横跨乌拉尔南部地区的Calluna vulgaris (L.) Hill的日蒸腾强度和季节蒸腾强度

Alena Kochubey, Olga Cherepanova, Irina Petrova
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引用次数: 0

摘要

外乌拉尔地区是普通石楠(C. vulgaris)分布区的南端。为了解决边缘种群对干旱气候的适应问题,对石楠植物的蒸腾强度(IT)进行了实地生态生理学研究。研究在生长着大量石楠的外乌拉尔地区(库尔干州)森林草原进行。在一个生长季节(2016 年 4 月至 9 月)里,研究人员在松树林树冠下和邻近空地上研究了 IT 的日变化,同时考虑了一组记录的生态气候限制因素(风速、光照、空气温度和湿度动态、土壤温度)。为了研究 IT,每个时间段都使用了 4 厘米长的一年生植物顶端嫩枝,一式三份。一天测量的总样本量为 30-35 株。蒸腾速率是通过快速称重法测定的,该方法考虑到了嫩枝在一定时间内的失水量。在处理数据时,我们使用了相关分析法(皮尔逊相关系数 r),从而明确了两个连续(度量)变量相互作用的强度和方向。在林冠下和空地上生长的植物的 IT 日变化存在差异。在该地区常见的大气和土壤长期干旱条件下,2016 年石楠含水量急剧下降,从上午 10 点开始,整个生长季节都是如此,只有 4 月份例外,当时土壤和石楠组织中的水分亏缺仍然很小。五月份,空地上的最大 IT 值出现在 14:00(8.5 mg/h×10 -4),而在树冠下,IT 峰值则出现在上午 10:00(12.7 mg/h×10 -4)。普通石楠(C. vulgaris)的夏季白天蒸腾作用甚至比春季蒸腾作用(3-5 毫克/小时×10-4)还要低。在露天伐木区,决定因素是 PAR(0.81,p < 0.05),其次是大气温度(0.69,p < 0.05),而在树冠下,只有 PAR(0.96,p < 0.05)。IT 的减少以及光合作用的相应减少会导致种群活力下降和种子不成熟,这是库尔干市南部石楠缺失的一个生态生理因素。
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Daily and season transpiration intensive of Calluna vulgaris (L.) Hill in the trans-Ural south area
The Trans-Ural region is the southern point of the common heather (C. vulgaris) range. Field ecophysiological study of C. vulgaris plants transpiration intensity (IT) was carried out in connection with the problem of marginal populations adaptation to arid climate. The research was carried out in the forest-steppe of the Trans-Ural region (Kurgan region), where an abundant population of heather grows. The dailyvariation of IT was studied taking into account a set of recorded ecoclimate limiting factors (wind speed, illumination, dynamics of air temperature and humidity, soil temperature) during one growing season (from April to September 2016) under the canopy of a pine forest and in the adjacent clearing. To study IT, annual apical shoots of plants 4 cm long were used in triplicate for each time period. The total sample size on one day of measurements ranged from 30-35 shoots. The transpiration rate was determined by the rapid weighing method, which takes into account the water lost by the shoot over a certain time period. When processing the data, we used correlation analysis (Pearson's correlation coefficient r), which made it possible to clarify the strength and direction of two continuous (metric) variables interaction. Differences in IT daily changes were revealed in plants growing under the forest canopy and in the open areas. Under conditions of long-term atmospheric and soil drought, which is common for the region, in 2016 a sharp decrease in heather water content was observed, starting from 10 a.m. throughout the entire growing season, with the exception of April, when the moisture deficit in the soil and heather tissues was still minimal. In May, maximum IT values in the clearing were noted at 14:00 (8.5 mg/h×10 –4) whereas under the canopy of the tree stand, peak IT values begin at 10 a.m. (12.7 mg/h×10 –4). Daytime summer transpiration in common heather (C. vulgaris) is even less intense than spring transpiration ((3–5 mg/h×10–4).It was revealed that meteorological factors play a decisive role in IT in various types of forest. In open felled areas, the determining factor is PAR (0.81, p < 0.05) and, to a lesser extent, atmospheric temperature (0.69, p < 0.05), and under the canopy - only PAR (0.96, p <0.05). A decrease in IT and, accordingly, photosynthesis leads to a decrease in the population’s vitality and non-ripening of seeds, which is an ecophysiological factor of the heather absence south of Kurgan city.
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