Determination of temporal changes in serum and urinary lactate and 3-hydroxybutyrate enantiomers in mice with nephrotoxic serum nephritis by multi-dimensional HPLC

2020 ◽  
Vol 188 ◽  
pp. 113367 ◽  
Author(s):  
Po-Yeh Lin ◽  
Shih-Ming Chen ◽  
Chin-Ling Hsieh ◽  
Chia-Yu Lin ◽  
Yu-Sheng Huang ◽  
...  
2011 ◽  
Vol 48 (2) ◽  
pp. 50-55
Author(s):  
I. Saknite ◽  
D. Jakovels ◽  
J. Spigulis

Distant Determination of Bilirubin Distribution in Skin by Multi-Spectral Imaging For mapping the bilirubin distribution in bruised skin the multi-spectral imaging technique was employed, which made it possible to observe temporal changes of the bilirubin content in skin photo-types II and III. The obtained results confirm the clinical potential of this technique for skin bilirubin diagnostics.


2019 ◽  
Vol 126 (2) ◽  
pp. 203
Author(s):  
Т.Б. Кузьмина ◽  
Н.В. Андреева ◽  
А.О. Исмагилов ◽  
О.В. Андреева

AbstractWe present the results of a study of milk as a complex biological fluid. The simultaneous occurrence of both direct and reverse sedimentation associated, respectively, with the protein and fat components of milk is demonstrated. Digital holographic interferometry enables the determination of the spatial and temporal changes in the refractive index of the suspension under study caused by fractionation processes with an accuracy of 10^–6, which exceeds the capabilities of other research methods. The results can be used to create a mathematical model of biological fluid fractionation processes and to develop physical models (phantoms) of such systems.


1987 ◽  
Vol 43 ◽  
pp. 86
Author(s):  
Yoshihisa Kudo ◽  
Toshio Iijima ◽  
Akihiko Ogura ◽  
Kyoko Akita ◽  
Keiko Takeda

This paper concerns the determination of the stress deviator from a set of striated faults or of focal mechanisms of earthquakes. Southern Tibet and the Cuzco region of the High Andes illustrate the applied methodology. Then, the spatial and temporal changes in the tectonic regimes of Tibet and Central Andes are briefly examined. The Quaternary—Present-day stress patterns in these two high plateaus favour models explaining the spatial changes in the state of stress at a large wavelength as a result of a compensated elevated topography. Major temporal changes in the tectonic regimes are attributed tentatively to uplift for the Tibetan plateau and, for the already elevated Andean Plateau, to changes in the magnitude of the boundary forces due to subduction processes .


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