In situ differentiation between nevi and malignant melanomas by fluorescence measurements

1991 ◽  
Vol 78 (10) ◽  
pp. 456-457 ◽  
Author(s):  
W. Lohmann ◽  
M. Nilles ◽  
R. H. B�deker
2016 ◽  
Vol 24 (21) ◽  
pp. 23635 ◽  
Author(s):  
Shengqiang Wang ◽  
Cong Xiao ◽  
Joji Ishizaka ◽  
Zhongfeng Qiu ◽  
Deyong Sun ◽  
...  

2011 ◽  
Vol 88 (1-4) ◽  
pp. 28-45 ◽  
Author(s):  
Walker O. Smith ◽  
Vernon Asper ◽  
Sasha Tozzi ◽  
Xiao Liu ◽  
Sharon E. Stammerjohn

2002 ◽  
Vol 4 (5) ◽  
pp. 540-540
Author(s):  
Daniel P. Walsh ◽  
Christopher Pang ◽  
Puja B. Parikh ◽  
Young-Soo Kim ◽  
Young-Tae Chang

2014 ◽  
Vol 2014 ◽  
pp. 1-16 ◽  
Author(s):  
Mark R. Jury

The Southern Benguela cape upwelling plumes have inshore wind shadows prone to red tides in late summer. Their intensity and coverage are estimated by satellite fluorescence measurements in the period 1997–2012 and qualified by in situ reports. High satellite fluorescence cases are identified at daily to seasonal time scales, and characteristics of the upper ocean and lower atmosphere are studied using third generation reanalyses. A dominant feature is easterly winds over the Cape Peninsula (34°S, 18°E) induced by a ridging anticyclone-coastal low weather pattern. Over Cape Columbine (33°S), there is a wind shadow with cyclonic wind and current shear. Composite atmospheric profiles reveal a 4°C temperature inversion near 500 m that traps a coastal wind jet >6 m/s below 200 m. The composite shelf oceanography shows a relic upwelling plume below 10 m overtopped by warmer water near the coast, providing the thermal stratification needed for biotic aggregation. Data from the IPSL5 coupled climate model over the period 1980–2080 indicates that environmental conditions favoring red tides may become more frequent.


2015 ◽  
Vol 33 (4) ◽  
pp. 816-825 ◽  
Author(s):  
Daniel J. Duke ◽  
Alan L. Kastengren ◽  
Nicholas Mason-Smith ◽  
Yang Chen ◽  
Paul M. Young ◽  
...  

2020 ◽  
Author(s):  
Srikanth Nayak ◽  
Kaitlin Lovering ◽  
Wei Bu ◽  
Ahmet Uysal

Anions are expected to be repelled from negatively charged surfaces. At aqueous interfaces, however, ion-specific effects can dominate over direct electrostatic interactions. Using multiple <i>in situ</i> surface sensitive experimental techniques, we show that surface affinity of SCN<sup>-</sup> ions are so strong that they can adsorb at a negatively charged floating monolayer at the air/aqueous interface. This extreme example of ion-specific effects may be very important for understanding complex processes at aqueous interfaces, such as chemical separations of rare earth metals. Adsorbed SCN<sup>-</sup> ions at the floating monolayer increase the overall negative charge density, leading to enhanced trivalent rare earth adsorption. Surface sensitive X-ray fluorescence measurements show that the surface coverage of Lu<sup>3+</sup> ions can be triple of the apparent surface charge of the floating monolayer in the presence of SCN<sup>-</sup>. Comparison to NO<sub>3</sub><sup>-</sup> samples show that the effects are strongly dependent to the character of the anion, providing further evidence to ion-specific effects dominating over electrostatics.


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