Gp. Sparling et al., Topsoil characteristics of three contrasting New Zealand soils under four long-term land uses, NZ J AGR RE, 43(4), 2000, pp. 569-583
Marton (Argillic Perched-gley Pallic, Typic Endoaqualf), Ohakune (Typic Ort
hic Allophanic, Typic Hapludand), and Westmere (Mottled Mafic Melanic, Moll
ic Hapludalf) soils with differing structural vulnerability were compared a
t matched sites under different land uses. Topsoil samples (0-10 cm) from i
ndigenous forest (>50 yr), permanent pasture (>50 yr), pine plantation (>20
yr), or arable cropping (>13 yr) sites were characterised using a range of
17 chemical, physical, and biological properties. Land-use effects masked
overall differences in the physical and chemical properties of the soils, d
espite their differing mineralogy. However, the biological properties of re
spiration, microbial C, and mineralisable N were generally significantly lo
wer under arable cropping and pine plantations compared with pastures and i
ndigenous forest. Within each soil type, land use caused significant but va
rying effects on soil properties. There was considerable decline in the phy
sical condition of the Ohakune topsoil under arable cropping despite the ve
ry low vulnerability rating. The findings suggest that the degradative pres
sures caused by cropping for carrots on Ohakune soil were considerably grea
ter than those of cereal cropping on Marton and Westmere soils. Deteriorati
ng soil physical structure is likely to be the main limitation to continued
arable cropping on Marton and Ohakune soils.