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Conyza canadensis seed ascent in the lower atmosphere

机译:加拿大低层Conyza canadensis种子上升

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Long-distance dispersal of wind dispersed plant seed is dependent on seeds ascending in the atmosphere's surface boundary layer (SL). However, seed dispersal research often focuses on the near-surface dynamics of abscission and deposition, with little attention paid to seed ascent and transport beyond the surface boundary layer. Our research sought to estimate the vertical seed density flux of Conyza canadensis, a common agricultural weed, in the surface boundary layer. Using a 2.7ha field infested with Conyza canadensis, the vertical seed concentration profile was measured on 5 days, three times per day while simultaneously monitoring micrometeorological conditions to connect the mechanisms of release with the process of ascent. Vertical seed sampling was conducted from two to six meters above ground level using removable screen frames. Remotely piloted airplanes were used to quantify seed concentration at 68 and 120m above ground level and provide a connection between near surface dynamics and dynamics higher in the SL. Seed flux density (area under seed concentration curve) decreased with height and decreased from morning to afternoon. The seed flux density was significantly correlated with mean mechanical turbulence and the interaction of mean mechanical and mean thermal turbulence, supporting earlier research of meteorological effects on seed dispersal. While fewer total seeds were collected in the afternoon, more seeds were collected at 68 and 120m during this period and may suggest more seeds were present in the upper SL where dispersal distance may be greater. Seeds collected above the SL will potentially be carried for hours before descending, depositing seeds in the range of 2-122m, and influencing a much greater area than seeds unable to ascend through the lower SL. While this range is very wide, the dispersal distances reported herein are several orders of magnitude greater than previously reported for plants. These findings are all the more striking since the study species has evolved resistance to glyphosate herbicide, an herbicide now widely used in soybean, cotton, and corn crops in the US. Therefore, aerial transport of C. canadensis seeds carrying genes coding for glyphosate resistance enables seed to move tens or hundreds of kilometers in a single dispersal event, a spread rate corroborated by number of cases of reported glyphosate resistance occurrences in North America.
机译:风分散的植物种子的长距离散布取决于种子在大气表面边界层(SL)中上升。但是,种子传播研究通常集中在脱落和沉积的近地表动力学上,很少关注种子的上升和表面边界层以外的运输。我们的研究试图估计加拿大Conyza canadensis(一种常见的农业杂草)在表面边界层的垂直种子密度通量。使用一个感染了加拿大康乃滋的2.7公顷田地,垂直种子浓度分布图每5天测量一次,每天3次,同时监控微气象条件,以将释放机理与上升过程联系起来。使用可移动的筛网框架在地面上方两到六米处进行垂直种子采样。远程驾驶飞机用于量化地面以上68和120m处的种子浓度,并提供近地面动力学与SL中较高动力学之间的联系。种子通量密度(种子浓度曲线下的面积)随着高度的增加而降低,从早上到下午降低。种子通量密度与平均机械湍流以及平均机械湍流和平均热湍流之间的相互作用显着相关,这支持了气象对种子传播的影响的早期研究。虽然下午收集的种子较少,但在此期间分别在68和120m处收集了更多种子,这可能表明在上层SL中存在更多的种子,那里的散布距离可能更大。在SL上方收集的种子在下降之前可能会被携带数小时,在2-122m的范围内沉积,影响范围比无法通过较低SL上升的种子更大。尽管该范围非常宽,但是本文报道的分散距离比以前报道的植物大几个数量级。自从研究物种对草甘膦除草剂产生抗药性以来,这些发现更加惊人。草甘膦除草剂现已在美国的大豆,棉花和玉米作物中广泛使用。因此,携带加拿大草甘膦抗性编码基因的加拿大念珠菌种子的空中运输能够使种子在单个扩散事件中移动数十或数百公里,其传播速度与在北美报道的草甘膦抗药性案例数相符。

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