2006
DOI: 10.1016/j.geoderma.2005.10.004
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The effect of kauri (Agathis australis) on grain size distribution and clay mineralogy of andesitic soils in the Waitakere Ranges, New Zealand

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Cited by 14 publications
(6 citation statements)
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“…This study was undertaken within the Waitakere Ranges, located in northern New Zealand. The Waitakere Ranges encompasses 17,000 ha, ranging from sea level to 474 m, with mean annual temperature from 12.5 to 14.5 °C and mean annual precipitation between 1,400 and 2,000 mm ( Jongkind & Buurman, 2006 ). The vegetation is comprised of a podocarp-broadleaf mixture, with aggregated stands of the endemic conifer, Kauri ( Agathis australis ).…”
Section: Methodsmentioning
confidence: 99%
“…This study was undertaken within the Waitakere Ranges, located in northern New Zealand. The Waitakere Ranges encompasses 17,000 ha, ranging from sea level to 474 m, with mean annual temperature from 12.5 to 14.5 °C and mean annual precipitation between 1,400 and 2,000 mm ( Jongkind & Buurman, 2006 ). The vegetation is comprised of a podocarp-broadleaf mixture, with aggregated stands of the endemic conifer, Kauri ( Agathis australis ).…”
Section: Methodsmentioning
confidence: 99%
“…This study was undertaken within the Waitakere Ranges, located in northern New Zealand. The Waitakere Ranges encompasses 17,000 hectares, ranging from sea level to 474 m, with mean annual temperature from 12.5 to 14.5°C and mean annual precipitation between 1400 to 2000 mm (Jongkind & Buurman 2006). The vegetation is comprised of a podocarp-broadleaf mixture, with aggregated stands of the endemic conifer, Kauri (Agathis australis).…”
Section: Materials and Methods Study Sitesmentioning
confidence: 99%
“…In a later study, Pai et al (2007) found that acidification at the surface of forest soil elsewhere in Taiwan decreased the charge of the K-depleted aluminosilicate layers, which they characterized as vermiculite, occurring either as the discrete phase or in mixed-layers with vermiculite. In the North Island of New Zealand, Jongkind and Buurman (2006) found that weathering under kauri (Agathis australis) trees, which produce especially low pHs (4.0 ± 0.2), left vermiculites depleted of hydroxyl interlayering and even brought about some conversion of vermiculite to smectite, as Churchman (1980) had found to occur in soils under another native beech tree species (Nothofagus sp.) in the South Island of New Zealand.…”
Section: Plants As Weathering Agentsmentioning
confidence: 99%
“…There is a general trend from halloysite at depth towards kaolinite at the surface of profiles on residual rock materials (e.g., Eswaran and Wong, 1978;Calvert et al, 1980;Churchman and Gilkes, 1989;Churchman, 1990;Takahashi et al, 2001;Singer et al, 2004;Jongkind and Buurman, 2006). These studies together have covered a range of parent rock types and also climates, including tropical (Eswaran and Wong, 1978, and part of Churchman, 1990), temperate (Calvert et al, 1980;part of Churchman, 1990;Jongkind and Buurman, 2006), and Mediterranean, or xeric (Churchman and Gilkes, 1989;Takahashi et al, 2001;Singer et al, 2004). According to Papoulis et al (2004), these trends with depth were explained in the context of their morphological and compositional development sequence of halloysite and kaolinites.…”
Section: Occurrence Of Halloysite In Soilsmentioning
confidence: 99%