1994
DOI: 10.1071/sr9940213
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Surface soil-pH map of Queensland

Abstract: Surface soil pH can influence biological activity, nutrition and various chemical processes in the soil. Low pH or acidity is causing major concern in southern Australia, prompting requests for details on the extent, severity and distribution of acidic soils in Queensland. By creating a soil pH database, using an appropriate base map, rainfall isohyets and GIS technology, a coloured pH map of surface soils was produced at a 1:5000000 scale for the entire State. As most samples were from virgin or little distur… Show more

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Cited by 7 publications
(5 citation statements)
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“…Within ES 1, rhizosphere adaptations may be a key trait to cope with the annual extremes of cyclically waterlogged and parched tropical monsoon soils (Bui et al , ). Soil pH tends to decrease with rainfall: tropical monsoon soils tend to be acidic, whereas those to the south are often more alkaline (Ahren et al , ; Henderson et al , ). The concentration of tropical monsoon species into a few diverse clades (Fig.…”
Section: Discussionmentioning
confidence: 99%
“…Within ES 1, rhizosphere adaptations may be a key trait to cope with the annual extremes of cyclically waterlogged and parched tropical monsoon soils (Bui et al , ). Soil pH tends to decrease with rainfall: tropical monsoon soils tend to be acidic, whereas those to the south are often more alkaline (Ahren et al , ; Henderson et al , ). The concentration of tropical monsoon species into a few diverse clades (Fig.…”
Section: Discussionmentioning
confidence: 99%
“…6. Compared to a map generated by linking a chloropleth map to a soil database such as the one presented in Ahern et al (1994) for surface pH in Queensland, the ASRIS map clearly represents much more local variability. The digital maps for all soil property predictions are available at http://audit.ea.…”
Section: Example: Ph In Layermentioning
confidence: 98%
“…The soil pH at the two experimental sites was 5.20 in Kakamega and 6.08 in Busia and, therefore, officially characterized as acidic (less than 6.5) [35]. The exchangeable amounts of Al, Mn, and Cu were 1.72 Cmol/kg, 63.1 ppm, and 2.3 ppm in Kakamega and 0.95 Cmol/kg, 35.1 ppm, and 1.60 ppm in Busia soils, respectively.…”
Section: Analysis Of Soil Sample From Western Kenyamentioning
confidence: 99%