东北半干旱风沙区 7 年生与 20 年生杨树的蒸腾作用和水分利用来源

IF 5.6 1区 农林科学 Q1 AGRONOMY
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引用次数: 0

摘要

确定干旱和半干旱地区树木的蒸腾作用和水分利用源对于气候变化情况下的森林管理至关重要。本文采用热耗散法和稳定同位素法测定了树龄为 7 年(1167 棵/公顷-1)和 20 年(475 棵/公顷-1)的杨树(Populus × xiaozhuanica)人工林的蒸腾作用和水分利用源的季节变化。结果表明,在测量期间,7 年树龄和 20 年树龄种植园的单位叶面积平均蒸腾量分别为 1.6 和 1.7 mm d-1,而林分蒸腾量(Es)分别为 1.5 和 1.4 mm d-1。两个种植园的蒸腾量对气候变量的敏感性都随着土壤水分的减少而降低,但 7 年种植园的蒸腾量降幅更大,表明其对干旱的敏感性更高。随着地下水位的下降,两个种植园的Es都明显下降,但在干旱条件下,7年种植园的Es受地下水位下降的限制更大。在测量期间,7 年树龄和 20 年树龄植株的累积蒸散发分别占降水量的 45% 和 44%,这表明植株的耗水量并没有随着树龄的增加而增加。同位素数据表明,随着土壤水分和地下水位的降低,7 年树龄和 20 年树龄的树木都将水源从春季的 0 至 100 厘米土层和地下水转换为夏季的 0 至 200 厘米土层水和地下水,但 7 年树龄和 20 年树龄的树木地下水的贡献率分别从 47% 降至 32.3%,从 39.6% 降至 37%。这些结果表明,杨树种植园的蒸腾作用并不随树龄而变化,但地下水位的下降降低了地下水对 7 年树龄杨树种植园蒸腾作用的贡献,因此与 20 年树龄杨树种植园相比,土壤干旱对蒸腾作用的负面影响加剧。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Transpiration and water use sources of poplar (Populus × xiaozhuanica) plantations with 7-years vs. 20-years old in a semiarid sandy region of Northeast China

Determination of transpiration and water use sources of trees in arid and semiarid areas is crucial for forest management under climate change scenes. Here, seasonal variations in transpiration and water use sources of the 7– (1167 trees ha−1) and 20 (475 trees ha−1)–year–old poplar (Populus × xiaozhuanica) plantations were determined based on thermal dissipation and stable isotope methods. Results showed that transpiration per unit leaf area averaged 1.6 and 1.7 mm d−1 for the 7– and 20–year–old plantations during the measurement period, respectively, whereas stand transpiration (Es) was 1.5 and 1.4 mm d−1. Sensitivity of Es to climatic variables decreased with reduction of soil moisture for both plantations, but larger decrease for 7–year–old plantation indicated higher sensitivity to drought. Es of both plantations significantly decreased with decline of groundwater levels, but Es of 7–year–old plantation was more limited by decline of groundwater level under drought conditions. During the measurement period, accumulated Es occupied 45 % and 44 % of precipitation for 7– and 20–year–old plantations, respectively, indicating that water consumption of plantation did not increase with increasing stand age. Isotope data indicated that both 7– and 20–year–old trees switched water sources from 0 to 100 cm soil layer and groundwater in spring to 0–200 cm soil water and groundwater in summer as soil moisture and groundwater level decreased, but contribution of groundwater decreased from 47 % to 32.3 % and from 39.6 % to 37 % for 7– and 20–year–old plantation, respectively. These findings indicated that transpiration of poplar plantations did not vary with stand age, but a decline of groundwater level reduced contribution of groundwater to transpiration for 7–year–old poplar plantations and thus exacerbated negative effect of soil drought on transpiration compared with 20–year–old poplar plantation.

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来源期刊
CiteScore
10.30
自引率
9.70%
发文量
415
审稿时长
69 days
期刊介绍: Agricultural and Forest Meteorology is an international journal for the publication of original articles and reviews on the inter-relationship between meteorology, agriculture, forestry, and natural ecosystems. Emphasis is on basic and applied scientific research relevant to practical problems in the field of plant and soil sciences, ecology and biogeochemistry as affected by weather as well as climate variability and change. Theoretical models should be tested against experimental data. Articles must appeal to an international audience. Special issues devoted to single topics are also published. Typical topics include canopy micrometeorology (e.g. canopy radiation transfer, turbulence near the ground, evapotranspiration, energy balance, fluxes of trace gases), micrometeorological instrumentation (e.g., sensors for trace gases, flux measurement instruments, radiation measurement techniques), aerobiology (e.g. the dispersion of pollen, spores, insects and pesticides), biometeorology (e.g. the effect of weather and climate on plant distribution, crop yield, water-use efficiency, and plant phenology), forest-fire/weather interactions, and feedbacks from vegetation to weather and the climate system.
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