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Volume 55 No 2 April 2007 - New Zealand Society of Soil Science

Volume 55 No 2 April 2007 - New Zealand Society of Soil Science

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McCraw moved to Alexandra to initially begin soil surveys <strong>of</strong> existing and potential fruit growing<br />

areas <strong>of</strong> Central Otago from Cromwell to Roxburgh. These were to be followed by irrigation surveys.<br />

The Alexandra <strong>of</strong>fice grew with the addition successively <strong>of</strong> Cowie, Ward, Leamy and lastly Gary<br />

Orbell. By the early 1960s these pedologists had mapped the soils <strong>of</strong> the Alexandra District, and the<br />

Ida, Upper Clutha and mid Manuherikia valleys. These were areas where irrigation was the key to<br />

pastoral and horticultural development <strong>of</strong> the dry basin floors.<br />

Cowie was briefly in Foxton before establishing the soil survey <strong>of</strong>fice in Palmerston <strong>No</strong>rth with<br />

Fitzgerald as his assistant. Together they surveyed the Manawatu sand country, recognizing a<br />

topographically consistent soil pattern, referred to as soil associations. The soils on dunes and sand<br />

plains differentiated the progradational Manawatu sand plain into successively older, but overlapping<br />

Holocene dunes systems. In a career, the bulk <strong>of</strong> which was spent in the Manawatu, Cowie built-up a<br />

comprehensive knowledge <strong>of</strong> the soils and their varied uses for horticulture and agriculture. Like<br />

Pullar in Gisborne, he was able to use his knowledge <strong>of</strong> the soils to interpret the evolution <strong>of</strong> the<br />

Rangitikei and Manawatu floodplains and <strong>of</strong> the many smaller rivers between. The presence <strong>of</strong> a<br />

widespread tephra layer interbedded with silty coverbeds on the Manawatu downlands was the key to<br />

recognizing loess, for the first time in the <strong>No</strong>rth Island. In the late 1950s Cowie, Brian Kear and Orbell<br />

mapped the soils <strong>of</strong> Kairanga Count an area <strong>of</strong> the Manawatu downlands comprising small<br />

floodplains, and terraces and floodplains <strong>of</strong> the major rivers, bordering the eastern side <strong>of</strong> the main<br />

ranges. This survey further developed the idea <strong>of</strong> soil association mapping, producing cross-sectional<br />

diagrams <strong>of</strong> landscape segments that depicted the relationship between the soil pattern, the landforms<br />

and the underlying sediments. In the 1950s Wright moved to the Taita Research Station to establish<br />

the soil biology section <strong>of</strong> DSIR <strong>Soil</strong> Bureau.<br />

A new headquarters for DSIR <strong>Soil</strong> Bureau<br />

Up until the end <strong>of</strong> the 1950s the DSIR <strong>Soil</strong> Bureau had been housed in less than adequate conditions<br />

in a number <strong>of</strong> buildings in Wellington including the infamous 54 Molesworth Street opposite the<br />

Parliament buildings. In 1949 Dr Grange had negotiated the acquisition <strong>of</strong> land at Taita on the eastern<br />

side <strong>of</strong> the Hutt Valley and by 1962 the new buildings were ready for occupation. This was the first<br />

time DSIR <strong>Soil</strong> Bureau staff, with the exception <strong>of</strong> the field <strong>of</strong>fices, had been located on one site. By<br />

the late 1950s the soil survey <strong>of</strong>fices in the South Island were at Christchurch, Dunedin and<br />

Alexandra, and those in the <strong>No</strong>rth Island at Whangarei, Rotorua, Palmerston <strong>No</strong>rth, and Gisborne,<br />

with Gibbs the Chief Pedologist based in Wellington.<br />

In 1962 Taylor and Pohlen published <strong>Soil</strong> Survey Method, at this time one <strong>of</strong> the most comprehensive<br />

manuals available for soil surveyors, and the first formally published in <strong>New</strong> <strong>Zealand</strong>. It set standards<br />

for soil description and mapping, and included the first published version <strong>of</strong> the <strong>New</strong> <strong>Zealand</strong> Genetic<br />

<strong>Soil</strong> Classification with the common and a novel technical nomenclature. It was republished in 1968 as<br />

part <strong>of</strong> the <strong>Soil</strong>s <strong>of</strong> <strong>New</strong> <strong>Zealand</strong> volumes. The technical nomenclature was used for a time and<br />

subsequently abandoned.<br />

Taylor had invited the International <strong>Society</strong> <strong>of</strong> <strong>Soil</strong> <strong>Science</strong> to hold their 8th Congress in <strong>New</strong><br />

<strong>Zealand</strong>, but this was not acceptable to the Europeans, so he settled for an inter-congress meeting <strong>of</strong><br />

Commissions IV (<strong>Soil</strong> Fertility) and V (Pedology). In the years prior to this meeting, field and<br />

laboratory staff made a <strong>New</strong> <strong>Zealand</strong>-wide collection <strong>of</strong> reference soils with descriptions, to which<br />

were added chemical, physical and mineralogical analyses. The conference was held at Massey<br />

University in 1962 and included field tours throughout both islands. The conference and tours were a<br />

success, and illustrated the integration between soil survey and soil fertility, and the application <strong>of</strong> this<br />

knowledge to agricultural, horticultural and forestry land-uses in <strong>New</strong> <strong>Zealand</strong>. It was an appropriate<br />

culmination <strong>of</strong> Taylor’s career, as a soil surveyor and latterly as Director <strong>of</strong> DSIR <strong>Soil</strong> Bureau, from<br />

which he retired at the end <strong>of</strong> 1962.<br />

By this time Gibbs, Raeside, and Cutler were devoting more time to questions <strong>of</strong> land-use,<br />

highlighting the limited areas <strong>of</strong> <strong>New</strong> <strong>Zealand</strong> soils with high versatility, producing classifications for<br />

pastoral and cropping uses, and arguing for a limitation to urban spread on to the high value soils that<br />

surrounded most <strong>of</strong> the <strong>New</strong> <strong>Zealand</strong>’s towns and cities. This case was well illustrated by later soil<br />

67

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