Skip to main content
Log in

Bleaching of blue light stimulated luminescence of quartz by moonlight

  • Published:
Journal of Earth System Science Aims and scope Submit manuscript

Abstract

Moonlight is sunlight reflected from the moon’s surface. It is additionally modulated by the Earth’s atmosphere, dust and pollutants on its way to the surface of the Earth. This contribution reports the bleaching rates of blue light stimulated luminescence (BLSL) signal of Quartz under full moonlight exposure at the Earth’s surface. Quartz BLSL reduced to 70% by an exposure of 5 hrs moonlight, is in contrast to ~90% reduction in < 3 s with daylight. This was anticipated due to (a) reduced moonlight flux by about a factor of half a million (Agrawal in Lat. Am. J. Phys. Educ. 4(2):325–328, 2010; J. Phys. Astron. 5(1):1–15, 2017); (b) inverse power law dependence of bleaching efficiency on wavelength (Spooner in The validity of optical dating based on feldspar, Ph.D. Thesis, Oxford University, Oxford, 1993; Chen and McKeever in Theory of Thermoluminescence and related phenomena, World Scientific Publications, London, 1997, Chen and Pagonis in Thermally and optically stimulated luminescence: A simulation approach, Wiley and Sons, Chichester, 2011); and (c) moonlight and daylight have spectral peaks around 650 and 550 nm, respectively. Deconvolution of OSL components suggests that moonlight affects the fast component of OSL signal the most. This has ramification for the application in polar regions, where the availability of daylight is at a premium during the winter months. Within a given context, it is conjectured that this could be used to infer the seasonality of sediment transport.

Research highlights

  1. 1.

    Up to 40% reduction of quartz luminescence signal observed over long moonlight exposure.

  2. 2.

    Moonlight can bleach up to 70% of the fast component of blue light stimulated luminescence signal.

  3. 3.

    Moonlight bleaching may hamper the accuracy of ages of sediments which are only transported during night.

  4. 4.

    Seasonality of sediment deposition can be studied using the bleaching effect of moonlight on quartz.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Institutional subscriptions

Figure 1
Figure 2

References

  • Agrawal D C 2010 Solar luminous constant versus lunar luminous constant; Lat. Am. J. Phys. Educ. 4(2) 325–328.

    Google Scholar 

  • Agrawal D C 2017 Moon, super-moon, planets of the solar system and star vega: Brightness and size; J. Phys. Astron. 5(1) 1–15.

    Google Scholar 

  • Aitken M J 1985 An Introduction to Optical Dating; Academic Press, Cambridge.

  • Aitken M J 1998 Thermoluminescenec Dating; Oxford University Press, ISBN 0-19-854092-2.

  • Bailey R M 2000 Slow component of quartz optically stimulated luminescence; Radiat. Meas. 32(3) 233–246.

    Article  Google Scholar 

  • Bailey R M 2001 Towards a general kinetic model for optically and thermally stimulated luminescence of quartz; Radiat. Meas. 33(1) 17–45.

    Article  Google Scholar 

  • Bailey R M, Smith B W and Rhodes E J 1997 Partial bleaching and the decay form characteristics of quartz OSL; Radiat. Meas. 27(2) 123–136.

    Article  Google Scholar 

  • Bøtter-Jensen L and Murray A S 1999 Developments in optically stimulated luminescence techniques for dating and retrospective dosimetry; Radiat. Protect. Dosimetry 84(1–4) 307–315.

    Article  Google Scholar 

  • Bøtter-Jensen L, Solongo S, Murray A S, Banerjee D and Jungner H 2000 Using the OSL single-aliquot regenerative-dose protocol with quartz extracted from building materials in retrospective dosimetry; Proceedings of the 9th Int. Conf. Luminescence and Electron-Spin Resonance Dating (LED99), 32(5) 841–845.

  • Bøtter-Jensen L, Andersen C E, Duller G A T and Murray A S 2003 Developments in radiation, stimulation and observation facilities in luminescence measurements; Radiat. Meas. 37 535–541.

    Article  Google Scholar 

  • Carver J H, Horton B H, O’Brien R S and O’Connor G G 1974 The ultraviolet reflectivity of the Moon; The Moon 9(3–4) 295–303.

    Article  Google Scholar 

  • Chen R and McKeever S W S 1997 Theory of Thermoluminescence and Related Phenomena; World Scientific Publications, London, NJ, Singapore.

    Book  Google Scholar 

  • Chen R and Pagonis V 2011 Thermally and Optically Stimulated Luminescence: A Simulation Approach; Wiley and Sons, Chichester.

    Book  Google Scholar 

  • Cramer C E, Lykke K R, Woodward J T and Smith A W 2013 Precise measurement of Lunar spectral irrediance at visible wavelengths; J. Res. Nat. Inst. Stand. Technol. 118 396–402.

    Article  Google Scholar 

  • David M and Sunta C M 1985 Quartz dosimeter for archaeological dating; Nucl. Tracks Radiat. Meas. 10 625–629.

    Article  Google Scholar 

  • Godfrey-Smith D I, Huntley D J and Chen W-H 1988 Optical dating studies of quartz and feldspar sediment extracts; Quat. Sci. Rev. 7 373–380.

    Article  Google Scholar 

  • Jain M, Murray A S and Botter-Jensen L 2003 Characterisation of blue-light stimulated luminescence components in different quartz samples: Implications for dose measurement; Radiat. Meas. 37(4–5) 441–449.

    Article  Google Scholar 

  • Jain M, Choi J H and Thomas P J 2008 The ultrafast OSL component in quartz: Origins and implications; Radiat. Meas. 43(2–6) 709–714.

    Article  Google Scholar 

  • Lindvall A, Stjern R and Alexanderson H 2017 Bleaching of quartz OSL signals under natural and laboratory light conditions; Ancient TL 35(2) 12–20.

    Google Scholar 

  • Murari M K 2006 Component Specific Luyminescence of Natural Minerals and their Application to the Dosimetry of Natural Radiation Environment; Ph.D. Thesis, Mohanlal Sukhadiya University, Udaipur, India.

  • Matthews G 2008 Celestial body irradiance determination from an under filled satellite radiometer: Application to albedo and thermal emission measurements of the Moon using CERES; Appl. Opt. 47 4981–4993.

    Article  Google Scholar 

  • Murray A S and Wintle A G 2000 Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol; Radiat. Meas. 32(1) 57–73.

    Article  Google Scholar 

  • Porat N 2006 Use of magnetic separation for purifying quartz for luminescence dating; Ancient TL 24(2) 33–36.

    Google Scholar 

  • Sohbati R, Murray A S, Lindvold L, Buylaert J-P and Jain M 2017 Optimization of laboratory illumination in optical dating; Quat. Geochronol. 39 105–111.

    Article  Google Scholar 

  • Spooner N A 1987 The Effect of Light on the Thermoluminescence of Quartz; Unpublished MSc thesis, University of Adelaide, Australia.

  • Spooner N A 1993 The Validity of Optical Dating Based on Feldspar; Ph.D. Thesis, Oxford University, Oxford.

  • Singhvi A K, Sharma Y P and Agrawal D P 1982 Thermoluminescence dating of sand dunes in Rajasthan, India; Nature 295(5847).

  • Singhvi A K, Stokes S, Chauhan N, Nagar Y and Jaiswal M K 2011 Changes in natural OSL sensitivity during single aliquot regeneration procedure and their implications for equivalent dose determination; Geochronometria 38 231–241.

    Article  Google Scholar 

  • Wintle A G and Murray A S 2006 A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols; Radiat. Meas. 41(4) 369–391.

    Article  Google Scholar 

Download references

Acknowledgements

AKS thanks the Department of Science and Technology, India for JC Bose National Fellowship and Year of Science Chair Professorship (YOSCP); the Department of Atomic Energy, India for a Raja Ramanna Fellowship. HMR thanks the DST – JC Bose/YOSCP fellowship to AKS for the research fellowship. We thank Prof. R J Wasson and Prof. Stephen Garnett for the sample.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to H M Rajapara.

Additional information

Communicated by Arkoprovo Biswas

Appendices

Appendix

Results of IRSL test conducted for feldspar contamination:

We have conducted an IRSL test on three representative quartz aliquots prepared from an extracted bulk quartz sample. The step of measurement protocol involves: Natural dose + preheat + IRSL + OSL + test dose + preheat + IRSL + OSL + test dose + preheat + OSL + test dose + TL.

Referring figures A1A3, it is concluded that there is no feldspar contamination to the quartz.

Figure A1
figure 3

TL glow curve measured after 5 Gy irradiation dose to the bleached quartz aliquot. This clearly suggests that there is no feldspar contamination in measured quartz.

Figure A2
figure 4

IRSL shine down curve for IRSL after 5 Gy test dose irradiation and prior preheat of 240°C for 10 sec.

Figure A3
figure 5

OSL shine down curve for OSL after 5 Gy test dose irradiation and prior preheat of 240°C for 10 sec.

Author statement

HMR, PNG and AKS developed the hypothesis; HMR and NC designed experiments, selected quartz sediments and analysed the results; HMR and VK performed luminescence measurements and components specific analysis. All authors contributed to the writing of the manuscript.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Rajapara, H.M., Kumar, V., Chauhan, N. et al. Bleaching of blue light stimulated luminescence of quartz by moonlight. J Earth Syst Sci 129, 212 (2020). https://doi.org/10.1007/s12040-020-01474-1

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s12040-020-01474-1

Keywords

Navigation