Preparation and characterization of calcium oxalate dihydrate seeds suitable for crystal growth kinetic analyses

2018 ◽  
Vol 500 ◽  
pp. 91-97 ◽  
Author(s):  
Anamarija Stanković ◽  
Jasminka Kontrec ◽  
Branka Njegić Džakula ◽  
Davor Kovačević ◽  
Berislav Marković ◽  
...  
1996 ◽  
Vol 51 (5-6) ◽  
pp. 426-428 ◽  
Author(s):  
P.V. Monje ◽  
E.J. Baran

Abstract The isolation of well formed crystals of the biomineral weddellite (calcium oxalate dihydrate) from Chamaecereus silvestrii, a Cactaceae species found in the northern part of Argentina, is described. Infrared spectroscopic measurements allow an unambiguous characterization of the nature of the crystals. This is the first report of the presence of a biomineral in this plant species.


1987 ◽  
Vol 42 (2) ◽  
pp. 89-93 ◽  
Author(s):  
Toshitsugu Oka ◽  
Toshiaki Yoshioka ◽  
Takuo Koide ◽  
Minato Takaha ◽  
Takao Sonoda

2013 ◽  
Vol 21 (3) ◽  
pp. 341-346 ◽  
Author(s):  
Kiyoko Kaneko ◽  
Yosuke Matsuta ◽  
Manabu Moriyama ◽  
Makoto Yasuda ◽  
Noriharu Chishima ◽  
...  

2000 ◽  
Vol 15 (2) ◽  
pp. 94-100
Author(s):  
K. D. Rogers ◽  
M. W. Sperrin ◽  
E. J. MacLean

The principal aim of this study was to assess a new approach to the characterization of uroliths using synchrotron radiation. To achieve this, a detailed investigation of the crystalline nature of a human bladder urolith has been undertaken. Changes in the phase composition and crystalline mineral nature have been measured from the urolith core center to its outer surface. Data were collected using a microbeam, synchrotron probe, and image plate. Rietveld analysis has enabled us to determine that the unit cell dimensions of the majority phases (anhydrous uric acid and calcium oxalate monohydrate) are significantly greater in the core region but become progressively smaller from the outer to inner regions. The crystallites of both phases are also shown to possess significant radial orientation which varies through the urolith and reaches a maximum at a point of principal fracture. The analysis has also allowed us to study the change in average crystallite morphology; the crystallites of both phases are shown to decrease in size toward the outer parts of the urolith although this is in a nonuniform fashion. Evidence of calcium oxalate dihydrate was also found, but only within the outermost region of the urolith.


Sign in / Sign up

Export Citation Format

Share Document