New Zealand soils in a nutshell
Soil diversity and how to tackle it
A quick summary of the nature and properties of soils appearing in the New Zealand landscape of today.
One of the key characteristics of soils in the landscape is their diversity. The nature and properties of New Zealand soils change in space and over time. Sometimes it can be surprising to see the differences in soils that are only a few metres apart! In our section on 'How do soils form?' you can read about the various soil forming factors that are behind these differences. What can we do to get on top of this amazing variety of soil types?
First of all it is important to realise that – unlike plants and animals – soils form a continuum, meaning that soil changes in the landscape are gradual. And whereas you can easily identify a southern brown kiwi or a red beech tree, soils are not nearly as clearly distinguishable. Instead we use observable and measurable soil properties to distinguish the various soils and group them into different classes.
The New Zealand Soil Classification (NZSC) is our current system to name and classify soils across the country. It helps us to conceptualise what we find, and to communicate about a particular soil and its properties. At its highest levels the NZSC has 15 so-called ‘soil orders’. These are groups of soils, each with a similar appearance, formation, or behaviour.
Soils develop over time
Most soils – especially those in the South Island – are rather ‘young’ in geological terms and have formed since the end of the last Ice Age, approximately 14,000 years ago. Where soil formation can continue for a longer time (as in in warmer climates on stable land surfaces), deeper and more strongly weathered soil orders – such as Ultic or Granular Soils – will form.
Explore the distribution of soils in New Zealand in our SoilsMapViewer tool
Maps come from three main sources – the Fundamental Soil Layers, which contain spatial information for 16 key soil attributes; the New Zealand Soil Classification, which represents the best attempt to classify New Zealand soils; and the Ross Sea Regions database, which contains historic and recent soil site and soil pit horizon data from Antarctica.
These pages attempt to provide background information about the different naming systems that have been used over the years, and, where possible, indicate how they relate to each other.