Dataset: Particle abundances and characteristics from the video plankton profiler with matching CTD data, from casts on RVIB Nathaniel B. Palmer NBP1302, Feb/Mar 2013 (TRACERS project)

This dataset has not been validatedFinal no updates expectedDOI: 10.26008/1912/bco-dmo.683064.1Version 1 (2017-02-28)Dataset Type:Cruise Results

Principal Investigator: Alexander B. Bochdansky (Old Dominion University)

BCO-DMO Data Manager: Nancy Copley (Woods Hole Oceanographic Institution)


Project: TRacing the fate of Algal Carbon Export in the Ross Sea (TRACERS)


Abstract

Ocean Data View (ODV) and conductivity, temperature and depth (CTD) casts from NBP13-2 in the Ross Sea in February and March 2013. Data include temperature, salinity, density, fluorescence, light transmission, oxygen concentration, particle number, size, roundness, roughness, calculations of patchiness and index of aggregation.

Video particle profiler (VPP): (from Bochdansky,et al (2017) JMS)

The VPP was similar to that published in Bochdansky et al. (2010). However, instead of 45° angle lighting from both sides, side lighting with two white high-intensity LED lights was used ~7 cm in front of the lens. Some backscatter from transparent exopolymers (TEP), or from small particles embedded in that matrix, was possible using high-intensity light. The light beams were restricted using a slit width of 1 cm; however, as the light intensity dropped exponentially in the front and back of the image beam, only the brightest lit image plane was used for analysis. This method reduced bias caused by overlapping particles, removed motion blur streaks, and provided more accurate particle size estimates. At the focal plane, the field of view was 3.5 cm tall and 4.7 cm wide. The analysis program for the VPP was expanded from that in Bochdansky et al. (2010) to include more variables for particle characterization (including perimeter, volume and porosity). The VPP can record 30 images per second, with image analysis by a Linux-based image analysis program (an adapted Avidemux video editing software) at high speeds (approximately in real time after retrieval). The images were later aligned with depth from the CTD using time as the common variable and by filming a clock displaying UTC at the beginning and the end of each video sequence. In Matlab, CTD data were matched at one-second resolution with the particle data. The raw data consisted of millions of particles with associated CTD data. These raw data allow us to resample particle metrics at all scales. Particle volumes were calculated as shown in Fig. 2. Instead of assuming a specific geometric shape, the projected area of the particle on the screen (sum of white and black pixels within the perimeter of the particle) was converted into a circle that was then converted to volume. This method reduces error in volume calculations greatly because 2-dimensional information rather than 1-dimensional information is used to reconstruct volumes, thus avoiding the bias of assigning disproportionally large volumes to elongated objects. This approach is widely used in image analysis of ocean particles (e.g., Iversen et al., 2010). Total particle volume (pixel3 frame-1) was approximated by multiplying the mean volume of particles with the mean particle number.


Related Datasets

IsRelatedTo

Dataset: Phaeocystis counts
Bochdansky, A. B. (2021) Phaeocystis colony counts from raw Digital Holographic Microscope images from casts on RVIB Nathaniel B. Palmer NBP1302, March 2013 (TRACERS project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2017-02-28 doi:10.26008/1912/bco-dmo.683038.1

Related Publications

General

Bochdansky, A. B., Jericho, M. H., & Herndl, G. J. (2013). Development and deployment of a point-source digital inline holographic microscope for the study of plankton and particles to a depth of 6000 m. Limnology and Oceanography: Methods, 11(1), 28–40. doi:10.4319/lom.2013.11.28
General

Xu, W., Jericho, M. H., Meinertzhagen, I. A., & Kreuzer, H. J. (2001). Digital in-line holography for biological applications. Proceedings of the National Academy of Sciences, 98(20), 11301–11305. doi:10.1073/pnas.191361398
Methods

Bez, N. (2000). On the use of Lloyd’s index of patchiness. Fisheries Oceanography, 9(4), 372–376. doi:10.1046/j.1365-2419.2000.00148.x
Methods

Bochdansky, A. B., Clouse, M. A., & Hansell, D. A. (2017). Mesoscale and high-frequency variability of macroscopic particles (> 100 μm) in the Ross Sea and its relevance for late-season particulate carbon export. Journal of Marine Systems, 166, 120–131. doi:10.1016/j.jmarsys.2016.08.010
Methods

Bochdansky, A. B., van Aken, H. M., & Herndl, G. J. (2010). Role of macroscopic particles in deep-sea oxygen consumption. Proceedings of the National Academy of Sciences, 107(18), 8287–8291. doi:10.1073/pnas.0913744107