< back to Actions home

Table of Actions

Actions have been scored for effectiveness, relative cost, and response using science and expert knowledge developed within the Our Land and Water National Science Challenge.

Sort contaminants by high to low for N (Nitrogen), P (Phosphorus), S (Sediment), and M (Microbes).

Effectiveness = kg of nutrient or sediment or coliform forming units retained or immobilised and categorised into Low (0-33%), Medium (34-66%) and High (67-100%).

Relative cost = Cost breakdowns are assessed as Low, Moderate, and High for each contaminant with in indicative cost in $/ha/yr. Nitrogen (Low <100, Moderate 101-366, and High >366 $/ha/yr); Phosphorus (Low <111, Moderate 112-476, and High >476 $/ha/yr); Sediment (Low <81, Moderate 82-169, and High >169 $/ha/yr); Microbes (Low <129, Moderate 130-192, and High >193 $/ha/yr).

Response rate = Fast - within a season, Moderate - within a year, and Slow - longer than a year.

The ratings for actions were assessed independently from the Physiographic Environment classification. Effectiveness of actions can be increased by matching the right actions to the landscape setting.

StrategyDescription of functionEffectiveness %Relative cost ($/ha/yr)Response rateReaons for variabilityFactors limiting uptakeCo-benefitsExample references
NPSMNPSMNPSM
Bridging stock stream crossingsAvoid direct entry of faeces, urine and entrained hoof mud, and substrate disturbance during stream crossings.LowLowModModLowModFastFastFastHighly dependent on stream length, width and number of crossings per farm. Too many crossings Avoiding stock losses in high flows.Davies‐Colley et al. 2004
Constructed wetlandsModification of landscape features such as depressions and gullies to form wetlands. Slow water movement encourages deposition of suspended sediment and entrained contaminants (e.g. P). HighLowModModHighLowModFastFastWetland performance depends on intercepting the maximum amount of run-off from the catchment at the right flow rate.No suitable areas on farm (i.e. catchment lies outside of farm area).Flood attenuation, wildlife habitat and biodiversityMcKergow et al. 2007
Natural seepage wetlandsNatural seepage wetlands at the heads and sides of streams slow water movement through them and encourage the deposition of suspended sediment and entrained contaminants (e.g. P). HighLowModModHighHighFastFastFastInterception of run-off depends on landscape, hydrogeology and human modification. Price of permanent fencing ≫ temporary fencing.Flood attenuation, wildlife habitat and biodiversityBurns and Nguyen 2002, McKergow et al. 2007
Sediment traps and retention pondsIn-stream traps and retention ponds allow coarse sized sediment and associated N and P to settle out. LowHighLowHighHighModFastFastFastAlthough design can be modified to maximise removal via settling, traps are ineffective at high flows when most sediment is transportedMay require resource consentPotential to buffer storm events and therefore potential downstream flooding.Hicks 1995, Clark et al. 2013
Stream fencingPreventing livestock access to stream, decreases stream bank damage (and sediment inputs via bank erosion) bed disturbance of sediments (and entrained E. coli, N and P) and stops the direct deposition of excreta into streams.HighLowModLowLowLowFastFastFastGain is dependent on the area of the farm currently unfenced and stream density.Price of permanent fencing ≫ temporary fencing.Stream shading decreasing water temperature and light for periphyton and macrophyte growth.James et al. 2007, McDowell 2008, Muirhead and Monaghan 2012
Vegetated buffer stripsVegetated buffer strips work to decrease contaminant loss in surface runoff by a combination of filtration, deposition, and improving infiltration. ModModHighModFastFastStrip can become clogged with sediment and function poorly in areas that are often saturated due to limited infiltration or where surface runoff converges and breaks through strips.Land adjacent to stream may not be available or suitable for a buffer strip.Potential to stabilise stream banks.Smith 1989, Redding et al. 2008
Restricted grazing of winter forage cropsRestricted grazing of a forage crop in winter to reduce deposition of excreta and surface erosion by grazing animals.HighModModModHighLowFastFastFastCosts vary widely due to variations in soil type and climate, and on the frequency of use of a restricted grazing strategy.Must be accompanied by a stand-off area that has no connection to a waterway (e.g. runoff/effluent is captured).Decreased pasture damage and N2O emissions.Ledgard et al. 2006, McDowell et al. 2009
Greater effluent pond storage and deferred irrigationEffluent is stored in larger ponds allowing it to be applied to land when soil moisture deficit and physical conditions allow it to be adsorbed and not thus lost in runoff.ModModLowModLowModModModModDepends on the number of cows, size of pond required, material and suitable location to build a pond. Inaccurate pond size can result in applications during wet periods and N and P losses. Differs with soil types and drainage status.The requirement for storage is dictated by local climate and if too wet may make practice unrealistic.Added water and carbon during summer and decreased (but unquantified) E. coli losses.Houlbrooke et al. 2008b
Low rate effluent application to landCoupling pond storage with low rates of effluent application can decrease N, P and E. coli loss by minimising the potential for surface runoff and sub-surface losses via preferential flow.ModModLowModLowModFastFastFastThe requirement for solid separation (using low-rate sprinklers) and degree of existing infrastructure that is already suitable. Differences due to soil types and drainage status.Increased labour requirements compared to travelling irrigator.Added water and carbon during summer better matched to pasture growth.Houlbrooke et al. 2008b
Enhanced Pond SystemsCovered Anaerobic Ponds to remove and digest organic suspended solids to methane-rich biogas for energy recovery. High Rate Algal Ponds remove N and P in harvest algae. Maturation Ponds also remove faecal contaminants as indicated by E. coli.HighModHighHighHighHighFastFastFastRemoval efficiency varies seasonally so designed for winter performance specifications and have higher performance in summer. Requires substantial land area (10 to 40 m2/cow)Energy recovery / production. Fewer greenhouse gas emissions.Craggs et al. 2014
Restricted grazing and off pasture animal confinement systemsReduced direct deposition by grazing animals and surface erosion is coupled with a stand-off area to reduce losses during heavy rainfall. HighModLowHighHighLowModModModCosts vary widely due to variations in soil type and climate, and on the frequency of use of a restricted grazing strategy.High capital and operational costs and increased management complexity; potential animal welfare and manure management issues due to the close proximity of animals.Decreased soil and pasture damage and N2O emissions.Ledgard et al. 2006, de Klein and Monaghan 2011, Christensen et al. 2012
Alternative wallowingFencing off of existing connected wallows and the creation of a wallow that is not connected to a stream.LowHighModHighLowLowFastFastFastPoor performance could occur if runoff from alternative wallow reaches stream in large storms.There must be an area close by that is suitable for an artificial wallow.Allowance for natural behaviour may decrease stress (unquantified).McDowell 2009
Preventing fence-line pacingTree planting to provide shelter and maintaining sufficient feed to avoid stress when, for example, when feed is low or near calving.LowLowHighHighModModPlanting, maintenance and effect of tree planting is subject to climatic influences (primarily wind direction).Supplying sufficient feed to avoid animal stress is dependent on the skill of the farm manager.Trees decrease stress and may have anthelmintic properties (if grazed).McDowell et al. 2006
Denitrification bedsLarge containers filled with woodchips that intercept drain flow and denitrify nitrate in water to nitrogen gas which is released to the atmosphere. HighHighModHigh cost when bioreactor was underloaded. True value much more likely to be at lower end when systems properly designedAppropriate hydrology needed - tile/sub-surface drained land or small surface drains.Might be integrated to support dissolved P removalBarkle 2006, Schipper et al. 2010
Precision agricultureSensors and automation of irrigation and nutrient inputs optimises crop utilisation at fine scales.ModLowFastEffect improves with soil heterogeneity, past mismatches between nutrient inputs and requirements and farmer skill.Insufficient communication and training on benefits.Improved farm and herd management; improved crop reliability and quality; conservation of water.Hedley et al. 2010
Change animal typeAnimal type influences N leaching due to inherent differences in the spread of urinary N (the major source of N loss in grazed pastures). N leaching from sheep and deer is approximately half that from beef cows at the same level of feed intake. HighLowSlowHighly variable over time due to changes in relative prices between cattle and sheep meat. Changing relative prices between animal types over time; possibly a need for a mix of animals on a farm; and better farm management skills and farm infrastructure (e.g. extent of fencing). This may also lead to decreased N2O emissions. However, a change to deer may lead to greater sediment and P loss.Haynes and Williams 1993, Hoogendoorn et al. 2011
Diuretic supplementation or N modifierDiuretics such as common salt generally result in increased water consumption by animals with an associated increase in the spread of urinary N by the animals.LowLowFastPotential adaptation by the animal to supplementation or N-modifier leading to less efficacy of the strategy with time.Salt is more appropriate in well-structured soils for long-term use since excess sodium in soil can potentially lead to soil structure degradation.May also lead to decreased nitrous oxide and greenhouse gas emissionsLedgard et al. 2007
Improved N use efficiencyEfficiency gains via: i) reduced use of N fertiliser on winter forage crops coming out of long term pasture; and ii) avoiding excessive N inputs to effluent blocks.LowLowModThe ability to decrease N losses to water depends on (i) the existing level of farm intensity and N loss, and (ii) the management expertise to implement required changes in farm practices. Expertise is required to maximise harvested feed under a low input farming system, while an increase in per cow production (to allow a decrease in stocking rate) takes time as improved genetics is introduced into herds.Decrease emissions of greenhouse gases and an improvement in energy useBeukes et al. 2012, Gourley and Weaver 2012
Supplementary feeding with low-N feedsLowering the protein concentration of supplementary feed to decrease N surplus and N excreted in urine and lost via subsurface flow.LowLowModDepends on source and price of feed and the efficiency with which it is fed to animals.Lack of facilities for feeding out supplementary feed and costs of introducing them; requirement for increased skills in feed utilisation; and increased risk, depending on milk or meat payout and feed pricesMay also lead to reduced N2O, but greater CO2 production in the production and feeding of the low-N feed sources.Clark et al. 2007, Beukes et al. 2012
Low water soluble P fertiliserLess fertiliser-P is lost in runoff due to the low water solubility of products such as reactive phosphate rock resulting in increased P use efficiency.ModLowModGain compared to highly water soluble P fertiliser is dependent on time of year that fertiliser is applied. Larger gains are evident where the coincidence of surface runoff soon after application is frequent.Soil pH < 6.0, rainfall > 800 mm. Also cannot be used for capital applications and must gradually replace maintenance highly-water soluble P applications at a rate of one-third per annum (i.e. 100% low water soluble P in year 3)Has a slight liming effect.McDowell et al. 2003a
Optimum soil test P concentrationMatching soil Olsen P concentrations to pasture and forage crop requirements avoids enriched soil P concentrations that are more likely to lose more P in runoff compared to that at an agronomic optimum concentration.LowLowSlow-FastGain is dependent on soils being enriched beyond their optimum and method of decrease e.g. natural depletion = slow while cultivation = fastNoneNoneMcDowell et al. 2003b
Tile drain amendmentsUse of P-sorbing Ca, Al and Fe materials as backfill for artificial drainage systems. HighLowFastQuantities of sorbing materials (e.g. Al, Fe and Ca). Coarse enough particle size of the material needs to maintain good flow and interaction with materialSource may be far away and the cost of transport prohibitivePotential to decrease (via filtration) the loss of sediment and faecal bacteria (both unquantified).McDowell et al. 2008
Applying alum to forage croplandP-sorbing aluminium sulphate (alum) sprayed onto a winter forage crop just after grazing to prevent surface runoff losses of P.ModModFastMay be ineffective in high rainfall environments where it may be washed from the soil.Few supplies and competing use as a water treatment additiveNoneMcDowell and Houlbrooke 2009
Applying alum to pastureP-sorbing aluminium sulphate (alum) sprayed onto pasture a week before grazing to prevent subsequent surface runoff losses of P.ModModFastMay be ineffective in high rainfall environments where it may be washed from the soil.Few supplies and competing use as a water treatment additiveNoneMcDowell and Norris 2014, McDowell 2015
Red mud (bauxite) to landP-sorbing and caustic red mud (Al-oxide) incorporated into soil at rate of up to 20 Mg ha-1 to prevent P losses in runoff and leaching.HighModFastIncreases soil pH which may increase P solubility if outside pH range 5.5-5.9. Few suppliers. If used for liming effect, grazing animals need to avoid treated area otherwise ingestion may impair rumen function.Alkaline and hence can be used instead of lime.Vlahos et al. 1989
Refurbishing and widening flood irrigation baysWater exiting flood irrigation bays as outwash represents about 20-50% of that applied. Re-contouring irrigation bays, and/or preventing outwash/wipe-off from accessing the stream network decreases P loss. HighModModInaccurate level resulting in flow (and outwash) faster than anticipated. Variation in the water supply rates.A move to spray irrigation is likely to be more cost-effective.More efficient use of flood irrigation water.Houlbrooke et al. 2008a
Dams and water recyclingRecycling systems divert irrigation outwash for use in others part of the farm increases nutrient use efficiency.HighModModLeakage from infrastructureA move to spray irrigation more cost-effective.More efficient use of flood irrigation water.Barlow et al. 2005
Soil conservation plan to plant treesCombination of retirement and pole planting on highly erodible land. Introduction of tree roots to soil regolith protects soil on steep slopes from mass movement erosion. ModHighSlowBenefit depends on severity of erosion and the number of years the trees take to glowNoneDecreased P inputs to waterways, improved shelter for animals.Hicks 1995
Benched headlandsConstructed level bench that runs across the slope of a field. Suitable for use on cultivated soil where slopes are greater than 3 degrees. These encourage infiltration of water on the bench and reduce the slope length of water pathways. ModLowFastDepends on infiltration capacity of soilManagement expertiseIncreased sustainability of cropping. Decreased P input (unquantified) to waterways.Basher 2013
BundsEarthen barrier constructed along paddock edge to prevent water flowing onto or from field. Suitable for use on cropping land with slope greater than 3 degrees. Creates ponds of water at bottom of field where sediment settles out.HighModFastDepends on infiltration capacity of soilManagement expertiseIncreased sustainability of cropping. Decreased P input (unquantified) to waterways.Barber 2014
Contour cultivationCultivation along contours of cropping land with slopes greater than 3 degrees. Reduces the speed and eroding power of runoff water. ModLowFastDepends on infiltration capacity of soil and slope angleEducationIncreased sustainability of cropping. Decreased P input (unquantified) to waterways.Barber 2014
Contour drainsTemporary drains that run across the slope of a field and into a permanent drain on the side of the field reduce the slope length of water pathways and thereby reduce the eroding power. ModLowFastDepends on density of drainsManagement expertiseIncreased sustainability of cropping. Decreased P input (unquantified) to waterways.Basher and Ross 2002
Cover cropGreen manure or cover crop after harvesting of main crop is ploughed into the soil stabilising bare soil from erosion and improves water penetration and drainage. HighLowModDepends on soil structureWillingness of manager to forgo short term gain for long term gainIncreased sustainability of cropping. Basher 2013, Barber 2014
Minimum tillageDirect drilling of seed into stubble or pasture reduces the proportion of time that land is bare and erodible during the growing cycle. LowLowModDepends on the amount of time land is bareManagement expertise. Could increase dissolved P losses.-Basher et al. 1997, Jarvie et al. 2017
Silt fenceMaterial fastened to a wire fence for filtering out sediment from surface runoff. HighHighFastVariability of material and contracting costsHigh costDecreased P input (unquantified) to waterways.Barber 2014
Stubble mulchingStubble is mulched and left on field. Partial ground cover protects soil from erosion. LowModModDepends on the amount of partial ground coverManagement expertiseDecreased P input (unquantified) to waterways.Basher 2013
Wheel track dykingSeries of closely-spaced indentations in wheel tracks created by tillage machinery. Slows surface runoff water down and settles suspended sediment. ModLowFastDepends on the proportion of runoff coming from compacted soilManagement expertiseDecreased P input (unquantified) to waterways.Barber 2014
Wheel track rippingRipping of wheel tracks is suitable for use on cropping land after the use of heavy vehicles on cultivated soil. Ripping allows water to percolate into the soil rather than flow down the tracks. ModLowFastDepends on the proportion of runoff coming from compacted soilManagement expertiseDecreased P input (unquantified) to waterways.Barber 2014
Wind break cropTall crop in paddock providing shelter for neighbouring cultivated paddock from wind erosion. LowModModDepends on value of wind break cropManagement expertiseDecreased P input (unquantified) to waterways.Basher 2013 McDowell and Sharpley 2009

References

Barber, A. 2014. Erosion and sediment control guidelines for vegetable production. Agrilink New Zealand, Auckland, New Zealand.

Barkle, G. 2006. Evaluating strategic retention of artificial drainage flows for nitrate-N reduction under waikato conditions. Environment Waikato, Hamilton, New Zealand.

Barlow, K., D. Nash, and R. B. Grayson. 2005. Phosphorus export at the paddock, farm-section, and whole farm scale on an irrigated dairy farm in south-eastern Australia. Australian Journal of Agricultural Research 56:1-9.

Basher, L., D. Hicks, B. Handyside, and C. Ross. 1997. Erosion and sediment transport from the market gardening lands at Pukekohe, Auckland, New Zealand. Journal of hydrology. New Zealand 36:73-95.

Basher, L. R. 2013. Erosion processes and their control in New Zealand. Pages 363-374 in J. Dymond, editor. Ecosystem services in New Zealand. Manaaki Whenua Press, Lincoln, New Zealand.

Basher, L. R., and C. W. Ross. 2002. Soil erosion rates under intensive vegetable production on clay loam, strongly structured soils at Pukekohe, New Zealand. Soil Research 40:947-961.

Bay of Plenty Regional Council, Rotorua District Council, and Te Arawa Lakes Trust. 2007. Memorandum of Understanding Memorandum of Understanding Rotorua Lakes Restoration Between The Crown And The Rotorua Lakes Strategy Group Bay of Plenty Regional Council, Rotorua, New Zealand.

Beukes, P. C., M. R. Scarsbrook, P. Gregorini, A. J. Romera, D. A. Clark, and W. Catto. 2012. The relationship between milk production and farm-gate nitrogen surplus for the Waikato region, New Zealand. Journal of Environmental Management 93:44-51.

Beutel, M. W., and A. J. Horne. 1999. A review of the effects of hypolimnetic oxygenation on lake and reservoir water quality. Lake and Reservoir Management 15:285-297.

Burns, D. A., and L. Nguyen. 2002. Nitrate movement and removal along a shallow groundwater flow path in a riparian wetland within a sheep-grazed pastoral catchment: Results of a tracer study. New Zealand Journal of Marine and Freshwater Research 36:371-385.

Christensen, C., M. Hedley, J. Hanly, and D. Horne. 2012. Nitrogen loss mitigation using duration-controlled grazing: Field observations compared to modelled outputs. Proceedings of the New Zealand Grassland Association 74:115-120.

Clark, D., J. Paterson, D. Hamilton, J. Abell, M. Scarsbrook, K. Thompson, R. B. Moore, and A. Bruere. 2013. Overview of using detainment bunds for mitigating diffuse-source phosphorus and soil losses from pastoral farmland.in C. L. Christensen and L. D. Currie, editors. Accurate and efficient use of nutrients on farms. Fertilizer and Lime Research Centre, Massey University, Palmerston North, New Zealand.

Clark, D. A., J. R. Caradus, R. M. Monaghan, P. Sharp, and B. S. Thorrold. 2007. Issues and options for future dairy farming in New Zealand. New Zealand Journal of Agricultural Research 50:203-221.

Craggs, R., J. Park, S. Heubeck, and D. Sutherland. 2014. High rate algal pond systems for low-energy wastewater treatment, nutrient recovery and energy production. New Zealand Journal of Botany 52:60-73.

Craig, L. S., M. A. Palmer, D. C. Richardson, S. Filoso, E. S. Bernhardt, B. P. Bledsoe, M. W. Doyle, P. M. Groffman, B. A. Hassett, S. S. Kaushal, P. M. Mayer, S. M. Smith, and P. R. Wilcock. 2008. Stream restoration strategies for reducing river nitrogen loads. Frontiers in Ecology and the Environment 6:529-538.

Crisman, T. L., C. Mitraki, and G. Zalidis. 2005. Integrating vertical and horizontal approaches for management of shallow lakes and wetlands. Ecological Engineering 24:379-389.

Davies‐Colley, R. J., J. W. Nagels, R. A. Smith, R. G. Young, and C. J. Phillips. 2004. Water quality impact of a dairy cow herd crossing a stream. New Zealand Journal of Marine and Freshwater Research 38:569-576.

de Klein, C. A. M., and R. M. Monaghan. 2011. The effect of farm and catchment management on nitrogen transformations and N2O losses from pastoral systems — can we offset the effects of future intensification? Current Opinion in Environmental Sustainability 3:396-406.

Faithfull, C. L., D. P. Hamilton, D. F. Burger, and I. Duggan. 2006. Waikato peat lakes sediment nutrient removal scoping exercise. Waikato Regional coumcil, Hamilton, New Zealand.

Gibbs, M. M., C. W. Hickey, and D. Özkundakci. 2010. Sustainability assessment and comparison of efficacy of four P-inactivation agents for managing internal phosphorus loads in lakes: sediment incubations. Hydrobiologia 658:253-275.

Gourley, C. J. P., and D. M. Weaver. 2012. Nutrient surpluses in Australian grazing systems: management practices, policy approaches, and difficult choices to improve water quality. Crop and Pasture Science 63:805-818.

Haynes, R. J., and P. H. Williams. 1993. Nutrient cycling and soil fertility in the grazed pasture ecosystem. Advances in Agronomy 49:119-199.

Headley, T. R., and C. C. Taner. 2008. Floating Treatment Wetlands: an Innovative Option for Stormwater Quality Applications. Pages 1101-1106 11th International Conference on Wetland Systems for Water Pollution Control, Indore, India.

Hedley, C. B., S. Bradbury, J. Ekanayake, I. J. Yule, and S. Carrick. 2010. Spatial irrigation scheduling for variable rate irrigation. Proceedings of the New Zealand Grassland Association 72:97-101.

Hickey, C. W., and M. M. Gibbs. 2009. Lake sediment phosphorus release management - Decision support and risk assessment framework. New Zealand Journal of Marine and Freshwater Research 43:819-856.

Hicks, D. L. 1995. Control of soil erosion on farmland: a summary of erion's impact on New Zealand agriculture, and farm management practices which counteract it. Wellington, New Zealand.

Hoogendoorn, C. J., K. Betteridge, S. F. Ledgard, D. A. Costall, Z. A. Park, and P. W. Theobald. 2011. Nitrogen leaching from sheep-, cattle- and deer-grazed pastures in the Lake Taupo catchment in New Zealand. Animal Production Science 51:416-425.

Houlbrooke, D., P. Carey, and R. Williams. 2008a. Management practices to minimise wipe-off losses from border-dyke irrigated land.in L. D. Currie and L. J. Yates, editors. Carbon and nutrient management in agriculture. Fertilizer and Lime Research Centre, Massey University, Palmerston North, New Zealand.

Houlbrooke, D. J., D. J. Horne, M. J. Hedley, V. Snow, and J. A. Hanly. 2008b. Land application of farm dairy effluent to a mole and pipe drained soil: implications for nutrient enrichment of winter-spring drainage. Australian Journal of Soil Research 46:45-52.

Howard-Williams, C. 1987a. In-lake control of eutrophication. Pages 195-202 in W. N. Vant, editor. Lake Managers’ Handbook. Water & Soil Miscellaneous Publication, Wellington, New Zealand.

Howard-Williams, C. 1987b. In-lake control of eutrophication. Pages 195-204 in W. N. Vant, editor. Lake Managers’ Handbook. National Water and Soil Conservation Authority Wellington, New Zealand.

Jacoby, J. M., C. W. Anderson, and E. B. Welch. 1997. Pine Lake response to diversion of wetland inflow. Lake and Reservoir Management 13:302-314.

James, E., P. Kleinman, T. Veith, R. Stedman, and A. Sharpley. 2007. Phosphorus contributions from pastured dairy cattle to streams of the Cannonsville Watershed, New York. Journal of Soil and Water Conservation 62:40-47.

Jarvie, H. P., L. T. Johnson, A. N. Sharpley, D. R. Smith, D. B. Baker, T. W. Bruulsema, and R. Confesor. 2017. Increased Soluble Phosphorus Loads to Lake Erie: Unintended Consequences of Conservation Practices? Journal of Environmental Quality 46:123-132.

Jellyman, D., J. Walsh, M. de Winton, and D. Sutherland. 2009. A review of the potential to re-establish macrophyte beds in Te Waihora (Lake Ellesmere). NIWA, Christchurch, New Zealand.

Klapper, H. 2003. Technologies for lake restoration. Journal of limnology 62:73-90.

Ledgard, S., M. Sprosen, A. Judge, S. Lindsey, R. Jensen, D. Clark, and J. Luo. 2006. Nitrogen leaching as affected by dairy intensification and mitigation practices in the Resource Efficient Dairying (RED) trial. Pages 263-268 in L. D. Currie and J. A. Hanly, editors. Implementing sustainable nutrient management strategies in agriculture. Ferilzer and Lime Research Centre, Massey University, Palmerston North, New Zealand.

Ledgard, S. F., B. Welten, J. C. Menneer, K. Betteridge, J. R. Crush, and M. D. Barton. 2007. New nitrogen mitigation technologies for evaluation in the Lake Taupo catchment. Proceedings of the New Zealand Grassland Association 69:117-121.

Lessard, J., D. Murray Hicks, T. H. Snelder, D. B. Arscott, S. T. Larned, D. Booker, and A. M. Suren. 2013. Dam Design can Impede Adaptive Management of Environmental Flows: A Case Study from the Opuha Dam, New Zealand. Environmental Management 51:459-473.

McDowell, R. W. 2008. Water quality of a stream recently fenced‐off from deer. New Zealand Journal of Agricultural Research 51:291-298.

McDowell, R. W. 2009. Maintaining good water and soil quality in catchments containing deer farms. International Journal of River Basin Management 7:187-195.

McDowell, R. W. 2015. Treatment of pasture topsoil with alum to decrease phosphorus losses in subsurface drainage. Agriculture, Ecosystems & Environment 207:178-182.

McDowell, R. W., C. Gongol, and B. Woodward. 2012. Potential for controlled drainage to decrease nitrogen and phosphorus losses to Waituna Lagoon. AgResearch, Mosgiel, New Zealand.

McDowell, R. W., M. Hawke, and J. J. McIntosh. 2007. Assessment of a technique to remove phosphorus from streamflow. New Zealand Journal of Agricultural Research 50:503-510.

McDowell, R. W., and D. J. Houlbrooke. 2009. Management options to decrease phosphorus and sediment losses from irrigated cropland grazed by cattle and sheep. Soil Use and Management 25:224-233.

McDowell, R. W., S. T. Larned, and D. J. Houlbrooke. 2009. Nitrogen and phosphorus in New Zealand streams and rivers: Control and impact of eutrophication and the influence of land management. New Zealand Journal of Marine and Freshwater Research 43:985-995.

McDowell, R. W., R. M. Monaghan, and P. L. Carey. 2003a. Potential phosphorus losses in overland flow from pastoral soils receiving long‐term applications of either superphosphate or reactive phosphate rock. New Zealand Journal of Agricultural Research 46:329-337.

McDowell, R. W., R. M. Monaghan, and J. Morton. 2003b. Soil phosphorus concentrations to minimise potential P loss to surface waters in Southland. New Zealand Journal of Agricultural Research 46:239-253.

McDowell, R. W., and M. Norris. 2014. The use of alum to decrease phosphorus losses in runoff from grassland soils. J Environ Qual 43:1635-1643.

McDowell, R. W., and A. N. Sharpley. 2009. Atmospheric deposition contributes little nutrient and sediment to stream flow from an agricultural watershed. Agriculture, Ecosystems & Environment 134:19-23.

McDowell, R. W., A. N. Sharpley, and W. Bourke. 2008. Treatment of drainage water with industrial by-products to prevent phosphorus loss from tile-drained land. J Environ Qual 37:1575-1582.

McDowell, R. W., D. R. Stevens, V. Cave, R. J. Paton, and M. Johnson. 2006. Effects of shelter belts on fence-line pacing of deer and associated impacts on water and soil quality. Soil Use and Management 22:158-164.

McIntosh, J. 2004. Hypolimnetic discharge Lake Okareka. Environment Bay of Plenty, Rotorua, New Zealand.

McKergow, L. A., C. C. Tanner, R. M. Monaghan, and G. Anderson. 2007. Stocktake of diffuse pollution attenuation tools for New Zealand pastoral farming systems. NIWA, Hamilton, New Zealand.

Miller, N. 2006. Summary report on possible dredging of lakes in the Rotorua district. A & E Consultants, Rototua, New Zealand.

Mitsch, W. J. 1995. Restoration of our lakes and rivers with wetlands — An important application of ecological engineering. Water Science and Technology 31:167-177.

Muirhead, R. W., and R. M. Monaghan. 2012. A two reservoir model to predict Escherichia coli losses to water from pastures grazed by dairy cows. Environment International 40:8-14.

Nϋrnberg, G. K. 2007. Lake responses to long-term hypolimnetic withdrawal treatments. Lake and Reservoir Management 23:388-409.

Özkundakci, D., D. P. Hamilton, and P. Scholes. 2010. Effect of intensive catchment and in-lake restoration procedures on phosphorus concentrations in a eutrophic lake. Ecological Engineering 36:396-405.

Paul, W. J., D. P. Hamilton, and M. M. Gibbs. 2008. Low-dose alum application trialled as a management tool for internal nutrient loads in Lake Okaro, New Zealand. New Zealand Journal of Marine and Freshwater Research 42:207-217.

Pilgrim, K. M., and P. L. Brezonik. 2005. Evaluation of the Potential Adverse Effects of Lake Inflow Treatment with Alum. Lake and Reservoir Management 21:77-87.

Redding, M. R., B. Welten, and M. Kear. 2008. Enhancing the P trapping of pasture filter strips: successes and pitfalls in the use of water supply residue and polyacrylamide. European Journal of Soil Science 59:257-264.

Schallenberg, M., S. T. Larned, S. Hayward, and C. Arbuckle. 2010. Contrasting effects of managed opening regimes on water quality in two intermittently closed and open coastal lakes. Estuarine, Coastal and Shelf Science 86:587-597.

Schallenberg, M., and L. Schallenberg. 2017. Lake Hayes restoration and monitoring plan. Hydrosphere Ltd, Dunedin, New Zealand.

Schipper, L. A., W. D. Robertson, A. J. Gold, D. B. Jaynes, and S. C. Cameron. 2010. Denitrifying bioreactors—An approach for reducing nitrate loads to receiving waters. Ecological Engineering 36:1532-1543.

Scholes, P., and J. McIntosh. 2010. The tale of two lakes: Managing lake degradation, Rotorua lakes, New Zealand. Pages 157-168 in A. M. Marinov and C. A. Brebbia, editors. Water pollution X. Wit Press, Southampton, U.K.

Shepherd, M., A. Stafford, and D. Smeaton. 2012. The use of a nitrification inhibitor (DCn™) to reduce nitrate leaching under a winter-grazed forage crop in the Central Plateau. Proceedings of the New Zealand Grassland Association 74:103-108.

Smith, C. M. 1989. Riparian pasture retirement effects on sediment, phosphorus, and nitrogen in channellised surface run-off from pastures. New Zealand Journal of Marine and Freshwater Research 23:139-146.

Vlahos, S., K. J. Summers, D. T. Bell, and R. J. Gilkes. 1989. Reducing phosphorus leaching from sandy soils with red mud bauxite processing residues. Australian Journal of Soil Research 27:651-662.