Abstract

When laser beams propagate through media with non-vanishing absorption, the media is heated resulting in a change of the refractive index, which can lead to thermal lensing and thermal blooming. However, experimental details about both phenomena for propagations in water are lacking, especially for high-power lasers in the kilowatt range. We show that significant thermal lensing occurs only for high input powers before the onset of convective flow, while for low input powers, no strong thermal lens arises. After the onset of water flow, thermal blooming occurs at low input powers comparable to that known for propagations over kilometres in the air. However, for high input powers a thermal blooming on a qualitatively higher level is shown. By wavefront sensing, the change of refractive index distribution in water is investigated. This clearly shows the fast development of a strong thermal lens for high input powers and the onset of convection. Furthermore, a qualitatively good agreement of the accompanying simulations is observed. It is found that the absorption coefficient is linear with a value of mu ={13.7},{mathrm{m}^{-1}} at least up to 7.5 kW, i.e. 8 mathrm{kW/cm}^2. However, the directed transmission into an aperture is only constant before any thermal lensing of blooming occurs.

Highlights

  • When laser beams propagate through media with non-vanishing absorption, the media is heated resulting in a change of the refractive index, which can lead to thermal lensing and thermal blooming

  • Thermal lensing is known to occur for laser beams that propagate in transparent media without vanishing ­absorption[1,2,3,4]

  • By imaging the intensity distribution of the laser spot after propagation through a water layer, we show the occurrence of thermal blooming for lower input powers

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Summary

Introduction

When laser beams propagate through media with non-vanishing absorption, the media is heated resulting in a change of the refractive index, which can lead to thermal lensing and thermal blooming. After the onset of water flow, thermal blooming occurs at low input powers comparable to that known for propagations over kilometres in the air. The change of refractive index distribution in water is investigated This clearly shows the fast development of a strong thermal lens for high input powers and the onset of convection. Techniques based on the Hartmann-mask p­ rinciple[20] can be single-exposure measurement ­methods[21] In this case, a reference image must be acquired before starting the experiment, and only one image per acquisition is needed to determine the wavefront distortion. For investigations with a large field of view, wavefront sensors that image directly onto a focal plane array are not convincing because large detectors are ­required[3, 22, 23]

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