Wind erosion rates on terraces in the Mackenzie Basin

Publisher Website
Google Scholar
Abstract
The extent of soil erosion was estimated at six transects on terraces in the Mackenzie Basin using the 137Cs technique to quantitatively estimate erosion since 1953. Mean 137Cs areal activity over all sites was 351±9 Bq/m2, compared with an input value of 422±63 Bq/m2, and indicated a mean soil loss of 2.2 cm. 137Cs areal activities exceeded the input value at few sites; most of the sites that did exceed the input value were tussock pedestals or well vegetated areas. There was a good correlation between decreasing vegetation cover and decreasing mean 137Cs areal activity for Mackenzie soils, but not for Pukaki soils. However, there were strong contrasts in 137Cs levels between bare sites (268±17 Bq/m2) and vegetated sites (418± 15 Bq/m2) for Pukaki soils. Mean loss of 137Cs from bare ground was 36%, equivalent to a soil loss of 3.9 cm. By contrast, vegetated sites showed no soil loss. The mean 137Cs areal activity for all pedestals was slightly greater (457±25 Bq/m2) than the input value, while non‐pedestalled sites had a mean of 326±9 Bq/m2 (an average loss of 2.8 cm of soil). This suggested that vegetated areas, including pedestals, were stable or gaining soil, while bare deflated sites were losing soil. Topsoil depths tended to show similar trends to 137Cs areal activity, with thinner topsoils occurring where vegetation cover was poorer. Pedestals had topsoils that were on average 4 cm deeper than non‐pedestalled sites. The soil losses estimated using 137Cs, contrasts in topsoil depth between pedestals and non‐pedestalled sites, and the trend for topsoil depth to decrease as vegetation cover decreased suggest erosional losses of a large proportion of the A horizon. The contrasts in topsoil depth are greater than the erosional losses measured using 137Cs, suggesting considerable erosion before 1953.