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Linking the patterns in soil moisture to leaf water potential, stomatal conductance, growth, and mortality of dominant shrubs in the Florida scrub ecosystem

机译:将土壤水分的模式与佛罗里达灌丛生态系统中主要灌木丛的叶片水势,气孔导度,生长和死亡率联系起来

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Patterns in soil moisture availability affect plant survival, growth and fecundity. Here we link patterns in soil moisture to physiological and demographic consequences in Florida scrub plants. We use data on different temporal scales to (1) determine critical soil moisture content that leads to loss of turgor in leaves during predawn measurements of leaf water status (Ψ crit), (2) describe the temporal patterns in the distribution of Ψ crit, (3) analyze the strength of relationship between rainfall and soil moisture content based on 8 years of data, (4) predict soil moisture content for 75 years of rainfall data, and (5) evaluate morphological, physiological and demographic consequences of spring 2006 drought on dominant shrubs in Florida scrub ecosystem in the light of water-uptake depth as determined by stable isotope analysis (δ18O). Based on 1998–2006 data, the soil moisture content at 50 cm depth explained significant variation in predawn leaf water potential of two dominant shrubs, Quercus chapmanii and Ceratiola ericoides (r 2 = 0.69). During 8 years of data collection, leaves attained Ψ crit only during the peak drought of 2000 when the soil moisture fell below 1% by volume at 50 and 90 cm depth. Precipitation explained a significant variation in soil moisture content (r 2 = 0.62). The patterns in predicted soil moisture for 75 year period, suggested that the frequency of drought occurrence has not increased in time. In spring 2006, the soil reached critical soil moisture levels, with consequences for plant growth and physiological responses. Overall, 24% of plants showed no drought-induced damage, 51% showed damage up to 50%, 21% had intense leaf shedding and 2% of all plants died. Over the drought and recovery period (May–October 2006), relative height growth was significantly lower in plants with greater die-back. All species showed a significant depression in stomatal conductance, while all but deep-rooted palms Sabal etonia and Serenoa repens showed significantly lower predawn (Ψ pd) and mid-day (Ψ md) leaf water potential in dry compared to wet season. Plants experiencing less severe die-back exhibited greater stomatal conductance, suggesting a strong relationship between physiology and morphology. Based on results we suggest that the restoration efforts in Florida scrub should consider the soil moisture requirements of key species.
机译:土壤水分有效性的模式影响植物的存活,生长和繁殖力。在这里,我们将土壤水分的模式与佛罗里达灌丛植物的生理和人口后果联系起来。我们使用不同时间尺度的数据来(1)确定在黎明前测量叶片水分状况(Ψ crit )期间导致叶片失去膨胀的临界土壤水分含量,(2)描述时间模式在c crit 的分布中,(3)基于8年的数据分析了降雨与土壤水分之间关系的强度,(4)预测了75年的降雨数据中的土壤水分,并且(5)根据稳定同位素分析(δ 18 O)确定的吸水深度,评估了2006年春季干旱对佛罗里达灌丛生态系统优势灌木的形态,生理和人口统计学影响。根据1998–2006年的数据,深度为50 cm的土壤水分解释了两种优势灌木Quercus chapmanii和Ceratiola ericoides的黎明前叶片水势的显着变化(r 2 = 0.69)。在8年的数据收集过程中,仅在2000年的峰值干旱期间,当土壤水分在50和90 cm深度下降至体积的1%以下时,叶子才达到 crit 。降水解释了土壤含水量的显着变化(r 2 = 0.62)。 75年的预测土壤湿度模式表明干旱发生的频率没有及时增加。 2006年春季,土壤达到了临界土壤湿度水平,对植物生长和生理反应产生了影响。总体而言,有24%的植物没有干旱引起的损害,有51%的损害高达50%,有21%的叶片强烈脱落,而所有植物中有2%死亡。在干旱和恢复期(2006年5月至10月)中,具有较高回死率的植物的相对高度增长明显较低。所有种类均显示出明显的气孔导度降低,而除了深根的棕榈树Sabal etonia和Serenoa repens的黎明前(Ψ pd )和中午(Ψ md )均显着降低。 >)与潮湿季节相比,干燥时的叶子水势较大。经历不那么严重的死亡的植物表现出更大的气孔导度,表明生理学和形态之间有很强的关系。根据结果​​,我们建议佛罗里达灌木丛的恢复工作应考虑关键物种对土壤水分的需求。

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