A simulated rainfall study carried out as part of a larger grazing experiment was conducted to investigate the effects of a 2-3 day cattle-treading event in winter on soil physical properties and contaminant (sediment and nutrient) runoff in topographically variable hill land. Measurements were made on two land zones: easy contoured ridges and gullies (15-24° slope) and steep inter-track land (28-39° slope). Simulated rainfall was applied to 16 plots (0.5 m 2 ) with a range of treading damage for each land zone within 14 days of the treading event. Simulated rainfall was repeated on the same plots in the following summer and winter to assess the recovery of soil from treading damage. A97034 Received 28 April 1997; accepted 22 January 1998Treading damage reduced water infiltration rate, particularly in the steep zone. It also caused a significant increase in the transport of suspended solids (SS), total Kjeldahl nitrogen (TKN), and total phosphorus (TP) from the plots during simulated runoff. On the steep inter-track zone, damaged areas had a 46% lower infiltration rate, and runoff from these areas contained on average 87% more sediment, and 89% more N and 94% more P compared with undamaged areas. These effects had disappeared six months later. The rainfall simulation and soil physical studies show that a 2-3 day winter treading event may increase soil bulk density, reduce soil macroporosity and total porosity, and lead to a decrease in the water infiltration rate and an increase in contaminant runoff.
An experiment was conducted on steep hill land in New Zealand to describe the pattern of cattle treading that occurred from a single damage event during winter. The experiment also measured some of the consequences of treading and sought to define the subsequent grazing management which promoted the most rapid recovery of pasture.In hill paddocks of mixed topography, damage of the soil surface was greatest on animal tracks/ camps and easy contoured areas (<25°) where cattle prefer to walk. Evidence of this initial winter impact disappeared over spring, most rapidly on easy contoured areas and under continuous sheep grazing. To promote rapid recovery of damaged paddocks continued grazing of cattle during spring should be avoided.At high levels of damage (>50% soil surface), puddling on tracks/camps and skid damage on steep inter-tracks became frequent. These processes are significant because animal tracks/camps act as important channels for surface water flow in hill lands; and disturbed, inter-track areas are an important source of sediment runoff.During spring, pasture growth rates were reduced by treading damage. From a systems context this could represent losses of 5-10 kg DM ha -1 d -1 during early-mid spring. Pasture cover and growth rates had fully recovered by early December.
Aspect and land slope have a major influence on winter and spring pasture growth. Possible physiographic, soil, and plant factors contributing directly to this influence were examined across a range of microsites in steep North Island hill country. As land slope increased, organic and inorganic nitrogen in the soil decreased. Similarly, organic carbon decreased and this was associated with a decline in soil water-holding capacity. Soil water potentials were high during winter and spring and showed little effect of aspect. Pasture growth was greater on warmer, north-facing than on colder, south-facing aspects, the difference being less for ryegrass-dominant sites than for browntop associations. Where long-term site conditions (e.g., slope, fertility, moisture) allow the development and maintenance of perennial rye grass populations, greater winter and spring growth rates were recorded. The importance of developing an effective N cycle based on stable legume populations for improving soil N status, ryegrass content, and cool-season pasture production in hill country is highlighted.
Nine subterranean clover cultivars and 11 white clover lines were evaluated for persistence and production, under a combination of rotational grazing or cutting, for 4 years on rolling pumice hill country. The most successful subterranean clover cultivarwas 'Tallarook' , whichfor 4 yearsproduced the most dry matter (DM) (average 700 kg DM/ha per year) and accumulated the largest soil seed reserve (1500 kg seed/ha), Soil moisture stress over the summer severely limited persistence and hence production of all white clovers (average 400 kg DM/ha per year). Persistence was not assured by larger roots associated with large-leaved lines. Hill country types (e.g., 'Whatawhata Early Flowering') with a high stolon densityand/or free seedingability were the best adapted to this environment
Variations in soil moisture content, nutrient levels, and temperature were measured for a range of micro-sites located on a steep, northfacing hillside. Species distribution and plant responses to changing moisture conditions and different grazing treatments were related to these physical conditions. Soil nutrient levels (organic carbon; total, inorganic, and mineralised nitrogen; Olsen phosphorus; potassium) were highest in camp/old track areas reflecting nutrient transfer by grazing animals. Variation in nutrient level between other flat and sloping areas was low. Soil moisture holding capacities were similar for most areas, but sloping areas were consistently drier in the surface horizon (0-50 mm) because of less effective rewetting compared with flatter areas. Maximum soil surface temperatures of 45-50°C were reached on clear days where low pasture cover existed on sloping areas. The effects of grazing treatments on ryegrass and browntop tiller number, white clover leaf number, and seedling establishment were similar across a wide range of micro-sites. However, pasture species content varied between micro-sites: ryegrass was dominant on camps and tracks; brown top increased with steepness of slope; white clover peaked on rolling and easy sloping areas; grass seedlings were most numerous on camps and tracks; and legume seedlings were most numerous on steeper slopes. Pasture type would appear to be determined more by nutrient fluxes (e.g., mineralisation rate, excreta return) and summer rewetting of the soil surface than by nutrient pool size and inherent water-holding capacity of the soil.
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