The importance of topographic controls on groundwater recharge for plantation forestry in southeast Australia

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dc.contributor.authorDean, JFen_AU
dc.contributor.authorWebb, JAen_AU
dc.contributor.authorJacobsen, GEen_AU
dc.contributor.authorChisari, Ren_AU
dc.contributor.authorDresel, PEen_AU
dc.date.accessioned2022-10-25T00:13:12Zen_AU
dc.date.available2022-10-25T00:13:12Zen_AU
dc.date.issued2013-09-16en_AU
dc.date.statistics2022-01-24en_AU
dc.description.abstractThe trade off between water use and carbon sequestration by F plantation forestry is the subject of ongoing debate in Australia. Many tree plantations are planted without consideration for their impact on groundwater recharge. The spatial variation of recharge across a landscape can provide useful information on where to best situate a plantation while minimising its impact on groundwater recharge. Recharge is generally assumed to take place at topographic high points across a landscape, especially when rocky outcrops occur. This study analysed recharge rates at several points across a small paired catchment site to determine the most prevalent areas of recharge. Water-table fluctuations, Cl- mass balances, tritium and 14C ages were used to estimate recharge at 23 points across a 0.8 km2 catchment covered predominantly in a blue gum tree plantation, and an adjacent 0.5 km2 pasture catchment, in southwest Victoria, Australia. The CI- mass, balance method and water-table fluctuation methods were modified to better reflect the recharge processes taking place at the study site, including longer term hydrograph fluctuations and input from streams. Hydrographs from data loggers (since 2009) in bores situated close to the drainage line show considerably more recharge taking place compared to bores situated further upslope. Cl-mass balances show a similar trend, as do the hydrographs for the past 20-30 years, indicating that the majority of recharge is occurring along the drainage lines and towards the bottom of the slopes. Hydrograph fluctuations from these areas of the study site also often show significant response to runoff, measured at weirs on both catchments. Fracture heterogeneity contributes to some of the recharge variations, but the general trend is for recharge to occur more consistently in the topographically lower areas. ln order to minimise the interception of groundwater recharge by tree plantations in regions similar to the study area, the bulk of the plantation should be situated on the upper slopes, away from drainage lines and the immediately adjacent slopes. This would have less of an effect on the groundwater levels, as the plantation is not intercepting recharge in the zones where the majority of infiltration is occurring.en_AU
dc.identifier.citationDean, J, F., Webb, J. A., Jacobsen, G. E., Chisari, R., & Dresel, P. E. (2013). The importance of topographic controls on groundwater recharge for plantation forestry in southeast Australia. Paper presented to the IAH 2013 Perth Australia : "Solving the groundwater challenges of the 21st century", International Association of Hydrogeologists 40th International Conference, Perth, Western Australia, 15-20 September 2013. (pp. 92-93).en_AU
dc.identifier.conferenceenddate20 September 2013en_AU
dc.identifier.conferencenameIAH 2013 Perth Australia : 'Solving the groundwater challenges of the 21st century', International Association of Hydrogeologists 40th International Conferenceen_AU
dc.identifier.conferenceplacePerth, Western Australiaen_AU
dc.identifier.conferencestartdate15 September 2013en_AU
dc.identifier.otherSession Two G, 353en_AU
dc.identifier.pagination92-93en_AU
dc.identifier.urihttps://apo.ansto.gov.au/dspace/handle/10238/13918en_AU
dc.language.isoenen_AU
dc.publisherInternational Association of Hydrogeologistsen_AU
dc.subjectGroundwater rechargeen_AU
dc.subjectForestryen_AU
dc.subjectCarbon 14en_AU
dc.subjectAustraliaen_AU
dc.subjectVictoriaen_AU
dc.subjectTritiumen_AU
dc.subjectWater tablesen_AU
dc.titleThe importance of topographic controls on groundwater recharge for plantation forestry in southeast Australiaen_AU
dc.typeConference Abstracten_AU
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