Geibert, Walter; Charette, Matthew A; Kim, Guebuem; Moore, Willard S; Street, Joseph H; Young, Megan; Paytan, Adina (2008): Dissolved actinium in the ocean. PANGAEA, https://doi.org/10.1594/PANGAEA.695909, Supplement to: Geibert, W et al. (2008): The release of dissolved actinium to the ocean: A global comparison of different end-members. Marine Chemistry, 109(3-4), 409-420, https://doi.org/10.1016/j.marchem.2007.07.005
Always quote above citation when using data! You can download the citation in several formats below.
The measurement of short-lived 223Ra often involves a second measurement for supported activities, which represents 227Ac in the sample. Here we exploit this fact, presenting a set of 284 values on the oceanic distribution of 227Ac, which was collected when analyzing water samples for short-lived radium isotopes by the radium delayed coincidence counting system. The present work compiles 227Ac data from coastal regions all over the northern hemisphere, including values from ground water, from estuaries and lagoons, and from marine end-members. Deep-sea samples from a continental slope off Puerto Rico and from an active vent site near Hawaii complete the overview of 227Ac near its potential sources.
The average 227Ac activities of nearshore marine end-members range from 0.4 dpm/m**3 at the Gulf of Mexico to 3.0 dpm m? 3 in the coastal waters of the Korean Strait. In analogy to 228Ra, we find the extension of adjacent shelf regions to play a substantial role for 227Ac activities, although less pronounced than for radium, due to its weaker shelf source. Based on previously published values, we calculate an open ocean 227Ac inventory of 1.35 * 1018 dpm 227Acex in the ocean, which corresponds to 37 moles, or 8.4 kg. This implies a flux of 127 dpm/m**2/y from the deep-sea floor. For the shelf regions, we obtain a global inventory of 227Ac of 4.5 * 10**15 dpm, which cannot be converted directly into a flux value, as the regional loss term of 227Ac to the open ocean would have to be included.
Ac has so far been considered to behave similarly to Ra in the marine environment, with the exception of a strong Ac source in the deep-sea due to 231Paex. Here, we present evidence of geochemical differences between Ac, which is retained in a warm vent system, and Ra, which is readily released [Moore, W.S., Ussler, W. and Paull, C.K., 2008-this issue. Short-lived radium isotopes in the Hawaiian margin: Evidence for large fluid fluxes through the Puna Ridge. Marine Chemistry]. Another potential mechanism of producing deviations in 227Ac/228Ra and daughter isotope ratios from the expected production value of lithogenic material is observed at reducing environments, where enrichment in uranium may occur. The presented data here may serve as a reference for including 227Ac in circulation models, and the overview provides values for some end-members that contribute to the global Ac distribution.
Median Latitude: 33.553445 * Median Longitude: 165.805291 * South-bound Latitude: 18.548000 * West-bound Longitude: 7.500000 * North-bound Latitude: 54.110000 * East-bound Longitude: -66.613000
Minimum DEPTH, water: 0 m * Maximum DEPTH, water: 3458 m
|#||Name||Short Name||Unit||Principal Investigator||Method||Comment|
|3||DEPTH, water||Depth water||m||Geocode|
|4||Sample code/label||Sample label||Geibert, Walter|
|9||Actinium 227, dissolved||227Ac diss||dpm/m3||Geibert, Walter|
|10||Actinium 227, dissolved, standard deviation||227Ac diss std dev||±||Geibert, Walter||1-sigma|
|11||-||-||Geibert, Walter||35% error estimate|
1900 data points