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HCS412 Forage Crops
Nitrogen - Chapter 4 pg 84-87 & Chapter 12 pg 267-275
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Introduction
N-balance
N-fixation
Fertilizer N
Losses in hay, silage and animal products
Other components of the N balance
| N is the most limiting nutrient in all of agriculture | |
| soil N is generally related to soil fertility - both are extremely difficult to measure and quantify (although N is so important, farmers have no test for soil N). | |
| soil N forms include NO3 and NH4, and also numerous organic-N molecules which vary in plant availability | |
| NO3 and NH4 are extremely soluble and don't stay in the soil for long. | |
| Forage production is poorly related to soil N, it is more closely related to flow through the soil N pool than the size of the soil N pool. |
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NB "balance" approach varies from a "cycling" approach |
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For any site, change in soil N status = inputs - losses |
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inputs = N-fixation + fertilizer N + release from soil organic matter + atmospheric
deposition |
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Losses = atmospheric losses + leaching + loss to plant & animal products |
Legumes
and N-fixation (pg 85)
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Fertilizer nitrogen (pg 273)
responses to applied N are 0-60 kg DM/kgN - typically 20 kg DM/kg N |
Losses in hay/silage and animal products
| Removal
in hay/silage or animal products Often underestimated - but is usually the greatest loss of N from the soil |
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| Hay
typically 25% protein (protein is 16% N = hay is 4%N) Typical alfalfa harvest 4 crops each of 1.5 ton/acre (12,000 lb/acre, 13.4 T/ha) = 480 lbN/ac (540 kgN/ha) |
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| Cow-calf
operation Grazing 1 cow per acre, producing a 600 lb (275 kg) stocker calf per acre 60% protein (16%N) = 58 lbN/acre |
Other Components of the N-balance
| Atmospheric
deposition = pollution 20 kgN/ha/yr in North America 50 kgN/ha/yr in Europe |
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| Volatilization Release of NH3 from fertilizers - results in inefficiency of fertilizer application Unless nitrogenous fertilizers are washed into the soil by rainfall soon after application they can "evaporate" as NH3 and reduce the fertilizer response |
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| Leaching Not usually significant for most soils (being N deficient) Can be extremely high if total N inputs (fixation and fertilizer) exceed 250 kgN/ha Is usually high in areas with repeated applications of effluent |
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| Nitrification
& Denitrification An environmental issue. In extreme cases can account for up 30% of N losses from soil Nitrification = oxidation of NH4 to NO3 Denitrification = reduction of NO3 to N2O, NO2 and N2 (released to the atmosphere), high in wet soils |
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