Miller Patrick J O, Johnson Mark P, Tyack Peter L, Terray Eugene A
Sea Mammal Research Unit, University of St Andrews, Fife, KY16 8LB, Scotland.
J Exp Biol. 2004 May;207(Pt 11):1953-67. doi: 10.1242/jeb.00993.
Drag and buoyancy are two primary external forces acting on diving marine mammals. The strength of these forces modulates the energetic cost of movement and may influence swimming style (gait). Here we use a high-resolution digital tag to record depth, 3-D orientation, and sounds heard and produced by 23 deep-diving sperm whales in the Ligurian Sea and Gulf of Mexico. Periods of active thrusting versus gliding were identified through analysis of oscillations measured by a 3-axis accelerometer. Accelerations during 382 ascent glides of five whales (which made two or more steep ascents and for which we obtained a measurement of length) were strongly affected by depth and speed at Reynold's numbers of 1.4-2.8x10(7). The accelerations fit a model of drag, air buoyancy and tissue buoyancy forces with an r(2) of 99.1-99.8% for each whale. The model provided estimates (mean +/- S.D.) of the drag coefficient (0.00306+/-0.00015), air carried from the surface (26.4+/-3.9 l kg(-3) mass), and tissue density (1030+/-0.8 kg m(-3)) of these five animals. The model predicts strong positive buoyancy forces in the top 100 m of the water column, decreasing to near neutral buoyancy at 250-850 m. Mean descent speeds (1.45+/-0.19 m s(-1)) were slower than ascent speeds (1.63+/-0.22 m s(-1)), even though sperm whales stroked steadily (glides 5.3+/-6.3%) throughout descents and employed predominantly stroke-and-glide swimming (glides 37.7+/-16.4%) during ascents. Whales glided more during portions of dives when buoyancy aided their movement, and whales that glided more during ascent glided less during descent (and vice versa), supporting the hypothesis that buoyancy influences behavioural swimming decisions. One whale rested at approximately 10 m depth for more than 10 min without fluking, regulating its buoyancy by releasing air bubbles.
拖拽力和浮力是作用于潜水海洋哺乳动物的两种主要外力。这些力的强度会调节运动的能量消耗,并可能影响游泳方式(步态)。在此,我们使用高分辨率数字标签记录了利古里亚海和墨西哥湾23头深潜抹香鲸的深度、三维方向以及听到和发出的声音。通过分析三轴加速度计测量的振荡,确定了主动推进与滑行的时间段。在雷诺数为1.4 - 2.8×10⁷时,五头鲸(进行了两次或更多次陡峭上升且我们获得了体长测量值)的382次上升滑行过程中的加速度受到深度和速度的强烈影响。加速度符合一个包含拖拽力、空气浮力和组织浮力的模型,每头鲸的拟合度r²为99.1 - 99.8%。该模型给出了这五头动物的拖拽系数(0.00306±0.00015)、从水面携带的空气量(26.4±3.9升/千克体重)以及组织密度(1030±0.8千克/立方米)的估计值(平均值±标准差)。该模型预测在水柱顶部100米处有很强的正浮力,在250 - 850米处降至接近中性浮力。平均下降速度(1.45±0.19米/秒)比上升速度(1.63±0.22米/秒)慢,尽管抹香鲸在下降过程中稳定划水(滑行占5.3±6.3%),而在上升过程中主要采用划水 - 滑行游泳方式(滑行占37.7±16.4%)。在潜水过程中,当浮力有助于它们移动时,鲸滑行的时间更多,并且在上升过程中滑行较多的鲸在下降过程中滑行较少(反之亦然),这支持了浮力影响行为性游泳决策的假设。一头鲸在约10米深度处静止超过10分钟,没有摆动尾鳍,通过释放气泡来调节浮力。