Carbon concentration and sinking velocity of particles measured during the James Cook cruise JC087, March 2013

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Autores principales: Cavan, Emma, Belcher, Anna
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2014
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author Cavan, Emma
Belcher, Anna
author_facet Cavan, Emma
Belcher, Anna
collection Datos científicos de ciencias marinas y ambientales
contents Sinking organic particles were collected from the Porcupine Abyssal Plain in 2013. Collection was done using a marine snow catcher (MSC), which is essentially a large (95 L) settling column. The marine snow catcher is deployed to one depth, the water trapped inside and then brought to the surface and left to stand on deck for 2 hours during which time the particles settle down (or up) the MSC depending on their settling rate. The particles are then collected and due to position of collection from the snow catcher are determined as fast or slow sinking particles. Some fluxes are negative as they were positively buoyant and not sinking.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_833364
institution PANGAEA
language en
publishDate 2014
publisher PANGAEA
record_format pangaea
spellingShingle Carbon concentration and sinking velocity of particles measured during the James Cook cruise JC087, March 2013
Cavan, Emma
Belcher, Anna
Basin Scale Analysis, Synthesis and Integration; Calculated after Ploug and Jørgensen (1999); Carbon, organic, particulate, flux; Carbon, organic, particulate mass; DEPTH, water; EURO-BASIN; Event label; James Cook; JC087; JC087-010; JC087-038; JC087-039; JC087-063; JC087-064; JC087-070; JC087-071; JC087-082; JC087-113; JC087-114; JC087-133; Julian day; Latitude of event; Longitude of event; Marine snow catcher; MSC; Porcupine Abyssal Plain; Sample ID; Time in days
Sinking organic particles were collected from the Porcupine Abyssal Plain in 2013. Collection was done using a marine snow catcher (MSC), which is essentially a large (95 L) settling column. The marine snow catcher is deployed to one depth, the water trapped inside and then brought to the surface and left to stand on deck for 2 hours during which time the particles settle down (or up) the MSC depending on their settling rate. The particles are then collected and due to position of collection from the snow catcher are determined as fast or slow sinking particles. Some fluxes are negative as they were positively buoyant and not sinking.
title Carbon concentration and sinking velocity of particles measured during the James Cook cruise JC087, March 2013
topic Basin Scale Analysis, Synthesis and Integration; Calculated after Ploug and Jørgensen (1999); Carbon, organic, particulate, flux; Carbon, organic, particulate mass; DEPTH, water; EURO-BASIN; Event label; James Cook; JC087; JC087-010; JC087-038; JC087-039; JC087-063; JC087-064; JC087-070; JC087-071; JC087-082; JC087-113; JC087-114; JC087-133; Julian day; Latitude of event; Longitude of event; Marine snow catcher; MSC; Porcupine Abyssal Plain; Sample ID; Time in days
url https://doi.org/10.1594/PANGAEA.833364