1987
DOI: 10.33584/jnzg.1987.48.1801
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Soil Resources of Central Otago

Abstract: The broad soil pattern of Central Otago is outlined. Four soil zones are identified and their climate, vegetation and landscape characteristics given. The paper reviews causes of variation in soil properties at the detailed, farm scale. The highly variable soil pattern on many farms is caused by the wide variations in climate and topography which often occur within short distances in Central Otago. Farmers need to understand the soil pattern on their property to enable them to use soil resources effici… Show more

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Cited by 6 publications
(4 citation statements)
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“…As such it provides a hostile environment for farming with dry summers and long cold winters (120 days with little or no growth). The geology of the region includes broad intermontane basins between block uplift mountains (Brash & Beecroft 1987). The mountain regions have higher rainfall, increasing with altitude, but shorter growing seasons, restricted by temperature and snowfall.…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…As such it provides a hostile environment for farming with dry summers and long cold winters (120 days with little or no growth). The geology of the region includes broad intermontane basins between block uplift mountains (Brash & Beecroft 1987). The mountain regions have higher rainfall, increasing with altitude, but shorter growing seasons, restricted by temperature and snowfall.…”
Section: Introductionmentioning
confidence: 99%
“…lucerne is used in these systems in several ways. Basal soils of the valley floor have a natural pH of 6-7 (Brash & Beecroft 1987). Often lucerne is used on soils with low soil moisture holding capacity to maximise the production of these areas of the farm.…”
Section: Introductionmentioning
confidence: 99%
“…An experiment to test the agronomic value of subterranean clover was established in February 2016 on the infertile 'Red Flats' of Omarama Station in the Mackenzie Basin, New Zealand (GPS coordinates are -44.503479, 169.902127, 477 m a.s.l.). The flats were formed from alluvial schist and greywacke gravel deposits (Brash & Beecroft 1987). The resulting Mackenzie soils (Pallic Orthic Brown) are shallow (depth 20-45 cm) and well drained which results in low plant available water (30 -60 mm in the top 1 m) (S-MAP 2017).…”
Section: Methodology and Analysismentioning
confidence: 99%
“…These soils are frequently associated with short tussock/scrubland vegetation cover and are, on average, below FC for more than five months and below PWP for 1 to 5 months i.e. are sub-hygrous (Brash & Beecroft 1987).…”
Section: Soilsmentioning
confidence: 99%