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Influence of soil properties on the aggregate stability of cultivated sandy clay loams

Citation

Almajmaie, A and Hardie, M and Doyle, R and Birch, C and Acuna, T, Influence of soil properties on the aggregate stability of cultivated sandy clay loams, Journal of Soils and Sediments, 17, (3) pp. 800-809. ISSN 1439-0108 (2017) [Refereed Article]

Copyright Statement

Copyright 2016 Springer-Verlag Berlin Heidelberg

DOI: doi:10.1007/s11368-016-1568-1

Abstract

Purpose: Frequent cultivation and overhead irrigation have led to severe surface crusting, erosion and poor irrigation performance on sandy clay loam soils in the Coal River Valley, Tasmania, Australia. This study was established to identify the key soil properties related to aggregate breakdown determined by different methods, and explore options for reducing soil crusting.

Materials and methods: Soil aggregates were collected from 0 to 5 cm depth from 20 sites managed for packet salad and lettuce production. The stability of air-dried 2.00–4.75 mm aggregates was determined by rainfall simulation, wet sieving and clay dispersion. Soil aggregates were analysed for particle size, mineralogy, soluble and exchangeable cations, pH, EC, labile carbon and total carbon. The association between aggregate stability and the measured soil properties was explored using Spearman correlation, linear regression and regression tree analysis.

Result and discussion: Aggregate stability determined by rainfall simulation was closely associated with soil properties that promote aggregation, including effective cation exchangeable capacity (ECEC) and the proportion of polyvalent cations (Ca2+, Al3+). In contrast, aggregate stability determined by wet sieving was associated with soil properties that promote disaggregation, including quartz and sand content, and to lesser extent, the proportion of monovalent cations (especially K+). Clay dispersion was closely associated with pH, quartz content, soil texture and the sodium adsorption ratio. Soil carbon appeared to have only moderate influence on aggregate stability, but not clay dispersion, while labile carbon was not significantly related to any measure of aggregate stability or clay dispersion. Similarly, the proportion of Na+ ions was not related to either measure of aggregate stability and was only moderately related to clay dispersion.

Conclusions: Options for improving aggregate stability appear limited as aggregate stability was strongly related to the content of inherent soil properties such as sand/quartz and smectite contents. However, high correlation between exchangeable Ca2+ and aggregate stability determined by rainfall simulation indicates that soil crusting may be reduced through application of products that rich in Ca2+ such as gypsum.

Item Details

Item Type:Refereed Article
Keywords:aggregate stability, crusting, soil hydrology, sodicity
Research Division:Environmental Sciences
Research Group:Soil Sciences
Research Field:Land Capability and Soil Degradation
Objective Division:Environment
Objective Group:Land and Water Management
Objective Field:Farmland, Arable Cropland and Permanent Cropland Land Management
Author:Almajmaie, A (Mr Abbas Almajmaie)
Author:Hardie, M (Mr Marcus Hardie)
Author:Doyle, R (Dr Richard Doyle)
Author:Acuna, T (Associate Professor Tina Acuna)
ID Code:112272
Year Published:2017 (online first 2016)
Deposited By:Tasmanian Institute of Agriculture
Deposited On:2016-11-01
Last Modified:2017-11-13
Downloads:0

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