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首页> 外文期刊>日本作物學會紀事 >Studies on the Leaf Orientation-Adjusting Movement in Soybean Plants : II. Fundamental pattern of the leaf orientation-adjusting movement and its significance for the dry matter production
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Studies on the Leaf Orientation-Adjusting Movement in Soybean Plants : II. Fundamental pattern of the leaf orientation-adjusting movement and its significance for the dry matter production

机译:大豆植物中叶定向调整运动的研究:II。叶定向调整运动的基本模式及其对干物质生产的重要性

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Since the leaf orientation-adjusting movement is after all the alteration in the leaf inclination the author devised the analytical method based upon the value of actual measurment of the three elements for determining the leaf orientation: φ (azimuth of leaf), θ (main angle of leaf inclination) and ψ (sub-angle of leaf inclination) given in fig. 1 and 3, and applied the devised analytical method to the soybean leaf acting a typical adjusting movement, thus attempted to make investigations into the fundamental pattern of the leaf orientation-adjusting movement and its significance for the dry matter production. 1. The author took the alteration in the leaf inclination (i.e., leaf orientation-adjusting movement) as the change in the horizontal system of co-ordinate at the intersection between the normal on the leaf surface and the celestial sphere, and proposed such method which clarifies the change by using figure drawing and calculation based upon the value obtained from the actual measurement of the three elements necessary for the determining the leaf inclination. The method to draw figures was indicated in fig. 2 and 4 and the calculation was made by using the following expression. 1) The expressions to find out the horizontal system of co-ordinate P (intersection of the normal on the leaf surface with the celestial sphere) : x=-cos φ sin θ cos ψ + sin φ sin ψ y=-sin φ sin θ cos ψ - sin φ cos ψ z=cos θ cos ψ (1) 2) The expressions to find out φ' (azimuth) and θ' (altitude) of the normal on the leaf surface: φ'=tan-1y/x θ'=sin-1z (2) 3) The expressions to find out the angle α of the direction of the sun (or the brightest light in the sky) with the normal on the leaf surface: α=cos-1 (cos φs cos θs·x+sin φs cos θs·y+sin θs·z) (3) where φs : Azimuth of the sun θs : Altitude of the sun Notes : Azimuth : Oo : south, + : the east circuit line, and - : the west circuit line Main-angle of leaf inclination (θ) : + : upward inclination, - : downward inclination Sub-angle of leaf inclination (ψ) : + : turning-up to the left direction from the leaf base to the leaf apex, - : turning-up to the right direction from the leaf base to the leaf apex 2. The soybean plant was grown in a pot in isolation. By taking Madison variety acting a typical adjusting movement as a sample, the actual measurement was made extending over the duration from early to mid-September, 1965, in order to measure the three elements necessary for determining the leaf inclination for each of the leaflets in the compound leaf according to the selected hours on fine days and according to the climatic conditions at the same hours. Basing upon the value obtained from this actual measurement, the changes in the co-ordinate of normal on the leaf surface were observed by the figure drawing and calculating methods. Thus the fundamental pattern of the leaf orientation-adjusting movement was investigated. As to the changes in the three elements measured according to the selected hours on fine days, at first, the changes in each leaflet was observed according to the selected hours (changes in the compound leaf on the uppermost node are given in fig. 5), and the changes were classified according to the selected hours (fig. 6). α was also obtained by using tha calculating method (fig. 7). The changes due to the climatic conditions were observed also in the same ways (figs. 9 and 10). 3. The survey results indicated that, in the case of isolated individual small in the leaf number, as in the case with the present report, a remarkable adjusting movement was shown by the entire leaves. [the rest omitted]
机译:由于叶片定向调整运动是在叶倾角的所有改变之后,作者基于用于确定叶片定向的三个元件的实际测量值的分析方法:φ(叶子的方位角),θ(主角叶片倾斜度)和△(叶片倾斜角)在图2中给出的。在图1和3中,并将设计的分析方法应用于作用典型调节运动的大豆叶,从而试图对叶片定向调节运动的基本模式进行调查及其对干物质产生的重要性。 1,作者在叶倾角(即叶定向调节运动)中恢复了叶倾角(即,叶定向调节运动)作为叶片表面和天体球体之间的正常交叉口的坐标系统的变化,并提出了这种方法通过使用图形绘图和基于从确定叶倾斜所需的三个元件的实际测量获得的值来阐明变更。绘制图的方法在图2中示出。通过使用以下表达式进行图2和4和计算。 1)要查找协调P的水平系统的表达式(用天体球体上的叶片表面上的正常):x =-COSφINθCOSψ+ SINφINψY= -SINφIN θcosψ - sinφcosψz = cosθcosψ(1)2)在叶面上找到φ'(方位角)和θ'(高度)的表达式:φ'= tan-1y / xθ'= sin-1z(2)3)用正常的叶面上的阳光(或天空中最亮光灯中最亮光)的角度α的表达式:α= COS-1(COS φscosθs·x +sinφscosθs·y +sinθs·z)(3)其中φs:太阳的方位角θs:太阳的高度:azimuth:oo:south,+:东路线,和 - :西路线的叶片倾斜度(θ):+:向上倾斜, - :向下倾斜子角度的叶倾角(ψ):+:从叶底到左侧方向转向叶子顶点, - :从叶碱到叶子顶部的向右方向转动到叶子顶点2.大豆植物生长在一个孤立的锅里。通过将麦迪逊品种作用作为样本的典型调整运动,从1965年9月初到9月至9月中旬的持续时间进行实际测量,以测量确定每个传单中的叶片倾角所需的三个元件复合叶根据选定的时间在细日间,并根据相同时间的气候条件。基于该实际测量获得的值,通过图纸图和计算方法观察到叶面上正常的坐标的变化。因此,研究了叶定向运动的基本模式。关于根据细日测量的三个元素的变化,首先,根据所选择的时间观察每个叶片的变化(上最上节节点上的复合叶片的变化)观察到。 ,并且根据所选小时(图6)对变化进行分类。通过使用THA计算方法也获得α(图7)。以相同的方式观察到由于气候条件引起的变化(图9和10)。 3.调查结果表明,在叶片号中小的单个小的情况下,如本报告的情况下,整个叶子显示出显着的调节运动。 [省略了]

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