Comment on “On the atmospheric input of sulfur into the ocean” by E. Mészáros

Tellus B ◽  
1983 ◽  
Vol 35 (4) ◽  
pp. 290-293 ◽  
Author(s):  
Jennifer A. Logan
Keyword(s):  
Nature ◽  
1986 ◽  
Vol 321 (6068) ◽  
pp. 427-428 ◽  
Author(s):  
M. D. Loÿe-Pilot ◽  
J. M. Martin ◽  
J. Morelli

1989 ◽  
Vol 28 (1-3) ◽  
pp. 159-182 ◽  
Author(s):  
Jean-Marie Martin ◽  
Francoise Elbaz-Poulichet ◽  
Cécile Guieu ◽  
Marie-Dominique Loÿe-Pilot ◽  
Gengchen Han

2014 ◽  
Vol 87 ◽  
pp. 53-56 ◽  
Author(s):  
Jung-Suk Oh ◽  
Sang-Han Lee ◽  
Jong-Ki Choi ◽  
Jong-Man Lee ◽  
Kyung-Bum Lee ◽  
...  

Tellus ◽  
1982 ◽  
Vol 34 (3) ◽  
pp. 277-282 ◽  
Author(s):  
E. MÉSZÁros
Keyword(s):  

2001 ◽  
Vol 21 (18-19) ◽  
pp. 2073-2094 ◽  
Author(s):  
Gerrit de Leeuw ◽  
Leo Cohen ◽  
Lise Marie Frohn ◽  
Gary Geernaert ◽  
Ole Hertel ◽  
...  

2021 ◽  
Author(s):  
Ivana Tucaković ◽  
Sarah Mateša ◽  
Ivana Coha ◽  
Marija Marguš ◽  
Milan Čanković ◽  
...  

<p>Croatian Science Foundation MARRES project (MARine lake (Rogoznica) as a model for EcoSystem functioning in a changing environment) aims to investigate the unique environment (slow exchange of seawater with the sea; atmospheric input is the only source of freshwater) of the marine lake which is an example of highly stratified (permanent anoxia bellow 9 m depth), and by climate changes affected marine system in the middle of the eastern Adriatic coast (43.53° N, 15.95° E). The area of the lake is characterized by the extensive tourism and mariculture, and the low impact of local industrial activities. It is also affected by the combined influence of long-range transport of air masses and local emissions (open-fire events).</p><p>An important part of the project is focused on the exchange and interaction between atmosphere, water column and sediment by measuring the atmospheric input (wet and dry deposition) of sulphur compounds, organic carbon, trace metals and radionuclides (Be-7, Pb-210).</p><p>This work for the first time will present the current state of the measurements of radioactivity in the Rogoznica lake area, including samples of aerosol particulate matter, PM2.5 < 2.5 um, rainwater and lake water column. Namely, the concentrations of Be-7 and Pb-210 in PM2.5 are measured to determine and correlate the dynamics of particle transport, meteorological information, especially origin of air masses and seasonal variation of PM2.5. While presence of Be-7 indicates the recent wet or dry deposition from the upper parts of the atmosphere, Pb-210 may be used as a tracer for continental air masses. Therefore, it can also indicate the influence of the pollution induced by human activity. Regarding that, special attention will be paid to compare results before and during the Covid-19 lockdown periods.</p><p>So far, preliminary results do not show significant difference in PM2.5 masses and measured radionuclide activity concentrations for the lockdown period. Be-7 and Pb-210 were regularly detected in aerosols collected on a glass fiber filters during a one-week sampling periods with the air flow rate of 2.3 m<sup>3</sup>/h. Their activity concentrations are determined by gamma spectrometry using High Purity Germanium detectors. The results are found to be correlated with PM2.5 masses, ranging from 2.9 to 12.2 Bq/m<sup>3</sup> for Be-7 and from 0.5 to 2.5 Bq/m<sup>3</sup> for Pb-210. First analyses show that the highest values can be related to the long-range transport of air masses and to the recorded near open-fire event. As expected, Be-7 is also detected in almost every rainwater sample (event), with the activity concentration up to 5.6 Bq/L, while low activities of Pb-210 are detected only sporadically. Related to that, Be-7 is detected in lake water column as well, but only in the surface layer and in samples collected during, or immediately after the rain events. </p><p>Dynamics and seasonal variation of radionuclide activity concentrations in here studied samples will be discussed, and the relationships with some meteorological parameters (temperature, wind speed, relative humidity, precipitation level) as well as local and long-range transport and physico-chemical conditions in the lake water column will be established.</p>


2021 ◽  
Author(s):  
Adrianus Damanik ◽  
Martin Wille ◽  
Martin Grosjean ◽  
Sri Yudawati Cahyarini ◽  
Hendrik Vogel

<p>Molybdenum (Mo) isotopes are known as sensitive recorders for changes in redox conditions because the oxidized form of Mo (Mo VI) is more soluble, whereas its reduced form is more particle reactive. Previous studies suggest that Mo isotopic fractionation during the weathering process is controlled by atmospheric input, Mo host, and bedrock composition. However, Mo isotopic variation and processes influencing fractionation in weathering profiles overlying ultramafic bedrock, the early Earth analog, have yet to be explored. This study explores for the first time (1) Mo behavior and (2) isotopic fractionation in two representative and intensely-weathered lateritic profiles overlying ultramafic bedrock of the East Sulawesi Ophiolite, Indonesia. Mo concentrations measured on samples obtained from laterite successions studied here range between 60 - 537 ppb and are overall higher compared to bedrock values ranging between 9 - 45 ppb. The Mo isotope compositions of laterite samples vary between -0.043‰ to -0.161‰ δ<sup>98</sup>Mo<sub>NIST3134</sub>. The overall close to mantle Mo isotopic composition of the laterite samples, their small Mo isotope variability, and the covariation between Mo and Ti concentrations suggest low mobility of Mo during chemical weathering and laterite formation. This low Mo mobility is likely a consequence of a) the low Mo concentration of the ultramafic protolith and b) adsorption of Mo to secondary Fe-Oxides during laterite formation under oxic weathering conditions.</p>


Sign in / Sign up

Export Citation Format

Share Document