scholarly journals Advances in the Recovery of Uranium from Seawater: Studies Under Real Ocean Conditions

2018 ◽  
Author(s):  
Ken Buesseler ◽  
Jessica Drysdale
2003 ◽  
Vol 42 (23) ◽  
pp. 5900-5904 ◽  
Author(s):  
Alain Favre-Reguillon ◽  
Gerard Lebuzit ◽  
Jacques Foos ◽  
Alain Guy ◽  
Micheline Draye ◽  
...  

2021 ◽  
Vol 27 (9) ◽  
pp. 1737-1754
Author(s):  
Wing Yan Chan ◽  
John G. Oakeshott ◽  
Patrick Buerger ◽  
Owain R. Edwards ◽  
Madeleine J. H. Oppen

Chemosphere ◽  
2021 ◽  
pp. 130411
Author(s):  
Han Guo ◽  
Ying Li ◽  
Huihui Wang ◽  
Ning Zhang ◽  
Alhadi Ishag ◽  
...  

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Rebecca Jackson ◽  
Anna Bang Kvorning ◽  
Audrey Limoges ◽  
Eleanor Georgiadis ◽  
Steffen M. Olsen ◽  
...  

AbstractBaffin Bay hosts the largest and most productive of the Arctic polynyas: the North Water (NOW). Despite its significance and active role in water mass formation, the history of the NOW beyond the observational era remains poorly known. We reconcile the previously unassessed relationship between long-term NOW dynamics and ocean conditions by applying a multiproxy approach to two marine sediment cores from the region that, together, span the Holocene. Declining influence of Atlantic Water in the NOW is coeval with regional records that indicate the inception of a strong and recurrent polynya from ~ 4400 yrs BP, in line with Neoglacial cooling. During warmer Holocene intervals such as the Roman Warm Period, a weaker NOW is evident, and its reduced capacity to influence bottom ocean conditions facilitated northward penetration of Atlantic Water. Future warming in the Arctic may have negative consequences for this vital biological oasis, with the potential knock-on effect of warm water penetration further north and intensified melt of the marine-terminating glaciers that flank the coast of northwest Greenland.


2021 ◽  
Vol 168 (7) ◽  
Author(s):  
Kerri L. Dobson ◽  
Stephen Levas ◽  
Verena Schoepf ◽  
Mark E. Warner ◽  
Wei-Jun Cai ◽  
...  

Radiocarbon ◽  
1988 ◽  
Vol 30 (3) ◽  
pp. 282-284

These cores were chosen for our initial effort because they typified normal open ocean conditions (see Fig 9; Tables 10, 11).


2015 ◽  
Vol 55 (15) ◽  
pp. 4103-4109 ◽  
Author(s):  
S. Das ◽  
Y. Oyola ◽  
R. T. Mayes ◽  
C. J. Janke ◽  
L.-J. Kuo ◽  
...  

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