Oganov V S, Grigor'ev A I, Voronin L I, Rakhmanov A S, Bakulin A V, Schneider V S, LeBlanc A D
Aviakosm Ekolog Med. 1992 Sep-Dec;26(5-6):20-4.
A technique of quantitative digital roentgenography (QDR) being a current modification of dual photon absorptiometry (DPA) was used to measure bone mineral density (BMD) in the crewmembers of the 6-9th expeditions onboard Mir orbital station after space missions of 132 to 176 days in duration. Total mineral losses were, on average, 0.4% of a preflight level, and in the most test subjects the postflight BMD of the skull, ribs and arms increased and that of lumbar vertebrae, pelvis and legs decreased. The most marked local postflight mineral losses occurred in the proximal femur bone (the femoral neck and the greater trochanter--up to 14%). The observed changes did not depend on flight duration. These findings are being compared to the results of similar studies conducted during the 120-day (NASA) and 370-day (IBMP) hypokinesia experiments. The possibility of existing the general mechanism of modifying mineral status of the skeleton due to different situation related deficiency of musculoskeletal load.
一种作为双能光子吸收法(DPA)当前改进技术的定量数字X线摄影术(QDR),被用于测量和平号轨道站第6至9次考察队成员在为期132至176天的太空任务后的骨矿物质密度(BMD)。矿物质总损失平均为飞行前水平的0.4%,在大多数测试对象中,飞行后颅骨、肋骨和手臂的骨密度增加,而腰椎、骨盆和腿部的骨密度降低。飞行后最明显的局部矿物质损失发生在股骨近端(股骨颈和大转子——高达14%)。观察到的变化不取决于飞行持续时间。这些发现正在与在120天(美国国家航空航天局)和370天(苏联科学院生物医学问题研究所)运动减少实验期间进行的类似研究结果进行比较。由于与肌肉骨骼负荷缺乏相关的不同情况,存在改变骨骼矿物质状态的一般机制的可能性。