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    Assessment of the transport and transformation of nitrogen in the unsaturated and saturated zones under two dairy farms in the Manawatu River catchment : a thesis presented in partial fulfilment of the requirements for the degree of Master in Environmental Management at the Institute of Agriculture and Environment, Massey University, Palmerston North, Manawatu, New Zealand
    (Massey University, 2015) Espanto, Patrick Benson B
    The importance of dairy farming in New Zealand is reflected in the country’s export and gross domestic product earnings. While the economic and food production benefits are evident, there is an increasing concern about the effects of excess nutrient runoff on water quality and ecosystem health. Studies on the transport and transformation of nutrients, specifically nitrogen, are limited or mainly focused on the management and reduction of nutrient losses from the root zone. This is also the case in the Manawatu River catchment of New Zealand. The goal of this study was to assess the transport and transformation of nitrogen in the unsaturated (below the root zone) and saturated zones using field measurements, a tracer test, and identification of redox conditions in the shallow groundwater. Two sites were chosen in the Manawatu River catchment: Site 1 (Massey Dairy Farm No. 1, Palmerston North) and Site 2 (Te Matai Road, Whakarongo). Soil-water and groundwater were extracted using 12 porous cups (0.3, 0.6, 1.0, 2.0 m bgl) and four piezometers (5.8, 6.3, 7.4, 8.7 m bgl) installed at Site 1, and six piezometers (12, 18, 33, 51, 66, 87 m bgl) installed at Site 2. The extracted water samples were analysed for nitrate-nitrogen (NO3-N) and other water quality parameters. The average NO3-N concentrations in the unsaturated zone (0.3 – 2.0 m bgl) decreased with depth. At Site 1, a tracer test was conducted in November, 2013, using an application of urea (467 kg N/ha) and bromide (206 kg Br/ha). After fertiliser application, NO3-N concentrations increased in the root zone. The bromide reached only until the 2-m depth porous cup in January, 2014, after a total irrigation depth of 478 mm. The early appearance of bromide in the 0.3 m depth root zone suggested preferential flow, a pathway that speeds up transport of potential contaminants in the groundwater. The observed data of NO3-N, dissolved oxygen (DO), iron, manganese, and sulphate were utilised to assess the redox condition in groundwater at both sites. The decreasing NO3-N concentrations with increasing depth indicated dilution and/or the occurrence of denitrification in the groundwater. The groundwater redox conditions were mixed oxic-anoxic in the 5.8 – 51 m bgl and mainly anoxic below 51 m groundwater depth.
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    An investigation of composting poultry manure in relation to nitrogen conservation and phosphate rock dissolution : a thesis presented in partial fulfilment of the requirements for the degree of Doctor of Philosophy in Soil Science at Massey University
    (Massey University, 1993) Mahimairaja, Santiago
    Gaseous losses of nitrogen (N) through ammonia (NH3) volatilization and denitrification diminish the fertilizer value of animal and poultry manures and form atmospheric pollutants. Appropriate methods of composting can improve the fertilizer value by conserving manure N and minimise the risk of environmental pollution. Additionally, acids produced during composting and nitrification of conserved N in manure, provide a source of protons (H+) which have the potential to dissolve phosphate rock (PR) when composted with manure. The objective of this research was to examine the methods of composting poultry manure with different amendments in relation to N conservation and PR dissolution. Firstly, the methods for preserving and measuring N in manure samples were evaluated. The results suggested that freeze drying and inclusion of a strong oxidizing agent (KMnO4) prior to routine Kjeldahl digestion were required to achieve complete recovery and accurate measurement of N in manure samples. Methods for reducing the loss of N through NH3 volatilization and denitrification during aerobic and anaerobic composting of poultry manure with different amendments were investigated in controlled 'flow through' incubation experiments. The amendments included carbonaceous bedding materials (woodchip, paper waste, wheat straw and peat), acidifier (elemental sulphur-S°) and adsorbents (zeolite and soil). The loss of N through NH3 volatilization from aerobic composting was about 17% of the manure N which was reduced by 90-95% under anaerobic composting. Under aerobic composting the addition of various amendments reduced the volatilization loss by 33 to 60%. Although the rate of denitrification was negligible (<1µg kg-1 day-1) in fresh manure, it increased enormously (3.7mg kg-1 day-1) during composting. The presence of nitrate (NO3-) was found to be a rate determinant for denitrification in manure. Amongst the treatments, the addition of S° was very effective in reducing NH3 volatilization and denitrification. The dissolution of PR during composting with poultry manure was examined using radioactively (32P) labelled synthetic francolite and North Carolina phosphate rock (NCPR). The use of 32P labelled francolite indicated that PR dissolution in poultry manure/PR composts could be measured more accurately from the increases in NaOH extractable phosphorus (∆NaOH-P) than from the decreases in HCl extractable P (∆HCl-P). Low levels of francolite and NCPR dissolution (<16%) occurred when PR is mixed with poultry manure. This was attributed to the high concentrations (4.8 * 10-2mol L-1) of calcium (Ca2+) in manure solution which inhibited the dissolution of PR through the Ca common-ion effect. Addition of S° to poultry manure/PR compost reduced the pH and thereby enhanced PR dissolution. A system for the dissolution of PR, using the acid (H+) produced during the nitrification of NH3 released from poultry manure, was developed. The inhibitory effect of manure Ca on PR dissolution is avoided if the NH3 released from decomposing manure is absorbed in bark and soil materials containing PR, which are kept either as manure covers or in separate columns. Although both methods were found effective in the absorption of NH3, the result demonstrated that bark absorbs more NH3 than does soil. Extensive PR dissolution occurred in the bark (82.3%) and the soil (33.2%) even in the absence of NH3 absorption from poultry manure. Higher levels of PR dissolution in bark is attributed to its high exchangeable acidity (80.5cmol (+) kg-1) and large Ca sink size (82.7cmol (+) kg-1). However, when the bark and soil materials were kept as manure covers, accumulation of Ca in the covers due to the diffusion of manure Ca, reduced the PR dissolution. When the bark and soil materials were kept separately in columns, nitrification of absorbed NH3 resulted in small increases in PR dissolution in bark (15%) and soil (5%). However, most of the protons (50-95%) released during nitrification are involved in the buffering of the bark and soil materials. The laboratory studies showed that the addition of S° to poultry manure during aerobic composting not only reduced the loss of N, but also enhanced PR dissolution. Based on this observation, sulphocompost (a blend of poultry manure, woodchip with S° and PR) and phosphocompost (a blend of poultry manure, woodchip with PR) were prepared and their agronomic effectiveness were compared with fresh manure mixtures and urea using field grown winter cabbage and summer maize crops. The crop yield, N use efficiency and N recovery were greater for sulphocompost than for phosphocompost. The sulphocompost and phosphocompost were approximately 60% and 12%, respectively, as effective as urea treatments for winter cabbage. Both composts were equally effective as urea for the second season's maize crop. The study has shown that poultry manure enriched with PR and S° can be used as a source of N, P and S.