Water Sources in Canterbury

High country and intermontane basins

Lakes in the high country have the highest water quality of any surface water body in the Canterbury Region. However, all the small high country streams, small lakes, wetlands and tarns are vulnerable to contamination owing to their size.

Lake Alexandrina is the only high country lake recorded as being permanently enriched (i.e., having high nutrient concentrations) and is subject to periodic algal blooms. Lake Emma (Ashburton River catchment) and Lake Grasmere (Waimakariri River catchment) are also subject to nutrient enrichment.

High stock densities in the catchments of the small lakes and tarns, stock access to water bodies, grazing in lake margins and marginal wetlands, removal of riparian vegetation, high numbers of water birds, and drainage and/or over-sowing and top-dressing of wetlands will all adversely affect water quality and habitat values of high country water bodies

Foothills

Microbiological water quality in the foothills tends to be lower than in the High Country and Intermontane Basin zones owing to the more intensive land use and a general absence of dense riparian vegetation. The upper Selwyn River is an example, with sites around Glentunnel at times exceeding microbiological water quality guidelines for contact recreation.

Banks Peninsula

There is a high risk of microbiological contamination of Banks Peninsula streams owing to stock having access to streams and defecating in or near them. Incidents of stream and spring contamination by pesticides have also been recorded. Surface water contamination is of particular concern on Banks Peninsula as stream and spring water provide the main source of domestic water supply.

Lake Forsyth (Wairewa) is eutrophic and the lake is subject to frequent toxic algal blooms.

Sediment from accelerated erosion on the Banks Peninsula hills discolours coastal waters. Concern has been expressed over the possible effects of sedimentation on the local coastal fisheries and other coastal ecosystems and on the clarity of the water for diving.

The Plains

The impacts of human activity on water quality are of greatest concern in the smaller surface water bodies of the Plains, and in areas with high recreational use.

Foothill-sourced rivers and groundwater-fed streams

The Plains sections of the foothill-sourced rivers and groundwater-fed streams tend to be particularly vulnerable to contamination owing to the intensive land uses in their catchments combined with natural low flows (e.g., parts of the Opihi River system). The groundwater-fed streams often have nitrate concentrations, reflecting the quality of the groundwater. Many of the water bodies at times also support high populations of water birds that contribute microbiological contaminants (e.g., the Ashburton River).

All the water bodies in this area receive agricultural runoff, and some also have inputs from urban drainage systems. Most streams and the drains and stock water races that flow into them, are unfenced and stock generally have unrestricted access. Environment Canterbury is currently trying to identify the type and extent of contaminants in these systems and the need to manage them.

Concern has been expressed over present and future water contamination resulting from increases in dairying, especially in small catchments and where it is combined with border-dyke irrigation (e.g., North Waitaki floodplain streams, such as the Waikakahi Stream).

Braided rivers

Reduced water quality in the lower reaches of the Waimakariri River and the smaller foothill sourced braided rivers (the Selwyn, Ashburton and Opihi) is frequently a result of point sources of contamination, such as community sewage discharges, and, in the case of the Waimakariri River, meat processing wastes. However, these impacts are compounded by the cumulative effects of upstream non-point source activities, such as runoff from adjacent land and effects of large numbers of water birds.

Lowland lakes, coastal lagoons and estuaries

Lowland lakes, coastal lagoons, and estuaries, including Lakes Ellesmere (Te Waihora), Forsyth (Te Wairewa) and Wainono Lagoon, have the highest nutrient status of any water bodies in the region owing to their location at the lower reaches of their catchments where they act as a sink for contaminants from upstream. These water bodies also receive contaminants from runoff from surrounding intensive agricultural land uses.

Urban water bodies

The main water quality issues in urban water bodies result from contaminants (sediment, nutrients and hazardous substances) carried through the stormwater systems. Stormwater is contaminated predominantly from runoff from industrial and urban areas, and from runoff from roads and paved areas. Earthworks associated with residential developments can result in substantial increases in sediment discharge, particularly in hill catchments.

Groundwater

Although groundwater quality within the Plains' aquifers is generally very high, there are exceptions:

• Areas of high nitrate-nitrogen concentrations and concentrations of micro-organisms can occur in areas of intensive agricultural farming. Contamination of groundwater with nitrogen has resulted from the introduction of nitrogen-fixing plants, fertilisers, human and animal effluent disposal to land, and intensive agricultural production (both pastoral and arable). Soluble forms of nitrogen are leached into groundwater with rainfall and irrigation water. In typical Canterbury gravel aquifers, the common form of inorganic nitrogen is as nitrate (NO3- ). The reduced forms of nitrogen, ammonia and nitrite, may also be present in groundwater in small concentrations. Higher nitrate concentrations generally coincide with high water tables in the early spring, although the effects of irrigation can results in raised water tables during summer, and consequently higher nitrate concentrations in groundwater. In some parts of Canterbury the nitrate-nitrogen concentrations in shallow unconfined groundwater have been observed to periodically increase above the drinking-water standard of 11.3 mg/l nitrate-nitrogen, particularly in the heavily grazed area of farmland between Burnham, West Melton, Yaldhurst and Lincoln. Nitrate is believed to cause adverse health effects particularly in pregnant women and infants up to 6 months of age who are bottle-fed with high nitrate containing water.
• Triazine herbicides (atrazine, simazine and terbuthylazine), have been detected in shallow groundwater throughout the Levels Plain area in South Canterbury and at various other locations throughout Canterbury. Although the concentrations are low (to date only up to half of the 1995 New Zealand drinking water standard) there is concern that ongoing use of these pesticides could lead to more widespread, or increasing, contaminant loadings of groundwater.
• Shallow groundwater underlying industrial or urban areas is susceptible to contamination from hydrocarbons. Chlorinated hydrocarbons, such as those used as industrial solvents, have been detected in low concentrations in parts of Christchurch, and at Washdyke, near Timaru. Aromatic hydrocarbons, including petroleum products, have also been found in Canterbury groundwaters. The concentrations of these compounds are generally well below relevant drinking water standards, showing little current risk to groundwater users. However, it is of concern that these chemicals are routinely present over an extensive area.
• Shallow unconfined groundwater is vulnerable to contamination with micro-organisms. Throughout the Canterbury region indicator bacteria have been detected in the shallow groundwater (usually less than 30 m deep). While micro-organisms can leach from the soil into groundwater, it is believe that frequently, the organisms are transported directly into groundwater via poorly protected well heads.
• Groundwater in some parts of Canterbury can contain high concentrations of iron and/or manganese. These naturally occurring compounds can cause staining of clothing and white ware, and clogging of pipe work, and give water a metallic taste. High concentrations of manganese can pose a health risk if used as drinking-water. Typically the areas of high concentrations of iron and manganese occur in groundwater along the coastal strip, and are associated with peat deposits in the aquifers. In some areas along the coastal strip where iron and/or manganese is present, arsenic has also been detected in the groundwater. Areas where arsenic is known to be present are Waikuku, Saltwater Creek, and Kaikoura. While, the concentration of arsenic in the groundwater tends to be below the New Zealand drinking-water standard, groundwater from some wells in these areas has concentrations of arsenic above the standard, and therefore, is not suitable as a drinking-water source untreated.

Find out more about Groundwater.