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  • Bone  (48)
  • Calcium  (39)
  • Springer  (82)
  • American Association of Petroleum Geologists (AAPG)
  • American Meteorological Society (AMS)
  • 1980-1984  (36)
  • 1970-1974  (46)
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  • Springer  (82)
  • American Association of Petroleum Geologists (AAPG)
  • American Meteorological Society (AMS)
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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 12 (1973), S. 73-90 
    ISSN: 1432-0827
    Keywords: Bone ; Mineral ; Properties ; Deproteination ; Hydrazine
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé Une méthode, utilisant 95% d'hydrazine, permet de déprotéiniser et de déshydrater légèrement l'os dans des conditions presqu'anhydres, avec une élévation de température modérée. Cette méthode ne provoque que des modifications chimiques mineures, sans altération des propriétés structurales de la phase minérale. Les résultats physico-chimiques démontrent que bien que les cristaux d'os de rat sont viosins de cristaux synthétiques témoins constitués dans des milieux, riches en carbonate plutôt qu'en hydroxyde, l'apatite osseux de rat ne parait pas analogue à des modèles cristallins connus ou imaginés. Des déterminations de bande infra-rouge CO 3 2− , réalisées à partir de spectre d'os total, semblent faussées par la présence de bandes d'absorption protéique. L'absorption d'HPO 4 2− est étudiée à l'aide de spectres infra-rouges de minéral osseux de jeunes rats. Des comparaisons détaillées en diffraction par raysons X d'os déprotéinisé de rats, avant et après hydrolyse, démontrent nettement la présence de phosphate de calcium amorphe. La microscopie électronique indique que de petits cristaux d'apatite dans l'os de rat sont susceptibles de contribuer au pool minéral amorphe en diffraction en rayons X. La microscopie électronique montre des plages de minéral osseux de rat où des cristaux d'apatite en forme de plaque, présentent une maille cristalline avec axe C malgré l'élimination de leur matrice fibreuse.
    Abstract: Zusammenfassung Es wird eine Methode beschrieben, wobei durch Anwendung von 95% Hydrazin ohne Wasserzugabe und mit nur geringem Erhitzen dem Knochen das gesamte Protein und ein kleiner Teil des Wassers entzogen wird. Diese Methode führte nur zu geringen chemischen Veränderungen und veränderte die strukturellen Eigenschaften der Mineralphase in keiner Weise. Physikochemische Daten wurden erbracht, welche zeigen, daß — obwohl die Kristalle von Rattenknochen den synthetischen Kontrollen (in Karbonat- und nicht hydroxydreichen Medien hergestellt) eher gleichen — Apatit aus Rattenknochen nicht auf sinnvolle Weise mittels bekannten oder postulierten Kristallmodellen interpretiert werden kann. CO 3 2− -Infrarotbandenzuteilungen, welche von Spektren aus dem Gesamtknochen gemacht wurden, geben wegen der Anwesenheit von Proteinabsorptionsbändern falsche Resultate. Die Absorption von HPO 4 2− wurde in den Infrarotspektren von Knochenmineral aus jungen Ratten beobachtet. Ein Vergleich der detaillierten Röntgendiffraktion von deproteinisiertem Rattenknochen vor und nach der Hydrolyse wies deutlich auf die Anwesenheit von amorphem Calciumphosphat hin. Die Elektronenmikroskopie zeigte kleine Apatitkristalle im Rattenknochen, welche zum Gesamtmineralpool beitragen könnten, der bei der Röntgendiffraktion amorph ist. Die Elektronenmikroskopie zeigte auch Gebiete im Rattenknochenmineral, wo plättchenartige Apatitkristalle eine deutlichec-Achsenorientierung beibehielten, obwohl ihre fibröse Matrix entfernt worden war.
    Notes: Abstract A method is described employing 95% hydrazine which completely deproteinates and slightly dehydrates bone under nearly anhydrous conditions with only moderate heating. This method induced only minor chemical changes and no alterations in structural properties of the mineral phase. Physicochemical data are presented demonstrating that although rat bone crystals more closely resemble synthetic controls made in carbonate-rather than hydroxide-rich media, rat bone apatite cannot be interpreted in terms of known or postulated crystal models in any meaningful fashion. CO 3 2− infrared band assignments made from spectra of whole bone are shown to be in error due to the presence of protein absorption bands. Absorotion of HPO 4 2− was observed in infrared spectra of young rat bone mineral. Detailed X-ray diffraction comparisons of deproteinated rat bone before and after hydrolysis clearly demonstrated the presence of amorphous calcium phosphate. Electron microscopy indicated that very small apatite crystals were present in rat bone which might also contribute to the overall mineral pool amorphous to X-ray diffraction. Electron microscopy also showed domains in rat bone mineral where plate-like apatite crystals maintained a netc-axis orientation despite the removal of their fibrous matrix.
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  • 2
    Electronic Resource
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    Springer
    Calcified tissue international 32 (1980), S. 45-53 
    ISSN: 1432-0827
    Keywords: Dentin ; Periodicity ; Allometry ; Calcium ; Sulfur
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Notes: Summary We have described differences in the aspects of biological rhythms for calcium and sulfur deposition on the labial and lingual sides of the growing rabbit incisor, where growth occurs along a spiral axis. The calcium oscillations appear to be smoother on the labial side than on the lingual side. The lingual side is characterized by high-frequency rhythms with high amplitudes which possess the greatest percent of the power (Fourier analysis). These observations also reflect a difference in behavior of the mean Ca concentration across the labial and lingual sides. Sulfur rhythms on the labial side have higher amplitudes than those on the lingual side, but systematic differences in distribution of power between high and low frequencies is not as pronounced as in the case of Ca. The differences in Ca rhythms reflect differences in the growth rates of incisors on either side of the spiral axis. The labial side grows slightly faster than the lingual side, and its odontoblasts secrete Ca along the spiral axis and toward the pulp cavity at the same time. Thus the resultant direction of growth is more nearly opposite the extension of the occlusal end on the labial side, and Ca is consequently deposited over a wider area relative to that on the lingual surfaces. On the lingual side, Ca is deposited within a more limited area, and growth must therefore be continuous at high frequencies. The distribution of Ca on both sides of the tooth reflects these differences in growth rate and periodicity in two ways. First, given a unit area of tooth, the calcium concentration on the labial side is less than that of the lingual side. Second, whereas the calcium concentration on the labial side declines rapidly from the enamel-dentin junction to the pulp cavity, it is uniformly high across the lingual side because its growth is more continuous at high frequencies.
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  • 3
    Electronic Resource
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    Springer
    Calcified tissue international 32 (1980), S. 29-44 
    ISSN: 1432-0827
    Keywords: Rabbit ; Dentin ; Calcium ; Sulfur ; Periodicity ; Circadian ; Ultradian
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Notes: Summary We have identified a variety of biological rhythms involved in the apposition and mineralization of dentin in the rabbit incisor. Animals were injected during the day or night with lead acetate at 2-week intervals—to provide biological time markers in forming dentin—and transverse undecalcified sections of the lower incisors were prepared for electron microprobe analysis. The positions of the lead markers were identified, and the continuous distribution of calcium and sulfur was measured at 1 µm intervals between the markers. In thin sections stained with hematoxylin after decalcification, the widths of a series of structural increments (bands) were measured with an ocular micrometer. Fourier analysis of the data revealed spectra of structural and compositional rhythms with a range of periodicities which extended from a matter of hours [ultradian (〈24 h)] to days [infradian (〉24 h) and circadian (approximately 24 h)]. The structural and compositional rhythms appeared to be independent to the extent that they did not necessarily have the same periods, or amplitudes. Nor were there simple phase relationships between all of the rhythms. At some times, Ca and S fluctuations are inversely proportional (180° out of phase), but in other cases they are directly proportional or out of phase by varying degrees other than 180°. The analyses thus suggest that calcium and sulfur deposition (representing mineral and glycosaminoglycan deposition, respectively) are not simply inversely proportional, and that the hematoxylin-stained structural increments did not solely reflect differences in the distribution of the mineral components in dentin.
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  • 4
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    Calcified tissue international 13 (1973), S. 73-82 
    ISSN: 1432-0827
    Keywords: Bone ; Apatite ; Hydroxide ; Carbonate ; Infrared
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé L'étude de spectres infra-rouges montre que le minéral osseux de jeune rat et les apatites synthétiques, formés à des pH, force ionique et température physiologiques sont très déficients en ion OH; ces apatites biologiques et synthétiques présentent d'importants défauts internes de maille. En outre, une proportion significative des ions CO3 2- de mineral osseux de rat est structurée de façon lâche dans un environnement amorphe ou superficiel. Les ions carbonate dans l'os chauffé sous vide ou dans les apatites synthétiques formés à pH physiologique paraissent être situés dans des environnements locaux multiples. Le CO3 2- contenu dans ces structures peut se substituer dans des positions PO4 3- et (à un degré moindre) OH−, bien que des variations importantes de ou dans ces positions sont dues à des défauts de maille. Les carbonato-apatites, formés par transformation thermique (600o) de phosphates calciques amorphes et contenant 4–9% de CO3 2-, présentent surtout du CO3 2- dans des environnements OH−. Une recristallisation thermique des apatites biologiques et synthétiques, dans une atmosphère d'air, augmente le contenu en OH− et redispose les positions CO3 2-. Cependant, de telles formations bien cristallisées sont différentes des précurseurs apatitiques.
    Abstract: Zusammenfassung Die Infrarotspektroskopie ergab, daß sowohl natives Rattenknochenmineral als auch synthetische Apatite, welche bei physiologischem pH, Ionenstärke und Temperatur gebildet wurden, an Hydroxydionen stark defizient sind. Es ist ebenfalls ersichtlich, daß diese biologischen und synthetischen Apatitkristalle beträchtliche innere Verzerrungen aufweisen (Gitterdefekte). Weiterhin zeigt ein bedeutender Anteil der CO3 2--Ionen im Rattenknochenmineral eine lockere Struktur in amorpher Umgebung oder an der Oberfläche. In Vakuumerhitzem Knochen oder in synthetischen Apatit (mit physiologischem pH), welches in der Lösung gebildet wurde, scheinen sich die Carbonationen in verschiedenen Umgebungen zu finden. CO3 2- im Inneren dieser Stoffe kann in PO4 3--und (in viel kleineren Mengen) OH−-Positionen ausgetauscht werden, obwohl eine beträchtliche Abweichung von und innerhalb dieser Stellen wahrscheinlich auf Gitterdefekte zurückzuführen ist. Carbonat-Apatite, welche durch die thermische Umwandlung (600°C) von 4–9% CO3 2- enthaltendem amorphem Calciumphosphat gebildet wurden, zeigen in erster Linie in OH−-Umgebung CO3 2-. Die thermische Umkristallisierung von biologischen und synthetischen Apatiten in einer Luftatmosphäre erhöht den OH−-Gehalt und verteilt die CO3 2--Lokalisationen neu. Solche sehr schön kristallisierten Produkte spiegeln jedoch durchaus nicht ihre nativen Apatitvorbilder wider.
    Notes: Abstract Infrared spectral data indicate that both native rat bone mineral and synthetic apatites formed at physiological pH, ionic strength and temperature are extensively deficient in hydroxide ion content; the data also indicate that these biological and synthetic apatites contain considerable internal distortions (lattice defects). In addition, a significant portion of the CO3 2- ions in rat bone mineral is loosely-structured in either an amorphous or surface environment. Carbonate ions in vacuum-heated bone or solution-ripened synthetic (physiological pH) apatites appear to be in multiple local environments. Internal CO3 2- in these materials may be substituted in PO4 3- and (in much lesser amounts) OH− positions, although considerable deviation from or within these sites is probable due to lattice defects. Carbonateapatites produced by thermal conversion (600o) of amorphous calcium phosphates containing 4–9% CO3 2- exhibit CO3 2- mainly in OH− environments. Thermal recrystallization of biological and synthetic apatites in an air atmosphere increases OH− content and reorganizes CO3 2- locales. However, such extremely well-crystallized products are not at all representative of their native apatitic precursors.
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  • 5
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    Calcified tissue international 15 (1974), S. 303-314 
    ISSN: 1432-0827
    Keywords: Diphosphonates ; Calcium ; Mitochondria ; ATPase
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Notes: Abstract The effect of two diphosphonate compounds on calcium handling in rat kidney mitochondria has been studiedin vitro. Initial calcium uptake in the presence of an oxidisable substrate and ATP was not influenced by either diphosphonate tested. The release of accumulated calcium from the mitochondria was, however, delayed by these compounds and the effect was found to be dose dependent. Similarily, a second uptake of calcium, induced by re-addition of ATP following preliminary release, was also modified by diphosphonates, the mitochondrial suspensions incubated with diphosphonates accumulating more calcium than control suspensions. The effect of these compounds could not be detected on three mitochondrial ATPase systems. The results have been discussed in relation to knownin vivo effects of diphosphonates.
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  • 6
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    Calcified tissue international 33 (1981), S. 369-374 
    ISSN: 1432-0827
    Keywords: Histomorphometry ; Bone ; Reproducibility
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Notes: Summary To study bone histomorphometry reproducibility in normal subjects, we performed during orthopedic surgery bone biopsies in 16 post-menopausal women. Each woman had four bone biopsies, two at the usual site in the iliac crest, one on the left and one on the right side, and two other biopsies just behind the usual site, one at each side. We performed measurements of trabecular bone volume, relative osteoid volume, osteoid surfaces, osteoclastic resorption surfaces and calcification front. The average values of the 16 patients were compared, on the one hand, two by two, by a student test, and on the other hand, by a variance analysis. By these two methods the results showed no significant difference between the average values of the 16 patients at each location for any of the histomorphometric parameters studied. However, there was a location variation which was estimated by the intra-individual variation for a given patient. On the other hand, we calculated from the variance analysis the location variance for a group of 10 to 100 patients. In any case all the parameters had a location variation which was high for osteoclastic resorption surfaces and relative osteoid volume when expressed in % of the absolute value of these parameters. The variation of the trabecular bone volume was 0–46. 15% (95% confident limit interval) in a single patient and the hypothetical value of the location variation was 41.6% for a group of 10 patients and 13.0% for a group of 100 patients.
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  • 7
    ISSN: 1432-0827
    Keywords: Amorphous ; Apatite ; Electron Microscopy ; Crystallization ; Precipitation ; Calcium
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé Du phosphate de calcium amorphe (ACP) sèché peut se présenter sous forme discoide ou sphérique. Les particules discoides sont plus fréquents dans les specimens d'ACP sèché, isolés immédiatement après précipitation. Les formes sphériques dominent dans les specimens sèchés provenant de suspensions plus âgés. Les particules discoides résultent de la dessication de l'échantillon. Les sphères peuvent aussi se produire pendant la dessication, mais s'observent aussi dans la solution. Les disques et les sphères ont une origine commune sous la forme d'un agrégat d'ACP hautement hydraté de morphologie inconnue. La formation d'apatite cristallin en solution est intimement associée avec l'ACP. Les premiers cristaux apparaissent à la surface des sphères amorphes et en contact avec les disques amorphes. En cas de sphères, les cristaux initiaux augmentent de taille et forment de nouveaux cristaux par nucléation secondaire jusqu'à ce que les sphères soient enrobées par l'apatite. Cependant, lorsque la transformation est totale, l'apatite ne remplit pas l'espace occupé préalablement par les sphères amorphes dissoutes. Ces observations ne confirment pas le concept d'une conversion d'un état solidein situ dans ce cas mais suggèrent une transition hétérophasique d'un processus de translocation ionique par l'intermédiaire d'une solution. La production de cristaux dans les disques amorphes suggère que l'apatite peut aussi se former directement du précurseur dans la solution.
    Abstract: Zusammenfassung Getrocknetes amorphes Calciumphosphat (ACP) kann scheiben- und kugelförmig auftreten. Die scheibenförmigen Partikel herrschen in getrockneten ACP-Proben vor, welche direkt nach der Fällung isoliert wurden. Die kugeligen Formen herrschen in trockenen Proben aus älteren Suspensionen vor. Die Scheibenbildung ist ein Ergebnis des Trocknungsvorganges. Kugelige Formen können beim Trocknungsvorgang ebenfalls auftreten, sie sind aber in der nativen Suspension ebenfalls anwesend. Scheiben- und Kugelformen scheinen einen gemeinsamen Vorläufer in der Lösung zu haben, welcher ein hochhydratisiertes ACP-Aggregat unbekannter Morphologie zu sein scheint. Die Bildung von kristallinem Apatit in der Lösung steht in engem Zusammenhang mit ACP. Die ersten Kristalle erscheinen auf der Oberfläche der amorphen Kugeln und in Kontakt mit den amorphen Scheiben. Die ursprünglichen Kristalle auf den Kugeloberflächen nehmen an Größe zu und bilden durch sekundäre Nukleation weitere Kristalle, bis die Kugeln in Apatit eingehüllt werden. Wenn die Umwandlung abgeschlossen ist, füllt jedoch das Apatit den Platz nicht aus, der vorher von den aufgelösten amorphen Kugeln eingenommen wurde. Diese Beobachtungen bekräftigen die Auffassung einerin situ-Umwandlung in den festen Zustand bei dem beschriebenen Falle nicht, sondern deuten auf eine heterophasischen Übergang, welcher durch einen lösungsbedingten Ionenverschiebungs-Prozeß gefördert wird. Das Auftreten von Kristallen in den amorphen Scheiben deutet darauf hin, daß sich Apatit auch direkt aus dem Lösungsvorläufer bilden kann.
    Notes: Abstract Dried amorphous calcium phosphate (ACP) can exist in discoidal and spheroidal forms. The disk-shaped particles are most prominent in dried ACP specimens isolated immediately following precipitation. The spherical forms become dominant in dried specimens taken from older suspensions. The disk-like morphology is a result of sample drying. Spherules can also arise during the drying step but are present in the native suspension as well. Both the disks and spherules appear to have a common solution progenitor in the form of a highly hydrated ACP aggregate of unknown morphology. The formation of crystalline apatite in solution is intimately connected with ACP. The first crystals appear on the surface of the amorphous spherules and in contact with the amorphous disks. In the case of the spherules, the initial crystals increase in size and generate additional crystals by secondary nucleation until the spherules become enveloped by apatite. However, when conversion is completed, the apatite does not fill appreciably the space previously occupied by the dissolved amorphous spherules. These observations do not support the concept of anin situ solid state conversion in this case, but indicate a heterophase transition supported by a solution-mediated ion translocation process. The occurrence of crystals in the amorphous disks suggest that apatite can also form directly from the solution progenitor.
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  • 8
    Electronic Resource
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    Calcified tissue international 9 (1972), S. 95-108 
    ISSN: 1432-0827
    Keywords: Amorphous ; Calcium ; Phosphate ; Electron ; Microscopy ; Damage
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé Cinq précipités non-cristallins de phosphate de calcium, préparés à partir de solutions qui varient en pH, degré de saturation et contenu en carbonate, sont examinés par des méthodes physico-chimiques et morphologiques. Des mesures de diffractions électronique et en rayons X et de spectrophotométrie infra-rouge confirment la nature amorphe de chaque précipité. Le microscope électronique par transmission et par balayage démontre que les particules élémentaires des 5 produits synthétiques sont de forme sphérique, quelque soit la méthode de préparation. Quatre des précipités contiennent de petites sphères de taille identique (200 à 1200 Å de diamètre), alors que le dernier précipité, riche en carbonate, contient des particules plus grandes (700 à 2000 Å de diamètre). Ces sphères sont de densité électronique uniforme lorsqu'une intensité de courant, la moins élevée, est utilisée. Un faisceau d'électrons, d'intensité plus élevée, permet de mettre en évidence de nombreux centres, transparents aux électrons, dans chaque particule. In chauffage sous vide à 600° ne modifie pas la nature amorphe des précipités ou la morphologie et la taille des particules élémentaires, bien que la presque totalité de l'eau, contenu dans ces précipités, soit éliminée. L'échauffement ne provoque pas la formation de centres transparents aux électrons. Au contraire, les sphères deviennent résistantes à des dommages, causés par le faisceau. Il semble que le faisceau d'électrons agit sur les atomes d'oxygène et d'hydrogène de la phase aqueuse du phosphate de calcium amorphe et que cette réaction initiale est suivie par le déplacement et/ou la perte d'autres atomes.
    Abstract: Zusammenfassung Fünf nicht-kristalline Calciumphosphat-Niederschläge, welche aus Lösungen mit variierendem pH, Übersättigungsgrad und Karbonatgehalt gewonnen wurden, wurden mit physikochemischen und morphologischen Methoden untersucht. Röntgendiffraktion, Infrarot-Spektrophotometrie und Elektronendiffraktionsmessungen bestätigten die amorphe Natur jedes Niederschlages. Sowohl Durchstrahlungs-, als auch Raster-Elektronenmikroskopie zeigten, daß die nativen Elementarpartikel aller 5 synthetischen Produkte von kugeliger Form und unabhängig von den angewandten Präparativ-Techniken waren. Vier der Niederschläge enthielten Kügelchen von der gleichen Größe (200–1200 Å Durchmesser), während jener mit relativ hohem Karbonatgehalt viel größere Partikel aufwies (700–2000 Å Durchmesser). Die Kügelchen waren für den Elektronenstrahl von einheitlicher Dichte, wenn mit der Stromdichte bei niedrigster brauchbarer Stufe betrachtet. Wurden die Proben stärkeren Elektronenströmen ausgesetzt, so entwickelten sich sogleich in jedem Teilchen zahlreiche elektronendurchlässige Zentren. Erhitzen in Vakuum bis zu Temperaturen von 600° veränderte weder die amorphe Beschaffenheit der Niederschläge noch die Morphologie und Größe ihrer elementaren Partikel, obwohl beinahe alles Wasser, welches in den ursprünglich vorliegenden Proben enthalten war, durch dieses Vorgehen entfernt wurde. Die Hitzebehandlung verursachte keine Bildung von elektronendurchlässigen Zentren sondern machte die Kügelchen im Gegenteil in zunehmendem Maße widerstandsfähig gegenüber Strahlenschädigungen. Diese Befunde lassen vermuten, daß sich die ausgestrahlten Elektronen und die Sauerstoff- oder Wasserstoffatome der wäßrigen Komponente des amorphen Calciumphosphates gegenseitig beeinflussen und daß diese anfängliche Reaktion von einer Verdrängung und/oder einem Verlust anderer Atome gefolgt wird.
    Notes: Abstract Five non-crystalline calcium phosphate precipitates prepared from solutions varying in pH, degree of supersaturation and carbonate content were examined by physicochemical and morphological methods. X-ray diffraction, infrared spectrophotometry and electron diffraction measurements confirmed the amorphous nature of each precipitate. Both transmission and scanning electron microscopy demonstrated that the native elemental particles of all 5 synthetic products were spherical in shape and independent of the preparative procedures employed. Four of the precipitates contained spherules of similar sizes (200–1200 Å in diameter) while the one relatively rich in carbonate exhibited much larger particles (700–2000 Å in diameter). The spherules were uniformly dense to the electron beam when viewed with the current density at its lowest useful level. Exposure to higher electron currents immediately resulted in the development of numerous electron-lucent centers in each particle. Heating in vacuum to temperatures up to 600° did not change the amorphous nature of the precipitates or the morphology and size of their elemental particles even though almost all of the water contained in the original precipitates was removed by this process. Heat treatment did not induce formation of electron-lucent centers. On the contrary it, made the spherules increasingly resistant to beam damage. These findings suggest that the beam electrons interact with the oxygen or hydrogen atoms of the aqueous constituent of the amorphous calcium phosphate and that this initial reaction is followed by displacement and/or loss of other atoms.
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  • 9
    ISSN: 1615-6102
    Keywords: Calcium ; Contraction ; Discophrya ; Ionophore A23187 ; Ruthenium red ; Tentacles
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary The tentacles of the suctorian protozoonDiscophrya collini are stimulated to contract by externally applied Ca2+. The role of extracellular Ca2+ in tentacle contraction was studied by monitoring45Ca2+ uptake, using ionophore A23187 to facilitate membrane transport of calcium and ruthenium red (RR) as an inhibitor of transport. The degree of tentacle retraction was dependent upon external Ca2+ concentration and studies with45Ca2+ using scintillation counting indicated a linear relationship between external Ca2+ concentration and Ca2+ uptake. Uptake of Ca2+ was enhanced in the presence of the ionophore while RR caused little inhibition.45Ca2+ uptake was only partially inhibited by RR when cells were subjected to a Ca2+, ionophore and RR mixture. Grain counts from light microscope autoradiographs after treatment of cells with45Ca2+/ionophore,45Ca2+/RR or45Ca2+ alone showed heavy, light and intermediate labelling respectively. In all instances the grains were evenly distributed within the cell. These observations are interpreted as supporting the suggestion that the ionophore enhances both the uptake of extracellular Ca2+ and release of Ca2+from an internal source, while the RR could only partially prevent movement of Ca2+ through the plasma mebrane. A model is presented suggesting that tentacle retraction is mediated by cytosolic Ca2+ levels which are determined by the fluxing of Ca2+ across the plasma membrane and the membrane of elongate dense bodies which act as internal Ca2+ reservoirs.
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  • 10
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    Calcified tissue international 33 (1981), S. 35-39 
    ISSN: 1432-0827
    Keywords: Copper ; Resorption ; Bone
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Notes: Summary An investigation of the role of copper in bone metabolism was undertaken. Explanted calvaria from 6-day-old mice were grown for 48 h in medium with and without the addition of copper sulfate. Active resorption was found to be significantly inhibited in the presence of copper sulfate concentrations of 10−6M and above. Copper sulfate concentrations of 10−5M and above inhibited hydroxyproline, protein, and DNA synthesis. Lower concentrations were ineffective. The effect of 5 × 10−6M copper sulfate on resorption was reversible. Several other compounds were tested for similar effects and at 5 × 10−6M were found to inhibit bone resorption in the order: copper sulfate 〉 brown gold chloride 〉 sodium aurothiomalate 〉 zinc sulfate 〉 sodium sulfate. The copper sulfate effect was twice that of sodium aurothiomalate, and sodium sulfate was not significantly inhibitory. The results suggest that the high serum copper levels associated with rheumatoid arthritis may reflect the activity of a hypothetical control mechanism of bone resorption. In the diseased state this would act to restore the normal rate of bone resorption.
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