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  • Most people are familiar with the Linnean classification system used to identify living things. We use scientific names to describe and categorise living things precisely. For example, New Zealand has several subspecies of robins. By using the scientific name Petroica australis longipes, we know that this bird is the North Island robin or toutouwai in Māori.

    Rights: Waikato Regional Council

    New Zealand soils map

    Soil classification begins with a soil order. Soil orders are further divided into groups, subgroups and families. This map displays New Zealand’s soil orders.

    New Zealand soils also have special naming systems. The various soils have a scientific name, a common name and, in some cases, a Māori name.

    New Zealand Soil Classification System

    Soil scientists use the New Zealand Soil Classification System to identify specific soils. Soils are classified according to their physical, chemical and morphological characteristics (which refer to the soils’ appearance). Like the Linnean system for living things, soil classification also has a hierarchy. This level of detail allows for accurate communication among scientists.

    Rights: The University of Waikato Te Whare Wānanga o Waikato

    New Zealand Soil Classification System

    Soil scientists use the New Zealand Soil Classification System to identity soil names. Soils are classified according to their physical, chemical and morphological characteristics.

    All soil classification begins with a soil order. Soil orders are subdivided into soil groups, and these groups are divided even further into subgroups. For example, one soil order is Gley. Gley soils drain quite slowly after rain and are strongly affected by waterlogging. They occur throughout New Zealand in low-lying parts of the landscape. The Gley soil order has six soil groups – one of which is Orthic Gley. The Orthic Gley group has eight subgroups. This level of detail is often important to landowners to help them manage their land for optimal production.

    The New Zealand Soil Classification System has a fourth category – soil family – which uses parent material, particle size and permeability to further identify and classify the soil.

    Common New Zealand soil names

    New Zealand soils also have common names. The name usually has the location in which the soil was first discovered and describes the soil’s texture – Pakipaki silt loam, Taupō sand and Waikare clay are just a few examples. Scientists and farmers often use the common soil names because they are meaningful to a particular location. A dark greyish-brown silt loam found in the Waikato has the scientific classification Typic Orthic Gley, but locals are more likely to refer to its common name – Te Kōwhai silt loam.

    Māori soil names

    The Māori word for soil is oneone. Before Europeans arrived in New Zealand, Māori had already identified at least 30 types of soil.

    Rights: Waikato Regional Council http://www.nzsoils.org.nz

    Kenepuru Sound

    Some Māori place names relate to the soil in a particular area. One meaning of kenepuru is silt. In the foreground of this photo, silt can be seen extending out from shore.

    There are general soil names such as keretū (clay), parakiwai (silt), kenepuru (silt), onetai (sandy soil), oneparaumu (very dark fertile soil) and onenui (a rich soil made of clay, sand and decayed organic matter). Māori also classified soils by more specific characteristics. Keretū (clay) is broken up into several categories: kerewhenua (yellow clay), kerematua (stiff clay), kōtore (white clay), taioma (pipe clay), matapaia (baked hard and used as a stone for cooking) and uku (soft white or bluish clay).

    Just as the current common soil names are associated with a particular location, Māori place names may indicate the local soil type. For example, Kereone (in the Waikato) has sandy silt, and Onetea (in the Far North) has a light sandy soil.

    Nature of science

    Throughout history, humans have developed detailed knowledge of how soils differ from one another and used their local languages to name or describe these soils. These names and descriptions are meaningful on a local level, but scientific classification allows scientists to discuss soil characteristics on a global basis.

    Related content

    Explore Soil formation – climate, living organisms and topography influence how rocks (parent materials) are turned into soils over long periods of time.

    Discover more about Soil properties – all soils contain mineral particles, organic matter, water and air. The combinations of these determine the soil’s properties – its texture, structure, porosity, chemistry and colour.

    Activity idea

    Observing soil differences uses soil samples from students’ homes – and online resources – to view how soils differ from location to location.

    Useful links

    View soil maps and related information about New Zealand soils from Manaaki Whenua – Landcare Research.

    Visit Te Ara to read about New Zealand soil orders.

    Visit Te Ara to see Māori names for soil.

      Published 30 July 2013 Referencing Hub articles
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