Mineral and microelement compositions of urinary stones
The mineral and microelement compositions of urinary stones from patients in various districts of the Novosibirsk region are analyzed. The mineral composition is determined using X-ray powder diffraction and vibrational spectroscopy. The microelement composition is identified using synchrotron radia...
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| Veröffentlicht in: | Russian journal of inorganic chemistry 2006-07, Vol.51 (7), p.1098-1105 |
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| container_title | Russian journal of inorganic chemistry |
| container_volume | 51 |
| creator | Pal’chik, N. A. Moroz, T. N. Maksimova, N. V. Dar’in, A. V. |
| description | The mineral and microelement compositions of urinary stones from patients in various districts of the Novosibirsk region are analyzed. The mineral composition is determined using X-ray powder diffraction and vibrational spectroscopy. The microelement composition is identified using synchrotron radiation X-ray fluorescence analysis. Calcium oxalates (whewellite CaC2O4 · H2O and weddellite CaC2O4 · 2H2O) are the most frequent components of the urinary stones. Oxalate uroliths contain a variety of microelements in significant amounts. Phosphate uroliths, represented by hydroxylapatite Ca5(PO4)3(OH) and struvite MgNH4PO4 · 6H2O, account for about one-fifth of the collection. Apatite urinary stones contain maximal strontium amounts. The struvite uroliths have higher rubidium levels. Uric acid uroliths (C5H4N4O3) account for about 11% of the collection. Their strontium concentrations are minimal. The element composition of the urinary stones is a function of their mineral constituents, the environmental surroundings, and the metabolism specifics of the patient. |
| doi_str_mv | 10.1134/S0036023606070138 |
| format | Article |
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Uric acid uroliths (C5H4N4O3) account for about 11% of the collection. Their strontium concentrations are minimal. The element composition of the urinary stones is a function of their mineral constituents, the environmental surroundings, and the metabolism specifics of the patient.</description><identifier>ISSN: 0036-0236</identifier><identifier>EISSN: 1531-8613</identifier><identifier>DOI: 10.1134/S0036023606070138</identifier><language>eng</language><publisher>Heidelberg: Springer Nature B.V</publisher><subject>Apatite ; Hydroxyapatite ; Inorganic chemistry ; Oxalates ; Rubidium ; Stone ; Synchrotron radiation ; Synchrotrons ; Trace elements ; Uric acid ; X ray fluorescence analysis ; X ray powder diffraction</subject><ispartof>Russian journal of inorganic chemistry, 2006-07, Vol.51 (7), p.1098-1105</ispartof><rights>Pleiades Publishing, Inc. 2006.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c304t-99a0344f1deb6900fd0f74dbfbfb54c98b5b10cda0e06fa2f0eee8138955e8f83</citedby><cites>FETCH-LOGICAL-c304t-99a0344f1deb6900fd0f74dbfbfb54c98b5b10cda0e06fa2f0eee8138955e8f83</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,781,785,27929,27930</link.rule.ids></links><search><creatorcontrib>Pal’chik, N. 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Apatite urinary stones contain maximal strontium amounts. The struvite uroliths have higher rubidium levels. Uric acid uroliths (C5H4N4O3) account for about 11% of the collection. Their strontium concentrations are minimal. The element composition of the urinary stones is a function of their mineral constituents, the environmental surroundings, and the metabolism specifics of the patient.</description><subject>Apatite</subject><subject>Hydroxyapatite</subject><subject>Inorganic chemistry</subject><subject>Oxalates</subject><subject>Rubidium</subject><subject>Stone</subject><subject>Synchrotron radiation</subject><subject>Synchrotrons</subject><subject>Trace elements</subject><subject>Uric acid</subject><subject>X ray fluorescence analysis</subject><subject>X ray powder diffraction</subject><issn>0036-0236</issn><issn>1531-8613</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNplkE9LxDAQxYMouK5-AG8FwVt1pknT9CjiP1jxoJ5D2k4gS5usSXvw25tlPSnDMIf34_HeMHaJcIPIxe07AJdQ5ZXQAHJ1xFZYcyyVRH7MVnu53Oun7CylLYAQ0KgVa16dp2jGwvihmFwfA400kZ-LPky7kNzsgk9FsMUSnTfxu0hz8JTO2Yk1Y6KL37tmn48PH_fP5ebt6eX-blP2HMRctq0BLoTFgTrZAtgBbCOGzuapRd-qru4Q-sEAgbSmskBEKsdv65qUVXzNrg--uxi-FkqznlzqaRyNp7AkXWGFoARk8OoPuA1L9DmbrqQUosmemCk8ULloSpGs3kU35VoaQe8fqf89kv8A2zplXw</recordid><startdate>20060701</startdate><enddate>20060701</enddate><creator>Pal’chik, N. 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The mineral composition is determined using X-ray powder diffraction and vibrational spectroscopy. The microelement composition is identified using synchrotron radiation X-ray fluorescence analysis. Calcium oxalates (whewellite CaC2O4 · H2O and weddellite CaC2O4 · 2H2O) are the most frequent components of the urinary stones. Oxalate uroliths contain a variety of microelements in significant amounts. Phosphate uroliths, represented by hydroxylapatite Ca5(PO4)3(OH) and struvite MgNH4PO4 · 6H2O, account for about one-fifth of the collection. Apatite urinary stones contain maximal strontium amounts. The struvite uroliths have higher rubidium levels. Uric acid uroliths (C5H4N4O3) account for about 11% of the collection. Their strontium concentrations are minimal. 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| subjects | Apatite Hydroxyapatite Inorganic chemistry Oxalates Rubidium Stone Synchrotron radiation Synchrotrons Trace elements Uric acid X ray fluorescence analysis X ray powder diffraction |
| title | Mineral and microelement compositions of urinary stones |
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