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Water Use of Tree Lines: Importance of Leaf Area and Micrometeorology in Sub-Humid Kenya

机译:树系的用水:肯尼亚南部湿润地区叶面积和微气象学的重要性

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In this research the relative importance of leaf area and microclimatic factors in determining water use of tree lines was examined in sub-humid Western Kenya. Measurements of tree water-use by a heat-balance technique, leaf area, bulk air saturation deficit, daily radiation, and soil water content were done in an experiment with tree lines within crop fields. The tree species were Eucalyptus grandis W. Hill ex Maiden, Grevillea robusta A. Cunn. and Cedrella serrata Royle, grown to produce poles on a phosphorus-fixing Oxisol/Ferralsol with (+P) or without (−P) phosphorus application. Doubling the leaf area of Cedrella and Grevillea doubled water use in a leaf area (LA) range of 1–11 m2 per tree. The response of Eucalyptus water use (W) to increases in leaf area was slightly less marked, with W = LA n , n<1. Transpiration rate per unit leaf area (Tr) was the other important determinant of water use, being affected by both tree species and phosphorus fertilization. A doubling of the saturation deficit (SD) halved the water use of all trees except for Cedrella +P, in which water use increased. A direct effect of soil water content on water use was only found in Grevillea -P, with a small increase (60%) as available water increased from 1.4 to 8.9% above wilting point (32%). This low direct response to soil water content is probably due to the extensive tree-root systems and the deep clayey soils supplying sufficient water to meet the evaporative demand. Indirect responses to soil water content via decreases in leaf area occurred in the dry season. The results showed that water use of tree lines was more determined by leaf area and transpiration rate per unit leaf area than by micro meteorological factors. The linear response of tree water use to leaf area, over a wide range leaf areas, is a specific characteristic of tree line configurations and distinguished them from forest stands. In tree lines light interception and canopy conductance increase with leaf area much more than a similar leaf area increase would have caused in a closed forest canopy.
机译:在这项研究中,考察了肯尼亚西部半湿润地区叶面积和微气候因素在确定林木用水中的相对重要性。在作物田间的树线试验中,通过热平衡技术,树木面积,空气饱和度不足,日辐射和土壤含水量对树木用水进行了测量。这些树种是大桉树W.Hill ex Maiden,GrevillearobustaA.Cunn。和塞德拉(Cedrella serrata Royle),生长时在固磷(O)和固磷(P)的情况下会产生极点。塞德拉(Cedrella)和葛雷维拉(Grevillea)的叶子面积加倍,每棵树的叶子面积(LA)范围为1–11 m2 。桉树水分利用(W)对叶片面积增加的响应略显不足,W = LA n ,n <1。每单位叶面积的蒸腾速率(Tr)是用水的另一个重要决定因素,受树种和磷肥的影响。饱和度赤字(SD)的两倍使除Cedrella + P以外的所有树木的用水量减少了一半,后者的用水量增加了。土壤水分含量对水分利用的直接影响仅出现在Grevillea -P地区,随可利用水从萎点(1.4%)增加到8.9%(32%)时,增加很小(60%)。对土壤水分的低直接响应可能是由于广泛的树根系统和深层的黏土提供了足够的水以满足蒸发需求。通过减少叶面积对土壤水分的间接反应发生在干旱季节。结果表明,树系的用水更多地取决于叶面积和单位叶面积的蒸腾速率,而不是微观气象因素。在宽范围的叶面积上,树木用水对叶面积的线性响应是林线配置的特定特征,并将其与林分区分开。在林木中,光拦截和树冠电导随叶面积的增加远大于在封闭的森林树冠中引起的类似叶面积的增加。

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