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首页> 外文期刊>Ecological Applications >Interannual variation in leaf expansion and outbreak of a teak defoliator at a teak stand in northern Thailand
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Interannual variation in leaf expansion and outbreak of a teak defoliator at a teak stand in northern Thailand

机译:泰国北部柚木摊位的柚木落叶的叶片膨胀和爆发的年际变化

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摘要

The leaf area index (LAI) is a key factor affecting tree growth in forests. Following the outbreak of a defoliator, the LAI declines, serving as a useful indicator in forest management. In this study, daily radiative transmittance from above the canopy, which decreases exponentially with increasing LAI, was measured in a teak plantation (Tectona grandis L. f.) in northern Thailand from March through July in 2001-2008. Volumetric soil moisture was also measured at depths of 0.1, 0.2, 0.4, and 0.6 m. The negative logarithmic value of the ratio of daily downward solar radiation on the forest floor to that above the canopy (NLR;-ln[S_b↓/S↓.]), was calculated as an indicator of leaf flush and subsequent leaf expansion. The NLR data indicated that leaf expansion began in late March and continued to the beginning of May during all eight years (with the day the leaves began to expand defined as DB). In addition, the peak in NLR values (NLR_P), corresponding to the lowest value of a 99% confidence interval, occurred in July. The day when NLR first reached NLRP was defined as DP, which always occurred in June, 31-85 days after D_B. The NLR indicated an increase in the population of Hyblaea puera (a teak defoliator) that was associated with greatly decreased leaf areas during two growth periods (D_B-D_P): the earliest D_B-D _P in 2001 and the second-earliest D_B-D_P in 2008. In almost all cases, soil moisture data indicated that leaf expansion occurred after increases in soil moisture at depths of 0.1-0.4 m even without increases at 0.6 m; in contrast, increases in shallow soil moisture (0.1-0.2 m) were insufficient to trigger leaf expansion at the stand level. Periods of soil drought at 0.1-0.4-m soil depths inhibited leaf expansion, resulting in prolongation of the interval between D_B and D_P during those years in which the D_B's occurred chronologically close to one another. Moreover, when drought did not limit leaf expansion, the D _B-D_P growth periods characterized by earlier D _B's tended to be longer than those with later D_B's.
机译:叶面积指数(LAI)是影响森林树木生长的关键因素。落叶后,LAI下降,成为森林管理中的有用指标。在这项研究中,从2001年至2008年3月至7月,在泰国北部的柚木种植园(Tectona grandis L. f。)中测量了冠层上方每日辐射透射率,该辐射率随LAI的增加呈指数下降。还在0.1、0.2、0.4和0.6 m的深度处测量了土壤的体积水分。计算出每天在林地上向下的太阳辐射与树冠上方的太阳辐射之比的负对数值(NLR; -ln [S_b↓/ S↓。]),以作为叶片冲刷和随后叶片扩张的指标。 NLR数据表明,叶片膨胀开始于3月下旬,并在整个八年中一直持续到5月初(叶片开始膨胀的日子定义为DB)。此外,NLR值(NLR_P)的峰值对应于99%置信区间的最低值,出现在7月。 NLR首次到达NLRP的日期定义为DP,通常发生在D_B之后31-85天的6月。 NLR表明,Hyblaea puera(柚木落叶)的人口增加,这与两个生长时期(D_B-D_P)的叶面积大大减少有关:2001年最早的D_B-D_P和第二最早的D_B-D_P在2008年。几乎所有情况下,土壤湿度数据都表明,在0.1-0.4 m深度的土壤水分增加后,即使在0.6 m处没有增加,叶片膨胀才发生。相反,浅层土壤水分(0.1-0.2 m)的增加不足以触发林分水平的叶片膨胀。在土壤深度为0.1-0.4-m的土壤干旱时期抑制了叶子的扩张,从而导致D_B和D_P之间的时间间隔在时间上彼此接近。此外,当干旱不限制叶片扩张时,以较早的D _B为特征的D _B-D_P生长期往往比较晚的D _B更长。

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