首页> 外文期刊>日本作物學會紀事 >Studies on the Growth Phase and Effect of Fertilizer Application to Rice Plants in Malaya : III. Seasonal variations of evapo-transpiration and evapo-transpiration ratio of indica rice plants with special reference to leaf area
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Studies on the Growth Phase and Effect of Fertilizer Application to Rice Plants in Malaya : III. Seasonal variations of evapo-transpiration and evapo-transpiration ratio of indica rice plants with special reference to leaf area

机译:肥料应用对马来亚水稻植物的生长阶段及其影响研究:III。叶片区特殊参考籼稻植物蒸发蒸腾和蒸发蒸腾率的季节变异

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The seasonal changes in irrigation requirement were measured 1967 to 1969 in the Northwest coast of West Malaysia using three varieties, Ria (IR-8), Bahagia (sister line of IR-5) and Radin Ebos 33 (local long term variety) under flooded field condition. The evaporation ratio (E/Em, E: evaporation from water surface in paddy field, Em: pan evaporation in meteorological observation field), transpiration ratio (T/Em, T: transpiration from plant surface) and evapo-transpiration ratio (ET/Em) were mainly used for discussion in order to eliminate the weather effects. The results obtained are summarized as follows: 1. The E/Em gradually decreased due to the mutual shading of paddy plants according to the increase of leaf area index (LAI) and dry matter of plants (table 1, fig.1-3). On the contrary against for the above the T/Em and ET/Em were smaller during the early stage of growth and later on increased gradually. Two peaks were noticed the maximum tillering stage as a rule which fell roughly on 45 days after transplanting and heading stage (fig.1-2). The fornler peak was lower than the later, followed by a depression between two peaks. 2. The changes in the T/Em were largely due to the size of growth particularly LAI. However this was not always parallel with LAI and the exponential function was obtained between the T/Em per unit leaf area and LAI (fig.3). As such the T/Em per unit leaf area was constant and scarcely affected by growth when LAI became larger than 3.5. The fact and a depression of transpiration mentioned above might be largely due to the mutual shading of paddy plants. 3. The mean value of T/Em was about 0.6 and was almost equal to that of E/Em (table 1). The ET/Em showed the mean value of l.2 though it varied 1.0-1.2 during the early stage, 1.2∼1.3 during the maximum tillering stage and 1.4 during heading stage (fig.1∼2). Daily mean value of ET were 6.4 mm in the Off season (dry period) and 5.9 mm in the Main esason (wet period). It was also found that the longer in growing period, the greater in total ET. 4. The seasonal changes of ET was the dominant factor which caused the changes in irrigation requirement. Under the continuous flooded condition, the irrigation requirement including rainfall for Bahagia 130-140 days variety, was estimated approximately to be l, 340 mm (9.5 mm/day) during the 0ff season and 980 mm (7.4 mm/day) during the Main season (table 2). The 38% difference in the irrigation requirement could be attributed to the greater Em and lO days increase of growing period of the former.
机译:灌溉要求的季节性变化是在西马来西亚西北部的1967年到1969年,使用了三个品种,RIA(IR-8),乳酪线(IR-5)和Radin Ebos 33(当地长期品种)淹没了现场条件。蒸发率(E / EM,E:从水面蒸发稻田,气象观察场中的釜蒸发),蒸发比(T / Em,T:植物表面的蒸腾)和蒸发蒸腾率(ET / EM主要用于讨论以消除天气效应。所获得的结果总结如下:1。由于叶面积指数(LAI)和植物干物质的增加,因此e / e逐渐减少了水稻植物(表1,图1,图1) 。相反,在上述上述情况下,在增长的早期阶段,后来逐步增加T / ED和ET / ET。注意到两座峰值是一个最大的分蘖阶段,通常在移植和标题阶段(图2)后45天大致下降。 Fornler峰值低于后来,然后在两个峰之间的凹陷。 2. T / EM的变化很大程度上是由于含量的增长大小。然而,这并不总是与LAI并不平行,并且在每单位叶面积和LAI(图3)之间获得指数函数。由于当Lai大于3.5时,每单位叶面积的T / Em恒定并且几乎没有增长影响。上述事实和抑制的蒸腾可能在很大程度上是由于水稻植物的相互遮阳。 3. T / EM的平均值约为0.6,几乎等于E / EM(表1)。 ET / ET / ET显示L.2的平均值虽然在早期的阶段中变化1.0-1.2,但在最大分蘖期期间1.2〜3.3和标题阶段期间的1.4(图1~2)。 ET的每日平均值在淡季(干燥期)和5.9毫米的主要esason(潮湿时期)中为6.4毫米。还发现,生长期间的时间越长,总量越大。 4. ET的季节变化是导致灌溉需求变化的主导因素。在连续洪水的情况下,灌溉需求包括降雨量为Bahagia 130-140天,估计在0F季节期间的L,340 mm(9.5毫米/天),主要是980毫米(7.4毫米/天)季节(表2)。灌溉需求的38%差异可能归因于更大的EM和罗斯成长时期的增加。

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