination of warm, humid and rainy summer monsoons (before 70ka) to cold, wind, windy strengthened dry winter wind and back to warm and humid again after 55ka.
published_or_final_version
Applied Geosciences
Master
Master of Science
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5

Summa, Michelle Carlene. "Geologic Mapping, Alluvial Stratigraphy, and Optically Stimulated Luminescence Dating of the Kanab Creek Area, Southern Utah." DigitalCommons@USU, 2009. https://digitalcommons.usu.edu/etd/506.

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At the turn of the century, Kanab Creek incised 30-meters into its alluvium, leaving behind fluvial terraces and thick basin fill sediments exposed along arroyo walls. Research objectives were to determine the timing and causes of past valley-filling and arroyo-cutting episodes along a 20 km-long reach of Kanab Creek in southern Utah. Fluvial deposits were mapped at the 1:12,000 scale and sediments were described and dated using Optically Stimulated Luminescence (OSL) and radiocarbon dating. The Kanab Creek valley can be divided into a narrow, upper terraced reach and a broad lower basin fill reach near Kanab, Utah. The most prominent terrace in the upper reach is Quaternary alluvial terrace 4 (Qat4), followed by Qat3, Qat2/3, and Qat2 map units. These are composed of tabular-bedded, fine-grained sand, silt, and clay layers. The Qat2/3 map unit is a both a fill and fill-cut terrace underlain by Qa4, Qa3, and Qa2 alluvium and is used when the Qat3 fill-cut (fill-strath) terrace can not be differentiated from the Qat2 fill terrace due to their similar geomorphic position. The Qat3 fill-cut terrace upstream correlates to ~8 meters of aggradation downstream. The youngest terrace, Qat1, is a minor terrace, composed of coarse-grained channel facies. More recent channel and floodplain deposits were deposited over the last century following arroyo cutting. OSL and radiocarbon results suggest at least four cycles of fluvial cutting and filling: >6-3.5ka (Qa4), ~3->1ka (Qa3), 0.7-0.12ka (Qa2), and post-1880 AD (Qa1). Correlation to regional climate records suggests major periods of aggradation correlate to regionally cooler and wetter climatic intervals. Periods of arroyo cutting occurred at >6ka, ~3ka, 1-0.7ka, and during historic arroyo cutting (1882-1914 AD), and correlate to regionally warmer, drier intervals. These periods of aggradation and incision are roughly contemporaneous with regional drainages, except for the large aggradation seen in Kanab Creek 6-3.5ka (Qa4). Analysis of terrace longitudinal profiles indicates Qat4 has the lowest concavity suggesting that Qat4 aggraded during a period of greater sediment supply and/or reduced flood regime. Although OSL samples exhibited some degree of incomplete zeroing, calculated ages using a minimum age model are consistent with radiocarbon results.
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Fan, Anchuan, and 范安川. "Quartz OSL dating of quaternary sediments from China." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2010. http://hub.hku.hk/bib/B45700187.

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Togay, Evren. "Design And Implementation Of A Luminescence Emission Spectrometer." Master's thesis, METU, 2012. http://etd.lib.metu.edu.tr/upload/12614144/index.pdf.

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Luminescence is the emission of light resulting from radiative transition of an atom from an excited state to a ground state. This radiative transition yields emission of photons and the luminescence is the general name which is used to classify &ldquo
cold emission&rdquo
other than the blackbody radiation. Spectroscopy involves the measurement of intensity of emitted, absorbed or scattered electromagnetic radiation as a function of wavelength. Thus, it is a valuable tool in the study of understanding the luminescence production mechanisms. Measurement of emission spectra gives information about the energy levels of transition and structure, geometry and composition of the sample. In this study, a versatile luminescence emission spectrometer was designed and developed with the main aim of measuring Photoluminescence (PL), Thermoluminescence (TL) and Optically Stimulated Luminescence (OSL) emission spectra of materials relevant for dosimetry. The spectrometer was constructed around a Littrow type monochromator by developing the necessary hardware, firmware and software. Wavelength calibration, measurement of spectral response and determination of resolution of the spectrometer were done using calibration lamps and a calibrated spectroradiometer. Finally the performance of the constructed spectrometer was tested by measuring the emission spectra of materials such as BeO, Al2O3 and CaF2 wherever possible the measured spectra were compared with the ones reported in the literature.
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Ng, Sin-pan, and 吳善斌. "OSL dating of palaeoshorelines of saline lakes at Inner Mongolia." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2011. http://hub.hku.hk/bib/B46732883.

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Aygun, Sukran Gizem. "Detection Of Gamma Irradiated Spices With Osl Method And Its Reliability." Master's thesis, METU, 2010. http://etd.lib.metu.edu.tr/upload/12612333/index.pdf.

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The aim of this current work is to analyze the behavior of OSL (Optically Stimulated Luminescence) signals of irradiated spices with respect to time, temperature, origin and the type. Throughout the experiments, 3 different type spices from four different origins were stored at 4°
C and 25°
C for six months after irradiation. During experiments, unirradiated red pepper, thyme and cumin samples were analyzed by using OSL technique in order to determine the background OSL signal values of samples. Samples were irradiated 10 kGy by Cobalt 60 gamma source in TAEK (Turkey Atomic Energy Association). After irradiation process, OSL signal values of different samples were analyzed according to the given parameters. In order to determine the effect of temperature on OSL signal loss, temperature (4°
C- 25°
C) was set as storage temperature. The analyses were made monthly. According to the statistical analyses (ANOVA- General Linear Model), origin and type of samples were detected as significant parameters of design experiment. Time and temperature effect on OSL signal loss changed with respect to origin and type of samples. After six months storage period, OSL signal was lost for most of the origin and sample type. At the end of sixth month, an ESR analysis was performed to detect the accuracy of the OSL technique. With respect to the results of these experiments, it was seen that, due to optical fading, most of the samples was observed as unirradiated by OSL technique, however ESR analyze the samples as irradiated at the end of sixth month. Irradiation had a detrimental effect on the microbiological load of the samples and resulted 6 log reduction on the microbial population. After irradiation, no colony formation was observed in total bacteria and yeast- mold count. During six month period, no injury recovery was observed.
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Hayden, Anne E. "Reconstructing the Holocene Arroyo History of the Upper Escalante River, Southern Utah, Using Optically Stimulated Luminescence (OSL) and Radiocarbon Dating." DigitalCommons@USU, 2011. https://digitalcommons.usu.edu/etd/1105.

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Arroyos are steep-walled, entrenched, typically ephemeral streams commonly found in dryland river systems that form when streams incise into previously deposited alluvial fill. Arroyos in the southwestern U.S. have been studied extensively following the historic period of arroyo cutting in the late 1800s and early 1900s A.D. The upper Escalante River in south-central Utah similarly began incising in 1909, and records evidence for past cut and fill cycles in well-exposed walls along the now continuous arroyo. Establishing robust geochronologies of past arroyo cycles in these fluvial settings has been difficult. Recent improvements in accelerator mass spectrometry (AMS) radiocarbon (14C) and optically stimulated luminescence (OSL) dating provide an opportunity to link more highly resolved fluvial records to existing paleoclimate records. This allows hypotheses regarding the causes of arroyo cycles to be tested, and for the role of climate versus intrabasinal characteristics to be examined. One major objective of this research was to examine the applicability of OSL and AMS 14C dating in the upper Escalante, as both methods have proved problematic in similar settings. In total, 37 ages were obtained, 21 OSL and 16 14C ages. The Holocene fluvial history of the upper Escalante River was reconstructed using these age results and stratigraphic relationships. The chronostratigraphic record developed in this study suggests that at least six arroyo cycles have occurred in the upper Escalante since the middle Holocene, with incision occurring ~4.4 – 4.2 ka, ~2.6 – 2.4 ka, ~1.8 – 1.5 ka, ~1.0 – 0.9 ka, ~0.5 - 0.4 ka, and during the historic period of arroyo entrenchment. While semi-synchronous arroyo cutting (indicative of a climate signal) appears to have occurred in the Paria and Escalante drainages over the last 1 ka, correlations between proximal drainages are less clear prior to 1 ka, although this may be due in part to preservation effects. Overall, linkages to specific climate regimes and correlations to regional drainages are difficult to identify, suggesting that internal geomorphic thresholds are important in determining when arroyo entrenchment occurs in individual catchments.
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Books on the topic "Optically Stimulated Luminescence (OSL)"

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Yukihara, Eduardo G., and Stephen W. S. McKeever. Optically Stimulated Luminescence. Chichester, UK: John Wiley & Sons, Ltd, 2011. http://dx.doi.org/10.1002/9780470977064.

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McKeever, S. W. S., 1950- and Wintle A. G, eds. Optically stimulated luminescence dosimetry. Amsterdam: Elsevier, 2003.

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Chen, Reuven, and Vasilis Pagonis. Thermally and Optically Stimulated Luminescence. Chichester, UK: John Wiley & Sons, Ltd, 2011. http://dx.doi.org/10.1002/9781119993766.

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Yukihara, Eduardo G. Optically stimulated luminescence: Fundamentals and applications. Chichester, West Sussex: Wiley, 2011.

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Chen, R. Thermally and optically stimulated luminescence: A simulation approach. Chichester, West Sussex, UK: Wiley, 2011.

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Questions and answers on thermoluminescence and optically stimulated luminescence. Hackensack, N.J: World Scientific, 2008.

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Wallinga, Jakob. The Rhine-Meuse system in a new light: Optically stimulated luminescence dating and its application to fluvial deposits. Utrecht: The Royal Dutch Geographical Society, 2002.

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Ballarini, Mirko. Optical dating of quartz from young deposits: From single-aliquot to single-grain : proefschrift ... Delft: Delft University Press, 2006.

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Wallinga, Jakob. The Rhine-Meuse system in a new light: Optically stimulated luminescence dating and its application to fluvial deposits. Utrecht: Royal Dutch Geographical Society, Faculty of Geographical Sciences, Utrecht University, 2001.

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Optically Stimulated Luminescence Dosimetry. Elsevier, 2003. http://dx.doi.org/10.1016/b978-0-444-50684-9.x5077-6.

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Book chapters on the topic "Optically Stimulated Luminescence (OSL)"

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Jacobs, Zenobia. "Optically Stimulated Luminescence (OSL) Dating." In Encyclopedia of Geoarchaeology, 550–55. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-1-4020-4409-0_46.

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Kry, Stephen F., and Jennifer O'Daniel. "Optically Stimulated Luminescence Dosimeters in Clinical Practice." In Radiation Therapy Dosimetry: A Practical Handbook, 97–108. Names: Darafsheh, Arash, editor. Title: Radiation therapy dosimetry : a practical handbook / edited by Arash Darafsheh. Description: First edition. | Boca Raton : CRC Press, 2021.: CRC Press, 2021. http://dx.doi.org/10.1201/9781351005388-7.

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Martini, Marco. "Quartz Defects, Optically Stimulated Luminescence and Thermoluminescence." In Encyclopedia of Scientific Dating Methods, 650–56. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6304-3_68.

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Martini, Marco. "Quartz Defects, Optically Stimulated Luminescence and Thermoluminescence." In Encyclopedia of Scientific Dating Methods, 1–8. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-6326-5_68-6.

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Kairn, Tanya, Samuel Peet, Liting Yu, and Scott Crowe. "Long-Term Reliability of Optically Stimulated Luminescence Dosimeters." In IFMBE Proceedings, 561–64. Singapore: Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-10-9023-3_103.

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Kairn, Tanya, Holly Stephens, Scott Crowe, and Samuel Peet. "Optically Stimulated Luminescence Dosimeters as an Alternative to Radiographic Film for Performing “Head-Wrap” Linac Leakage Measurements." In IFMBE Proceedings, 553–55. Singapore: Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-10-9023-3_101.

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Sanderson, David C. W., and Timothy C. Kinnaird. "Optically Stimulated Luminescence Dating as a Geochronological Tool for Late Quaternary Sediments in the Red Sea Region." In Geological Setting, Palaeoenvironment and Archaeology of the Red Sea, 685–707. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99408-6_31.

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BOTTERJENSEN, L., S. MCKEEVER, and A. WINTLE. "OSL Measurement Technology." In Optically Stimulated Luminescence Dosimetry, 311–50. Elsevier, 2003. http://dx.doi.org/10.1016/b978-044450684-9/50084-2.

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Bøtter-Jensen, L., S. W. S. McKeever, and A. G. Wintle. "Retrospective OSL dosimetry." In Optically Stimulated Luminescence Dosimetry, 245–309. Elsevier, 2003. http://dx.doi.org/10.1016/b978-044450684-9/50093-3.

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Bøtter-Jensen, L., S. W. S. McKeever, and A. G. Wintle. "OSL measurement technology." In Optically Stimulated Luminescence Dosimetry, 311–50. Elsevier, 2003. http://dx.doi.org/10.1016/b978-044450684-9/50094-5.

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Conference papers on the topic "Optically Stimulated Luminescence (OSL)"

1

Liu, Yanping, Zhaoyang Chen, Yanwei Fan, Weizhen Ba, and Shilie Pan. "A Novel Radiation Dosimetry Based on Optically Stimulated Luminescence." In 16th International Conference on Nuclear Engineering. ASMEDC, 2008. http://dx.doi.org/10.1115/icone16-48023.

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A new generation of Alkaline earth sulfides (MgS, CaS, and BaS) doped with rare-earth ions have been identified by the University of Montpellier as the very high sensitivity of these phosphors, the short time constant of the luminescence and the perfectly separated spectra enable many applications in real time and online dosimetry. The online detecting technology of optically stimulated luminescent (OSL) radiation dosimeter main make use of the OSL characteristics of doping the alkaline-earth metal sulphides, makes the material into the thin films for storing energy from Ionizing radiation, the excitation light through optical fibers reached the where under radiation-field, with a sensitive detection device to read out the radiation dose from storing the OSL material, obtains a novel technology of radiation dose measurement. In the previous works, the dosimeter benefits from a printed circuit board mount. Both the sensor and the electronics are exposed to radiation, the problem of the radiation induced damage is supposedly being addressed. In both cases, the use of optical fibers can provide an elegant solution. Optical fibers offer a unique capability for remote monitoring of radiation in difficult-to-access and hazardous locations. Optical fiber can be located in radiation hazardous areas and optically interrogated from a safe distance. Hence, optical fiber dosemeters are immune to electrical and radio-frequency interference that can seriously degrade the performance of remote electronic dosimeters. In this paper, a novel remote optical fiber radiation dosimeter is described. The optical fiber dosimeter takes advantage of the charge trapping materials CaS:Ce, Sm and SrS:Eu, Sm that exhibit optically stimulated luminescence (OSL). The range of the dosimeter is from 0.01 to 1000Gy. The optically stimulated luminescent (OSL) radiation dosimeter technically surveys a wide dynamic measurement range and a high sensitivity. The equipment is relatively simple and small in size, and has low power consumption. This device is suitable for measuring the space radiation dose; it also can be used in high radiation dose condition and other dangerous radiation occasions.
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Vikulova, Natalya. "Experience and prospects of using the method of optically stimulated luminescence (OSL) in archeology." In Actual Archaeology 5. Institute for the History of Material Culture Russian Academy of Sciences, 2020. http://dx.doi.org/10.31600/978-5-907298-04-0-2020-13-16.

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Kleber, Emily, J. Ramón Arrowsmith, J. Ramón Arrowsmith, Duane E. DeVecchio, Duane E. DeVecchio, Tammy Rittenour, and Tammy Rittenour. "OPTICALLY STIMULATED LUMINESCENCE (OSL) GEOCHRONOLOGY OF AN ACTIVE BLIND THRUST FAULT, WHEELER RIDGE, CALIFORNIA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-284523.

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Garcia, Antonio F., Daniel Dean, and Shannon A. Mahan. "DEDUCING GEOMORPHIC PROCESS AND THE CHARACTER OF PALEOCLIMATE FROM SURFICIAL GEOLOGY AND GEOCHRONOLOGY BASED ON OPTICALLY STIMULATED LUMINESCENCE (OSL) DATING." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-298356.

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Magne, S., L. de Carlan, J. M. Bordy, A. Isambert, A. Bridier, and P. Ferdinand. "Multichannel dosimeter and α-Al2O3:C Optically Stimulated Luminescence (OSL) fiber sensors for use in Radiation Therapy - evaluation with photon beams." In 2009 1st International Conference on Advancements in Nuclear Instrumentation, Measurement Methods and their Applications (ANIMMA). IEEE, 2009. http://dx.doi.org/10.1109/animma.2009.5503670.

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Huot, Sebastien, and Henry M. Loope. "OPTICALLY STIMULATED LUMINESCENCE DATING (OSL) IN AWKWARD PLACES: A STORY OF THE LAST LAURENTIDE ICE SHEET ADVANCE IN SOUTH-CENTRAL INDIANA." In 50th Annual GSA North-Central Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016nc-275641.

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Tew-Todd, Victoria, Steven L. Forman, Connor Mayhack, Liliana Marin, Logan Wiest, and Griffin Money. "EOLIAN DEPOSITIONAL AND ENVIRONMENTAL HISTORY FOR THE MONAHANS DUNE SYSTEM, WEST TEXAS FOR THE PAST CA. 0.5 MA BY THERMAL-TRANSFER OPTICALLY STIMULATED LUMINESCENCE (TT-OSL) DATING." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-354752.

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Huot, Sebastien, Henry M. Loope, José Luis Antinao, and G. William Monaghan. "DATING THE GREENWOOD MORAINE (INDIANA) BY OPTICALLY STIMULATED LUMINESCENCE DATING (OSL): AN ALL TOO COMMON STORY OF APPLYING A TECHNIQUE IN A DIFFICULT ENVIRONMENT IN THE HOPE OF SHINING LIGHT ON AN EXCITING IDEA." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-291457.

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McKeever, Stephen W. "Optically stimulated luminescence dosimetry." In Photonics East (ISAM, VVDC, IEMB), edited by Tuan Vo-Dinh and Robert L. Spellicy. SPIE, 1999. http://dx.doi.org/10.1117/12.339035.

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Gaikwad, S. U., R. R. Patil, M. S. Kulkarni, B. C. Bhatt, and S. V. Moharil. "Optically stimulated luminescence in doped NaCl." In INTERNATIONAL CONFERENCE ON CONDENSED MATTER AND APPLIED PHYSICS (ICC 2015): Proceeding of International Conference on Condensed Matter and Applied Physics. Author(s), 2016. http://dx.doi.org/10.1063/1.4946561.

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Reports on the topic "Optically Stimulated Luminescence (OSL)"

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Gotthold, David W., Nigel Browning, Eric Jensen, Alan Joly, and Nathan Canfield. Optically Stimulated Luminescence Based Optical Data Storage. Office of Scientific and Technical Information (OSTI), May 2016. http://dx.doi.org/10.2172/1474181.

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Miller, Steven D., Brion J. Burghard, James R. Skorpik, Richard J. Traub, and Leslie J. Schwartz. Low-Resolution Imaging using Optically Stimulated Luminescence. Office of Scientific and Technical Information (OSTI), November 1999. http://dx.doi.org/10.2172/877102.

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Bernal, SM. Protocols for Thermoluninescence and Optically Stimulated Luminescence Research at DOSAR. Office of Scientific and Technical Information (OSTI), October 2004. http://dx.doi.org/10.2172/885724.

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Kristiansen, Søren M., Lars Agersnap Larsen, Aayush Srivastava, and Tim C. Kinnaird. Quartz SAR optically stimulated lumines-cence (OSL) dating of sands from Ulbjerg Klint, Central Jutland, Denmark. Aarhus University Library, 2020. http://dx.doi.org/10.7146/aul.388.

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Miller, Steven D., Paul L. Tomeraasen, Brion J. Burghard, and Richard J. Traub. Use of Optically Stimulated Luminescence Imaging Plates and Reader for Arms Control Applications. Office of Scientific and Technical Information (OSTI), July 2001. http://dx.doi.org/10.2172/943417.

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