Interpreting LISST-100X measurements of particles with complex shape using digital in-line holography

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Interpreting LISST-100X measurements of particles with complex shape using digital in-line holography. / Graham, G.W.; Davies, E.J.; Nimmo-Smith, W.A. et al.
In: Journal of Geophysical Research Oceans, Vol. 117, No. C5, 01.05.2012, p. C05034.

Research output: Contribution to journalArticlepeer-review

HarvardHarvard

Graham, GW, Davies, EJ, Nimmo-Smith, WA, Bowers, DG & Braithwaite, KM 2012, 'Interpreting LISST-100X measurements of particles with complex shape using digital in-line holography', Journal of Geophysical Research Oceans, vol. 117, no. C5, pp. C05034. https://doi.org/10.1029/2011JC007613

APA

Graham, G. W., Davies, E. J., Nimmo-Smith, W. A., Bowers, D. G., & Braithwaite, K. M. (2012). Interpreting LISST-100X measurements of particles with complex shape using digital in-line holography. Journal of Geophysical Research Oceans, 117(C5), C05034. https://doi.org/10.1029/2011JC007613

CBE

Graham GW, Davies EJ, Nimmo-Smith WA, Bowers DG, Braithwaite KM. 2012. Interpreting LISST-100X measurements of particles with complex shape using digital in-line holography. Journal of Geophysical Research Oceans. 117(C5):C05034. https://doi.org/10.1029/2011JC007613

MLA

VancouverVancouver

Graham GW, Davies EJ, Nimmo-Smith WA, Bowers DG, Braithwaite KM. Interpreting LISST-100X measurements of particles with complex shape using digital in-line holography. Journal of Geophysical Research Oceans. 2012 May 1;117(C5):C05034. doi: 10.1029/2011JC007613

Author

Graham, G.W. ; Davies, E.J. ; Nimmo-Smith, W.A. et al. / Interpreting LISST-100X measurements of particles with complex shape using digital in-line holography. In: Journal of Geophysical Research Oceans. 2012 ; Vol. 117, No. C5. pp. C05034.

RIS

TY - JOUR

T1 - Interpreting LISST-100X measurements of particles with complex shape using digital in-line holography

AU - Graham, G.W.

AU - Davies, E.J.

AU - Nimmo-Smith, W.A.

AU - Bowers, D.G.

AU - Braithwaite, K.M.

PY - 2012/5/1

Y1 - 2012/5/1

N2 - [1] Measurements of suspended sediment volume concentrations, particle size and number density are routinely collected in marine and fresh-water environments with LISST-100X instruments to understand sediment transport, biological processes and fundamental opto-acoustic problems. A LISST-100X was simultaneously deployed with a novel holographic camera (holocam) in UK coastal waters to assess the performance of the laser diffraction technique when measuring natural suspensions. Volume distributions from the LISST-100X, truncated to exclude non-overlapping size bins with the holocam, exhibit an increase in small particles and median particle size is elevated in comparison to the holocam by 20–40%. We observe positive offsets between LISST-100X and holocam number distributions of up to 2 orders of magnitude for particle sizes between 58–218μm, with discrepancies rising to 4 orders of magnitude for finer and coarser sizes. To explain these differences, a novel multiscale representation of particle size is used. The method quantifies individual dimensions that make up any two-dimensional geometrical structure, it can be used as a metric for particle complexity, and offers a plausible explanation for an apparent increase in small particles (

AB - [1] Measurements of suspended sediment volume concentrations, particle size and number density are routinely collected in marine and fresh-water environments with LISST-100X instruments to understand sediment transport, biological processes and fundamental opto-acoustic problems. A LISST-100X was simultaneously deployed with a novel holographic camera (holocam) in UK coastal waters to assess the performance of the laser diffraction technique when measuring natural suspensions. Volume distributions from the LISST-100X, truncated to exclude non-overlapping size bins with the holocam, exhibit an increase in small particles and median particle size is elevated in comparison to the holocam by 20–40%. We observe positive offsets between LISST-100X and holocam number distributions of up to 2 orders of magnitude for particle sizes between 58–218μm, with discrepancies rising to 4 orders of magnitude for finer and coarser sizes. To explain these differences, a novel multiscale representation of particle size is used. The method quantifies individual dimensions that make up any two-dimensional geometrical structure, it can be used as a metric for particle complexity, and offers a plausible explanation for an apparent increase in small particles (

U2 - 10.1029/2011JC007613

DO - 10.1029/2011JC007613

M3 - Article

VL - 117

SP - C05034

JO - Journal of Geophysical Research Oceans

JF - Journal of Geophysical Research Oceans

SN - 2169-9291

IS - C5

ER -