Friskopp J, Hammarström L
J Periodontol. 1980 Oct;51(10):553-62. doi: 10.1902/jop.1980.51.10.553.
The morphology of supragingival and subgingival calculus on extracted teeth was studied with the scanning electron microscope. Oral, crevicular, and fracture surfaces were examined. Both subgingival and supragingival calculus had a heterogenous core covered by a soft, loose layer of microorganisms. On supragingival calculus this layer was dominated by filamentous microorganisms while subgingival calculus was covered by a mixture of cocci, rods and filaments. The supragingival covering of filaments was oriented with the filaments approximately perpendicular to and in direct contact with the underlying dense calculus. This arrangement was rarely seen subgingivally where there was no distinct pattern of orientation. Some of the specimens of sub- and supragingival calculus were treated with sodium-hypochlorite. These lost the soft covering, and channels the same size as the filamentous organisms were found penetrating into the calculus. They were oriented prependicular to the surface in supragingival calculus but had no specific direction in subgingival calculus. The appearance of the channels supports the concept that calcification starts between the microorganisms in both subgingival and supragingival calculus.
利用扫描电子显微镜研究了拔除牙齿上龈上和龈下牙石的形态。对口腔、龈沟和断面进行了检查。龈下和龈上牙石均有一个异质核心,表面覆盖着一层柔软、疏松的微生物层。在龈上牙石上,这一层以丝状微生物为主,而龈下牙石则覆盖着球菌、杆菌和丝状菌的混合物。龈上的丝状覆盖物中,丝状物大致垂直于下方致密牙石并与之直接接触。这种排列在龈下很少见到,龈下没有明显的定向模式。一些龈下和龈上牙石标本用次氯酸钠处理。这些标本失去了柔软的覆盖物,发现有与丝状生物体大小相同的通道穿透到牙石中。在龈上牙石中,这些通道垂直于表面排列,但在龈下牙石中没有特定方向。这些通道的外观支持了这样一种观点,即龈下和龈上牙石中的钙化始于微生物之间。