Soil-driven variability in grapevine water uptake depth across seven soil types in Marlborough, New Zealand
- Takeaway: Isotope measurements showed large differences in water-uptake depth between vineyard soils. Compacted layers restricted access to deeper water at some sites (Renwick drew ~70% from 20–50 cm above a dense layer at ~50 cm); others supported uptake across the profile or mainly from depth (Hinds and Temuka up to ~70% from below 30 cm).
- Why it matters: For Central Otago, the practical implication is to match irrigation and soil-moisture monitoring depths to each block’s soil profile. A shallow sensor alone may poorly represent the water vines actually access, and frequent shallow irrigation is likely wasted where vines are drawing from depth.
- Worth reading: Figure 5, the depth-by-depth uptake heatmaps paired with each soil profile; Figure 3, for spotting compaction layers; and Table 2, which translates the findings into soil-specific management responses.
- Limits: Seven sites, one season (2024–25, warmer than average), generally low vine water stress. Soil, cultivar and rootstock effects could not be separated, and augers could not sample below ~50–70 cm at two sites. The irrigation recommendations are informed proposals, not demonstrated water savings or fruit-quality gains. This supports established site-specific irrigation principles; isotope-based diagnosis remains a specialist research tool.
