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author de Stigter, Henko
author_facet de Stigter, Henko
collection Datos científicos de ciencias marinas y ambientales
contents Sediment profiles of 210Pb and 226Ra, radio-isotopes from the 234U decay series with half-lives of respectively 22.3 and 1600 year, were measured in multicores collected from the DISCOL Experimental Area in the Peru Basin during SO242-1, for determining biological mixing rates integrated over a ~100 year time-scale. Total 210Pb and 226Ra activity were determined directly by gamma-spectrometry, whilst total 210Pb was also measured indirectly by alpha-spectrometry via its granddaughter isotope 210Po. Activities of anthropogenic 137Cs proved to be generally below detection level. Radionuclide activities are reported in the data base as mBq g-1 dry sediment. For alpha spectrometry measurement of 210Po, 0.5 g of freeze-dried and homogenised sediment contained in a plastic reaction tube was spiked with 1 ml of a standard solution of 209Po in 2M HCl, and then leached for 6 h in 10 ml of concentrated HCl heated to 85ºC. After diluting the fluid with 45 ml of demineralised water and adding 5 ml of an aqueous solution of ascorbic acid (40 g L-1), natural 210Po and added 209Po were collected from the fluid by spontaneous electrochemical deposition on silver plates, which were suspended in the fluid for at least 16 h while the fluid was heated to 70ºC. The Po isotopes collected on the silver plates were then measured by alpha-spectrometry using Canberra Passivated Implanted Planar Silicon detectors, with a count time of 1 day sufficient to reduce counting error to < 3%. 210Pb activity was calculated from 210Po, assuming secular equilibrium and correcting for the time elapsed since collection of the samples.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_905442
institution PANGAEA
language en
publishDate 2019
publisher PANGAEA
record_format pangaea
spellingShingle Radionuclide data (total 210Pb) measured on sediment multi cores during SONNE cruise SO242/1 at the DISCOL area, Peru Basin
de Stigter, Henko
BC; Box corer; Date/Time of event; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; JPI-OCEANS; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Latitude of event; Lead-210; Lead-210, error; Longitude of event; MUC; MultiCorer; Optional event label; SO242/1; SO242/1_108-1; SO242/1_108-1_MUC 26; SO242/1_119-1; SO242/1_119-1_MUC 31; SO242/1_129-1; SO242/1_129-1_BC 26; SO242/1_34-1; SO242/1_34-1_MUC 6; SO242/1_56-1; SO242/1_56-1_MUC 12; SO242/1_61-1; SO242/1_61-1_MUC 13; SO242/1_70-1; SO242/1_70-1_MUC 17; SO242/1_74-1; SO242/1_74-1_MUC 20; SO242/1_80-1; SO242/1_80-1_MUC 22; Sonne_2
Sediment profiles of 210Pb and 226Ra, radio-isotopes from the 234U decay series with half-lives of respectively 22.3 and 1600 year, were measured in multicores collected from the DISCOL Experimental Area in the Peru Basin during SO242-1, for determining biological mixing rates integrated over a ~100 year time-scale. Total 210Pb and 226Ra activity were determined directly by gamma-spectrometry, whilst total 210Pb was also measured indirectly by alpha-spectrometry via its granddaughter isotope 210Po. Activities of anthropogenic 137Cs proved to be generally below detection level. Radionuclide activities are reported in the data base as mBq g-1 dry sediment. For alpha spectrometry measurement of 210Po, 0.5 g of freeze-dried and homogenised sediment contained in a plastic reaction tube was spiked with 1 ml of a standard solution of 209Po in 2M HCl, and then leached for 6 h in 10 ml of concentrated HCl heated to 85ºC. After diluting the fluid with 45 ml of demineralised water and adding 5 ml of an aqueous solution of ascorbic acid (40 g L-1), natural 210Po and added 209Po were collected from the fluid by spontaneous electrochemical deposition on silver plates, which were suspended in the fluid for at least 16 h while the fluid was heated to 70ºC. The Po isotopes collected on the silver plates were then measured by alpha-spectrometry using Canberra Passivated Implanted Planar Silicon detectors, with a count time of 1 day sufficient to reduce counting error to < 3%. 210Pb activity was calculated from 210Po, assuming secular equilibrium and correcting for the time elapsed since collection of the samples.
title Radionuclide data (total 210Pb) measured on sediment multi cores during SONNE cruise SO242/1 at the DISCOL area, Peru Basin
topic BC; Box corer; Date/Time of event; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; JPI-OCEANS; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Latitude of event; Lead-210; Lead-210, error; Longitude of event; MUC; MultiCorer; Optional event label; SO242/1; SO242/1_108-1; SO242/1_108-1_MUC 26; SO242/1_119-1; SO242/1_119-1_MUC 31; SO242/1_129-1; SO242/1_129-1_BC 26; SO242/1_34-1; SO242/1_34-1_MUC 6; SO242/1_56-1; SO242/1_56-1_MUC 12; SO242/1_61-1; SO242/1_61-1_MUC 13; SO242/1_70-1; SO242/1_70-1_MUC 17; SO242/1_74-1; SO242/1_74-1_MUC 20; SO242/1_80-1; SO242/1_80-1_MUC 22; Sonne_2
url https://doi.org/10.1594/PANGAEA.905442