Sodicity and gypsum responsiveness in south-western WA

Document Type

Conference Proceeding

Publication Date

11-2018

Conference Title

National Soil Science Conference

Place of Publication

Bridgewater

ISBN

978-0-646-99723-0 (epubl)

Abstract

Proceedings of the National Soil Science Conference, Canberra, ACT, 18 to 23 November 2018.

Soil Science Society of Australia Inc.

Soils with strongly sodic subsoils, defined as having an exchangeable sodium percentage (ESP) greater than 15 % cover almost 6 million of the WA wheat belt (van Gool pers. com). When exposed to rainfall, high levels of sodicity cause aggregates to disperse resulting in reduced water infiltration, drainage, aeration, crop emergence and root growth (Cochrane et al., 1994). The combination of impaired drainage and cyclical salt from rainfall has further resulted in the development of transient salinity (Barrett-Lennard et al., 2016). The management of sodic soils requires knowledge of how crops respond to sodicity, how sodicity and other soil properties effect dispersion and how to identify dispersive soils in order to tactically remediate them where gypsum or other amendments are required. This paper outlines the research being conducted in southern Western Australia to investigate these issues.

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