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使用三氯化六氨合钌和吖啶橙对人龈上牙石和牙菌斑进行形态学和组织化学研究。

Morphological and histochemical study of supragingival human calculus and dental plaque using ruthenium hexammine trichloride and acridine orange.

作者信息

Silvestrini G, Lo Storto S, Bonucci E

机构信息

Department of Human Biopathology, University La Sapienza, Rome, Italy.

出版信息

Eur J Histochem. 1992;36(2):149-59.

PMID:1380849
Abstract

Ruthenium hexammine trichloride (RHT) and acridine orange were used to preserve and visualize anionic groups in human plaque and dental calculus. RHT-reacting material was present on the membrane of micro-organisms and in intermicrobial spaces of the calcifying areas, and seems to correspond to, and derive from, acidic glyco- and phospholipids of the plasma membrane of the micro-organisms. However, the presence of acidic salivary peptidoglycans cannot be ruled out. Two types of calcification were found: extramicrobial and intramicrobial. The former consisted of calcified deposits irregularly scattered in the intermicrobial matrix. They were in close relationship with RHT-reacting material, or were placed inside vesicular structures delimited by a membrane. Intramicrobial calcification consisted of small aggregates of needle-shaped crystals and/or of granular deposits; in both cases, they either masked the whole cytoplasm of the micro-organisms, or were located only over the plasma membrane. These results suggest that mineral deposition occurs in connection with acidic components of intermicrobial matrix, microbial plasma membranes, and cytoplasms. The addition of RHT and acridine orange to fixing and decalcifying solutions yields satisfactory preservation of dental calculus and plaque, and apparently reduces loss of their anionic organic components and increases their electron density. However, these substances are not sufficient to preserve all ultrastructural details in decalcified areas, probably because the inorganic substance prevents reaction of acridine orange and RHT with the organic components of the calcified matrix.

摘要

三氯化六氨合钌(RHT)和吖啶橙被用于保存和显示人牙菌斑及牙结石中的阴离子基团。RHT反应物质存在于微生物膜上以及钙化区域的微生物间隙中,似乎与微生物质膜的酸性糖脂和磷脂相对应并来源于此。然而,酸性唾液肽聚糖的存在也不能排除。发现了两种钙化类型:微生物外钙化和微生物内钙化。前者由不规则散布在微生物间基质中的钙化沉积物组成。它们与RHT反应物质密切相关,或者位于由膜界定的囊泡结构内。微生物内钙化由针状晶体的小聚集体和/或颗粒状沉积物组成;在这两种情况下,它们要么覆盖了微生物的整个细胞质,要么仅位于质膜上方。这些结果表明矿物质沉积与微生物间基质、微生物质膜和细胞质的酸性成分有关。在固定和脱钙溶液中添加RHT和吖啶橙可令人满意地保存牙结石和牙菌斑,并且明显减少其阴离子有机成分的损失并增加其电子密度。然而,这些物质不足以保存脱钙区域中的所有超微结构细节,可能是因为无机物阻止了吖啶橙和RHT与钙化基质的有机成分发生反应。

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