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局部风减弱区对稀疏植被土地上单个灌木元素种子传播的影响。

Effect of the local wind reduction zone on seed dispersal from a single shrub element on sparsely vegetated land.

作者信息

Fu Lin-Tao

机构信息

School of Architecture and Civil Engineering, Chengdu University, Chengdu 610106, Sichuan, China.

出版信息

AoB Plants. 2021 May 21;13(4):plab025. doi: 10.1093/aobpla/plab025. eCollection 2021 Aug.

Abstract

Accurate predictions of seed dispersal kernels are crucial for understanding both vegetation communities and landscape dynamics. The influences of many factors, including the physical properties of seeds, the time-averaged wind speed and the wind turbulence, on seed dispersal have been studied. However, the influence of local wind speed reduction around a single shrub element (e.g. a small patch of scrub) on seed dispersal is still not well understood. Here, the spatial distribution of the wind intensity (represented by the wind friction speed ) around a single shrub element is described, with an emphasis on the variation in the streamwise direction, and assuming that the time-averaged lateral and vertical speeds are equal to zero. The trajectories of the seeds were numerically simulated using a Lagrangian stochastic model that includes the effects of wind turbulence and particle inertia. The patterns of seed deposition with and without the effect of local wind reduction were compared. The variation in seed deposition with changing wind intensity, release height and shrub porosity were also simulated. The simulation results revealed that the local wind reduction increased seed deposition in nearby regions and therefore decreased seed deposition in the regions farther away. Local wind reduction had a greater impact on short-distance dispersal than on long-distance dispersal. Moreover, the dispersal in the circumferential direction decreased once the motion of a seed moving in the streamwise direction was reduced due to the local wind reduction. As the wind intensity and release height increased, the effect of local wind reduction on seed dispersal weakened. Seed dispersal was both wider and farther as the shrub porosity increased. These results may help explain the disagreement between the mechanistic models and the fitting curves in real cases. In addition, the results of this study may improve the currently used mechanistic models by either increasing their flexibility in case studies or by helping explain the variations in the observed distributions.

摘要

准确预测种子扩散核对于理解植被群落和景观动态至关重要。人们已经研究了包括种子物理特性、时间平均风速和风力湍流在内的许多因素对种子扩散的影响。然而,单个灌木元素(例如一小片灌木丛)周围局部风速降低对种子扩散的影响仍未得到充分理解。在此,描述了单个灌木元素周围风强度(以风摩擦速度表示)的空间分布,重点关注流向方向的变化,并假设时间平均横向和垂直速度等于零。使用包含风力湍流和颗粒惯性影响的拉格朗日随机模型对种子轨迹进行了数值模拟。比较了有无局部风减弱影响时的种子沉积模式。还模拟了种子沉积随风强度、释放高度和灌木孔隙率变化的情况。模拟结果表明,局部风减弱增加了附近区域的种子沉积,因此减少了较远区域的种子沉积。局部风减弱对短距离扩散的影响大于对长距离扩散的影响。此外,一旦由于局部风减弱使沿流向移动的种子运动速度降低,圆周方向的扩散就会减少。随着风强度和释放高度的增加,局部风减弱对种子扩散的影响减弱。随着灌木孔隙率的增加,种子扩散范围更广且更远。这些结果可能有助于解释实际案例中机理模型与拟合曲线之间的差异。此外,本研究结果可能会通过提高案例研究中的灵活性或帮助解释观测分布的变化来改进目前使用的机理模型。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/13d2/8266638/97066383e2ba/plab025_fig1.jpg

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