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首页> 外文期刊>Trees. Structure and Function >Transpiration in a eucalypt plantation and a savanna in Venezuela.
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Transpiration in a eucalypt plantation and a savanna in Venezuela.

机译:委内瑞拉的桉树人工林和热带稀树草原的蒸腾作用。

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摘要

In Venezuela 30,000 km2 of land is covered by savannas, of which 410,000 ha have been planted with several species and hybrids of Eucalyptus for lumber and pulp production. Popular concern about possible diminutions in water availability of reservoirs near eucalypt plantations prompted our interest in measuring water use by these trees. Since these savannas are markedly seasonal, the response of species to seasonal drought is important. We aimed to compare the seasonal changes in single-leaf and whole-plant transpiration in a seasonally dry savanna with that of trees of E. urophylla in an experimental plantation. We also examined the seasonal changes in xylem water potential and stomatal response to air water-vapour saturation deficit (D). Transpiration in eucalypts and the dominant savanna species Trachypogon vestitus and Curatella americana was evaluated using measurements of leaf gas exchange in all three species, sap flux in eucalypts, microclimatic variables and allometric and photometric determinations of green area. In E. urophylla and T. vestitus, but not in C. americana, stomatal conductance (gs) proved sensitive to D. Integrated values of daily courses of transpiration rate were scaled to one ha in a preliminary approach to estimating ecosystem transpiration (Eha). The Eha of the savanna (the sum of Eha of T. vestitus and C. americana) was on average 2.4 times that of eucalypts during the daytime; when nocturnal eucalypt transpiration was included, the value was 1.9. The evapotranspiration calculated by the Penman-Montieth equation (ETc) of eucalypts was lower than the savanna all year round. The reference crop ET (ETo) varied little throughout the seasons, the highest value occurring in March. The ratio Eha/ETo for the savanna was on average near one during the dry season and almost two during the rainy season; the corresponding value for E. urophylla was 0.6 for both seasons. The ratio Eha/ETc was on average 0.8 for the species and the savanna. The cumulative Eha for the days of measurements was higher in the savanna than in the eucalypts during the daytime (39.8 and 17.3 mm, respectively), as was the cumulative ETc (37.5 vs. 20.3 mm). Measured and calculated cumulative ET in eucalypts, including nocturnal values, were 22.0 and 28.4 mm, respectively. At the leaf level, both eucalypts and trees of C. americana apparently may have accessed water from deep horizons, since their values of Psi changed less seasonally than in T. vestitus. At the ecosystem level, the species that presented the largest changes in transpiration was T. vestitus, which markedly increased savanna transpiration during the rainy season. Our results suggest that, for the days of this study, and considering the environmental conditions of the ecosystems studied, the type of measurements and the scaling procedures, stands of E. urophylla transpire less water than the savanna.Digital Object Identifier http://dx.doi.org/10.1007/s00468-012-0745-0
机译:在委内瑞拉,大草原覆盖了30,000 km 2 的土地,其中410,000公顷已种植了几种桉树和杂种,用于木材和纸浆生产。人们普遍担心桉树人工林附近的水库的可用水量会减少,这促使我们对测量这些树木的用水量产生了兴趣。由于这些稀树草原是明显的季节性物种,因此物种对季节性干旱的反应非常重要。我们的目的是比较季节性干燥大草原中单叶蒸腾和整株植物蒸腾的季节性变化与实验性种植中的尾叶桉树的变化。我们还检查了木质部水势和气孔对空气水汽饱和度不足(D)的气孔响应的季节性变化。使用三种植物的叶片气体交换,桉树的汁液通量,微气候变量以及绿化面积的光度法和光度法来评估桉树和热带稀树大草原物种Trachypogonvesititus和美国Curatella美洲的蒸腾作用。在E. urophylla和T.vestitus中,但在C. americana中则不然,气孔导度(g s )被证明对D敏感。在初步研究中,蒸腾速率的每日过程的综合值被缩放为一公顷估算生态系统蒸腾量的方法(E ha )。白天,热带草原的E ha (平均水平),是桉树的E ha 之和,平均为桉树的2.4倍;当包括夜间桉树蒸腾作用时,该值为1.9。桉树的Penman-Montieth方程(ET c )计算的蒸散量全年都低于大草原。整个季节的参考作物ET(ET o )变化不大,最高值发生在3月。稀树草原的比率E ha / ET o 在旱季平均接近1,在雨季接近2。在两个季节中,尾叶大肠杆菌的对应值为0.6。物种和稀树草原的比率E ha / ET c 平均为0.8。大草原上白天的累积E ha 比白天的桉树高(分别为39.8和17.3 mm),累积ET c (37.5和20.3毫米)。在桉树中测得和计算出的累积ET(包括夜间值)分别为22.0和28.4 mm。在叶片水平上,美洲锥e的桉树和树木显然都可以从深处获取水,因为它们的Psi值季节变化不如T.vestitus。在生态系统层面,蒸腾变化最大的物种是猪笼草,在雨季,热带稀树草原的蒸腾作用明显增加。我们的结果表明,在本研究期间,考虑到所研究的生态系统的环境条件,测量类型和缩放程序,尾叶E. urophylla的蒸腾量比稀树草原的少。数字对象标识符http:// dx.doi.org/10.1007/s00468-012-0745-0

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