Leaching of from stony soils after effluent application.

Irrigation of dairy shed effluent (DSE) onto land is an integral part of New Zealand's farming practice. The use of inappropriate soils can result in contamination of ground waters with microbes and nutrients. A gap in our knowledge is the ability of stony soils to safely treat DSE. Replicates of four stony soils were collected from the Canterbury region of New Zealand as intact soil lysimeters 460 mm in diameter and up to 750 mm deep. The soils had either stones to the surface or 300 to 600 mm fines over stones. To determine breakthrough characteristics, a pulse of DSE (25 mm depth) spiked with bromide (2000 mg L) was applied to the soil cores followed by continuous artificial rainfall, for one pore volume, at 5 mm h. Leachate aliquots were analyzed for , bromide, and NH-N. The lysimeters were then subjected to hoof pugging using a mechanical hoof, and the leaching characteristics of the soil were determined again. breakthrough curves revealed that the potential for to leach through the soils was high for Selwyn very stony soil and low for other soils analyzed. After pugging, leaching of increased in Mackenzie soil with stones to the surface. For most other soil cores, concentrations in soil leachates were low. In soils where stones are close to the surface, especially where the soil matrix is sandy, we anticipate that shallow groundwater is vulnerable to microbial contamination under some land management practices.

Denitrification and availability of carbon and nitrogen in a well-drained pasture soil amended with particulate organic carbon.

A well-drained soil in N-fertilized dairy pasture was amended with particulate organic carbon (POC), either sawdust or coarse woody mulch, and sampled every 4 wk for a year to test the hypothesis that the addition of POC would increase denitrification activity by increasing the number of microsites where denitrification occurred. Overall mean denitrifying enzyme activity (DEA), on a gravimetric basis, was 100% greater for the woody mulch treatment and 50% greater for the sawdust treatment compared with controls, indicating the denitrifying potential of the soil was enhanced. Despite differences in DEA, no difference in denitrification rate, as measured by the acetylene block technique, was detected among treatments, with an average annual N loss of ∼22 kg N ha yr Soil water content overall was driving denitrification in this well-drained soil as regression of the natural log of volumetric soil water content (VWC) against denitrification rate was highly significant ( = 0.74, < 0.001). Addition of the amendments, however, had significant effects on the availability of both C and N. An additional 20 to 40 kg N ha was stored in POC-amended treatments as a result of increases in the microbial biomass. Basal respiration, as a measure of available C, was 400% greater than controls in the sawdust treatment and 250% greater than controls in the mulch. Net N mineralization, however, was significantly lower in the sawdust treatment, resulting in significantly lower nitrate N levels than in the control. We attribute the lack of measured response in denitrification rate to the high temporal variability in denitrification and suggest that diffusion of nitrate may ultimately have limited denitrification in the amended treatments. Our data indicate that manipulation of denitrification by addition of POC may be possible, particularly when nitrate levels are high, but quantifying differences in the rate of denitrification is difficult because of the temporal nature of the process (particularly the complex interaction of N availability and soil water content).

Regionalizing potential for microbial bypass flow through New Zealand soils.

Microbial breakthrough curves of 12 soils, generated by the application of dairy shed effluent followed by continuous artificial rainfall for one pore volume at 5 mm h(-1) onto large undisturbed soil cores, have been ranked as high, medium, or low potential for microbial bypass flow. The ranking is based on the position of the peak in the breakthrough curve. Knowledge of soil properties that affect microbial transport through soil gained from the microbial breakthrough curves was linked to soil classes, or to their accessory properties, of the New Zealand Soil Classification. Spatial depiction of the ratings has been achieved via the national 1:50,000 scale soil map. Soils with a drainage impediment or those with well developed soil structure have a high potential for microbial bypass flow, whereas soils from tephra and Recent Soils with less developed, porous, soil structure have a low potential for microbial bypass flow. The risk rankings should be considered as maxima because management may change some rankings.