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首页> 外文期刊>Field Crops Research >Toposequential effects on water balance and productivity in rainfed lowland rice ecosystem in Southern Laos.
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Toposequential effects on water balance and productivity in rainfed lowland rice ecosystem in Southern Laos.

机译:可能对老挝南部雨养低地水稻生态系统的水平衡和生产力产生后续影响。

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摘要

In the Mekong region, most paddies in rainfed lowland rice (Oryza sativa L.) lie in a sequence on gentle sloping land, and grain yield (GY) often depends on the toposequence position. There is, however, lack of information on toposequential effects on field water supply in rainfed lowland rice and how that influences GY. A total of eight field experiments were carried out on sandy, coarse-textured soils in Southern Laos (Champassak Province and Savannakhet Province) over three wet seasons (2000-2002). Components of the water balance, including downward and lateral water movement (D and L, respectively), were quantified at three different positions along toposequences (top, middle and bottom). GY, days-to-flower (DTF) and rainfall were measured, and the water productivity (WP) was determined. In most experiments, standing water disappeared first in the top position and gradually in lower positions. This was associated with the observation that when there was standing water in the field, the higher position had larger D in both the provinces and also larger L in Champassak Province. However, in one experiment, water loss appeared later in the higher position, as the result of lower L, apparently due to some water inputs other than rainfall occurring at this position. Despite larger D plus L at the top position, seasonal sum of D and L were not much affected by the toposequence position, as the daily rate of D plus L became minimal when the standing water was lost earlier in the top position. Lower GY was associated with earlier disappearance of standing water from the field. Relatively low GY was expected in the top toposequence position. This was clearly shown in the toposequence of Phonthong, Champassak Province, as the timing of standing water disappearance relative to flowering was earlier in the top position. Variation in GY across the toposequence positions was coupled with the WP variation, and both GY and WP tended to decline with increased DTF. Therefore, variation in productivity of rainfed lowland rice across toposequence positions depends mainly on the field water status around flowering time..
机译:在湄公河地区,雨养低地水稻(Oryza sativa L.)中的大多数稻米顺序排列在平缓的坡地上,谷物产量(GY)通常取决于后序位置。但是,缺乏关于雨养低地稻田对田间水供应的后续影响以及如何影响甘薯的信息。在三个湿季(2000年至2002年),对老挝南部(昌帕萨克省和沙湾拿吉省)的沙质粗糙纹理土壤进行了总共八次田间试验。水平衡的组成部分,包括向下和横向的水运动(分别为D和L),在沿后序的三个不同位置(顶部,中间和底部)进行了量化。测量了GY,开花天数(DTF)和降雨量,并确定了水生产率(WP)。在大多数实验中,死水首先在顶部消失,然后在下部逐渐消失。这与以下观察结果有关:当田间有积水时,较高的位置在两个省中都有较大的D,而在Champassak省中也有较大的L。但是,在一个实验中,由于L值较低,结果在较高位置出现了失水现象,这显然是由于该位置发生了降雨以外的一些水输入。尽管最高位置的D加L较大,但是D和L的季节总和受后置位置的影响不大,因为当最高位置较早失去静水时,D加L的日速率变得最小。 GY降低与田间死水较早消失有关。预期最高后序位置的GY相对较低。尚帕萨克省蓬蓬的后世现象清楚地表明了这一点,因为死水相对于开花的消失时间早于最高位置。前后序列中GY的变化与WP的变化有关,随着DTF的增加,GY和WP均趋于下降。因此,雨养低地水稻在不同位置的生产力差异主要取决于开花时间附近的田间水分状况。

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