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Longer-term effects of pine and eucalypt plantations on streamflow

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dc.contributor.author Scott, DF
dc.contributor.author Prinsloo, FW
dc.date.accessioned 2018-01-04T10:45:04Z
dc.date.available 2018-01-04T10:45:04Z
dc.date.issued 2008-10
dc.identifier.citation Scott, D.F. and Prinsloo, F.W. 2008. Longer-term effects of pine and eucalypt plantations on streamflow. Water Resources Research, vol. 44(W00A08): 1-8 en_US
dc.identifier.issn 0043-1397
dc.identifier.uri http://www.agu.org/contents/journals/ViewJournalContents.do?journalCode=WR&viewBy=date&year=2008&month=all&sortBy=pubDate
dc.identifier.uri http://onlinelibrary.wiley.com/doi/10.1029/2007WR006781/abstract
dc.identifier.uri http://hdl.handle.net/10204/9918
dc.description Copyright: 2008 American Geophysical Union. Due to copyright restrictions, the attached PDF file only contains the abstract of the full text item. For access to the full text item, please consult the publisher's website. en_US
dc.description.abstract The longer-term effects of afforestation with Pinus radiata and Eucalyptus grandis on streamflows were analyzed using data from two paired-catchment experiments in South Africa. The experiments are rare in that they have been maintained over longer periods than the typical rotation period for industrial timber plantations in the tropics or subtropics. In both experiments the planting treatments led to large reductions in streamflow, which increased with the age of the trees and were positively related to water availability. The pine plantation caused peak reductions in yield over a 5-year period of 44 mm a−1 or 7.7% a−1 for each 10% of catchment planted when the trees were between 10 and 20 years old. The eucalypt plantation caused peak reductions over a 3-year period of 48 mm a−1 and 10% a−1 for each 10% of catchment planted. However, as the plantations matured (over 30 years of age in the case of pines and over 15 years of age in the case of eucalypts) the flow reduction trend was reversed, and streamflow effects appear to be tending toward preafforestation levels. The longer-term effects of planted forests need not be as harmful on the water yield of catchments as has been predicted from shorter-term studies. The implication of these results is that if trees are grown on very long rotations, they may be used for restoring degraded catchments or as a means of storing carbon without completely denuding available water resources. en_US
dc.language.iso en en_US
dc.publisher Wiley en_US
dc.relation.ispartofseries Worklist;19905
dc.subject Streamflow en_US
dc.subject Eucalyptus en_US
dc.subject Timber plantations en_US
dc.subject Afforestation en_US
dc.title Longer-term effects of pine and eucalypt plantations on streamflow en_US
dc.type Article en_US
dc.identifier.apacitation Scott, D., & Prinsloo, F. (2008). Longer-term effects of pine and eucalypt plantations on streamflow. http://hdl.handle.net/10204/9918 en_ZA
dc.identifier.chicagocitation Scott, DF, and FW Prinsloo "Longer-term effects of pine and eucalypt plantations on streamflow." (2008) http://hdl.handle.net/10204/9918 en_ZA
dc.identifier.vancouvercitation Scott D, Prinsloo F. Longer-term effects of pine and eucalypt plantations on streamflow. 2008; http://hdl.handle.net/10204/9918. en_ZA
dc.identifier.ris TY - Article AU - Scott, DF AU - Prinsloo, FW AB - The longer-term effects of afforestation with Pinus radiata and Eucalyptus grandis on streamflows were analyzed using data from two paired-catchment experiments in South Africa. The experiments are rare in that they have been maintained over longer periods than the typical rotation period for industrial timber plantations in the tropics or subtropics. In both experiments the planting treatments led to large reductions in streamflow, which increased with the age of the trees and were positively related to water availability. The pine plantation caused peak reductions in yield over a 5-year period of 44 mm a−1 or 7.7% a−1 for each 10% of catchment planted when the trees were between 10 and 20 years old. The eucalypt plantation caused peak reductions over a 3-year period of 48 mm a−1 and 10% a−1 for each 10% of catchment planted. However, as the plantations matured (over 30 years of age in the case of pines and over 15 years of age in the case of eucalypts) the flow reduction trend was reversed, and streamflow effects appear to be tending toward preafforestation levels. The longer-term effects of planted forests need not be as harmful on the water yield of catchments as has been predicted from shorter-term studies. The implication of these results is that if trees are grown on very long rotations, they may be used for restoring degraded catchments or as a means of storing carbon without completely denuding available water resources. DA - 2008-10 DB - ResearchSpace DP - CSIR KW - Streamflow KW - Eucalyptus KW - Timber plantations KW - Afforestation LK - https://researchspace.csir.co.za PY - 2008 SM - 0043-1397 T1 - Longer-term effects of pine and eucalypt plantations on streamflow TI - Longer-term effects of pine and eucalypt plantations on streamflow UR - http://hdl.handle.net/10204/9918 ER - en_ZA


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