Schachar Ronald A
Department of Physics, University of Texas at Arlington, Dallas, 75360, USA.
Invest Ophthalmol Vis Sci. 2004 Aug;45(8):2691-5. doi: 10.1167/iovs.03-1267.
To determine the topographic effects of zonular tension on the anterior surface of the human crystalline lens.
Real-time topography of the anterior surface of seven fully relaxed, freshly extracted intact, clear, human crystalline lenses aged 3, 17, 45, 54, 54, 56, and 56 years was qualitatively obtained before, during, and after the application of zonular traction. Zonular traction was applied manually either by grasping a group of zonules 180 degrees apart with tying forceps (three lenses), or with micrometers by clamping four portions of the ciliary body that were 90 degrees apart (four lenses).
Zonular tension began with the lenses in the fully relaxed, baseline state. As zonular tension was increased across one meridian of all seven lenses, the center of the anterior surface steepened while the periphery of the anterior surface flattened across that meridian of traction. When the tension was reduced across that meridian of traction, the center of the lens flattened while the periphery steepened in that meridian. Four-point zonular traction applied 90 degrees apart produced symmetrical central steepening (four lenses). Reduction of zonular tension across both orthogonal meridians caused symmetrical central flattening.
These observations reveal that when zonular tension is applied to the fully relaxed lens, the center steepens and its periphery flattens in the meridian (or meridians) in which zonular tension is applied. The reverse of this process demonstrates that as tension is reduced, the center of the lens flattens while the periphery steepens either in the meridian of relaxation or symmetrically when zonular tension is released from two orthogonal meridians. These results are opposite to what would have been predicted on the basis of Helmholtz's theory of accommodation.
确定悬韧带张力对人晶状体前表面的地形学影响。
对7个完全松弛、新鲜摘除的完整、透明的人晶状体(年龄分别为3岁、17岁、45岁、54岁、54岁、56岁和56岁)的前表面进行实时地形学分析,在施加悬韧带牵引之前、期间和之后进行定性观察。悬韧带牵引通过以下方式手动施加:用结扎钳抓住相距180度的一组悬韧带(3个晶状体),或用测微计夹住相距90度的睫状体的四个部分(4个晶状体)。
悬韧带张力始于晶状体处于完全松弛的基线状态时。随着所有7个晶状体的一个子午线方向上的悬韧带张力增加,前表面的中心变陡峭,而在该牵引子午线方向上的前表面周边变平坦。当该牵引子午线方向上的张力降低时,晶状体中心变平坦,而在该子午线方向上周边变陡峭。相距90度施加的四点悬韧带牵引可产生对称的中心陡峭(4个晶状体)。两个正交子午线方向上的悬韧带张力降低会导致对称的中心平坦。
这些观察结果表明,当对完全松弛的晶状体施加悬韧带张力时,在施加悬韧带张力的子午线(或多个子午线)中,晶状体中心变陡峭而周边变平坦。该过程的逆过程表明,随着张力降低,晶状体中心变平坦,而周边在松弛子午线中变陡峭,或者当从两个正交子午线释放悬韧带张力时周边对称变陡峭。这些结果与基于亥姆霍兹调节理论的预测相反。