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The relationship between fog, floods, groundwater and tree growth along the lower Kuiseb River in the hyperarid Namib

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dc.contributor.author Schachtschneider, K
dc.contributor.author February, EC
dc.date.accessioned 2013-05-03T12:17:27Z
dc.date.available 2013-05-03T12:17:27Z
dc.date.issued 2010-12
dc.identifier.citation Schachtschneider, K and February, E.C. 2010. The relationship between fog, floods, groundwater and tree growth along the lower Kuiseb River in the hyperarid Namib. Journal of Arid Environments, vol. 74(12), 1632-1637 en_US
dc.identifier.issn 0140-1963
dc.identifier.uri http://www.sciencedirect.com/science/article/pii/S0140196310001692
dc.identifier.uri http://hdl.handle.net/10204/6716
dc.description Copyright: 2010 Elsevier. This is an ABSTRACT ONLY. The definitive version is published in Journal of Arid Environments, vol. 74(12), 1632-1637 en_US
dc.description.abstract There is a growing demand for increased water abstraction from ephemeral rivers such as the Kuiseb in western Namibia. Studies in the 1980.s recorded mortality rates of the most common riparian tree species in a prolonged drought from 1979 to 1984. These results show that mortality for the three species differed considerably with 16 % mortality for Acacia erioloba, 39 % for Faidherbia albida and 75 % for Tamarix usnoides. Here we determine the water sources and rooting strategy of three age groups of the three most common riparian tree species growing along the Kuiseb River using stable hydrogen and oxygen isotope analysis. We do this to better understand the relationship between germination and establishment of trees along river courses in hyperarid western Namibia. A secondary objective is to determine whether the mortality rates recorded in the drought in the 1980.s may be related to rooting strategy. We use a linear mixing model approach (IsoSource) to quantify probable contributions of multiple water sources to tree water uptake. Our results show that none of the tree species in this study use fog water. Rather, all of the trees are reliant on a seasonally fluctuating combination of groundwater, shallow soil water and deep soil water. All of these water sources are directly reliant on regular recharge from annual flood events. Our results also show that the mortality rates recorded in the early 1980.s need not necessarily relate to rooting depth or water source but that there may be a combination of possible causes including root growth and structure. If predictions for increased water abstraction and global climate change are realized then the vegetation structure along ephemeral river courses in Namibia will be seriously threatened. en_US
dc.language.iso en en_US
dc.publisher Elsevier en_US
dc.relation.ispartofseries Workflow;3880
dc.subject Ephemeral rivers en_US
dc.subject d18O/d2 H isotopes en_US
dc.subject IsoSources en_US
dc.subject Riparian trees en_US
dc.subject Water usage en_US
dc.subject Namib Desert rainfall en_US
dc.subject Kuiseb River en_US
dc.title The relationship between fog, floods, groundwater and tree growth along the lower Kuiseb River in the hyperarid Namib en_US
dc.type Article en_US
dc.identifier.apacitation Schachtschneider, K., & February, E. (2010). The relationship between fog, floods, groundwater and tree growth along the lower Kuiseb River in the hyperarid Namib. http://hdl.handle.net/10204/6716 en_ZA
dc.identifier.chicagocitation Schachtschneider, K, and EC February "The relationship between fog, floods, groundwater and tree growth along the lower Kuiseb River in the hyperarid Namib." (2010) http://hdl.handle.net/10204/6716 en_ZA
dc.identifier.vancouvercitation Schachtschneider K, February E. The relationship between fog, floods, groundwater and tree growth along the lower Kuiseb River in the hyperarid Namib. 2010; http://hdl.handle.net/10204/6716. en_ZA
dc.identifier.ris TY - Article AU - Schachtschneider, K AU - February, EC AB - There is a growing demand for increased water abstraction from ephemeral rivers such as the Kuiseb in western Namibia. Studies in the 1980.s recorded mortality rates of the most common riparian tree species in a prolonged drought from 1979 to 1984. These results show that mortality for the three species differed considerably with 16 % mortality for Acacia erioloba, 39 % for Faidherbia albida and 75 % for Tamarix usnoides. Here we determine the water sources and rooting strategy of three age groups of the three most common riparian tree species growing along the Kuiseb River using stable hydrogen and oxygen isotope analysis. We do this to better understand the relationship between germination and establishment of trees along river courses in hyperarid western Namibia. A secondary objective is to determine whether the mortality rates recorded in the drought in the 1980.s may be related to rooting strategy. We use a linear mixing model approach (IsoSource) to quantify probable contributions of multiple water sources to tree water uptake. Our results show that none of the tree species in this study use fog water. Rather, all of the trees are reliant on a seasonally fluctuating combination of groundwater, shallow soil water and deep soil water. All of these water sources are directly reliant on regular recharge from annual flood events. Our results also show that the mortality rates recorded in the early 1980.s need not necessarily relate to rooting depth or water source but that there may be a combination of possible causes including root growth and structure. If predictions for increased water abstraction and global climate change are realized then the vegetation structure along ephemeral river courses in Namibia will be seriously threatened. DA - 2010-12 DB - ResearchSpace DP - CSIR KW - Ephemeral rivers KW - d18O/d2 H isotopes KW - IsoSources KW - Riparian trees KW - Water usage KW - Namib Desert rainfall KW - Kuiseb River LK - https://researchspace.csir.co.za PY - 2010 SM - 0140-1963 T1 - The relationship between fog, floods, groundwater and tree growth along the lower Kuiseb River in the hyperarid Namib TI - The relationship between fog, floods, groundwater and tree growth along the lower Kuiseb River in the hyperarid Namib UR - http://hdl.handle.net/10204/6716 ER - en_ZA


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