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Effects of cattle,sheep and deer grazing on soil physical quality and losses of phosphorus and suspended sediment losses in surface runoff
Authors:Fiona Curran Cournane  Richard McDowell  Roger Littlejohn  Leo Condron
Institution:1. Federal University of Parana - UFPR, Agricultural Sciences Sector, Department of Crop Production and Protection, Rua dos Funcionários 1.540, CEP 80035-050 Curitiba, PR, Brazil;2. Federal University of Paraná - UFPR, Department of Soil Science and Agricultural Engineering, Rua dos Funcionários, 1540, 80035-050 Curitiba, Brazil;3. USDA-Agricultural Research Service, 3218 Williams Hall, NCSU Campus Box 7619, Raleigh, NC 27695, USA;4. Santa Catarina State University – UDESC, Av. Luís de Camões, 2090, CEP 88520-000 Lages, SC, Brazil;5. Federal University of Parana - UFPR, Biological Sciences Sector, Department of Biochemistry, Coronel Francisco H. dos Santos Avenue, without number, Curitiba, PR CEP 19031, Brazil;6. Federal University of Rio Grande do Sul - UFRGS, Faculty of Agronomy, Av. Bento Gonçalves 7712, CEP 91501-970, Cx Postal 776, Porto Alegre, RS, Brazil
Abstract:Livestock grazing and treading is strongly linked to a decrease in freshwater quality and promotes eutrophication. A two-year field trial was carried out to investigate the influence cattle, sheep and deer have on soil physical quality and the loss of phosphorus (P) and suspended sediment (SS) in surface runoff. Surface runoff plots (4 m long by 1 m wide) were installed within areas designated as stock or ungrazed (control). Surface runoff was collected and analysed for concentrations and loads of P fractions (dissolved reactive P-DRP, dissolved unreactive P-DUP, total dissolved P-TDP, particulate P-PP and total P-TP) and SS. Grazed at equivalent stocking density, soil physical samples (macroporosity, bulk density, and saturated hydraulic conductivity Ksat) were taken after each grazing event (n = 11). Soil physical data indicated differences between cattle, sheep and deer with cattle having greater negative effects. However, these differences had no impact on P and SS losses between stock types in surface runoff. Significant relationships showed that an increase in macroporosity, Ksat, and time (days) since grazing decreased concentrations and loads of P and SS losses. A separate rainfall simulation study also revealed that an increase in simulated cattle treading intensity increased the volume of surface runoff and SS losses. Most surface runoff (> 90%) occurred in winter when soil moisture was at or above field capacity. A seasonal effect was observed and showed that although the greatest P loads occurred in winter, the greatest P concentrations occurred in summer months, under infiltration-excess conditions. These summer losses could pose a risk to receiving waterways because increased light and warmth may induce an algal response compared to winter. While there is limited scope to manage for infiltration-excess surface runoff losses from pasture, with most runoff occurring in winter, these findings reinforce the use of mitigation strategies such as restricted or nil grazing in winter when soil moisture has reached field capacity to minimise P and SS loss to surface water, regardless of stock type.
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