Articles | Volume 12, issue 19
https://doi.org/10.5194/bg-12-5619-2015
https://doi.org/10.5194/bg-12-5619-2015
Research article
 | 
05 Oct 2015
Research article |  | 05 Oct 2015

Transpiration in an oil palm landscape: effects of palm age

A. Röll, F. Niu, A. Meijide, A. Hardanto, Hendrayanto, A. Knohl, and D. Hölscher

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Cited articles

Allen, K., Corre, M., Tjoa, A., and Veldkamp, E.: Soil nitrogen-cycling response to conversion of lowland forests to oil palm and rubber plantations in Sumatra, Indonesia, PLoS ONE, 10, e0133325, https://doi.org/10.1371/journal.pone.0133325, 2015.
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Banabas, M., Turner, M. A., Scotter, D. R., and Nelson, P. N.: Losses of nitrogen fertiliser under oil palm in Papua New Guinea: 1. Water balance, and nitrogen in soil solution and runoff, Aust. J. Soil Res., 46, 332–339, https://doi.org/10.1071/SR07171, 2008.
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Becker, P.: Sap flow in Bornean heath and dipterocarp forest trees during wet and dry periods, Tree Physiol., 16, 295–299, https://doi.org/10.1093/treephys/16.1-2.295, 1996.
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Short summary
The study provides first insight into eco-hydrological consequences of the continuing oil palm expansion in the tropics. Stand transpiration rates of some studied oil palm stands compared to or even exceeded values reported for tropical forests, indicating high water use of oil palms under certain conditions. Oil palm landscapes show some spatial variations in (evapo)transpiration rates, e.g. due to varying plantation age, but the day-to-day variability of oil palm transpiration is rather low.
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