Agriculture from the Ground Up
Jul 24, 2026 · 23 min · 10 segments
Send us Fan Mail In this episode of *Agriculture From The Ground Up*, we connect the dots between parent material and the soil profiles you dig into…
Leonie SmithHost
But before we look at soil profiles themselves, I want to remind you of the framework that we've discussed a couple of episodes ago that explains how those profiles form.

Soil scientists use that system called CLORP, which stands for Climate, Living Organisms, Relief, Paramaterial and Time plus us humans.

It controls how fast the rocks weather, how much water moves through the profile, and how organisms interact with the soil.

In WA, our Mediterranean climate, which means those cool wet winters and those hot dry summers, drives significant winter leaching on those sandy soils that we know so well.

But many of our deeply weathered soils actually formed millions of years ago under much warmer, wetter, tropical conditions.

When plants die, they add organic matter and the microbes break it down and cycle those nutrients.

Then we have our earthworms and other fauna mix in the soil and improve that structure.

On steep slopes, water runs off quickly, causing more erosion and thinning soils.

In our valleys, water slows down and collects, allowing sediments and organic matter and nutrients to build up and create those deeper, more fertile soils.

Parent material is the starting ingredient, which is exactly what we've covered in those recent episodes.

Soil formation is incredibly slow, taking hundreds to thousands of years to form just a few centimetres of good topsoil.

Here in WA, our ancient landscapes have had millions of years for weathering, which is exactly why our soils are so deeply weathered and loan those nutrients.

Everything we do on our land, including cropping and clearing, grazing, liming, ripping, spreading clay, all of it shapes the soil just as powerfully as climate or parent material.

But before we look at soil profiles themselves, I want to remind you of the framework that we've discussed a couple of episodes ago that explains how those profiles form.

Soil scientists use that system called CLORP, which stands for Climate, Living Organisms, Relief, Paramaterial and Time plus us humans.

It controls how fast the rocks weather, how much water moves through the profile, and how organisms interact with the soil.

In WA, our Mediterranean climate, which means those cool wet winters and those hot dry summers, drives significant winter leaching on those sandy soils that we know so well.

But many of our deeply weathered soils actually formed millions of years ago under much warmer, wetter, tropical conditions.

When plants die, they add organic matter and the microbes break it down and cycle those nutrients.

Then we have our earthworms and other fauna mix in the soil and improve that structure.

On steep slopes, water runs off quickly, causing more erosion and thinning soils.

In our valleys, water slows down and collects, allowing sediments and organic matter and nutrients to build up and create those deeper, more fertile soils.

Parent material is the starting ingredient, which is exactly what we've covered in those recent episodes.

Soil formation is incredibly slow, taking hundreds to thousands of years to form just a few centimetres of good topsoil.

Here in WA, our ancient landscapes have had millions of years for weathering, which is exactly why our soils are so deeply weathered and loan those nutrients.

Everything we do on our land, including cropping and clearing, grazing, liming, ripping, spreading clay, all of it shapes the soil just as powerfully as climate or parent material.
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