Quantification of Po-210 and Pb-210 as tracer of sediment resuspension rate in a shallow riverine system: Case study from southeast Michigan, USA

2020 ◽  
Vol 222 ◽  
pp. 106339
Author(s):  
Mark Baskaran ◽  
Rajalakshmi Mudbidre ◽  
Linda Schweitzer
2010 ◽  
Vol 67 (5) ◽  
pp. 871-874 ◽  
Author(s):  
Antonio Di Franco ◽  
Gaetano Ferruzza ◽  
Pasquale Baiata ◽  
Renato Chemello ◽  
Marco Milazzo

Abstract Di Franco, A., Ferruzza, G., Baiata, P., Chemello, R., and Milazzo, M. 2010. Can recreational scuba divers alter natural gross sedimentation rate? A case study from a Mediterranean deep cave. – ICES Journal of Marine Science, 67: 871–874. Submarine caves are environments with features distinguishing them from other littoral habitats but, despite their ecological importance, their response to anthropogenic disturbance has been seldom verified. One potential threat affecting natural communities within caves is represented by recreational scuba diving. Divers' disturbance within marine caves is mainly related to physical contacts and increased sediment resuspension potentially affecting sessile organisms. The aim was to assess the potential effect of recreational divers' frequentation on the natural gross sedimentation rate (GSR) in a Mediterranean deep-water cave. To achieve this, sediment traps were deployed along a scuba trail before, during, and after the peak season for tourist-related diving. No effects of divers' frequentation were evident in terms of alteration of natural GSR, but findings will need to be validated for other caves to asses whether potential disturbance depends on frequentation levels and/or cave characteristics, i.e. sediment grain size or cave depth.


2018 ◽  
Vol 85 ◽  
pp. 451-455
Author(s):  
Ho Kyung Ha ◽  
Jun Young Seo ◽  
Yoon Ho Jung ◽  
Hun Jun Ha ◽  
Soo Bin Kim ◽  
...  

2020 ◽  
Author(s):  
Siyuan-Sean Chen ◽  
Olivier Marchal ◽  
Paul Lerner ◽  
Dan McCorkle ◽  
Michiel Rutgers van der Loeff

<p>The naturally-occurring particle-reactive radionuclides protactinium-231 (<sup>231</sup>Pa) and thorium-230 (<sup>230</sup>Th) are used as tracers of a variety of oceanic processes, both at present and in the past. Most notably, the sediment <sup>231</sup>Pa/<sup>230</sup>Th ratio has been used to infer changes in the Atlantic Meridional Overturning Circulation over the last (de)glaciation. However, recent measurements along the U.S. GEOTRACES North Atlantic transect (GA03) revealed two features which are at odds with current understanding about <sup>231</sup>Pa and <sup>230</sup>Th behaviour in the ocean: (i) a sharp decrease in dissolved <sup>231</sup>Pa and <sup>230</sup>Th activities with depth below 2000-4000 m and (ii) very large particulate <sup>231</sup>Pa and <sup>230</sup>Th activities near the bottom, at a number of stations between the New England continental shelf and Bermuda. Concomitant measurements of particulate matter concentration and potential temperature showed that both features are associated with the benthic nepheloid layer (BNL) and the bottom mixed layer (BML) that are present at these stations.</p><p>Here we develop and apply a simplified model of the exchange of particles, <sup>231</sup>Pa, and <sup>230</sup>Th between the BNL and the upper sediment, to explore the extent to which the radionuclide anomalies observed near the bottom at a number of GA03 stations can be explained by local sediment resuspension. We find that the model can broadly reproduce the observed anomalies at two stations where samples for radionuclide analyses were collected near the seafloor. Sensitivity tests with the model show that the <sup>231</sup>Pa/<sup>230</sup>Th ratio of particles in the BML and the sediment varies by a factor of 3 as the sediment resuspension rate fluctuates within a range consistent with observational estimates. The modelled variability is comparable to the spatial variability of <sup>231</sup>Pa/<sup>230</sup>Th of suspended particles in the modern North Atlantic and to the variability of Atlantic sediment <sup>231</sup>Pa/<sup>230</sup>Th records across the last (de)glacial period. Two factors are found to contribute to the modelled sensitivity of the sediment <sup>231</sup>Pa/<sup>230</sup>Th to sediment resuspension rate: the vertical turbulent mixing in the BML and the differential scavenging intensity of Pa and Th due to variation in particle concentration. Overall, our study indicates that the exchange of material between the BNL and the upper sediment can affect the particulate <sup>231</sup>Pa/<sup>230</sup>Th ratio in the bottom water and the sediment, which may complicate the use of sediment <sup>231</sup>Pa/<sup>230</sup>Th as a palaeoceanographic tracer.</p>


2018 ◽  
Vol 123 (10) ◽  
pp. 7102-7119 ◽  
Author(s):  
Sarik Salim ◽  
Charitha Pattiaratchi ◽  
Rafael O. Tinoco ◽  
Ravindra Jayaratne

2014 ◽  
Vol 70 (1) ◽  
pp. 167-174 ◽  
Author(s):  
Jianjian Wang ◽  
Yong Pang ◽  
Yiping Li ◽  
Yawen Huang ◽  
Junjie Jia ◽  
...  

Contaminants released by wind-induced sediment resuspension could influence the water quality in shallow lakes. This study aims to reveal the quantitative relationship between wind speed (v) and sediment resuspension rate (r) in Meiliang Bay of Lake Taihu. The study was conducted in three steps. First, the in situ wind speed and current velocity were measured over a period of 2 days in Meiliang Bay to establish the relationship between wind and hydrodynamic conditions; second, an indoor experiment was conducted in a cylindrical simulator with sediment from the study area to determine sediment resuspension rates under different hydrodynamic conditions; and third, linkages between sediment resuspension and wind were determined. The average sediment resuspension rate was highly correlated with the wind speed (R2 = 0.99), and was expressed by r = 20.72v2.034 at wind speeds in the range of 0–14 m/s. The critical wind speed for sediment resuspension is about 7 m/s. Under these conditions, the average resuspension rate could reach 1,000 g/(m2d), with a total phosphorus release rate of 1.1 g/(m2d) and a total nitrogen release rate of 18.1 g/(m2d).


2014 ◽  
Vol 38 (01) ◽  
pp. 102-129
Author(s):  
ALBERTO MARTÍN ÁLVAREZ ◽  
EUDALD CORTINA ORERO

AbstractUsing interviews with former militants and previously unpublished documents, this article traces the genesis and internal dynamics of the Ejército Revolucionario del Pueblo (People's Revolutionary Army, ERP) in El Salvador during the early years of its existence (1970–6). This period was marked by the inability of the ERP to maintain internal coherence or any consensus on revolutionary strategy, which led to a series of splits and internal fights over control of the organisation. The evidence marshalled in this case study sheds new light on the origins of the armed Salvadorean Left and thus contributes to a wider understanding of the processes of formation and internal dynamics of armed left-wing groups that emerged from the 1960s onwards in Latin America.


2020 ◽  
Vol 43 ◽  
Author(s):  
Michael Lifshitz ◽  
T. M. Luhrmann

Abstract Culture shapes our basic sensory experience of the world. This is particularly striking in the study of religion and psychosis, where we and others have shown that cultural context determines both the structure and content of hallucination-like events. The cultural shaping of hallucinations may provide a rich case-study for linking cultural learning with emerging prediction-based models of perception.


2019 ◽  
Vol 42 ◽  
Author(s):  
Daniel J. Povinelli ◽  
Gabrielle C. Glorioso ◽  
Shannon L. Kuznar ◽  
Mateja Pavlic

Abstract Hoerl and McCormack demonstrate that although animals possess a sophisticated temporal updating system, there is no evidence that they also possess a temporal reasoning system. This important case study is directly related to the broader claim that although animals are manifestly capable of first-order (perceptually-based) relational reasoning, they lack the capacity for higher-order, role-based relational reasoning. We argue this distinction applies to all domains of cognition.


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