Foreword
Many technical terms are used throughout this report in the keys and definitions. These technical terms, printed with an underline, are defined in this book in the section Diagnostic horizons and other differentiae.
Further details and other technical terms are defined or can be found in the resources noted below:
- Horizon notations are consistent with Clayden and Hewitt (1989), Clayden and Hewitt (2015), recently updated in O’Brien et al. (2025).
- Soil morphology terms are defined by O’Brien et al. (2025).
- Classes of 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, denoted as a 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, are described by are defined by Churchman (1986) and Whitton and Churchman (1987) with updated overviews of soil mineralogy 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 Soil Survey Staff (2022). Note that the soil mineralogy class names given here are based on the following 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 are 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 are described by Gradwell and Birrell (1979), McQueen (1993), and Gray and Allbrook (2002), with Allbrook (1983) and Allbrook (1985) specifically targeting the physical properties of allophanic soil materials.
- A summary of the New Zealand Soil Classification is available in Hewitt (1998). 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), informs about the intentions of various aspects of the classification.
- A comprehensive overview of the diversity of soils and their properties, origins and associated landscapes in Aotearoa 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).