Understanding Soil Test Results Part 2: Phosphorus, Potassium, Other Cations, & %Base Saturation

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  • เผยแพร่เมื่อ 6 เม.ย. 2016
  • This video will give you insight into understanding your soil test results regarding Phosphorus, Potassium, Cations, and Percent Base Saturation.

ความคิดเห็น • 6

  • @ChilcoteForestryServices
    @ChilcoteForestryServices 4 ปีที่แล้ว

    how does gypsum reduce high Mg levels?

  • @MrBob58o
    @MrBob58o 3 ปีที่แล้ว

    So will the P1 Bray give an idea of what is readily available and the Strong Bray tell you what is in the slow release reserves?

    • @tw6721
      @tw6721 3 ปีที่แล้ว +2

      Not quite; its used to highlight any inconsistencies in testing, if the P2 is wildly differing from double the P1 number. If so, other factors could be attributing to nutrient lock or availability such as pH or soil texture. As an inhouse tool, this would alert the tester to possibly run the test again.

  • @franjaurro
    @franjaurro 7 ปีที่แล้ว

    Can i ask you something, I am from Chile and here in the south we have organic soils with very high organic matter 15% o more, they are soil of volcanic origin and they dont have good Ph, its difficult to find a soil with Ph 6.0 the more tipical is 5.0 or a media of 5.5, the think is that there can be Aluminuim problems but with Calcium Carbonate you can fix that but the Ph of the soil doesnt change D: , you can put 4ton/Ha and the Ph doesnt change why is so difficult to raise the Ph.

    • @johnwild-st4ed
      @johnwild-st4ed 7 ปีที่แล้ว

      You can think of the soil as having two main pools of acidity, active acidity (H+ in solution) and exchangeable acidity (H+ adsorbed to soil particles). In acidic soils with a high CEC the size of the exchangeable H+ pool will be MUCH larger than what is actually in solution (active H+). Since these two pools are in equilibrium (or trying to be), active acidity is 'buffered' by exchangeable acidity. In order to effectively raise soil-pH, both pools have to be neutralized.
      The size of the exchangeable H+ pool can not be measured by a normal pH measurement (requires titration). This is why soil labs also report a buffer index for soil-pH. The pH measurement is basically just provides a yes/no answer to the question "Do I need to to add CaCO3?" If that answer is yes (soil-pH is too low), then the buffer index answers the question "How much CaCO3 needs to be added?"
      I'm not terribly familiar with volcanic soils, but with that much OM I imagine your soil's CEC is quite high. With volcanic parent material there is also (probably) quite a bit of aluminum, which would provide a natural source of acidity through hydrolysis. The combination of the two would give a soil with low pH and high CEC, which basically means its going to take a lot of lime to raise soil-pH.

    • @Nicolasdu5
      @Nicolasdu5 5 ปีที่แล้ว

      4tons/ha is not that much