About Soil Names
The names people use for soils, will always reflect the needs of the day, and
the understanding people have for the part soil plays in underpinning many of our activities.
Sometimes the naming systems we use become more complex and sometimes, through a
breakthrough in understanding, they become simpler. So the names in use by scientists
change and evolve with time and purpose and sometimes they get out-of-step with everyday usage.
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.
Use the menu at the left to explore soem of the different types of soil name.
Soil names in New Zealand
Mäori: Pre-European Soil Classification
Soil classification in New Zealand was begun by Mäori horticulturalists who
recognised and named classes that were relevant to the establishment and
management of their gardens, in particular, kumara gardens. They recognised
classes such as oneharuru (a light but good sandy loam) and onetea (white soil
from sandy volcanic material). The need for soil classification has been part
of human activity in New Zealand since the arrival of the first Polynesian
Genetic: The First National Soil Nomenclature
Soil classification on a comprehensive national scale was not developed in New Zealand
until 1948. The pioneer New Zealand soil scientist, Norman Taylor, developed the New
Zealand Genetic Classification which recognised "soil groups" and
related them to the environmental factors that most influenced their character
(Taylor 1948; Taylor and Pohlen 1962,1968). Knowledge of these relationships
helped the prediction of soil classes from observations of geology, landscape,
climate and vegetation. Such predictions enabled rapid progress in the broad
scale exploratory mapping of New Zealand soils.
By the late 1970's, Taylor's New Zealand Genetic Soil Classification was
becoming outdated. Soil classes were vaguely defined so that only experts could
easily identify the correct class for many soils. The relationships between
soils and environment that were useful at a broad scale were less useful for
making soil maps at more detailed scales. Much new soil information was
becoming available that could not be explained within the framework of the old
system. A new synthesis was needed and the result was the New Zealand Soil
Regional Soil Names - Soil Series
Regional Soil Series names, sometimes known as common names are used to
distinguish similar soils at a finer level of classification than is possible
with either the Genetic and NZSC classifications. One of the problems with soil
series names is the use of different names for the identical soils in different
regions or even for adjacent soil survey areas. Because of their wide
everyday usage amongst farmers and farm advisors, Series names that were
evolved before the existance of NZSC are still used even though in some
instances they correspond to more than one NZSC category - care is therefore
needed when applying these names.
Regional Soil Names - Soil Sets
Once-upon-a-time there were also things called soil sets.
Soil sets were based on soil-landscape units and contained high soil variability.
They only survive in remote parts of the country that have only ever been
mapped using the 4-mile maps - but we try not to talk about them any longer.
Present Day National Soil Classification
The New Zealand Soil Classification was developed in the 1980s. The top three levels of the
classification (orders, groups, and subgroups) were described by Hewitt (1993, 2010-third edition) and the fourth
level (soilforms) by Clayden and Webb (1994). The new classification grew out of the New
Zealand Genetic Soil Classification and, where possible, preserved its useful features. The new
classification was also influenced by local experience in testing the United States soil classification
system "Soil Taxonomy" (Soil Survey Staff 1975, 1996; Leamy et al. 1983). The resulting
classification represents the best attempt to classify New Zealand soils, at our current state of
knowledge. As knowledge and understanding of soils grows, further revisions will be necessary.
Soil families in S-map
Soil families are objectively defined soil entities that consist of soils having the same Subgroup
classification (New Zealand Soil Classification, Hewitt 2010) and the same set of soil physical
characteristics comprising a) soil parent material class in the top 100 cm, b)the dominant texture
class in the top 60 cm and c) the slowest permeability class in the top 100 cm.
Soil families are given a geographic name but are also identified with a 4- or 5-character
abbreviated name. A geographic name, as used to name soil series, has been retained
because the users of soils are familiar with this usage and geographic names help in recalling
soil characteristics. The family name is suffixed with an italicised f (f) to distinguish the family
from the soil series.
International Soil Classification
New Zealand soil classification systems are related to those used
internationally, and for the purpose of global studies it is necessary to
relate NZ nomenclature to commonly used international practice.
US Soil Taxonomy
In 1975, Soil Taxonomy
was published by the United States Department of Agriculture's Soil Survey Staff. This
system for classifying soils has undergone numerous changes since that time,
and the 2nd edition was published in 1999. And the eleventh edition of the ‘Keys to
Soil Taxonomy’ was published in 2010. Correlation of the NZ new soil classification
with Soil Taxonomy is contained in Hewitt (2010).
World Reference Base for Soil Resources
The World Reference Base for
Soil Resources (WRB) is the international standard
taxonomic soil classification system endorsed by the International Union of Soil
Sciences (IUSS). It was developed by an international collaboration coordinated
by the International Soil Reference and Information Centre (ISRIC) and sponsored
by the IUSS and the FAO via its Land & Water Development division. It replaces
the previous FAO Soil Classification.