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Paul Poulton & Johnny Johnston Rothamsted Research

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Presentation on theme: "Paul Poulton & Johnny Johnston Rothamsted Research"— Presentation transcript:

1 Paul Poulton & Johnny Johnston Rothamsted Research
The ability of soil to ensure P nutrition for the crop – using data from the long-term trials at Rothamsted. Paul Poulton & Johnny Johnston Rothamsted Research

2 Phosphorus – the issues
Phosphorus is an essential, irreplaceable nutrient in crop and animal nutrition Phosphorus lost from agriculturally managed soils to surface water bodies, e.g. lakes, causes eutrophication Global reserves of phosphorus are limited

3 Exhaustion Land Treatments 1856-1901 No P or K fertilizer
NPK fertilizers Farmyard manure 300m Soil is a silty clay loam (Chromic Luvisol)

4 Microplots testing available soil P and fresh fertilizer P

5 Current concepts of the behaviour of P in soil
P offtake Fertilizers and manures P in crop Less readily available pool Readily available pool Slowly available pool Soil solution Losses Soil analysis measures P in the soil solution and the readily available pool

6 How much P should there be in the readily available pool?

7 Examples of critical values for arable crops

8 Saxmundham:- response to fresh P

9 Effect of soil organic matter
SOM % Yield t/ha Olsen P mg/ha % variance acc’ted for Barley grain Potato tubers S. beet sugar

10 Effect of plant available soil P on the response to N
Olsen P 140 mg/kg 13 mg/kg 3 mg/kg

11 Transport of P from soil to water
In eroded soil By movement through soil into drainage ditches and rivers Incidental losses from surface applied slurries and fertilizers when rainfall causes surface run-off

12 Relationship between yield, Olsen P and total P losses

13 Conclusions There is a critical level of plant available P in the soil below which yield will be limited and N used less efficiently. Thus, soils should be maintained at slightly above this value. BUT, there is also a threshold value for available P, above which there is an increasing risk of P being lost to ditches or streams. Unnecessarily high levels of available P should therefore be avoided. Both of the above values will vary; depending on eg soil type and soil organic matter.

14 Thanks to the many scientific and farm staff at Rothamsted Research
Acknowledgements Thanks to the many scientific and farm staff at Rothamsted Research


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