Lovvorn J R, Croll D A, Liggins G A
Department of Zoology, University of Wyoming, Laramie, WY 82071, USA, Institute of Marine Sciences, University of California, Santa Cruz, CA 95064, USA.
J Exp Biol. 1999 Jul;202(Pt 13):1741-52. doi: 10.1242/jeb.202.13.1741.
For fast flapping flight of birds in air, the maximum power and efficiency of the muscles occur over a limited range of contraction speeds and loads. Thus, contraction frequency and work per stroke tend to stay constant for a given species. In birds such as auks (Alcidae) that fly both in air and under water, wingbeat frequencies in water are far lower than in air, and it is unclear to what extent contraction frequency and work per stroke are conserved. During descent, compression of air spaces dramatically lowers buoyant resistance, so that maintaining a constant contraction frequency and work per stroke should result in an increased swimming speed. However, increasing speed causes exponential increases in drag, thereby reducing mechanical versus muscle efficiency. To investigate these competing factors, we have developed a biomechanical model of diving by guillemots (Uria spp.). The model predicted swimming speeds if stroke rate and work per stroke stay constant despite changing buoyancy. We compared predicted speeds with those of a free-ranging Brünnich's guillemot (U. lomvia) fitted with a time/depth recorder. For descent, the model predicted that speed should gradually increase to an asymptote of 1.5-1.6 m s-1 at approximately 40 m depth. In contrast, the instrumented guillemot typically reached 1.5 m s-1 within 10 m of the water surface and maintained that speed throughout descent to 80 m. During ascent, the model predicted that guillemots should stroke steadily at 1.8 m s-1 below their depth of neutral buoyancy (62 m), should alternate stroking and gliding at low buoyancies from 62 to 15 m, and should ascend passively by buoyancy alone above 15 m depth. However, the instrumented guillemot typically ascended at 1.25 m s-1 when negatively buoyant, at approximately 1.5 m s-1 from 62 m to 25 m, and supplemented buoyancy with stroking above 25 m. Throughout direct descent, and during ascent at negative and low positive buoyancies (82-25 m), the guillemot maintained its speed within a narrow range that minimized the drag coefficient. In films, guillemots descending against high buoyancy at shallow depths increased their stroke frequency over that of horizontal swimming, which had a substantial glide phase. Model simulations also indicated that stroke duration, relative thrust on the downstroke versus the upstroke, and the duration of gliding can be varied to regulate swimming speed with little change in contraction speed or work per stroke. These results, and the potential use of heat from inefficient muscles for thermoregulation, suggest that diving guillemots can optimize their mechanical efficiency (drag) with little change in net physiological efficiency.
对于鸟类在空中快速扑翼飞行而言,肌肉的最大功率和效率出现在有限的收缩速度和负荷范围内。因此,对于给定的物种,收缩频率和每次扑翼的功往往保持恒定。在海雀(海雀科)等既能在空中又能在水下飞行的鸟类中,在水中的拍翅频率远低于在空中时,目前尚不清楚收缩频率和每次扑翼的功在多大程度上得以保留。在下降过程中,空气腔的压缩显著降低了浮力阻力,因此保持恒定的收缩频率和每次扑翼的功应会导致游泳速度增加。然而,速度增加会导致阻力呈指数增加,从而降低机械效率与肌肉效率之比。为了研究这些相互竞争的因素,我们开发了一种海鸠(海鸠属)潜水的生物力学模型。该模型预测了在浮力变化时,如果 stroke rate(应是“划水频率”之类意思,此处原文可能有误,推测为 stroke rate)和每次划水的功保持恒定的情况下的游泳速度。我们将预测速度与一只佩戴时间/深度记录器的自由放养的厚嘴海鸠(乌燕鸥)的速度进行了比较。对于下降过程,该模型预测速度应逐渐增加至在约40米深度处达到1.5 - 1.6米/秒的渐近线。相比之下,配备仪器的海鸠通常在水面10米内达到1.5米/秒,并在下降至80米的整个过程中保持该速度。在上升过程中,该模型预测海鸠在低于其中性浮力深度(62米)时应以1.8米/秒稳定划水,在62米至15米的低浮力状态下应交替划水和滑行,在深度超过15米时应仅靠浮力被动上升。然而,配备仪器的海鸠在负浮力时通常以1.25米/秒上升,在62米至25米时约为1.5米/秒,并在超过25米时通过划水补充浮力。在整个直接下降过程以及在负浮力和低正浮力(82 - 25米)上升过程中,海鸠将其速度保持在一个狭窄范围内,使阻力系数最小化。在影片中,在浅深度对抗高浮力下降的海鸠相对于水平游泳增加了其划水频率,水平游泳有一个相当长的滑行阶段。模型模拟还表明,划水持续时间、下划与上划的相对推力以及滑行持续时间可以变化,以调节游泳速度,而收缩速度或每次划水的功变化很小。这些结果,以及低效肌肉产生的热量用于体温调节的潜在用途,表明潜水海鸠可以在净生理效率变化很小的情况下优化其机械效率(阻力)。