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Carbon Sequestration Breaking New Ground Building the Base
Carbon Sequestration ,[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object]
Time is critical   ,[object Object],[object Object],[object Object],[object Object]
All About Carbon ,[object Object],[object Object],[object Object],[object Object],[object Object]
Carbon is dynamic, but also constant: ,[object Object],[object Object],[object Object],[object Object],[object Object]
Carbon is critical to soil health because it influences : ,[object Object],[object Object],[object Object],[object Object],[object Object]
Soil Life: ,[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object]
The Value of Soil Carbon ,[object Object],[object Object],[object Object]
Carbon increases holding capacity
Moisture cycles in Nebraska
Teaching Points: ,[object Object],[object Object],[object Object],[object Object],[object Object]
Carbon comes from roots
Potential Carbon Impact Practice ( kg C / ha /year)
Unfortunately, many habitats are now too damaged to support the wildlif that once maintained them. ,[object Object]
Managed  livestock can successfully restore these areas, then maintain them until wildlife populations recover.
Early settlers plowing the prairie – To survive in a seemingly hostile environment
People who farmed sustainably for over 40 centuries  now lose 18 lbs of farmable soil for every 1 lb of food eaten
 
 
Historical Carbon Levels
The simple math behind Soil Carbon ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
The True Scale of “The Job” ,[object Object],[object Object]
FACT  FACT  FACT ,[object Object]
FACT  FACT  FACT ,[object Object]
FACT  FACT  FACT ,[object Object],[object Object],[object Object]

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Stewardship of Natural Resources 8.10.09

Notas do Editor

  1. This program will discuss the results of work sponsored by NETF and NRCS and performed by CFRA staff from 2002 to 2007. What do farmers need to know to…
  2. Bulk density ----------------- Soils vary in weight per given volume. Healthy, biologically active soils weigh around 1 tonne per cubic metre, whilst heavy clays that contain little or no organic matter (such as clays that might be used for brickmaking) weigh up to 1.8 tonnes per cubic metre. In general, healthy soils are more porous, have more air holes and contain more light weight organic matter than biologically degraded soils. For this example we have chosen to us a commonly occurring bulk density of 1.4 tonnes per cubic metre. % Change in Soil Organic Matter -------------------------------------------- Once the mass of a soil is calculated by multiplying volume by Bulk Density, it is possible to calculate the change in mass per % change in Soil Organic Matter (SOM). At any Bulk Density the change remains the same, regardless of whether the soil improves from 1% SOM to 2% or from 10% SOM to 11%. Soil Organic Matter contains approximately 58% elemental Carbon Converting Carbon Dioxide (CO2) to Carbon ------------------------------------------------------------ On the Periodic Table, carbon has a weight of 12 and oxygen 16. Carbon dioxide, which contains 2 x oxygen and 1 x carbon therefore weighs 44. To achieve a 1 unit move in carbon from carbon dioxide the conversion ratio is 44/12 or 3.67. For every tonne of carbon sequestered 3.67 tonnes of carbon dioxide must be removed from the atmosphere. The full maths for this slide ------------------------------------ 10,000 sq. metres x 33.55 cm = 3,355 cubic metres per hectare 3,355 cubic metre x 1.4 BD = 4,697 tonnes of soil per hectare to a depth of 33.5 cm A 1% change in this mass = 46.97 tonnes Which contains 46.97 x 58% = 27.24 tonnes of Carbon Captured Carbon 27.24 tonnes x 3.67 = 99.98 tonnes CO2