Agriculture from the Ground Up
Sep 22, 2026 · 28 min · 11 segments
Send us Fan Mail Last episode we unpacked what pH actually is. This one asks the better question: why is *your* number the number it is? Drive east…
Leonie SmithHost
Now, the question I think is the most interesting one, and the one nobody seems to ask: Why is your pH the number it is? Now, there are four drivers, and only one of them is out of your hands.

If the parent material contains carbonate, the soil starts life with a built-in supply of the very thing we're spreading out on our paddocks.

The limestone under much of the Swan Coastal Plain was originally calcareous sand blown in from the continental shelf during times of low sea level, and it's mainly shells and coral.

And soil sitting in close contact with that limestone carries a large calcium component in the exchange complex, the negatively charged surfaces on clay and organic matter that hold onto nutrients and give a neutral reaction.

So some country is alkaline because of what it's made of, and no amount of management made it that way.

Here is the driver I think explains more of Australia than any other, and it's really beautifully simple.

Acid soils are found in areas of high precipitation because the exchangeable cations, mainly calcium, magnesium, potassium, and sodium, get leached out of the soil, and acid-forming factors produce an increase in absorbed hydrogen and aluminum.

In dry climates, calcium, magnesium, potassium, and sodium occupy a greater percentage of the exchange sites, and soils are neutral to alkaline.

This is why you can drive across the state and watch the pH climb as that rainfall drops.

So an old landscape that has been rained on for a very long time has more of its cations removed than a young one.

That is why some of our most leached profiles are also our most acidic and our poorest.

In the southwestern agricultural region, the key drivers of acidification are the leaching of nitrogen and the export of alkalinity in produce.

Now, the question I think is the most interesting one, and the one nobody seems to ask: Why is your pH the number it is? Now, there are four drivers, and only one of them is out of your hands.

If the parent material contains carbonate, the soil starts life with a built-in supply of the very thing we're spreading out on our paddocks.

The limestone under much of the Swan Coastal Plain was originally calcareous sand blown in from the continental shelf during times of low sea level, and it's mainly shells and coral.

And soil sitting in close contact with that limestone carries a large calcium component in the exchange complex, the negatively charged surfaces on clay and organic matter that hold onto nutrients and give a neutral reaction.

So some country is alkaline because of what it's made of, and no amount of management made it that way.

Here is the driver I think explains more of Australia than any other, and it's really beautifully simple.

Acid soils are found in areas of high precipitation because the exchangeable cations, mainly calcium, magnesium, potassium, and sodium, get leached out of the soil, and acid-forming factors produce an increase in absorbed hydrogen and aluminum.

In dry climates, calcium, magnesium, potassium, and sodium occupy a greater percentage of the exchange sites, and soils are neutral to alkaline.

This is why you can drive across the state and watch the pH climb as that rainfall drops.

So an old landscape that has been rained on for a very long time has more of its cations removed than a young one.

That is why some of our most leached profiles are also our most acidic and our poorest.

In the southwestern agricultural region, the key drivers of acidification are the leaching of nitrogen and the export of alkalinity in produce.
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