https://ogma.newcastle.edu.au/vital/access/ /manager/Index ${session.getAttribute("locale")} 5 https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:41361 Wed 28 Feb 2024 15:22:01 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:36282 Wed 28 Feb 2024 15:20:41 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:48206 Wed 28 Feb 2024 14:51:42 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:53449 Wed 07 Feb 2024 16:36:43 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:31926 K_s) was assessed on a loam soil tilled by chisel plough. Soil sampling was conducted in the inter row area of six vineyards, which differed by the age from planting: 0 (Age 0; just planted), 1, 3, 6, 13, and 25 years (Age 1, Age 3, Age 6, Age 13, and Age 25, respectively). The One Ponding Depth (OPD) approach was applied to ring infiltration data to estimate soil K_s with an α* parameter equal to 0.012 mm^-1. Soil bulk density for Age 0 was about 1.5 times greater than for Age 25, i.e., the long-term managed vineyards. Saturated hydraulic conductivity at Age 0 was 86% less than at Age 25. The planting works were considered a major factor for soil compaction and the reduction of hydraulic conductivity. Compared to the long-term managed vineyards, soil compaction was a very short-term effect given that BD was restored in one year due to ploughing. Reestablishment of K_s to the long-term value required more time.]]> Mon 23 Sep 2019 14:07:32 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:34027 Fri 01 Feb 2019 13:10:56 AEDT ]]>