2010
DOI: 10.1007/s10973-010-0914-6
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Thermal analysis of kidney stones and their characterization

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Cited by 18 publications
(9 citation statements)
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“…Each form of hydrate can be easily recognised because COM usually precipitates in the form of dendrites or boat/coffin morphology, COD shows a bipyramidal morphology and COT gives plate-like morphology [3,4]. Calcium oxalates were up to now frequently studied as chemicals involved in formation of urinary calculi [5,6], main attention is paid to finding the factors and conditions giving support to calcium oxalate and consequently to kidney stone formation [7,8]. The most frequently published data on calcium oxalate describe the crystal growth (conditions and kinetics) [3,[9][10][11][12][13][14][15][16][17][18] and dissolution of hydrates [19][20][21][22].…”
Section: Introductionmentioning
confidence: 99%
“…Each form of hydrate can be easily recognised because COM usually precipitates in the form of dendrites or boat/coffin morphology, COD shows a bipyramidal morphology and COT gives plate-like morphology [3,4]. Calcium oxalates were up to now frequently studied as chemicals involved in formation of urinary calculi [5,6], main attention is paid to finding the factors and conditions giving support to calcium oxalate and consequently to kidney stone formation [7,8]. The most frequently published data on calcium oxalate describe the crystal growth (conditions and kinetics) [3,[9][10][11][12][13][14][15][16][17][18] and dissolution of hydrates [19][20][21][22].…”
Section: Introductionmentioning
confidence: 99%
“…Different processes, such as the simultaneous loss of absorbed water, the crystalline water of CaOx and the lattice water of hydroxyapatite, occur at partially or fully overlapping temperatures [31][32][33], making the total weight loss a superposition of weight losses associated with individual processes. Quantification of the underlying processes is therefore imprecise or even impossible, depending on the extent of overlap.…”
Section: Discussionmentioning
confidence: 99%
“…This is especially applicable to absorbed water content; due to the overlapping processes of loss of absorbed and hydroxyapatite lattice water [34] and crystalline water of COM at temperatures over 100˚C, we considered only losses below this temperature that result in underestimation of adsorbed water content. The content of organic matter quoted, determined as mass lost between 500˚C and 700˚C, can serve as a rough estimate only since pyrolysis can occur at about 300˚C [33], but dehydration of hydroxyapatite [32] and decomposition of CaOx [26], if present, can occur simultaneously at temperatures up to 500˚C.…”
Section: Discussionmentioning
confidence: 99%
“…Different processes, such as the simultaneous loss of absorbed water, the crystalline water of CaOx and the lattice water of hydroxyapatite, occur at partially or fully overlapping temperatures [31][32][33], making the total weight loss a superposition of weight losses associated with individual processes. Quantification of the underlying processes is therefore imprecise or even impossible, depending on the extent of overlap.…”
Section: Discussionmentioning
confidence: 99%
“…This is especially applicable to absorbed water content; due to the overlapping processes of loss of absorbed and hydroxyapatite lattice water [34] and crystalline water of COM at temperatures over 100˚C, we considered only losses below this temperature that result in underestimation of adsorbed water content. The content of organic matter quoted, determined as mass lost between 500˚C and 700˚C, can serve as a rough estimate only since pyrolysis can occur at about 300˚C [33], but dehydration of hydroxyapatite [32] and decomposition of CaOx [26], if present, can occur simultaneously at temperatures up to 500˚C.…”
Section: Discussionmentioning
confidence: 99%