Nitrate-nitrogen
These persistent levels have been attributed to historic arable or dairy farming. They occur in areas on the margin of the main aquifer where groundwater flow rates are lower, and correspondingly less dilution occurs than in the main Wairau Aquifer, where similar land-uses also exist.
This graph clearly shows this pattern of elevated or high levels along the southern margin of the Wairau Plain. Nitrate is subject to natural degradation processes in anaerobic conditions associated with confined aquifers, and this explains why levels are low beneath the Te Koko-o-Kupe/Cloudy Bay area.