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Related Concept Videos

Pore Size Distribution01:23

Pore Size Distribution

In concrete, the pore size distribution significantly influences the material's properties. Capillary pores, markedly larger than gel pores, form a vast network within partially hydrated cement paste, reducing the concrete's strength and increasing its permeability. This heightened permeability leads to a greater risk of damage from environmental factors like freeze-thaw cycles and chemical attacks, with the extent of vulnerability also being tied to the water-to-cement ratio.
Adequate...
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Boundary Layer Characteristics

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Precipitation Gravimetry

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Related Experiment Video

Updated: Jun 7, 2026

Measuring Spray Droplet Size from Agricultural Nozzles Using Laser Diffraction
08:14

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Published on: September 16, 2016

Cloud-droplet-size distribution from lidar multiple-scattering measurements.

Y Benayahu, A Ben-David, S Fastig

    Applied Optics
    |November 2, 2010
    PubMed
    Summary
    This summary is machine-generated.

    This study introduces a new lidar method to determine cloud droplet size distribution. By analyzing laser backscattering and multiple scattering, it accurately calculates droplet sizes in atmospheric clouds.

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    Last Updated: Jun 7, 2026

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    Area of Science:

    • Atmospheric optics
    • Cloud physics
    • Laser remote sensing

    Background:

    • Accurate measurement of cloud droplet size distribution is crucial for understanding cloud properties and climate.
    • Traditional methods for cloud droplet size measurement have limitations in resolution and scope.

    Purpose of the Study:

    • To present a novel lidar-based method for calculating atmospheric cloud droplet-size distribution.
    • To utilize laser backscattering and multiple scattering measurements for enhanced cloud characterization.

    Main Methods:

    • Employing a Nd:YAG laser lidar system with detectors for single and double scattering.
    • Measuring backscattering (primarily single scattering) along the laser beam path.
    • Measuring multiple scattering (primarily double scattering) at a specific angle to the laser beam, analyzing its angular domain change with penetration depth.

    Main Results:

    • Deriving the double-scattering phase function from the measured double-scattering signal as a function of cloud penetration depth.
    • Successfully inverting the phase function to obtain cloud droplet-size distribution.
    • Demonstrating the method's capability to determine droplet size distribution in the form of a log-normal function.

    Conclusions:

    • The presented lidar method offers a viable approach for determining cloud droplet-size distribution.
    • The combined analysis of single and multiple scattering provides a more comprehensive characterization of cloud microphysical properties.
    • This technique has potential applications in atmospheric research and climate modeling.