Reference soils of south-western Australia

By W. M. Mcarthur. 2004

336 citations recorded by the source corpus.

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Citations in the corpus

Variation in morphological and physiological parameters in herbaceous perennial legumes in response to phosphorus supply (2010, unknown): “In Western Australia, natural surface soils may contain less than 5 mg kg−1 of bicarbonate-extractable P (McArthur 1991).”
Plant mineral nutrition in ancient landscapes: high plant species diversity on infertile soils is linked to functional diversity for nutritional strategies (2010, background): “The ancient soils of Western Australia have had a major impact on historical patterns of settlement as local variations in soil quality, especially fertility, determined where agriculture could succeed before the large-scale application of fertilisers was feasible (McArthur 1991).”
Phosphorus uptake by grain legumes and subsequently grown wheat at different levels of residual phosphorus fertiliser (2005, background): “The different crop species showed a small growth response to residual soil P levels, presumably because the soils contained a base level of P that was well above that of most Western Australian soils (McArthur 1991).”
Provenance variation of ecologically important traits of forest trees: implications for restoration (2007, background): “Soils within the Darling Range are predominantly lateritic gravels overlying sandy clay subsoils (Churchward & McArthur 1980; McArthur 1991) but on the coastal plains to the west and south of this region E.”
Experimental assessment of nutrient limitation along a 2‐million‐year dune chronosequence in the south‐western Australia biodiversity hotspot (2012, background): “…were used for the +N and +P treatments, because we judged that Ca limitation was highly unlikely given the nature of the parent material (carbonate dunes) for most stages and the relatively high concentrations of Ca found in all soils, compared to that of other cations (McArthur 2004; see also Fig.”