Preface
The history of the New Zealand Soil Classification
The fourth edition of the Zealand Soil Classification is the culmination of a long period of development from its initiation in 1983. Preliminary draft versions 1.0 and 2.0 (Hewitt 1987; Hewitt 1989) were widely circulated for comment and testing, before the revised version 3.0 was formally published as the first edition in 1992 (Hewitt 1992a). Two further editions followed, in 1998 (Hewitt 1998a) and 2010 (Hewitt 2010). The latest (fourth) edition represents the best attempt, given the current state of knowledge, to classify New Zealand soils. As the knowledge and understanding of New Zealand soils grows, further revisions will be necessary.
The New Zealand Soil Classification is a national, hierarchical soil classification, which replaced the New Zealand Genetic Soil Classification (Soil Bureau Staff 1948; Taylor and Cox 1957; Taylor and Pohlen 1962; Taylor and Pohlen 1968; Taylor and Pohlen 1979)1. This earlier work grew out of the need for reconnaissance mapping of the nation’s soil resources. It was successful as a unifying factor in New Zealand soil science, and it played an essential role in the development of pastoral agriculture. However, modern soil surveys and land evaluations require precise definition of classes and keys for their recognition, and a new synthesis was needed of the large body of information collected since the 1950s (Hewitt 1992b).
The first edition of the New Zealand Soil Classification was developed from the New Zealand Genetic Soil Classification and preserved various parts of it. Since then, it has further evolved through experience gained using the earlier editions and the accumulation of new knowledge. It has also been influenced by experience testing the first edition of the Soil Taxonomy (Leamy et al. 1983; Leamy et al. 1990; Hewitt 1992b), and the development of subsequent versions of the Soil Taxonomy, including the most recent edition and keys (Soil Survey Staff 1999; Soil Survey Staff 2022).
With the fourth edition we also introduce an extended appendix, which now includes an additional soil order (the Cryic Soils) and associated diagnostic criteria. This is to accommodate the soils of the Ross Sea Region of Antarctica, a focal point of Antarctic soil research, incorporating leading contributions from New Zealand soil scientists. It addresses the anomaly of New Zealand workers having to use international classifications when working in Antarctica. If, in the future, more empirical evidence emerges that taxa of the Cryic Soil Order might also be applicable to New Zealand soil environments (e.g., alpine environments of the Southern Alps), it can be moved to the top of the main soil order key.
Terminology and further reading
Many technical terms are used throughout this handbook in the keys and definitions. The most relevant technical terms are printed with an underline and defined in section 2, Diagnostic horizons and other differentiae. Further details and other technical terms are defined or can be found in the resources noted below.
- The horizon notations are consistent with Clayden and Hewitt (2015), recently updated in O’Brien et al. (2026).
- Soil morphology terms are defined by O’Brien et al. (2026).
- Classes of the Soil Taxonomy are defined by Soil Survey Staff (1999) and Soil Survey Staff (2022).
- Soil colours are defined by Pantone (2017); see also Bigham and Ciolkosz (1993) for application of colour in soil science.
- Control sections are designated parts of the soil profile/pedon (depth, depth range, or thickness) in which specified diagnostic features occur to enable a soil to be categorised at each level in the classification. For example, a certain feature must occur “within 30 cm of the mineral surface” or a specific soil will have “a layer or layers of allophanic soil material that total 35 cm or more thick … within 60 cm of the mineral soil surface.”
- A lithological discontinuity is a stratigraphic break in a soil profile/pedon that is the result of a geological (not pedological) process or event. The deposition of new geological material, such as a tephra layer or an alluvial or colluvial deposit, forms a new parent material/lithology at the land surface, burying the antecedent soil. The stratigraphic break is normally marked by textural, mineralogical, and other compositional differences between the earlier and later lithologies (Palmer et al. 2025).
- Soil mineralogy terms are explained, and the methods of clay mineral analysis described, by Churchman (1986) and Whitton and Churchman (1987). Updated overviews of soil mineralogy are provided by Churchman and Lowe (2012) and Churchman and Velde (2019).
- Soil mineralogy classes originally proposed by Whitton and Childs (1989) and Childs and Whitton (1990) are now also defined in the Soil Taxonomy Soil Survey Staff (2022). Note that the soil mineralogy class names given here are based on the control section 25 cm to 100 cm, or to a lithic or paralithic contact if shallower.
- Soil chemical terms are explained, and the analytical methods described, by Blakemore et al. (1987). Note that soil pH measurements are made in water, with a ratio of 1 part of soil to 2.5 parts of water, by weight.
- Soil physical terms are explained, and the analytical methods described, by Gradwell and Birrell (1979), McQueen (1993), and Gray and Allbrook (2002). Allbrook (1983) and Allbrook (1985) focuses on the physical properties of allophanic soil materials.
- A summary of the New Zealand Soil Classification is available in Hewitt (1998b). The fourth and fifth levels of the classification are documented by Webb and Lilburne (2011).
- A companion document, the Methods and Rationale of the New Zealand Soil Classification (Hewitt 1993), discusses the intentions behind key decisions made in the classification.
- A comprehensive overview of the diversity of soils and their properties, origins, and associated landscapes in New Zealand, on an order-by-order basis, is given by Hewitt et al. (2021).
- Many other soil science concepts and technical terms are explained, in a New Zealand context, by McLaren and Cameron (1990).
Note that Soil Bureau Bulletin 3, ‘A genetic classification of New Zealand soils’, was never published, except for the ‘Soil map of New Zealand’ in 1948. To reference the New Zealand Genetic Soil Classification, we cite a range of readily accessible drafts, editions and summaries representing its evolution.↩︎