Date

2022/08/24

Soil Quality ebook

Soil Quality: 8 Sodic and Alkaline Soil

Organisations

SoilsWest

Department of Primary Industries and Regional Development

Grains Research and Development Corporation

Authors

Ed Barrett-Lennard

David Hall

Wayne Parker

Rushna Munir

Waterlogging causes huge trauma to plant roots because under its influence, soil becomes oxygen deficient within a few days. With oxygen deficiency, the root cells experience a catastrophic energy deficiency: the rates of energy production decrease by about 95%. Under these conditions, all cellular processes that require energy are jeopardised.

One consequence of waterlogging in saline soil, is that for most plants there is a major increase in the rate of sodium (and chloride) ion uptake, and a decrease in the rate of potassium ion uptake. As a consequence, there can be a rapid increase of sodium in leaves.

Interaction of salinity and waterlogging in 7-day old wheat seedlings Chart from: Barrett-Lennard EG (1986). Effects of waterlogging on the growth and NaCl update of vascular plants under saline conditions. Reclamation and Revegetation Research 5: 245-261. Chart redesign: Science with Style.

The chart above shows these effects for an experiment with wheat. In this trial the plants were either grown in aerated nutrient solutions (simulating drained soil), or nitrogen bubbled nutrient solutions (simulating waterlogged soil) at three salinities (1, 60 and 120 mM sodium chloride). After 7 days in aerated solutions, sodium concentrations in shoots increased with increasing salinity, but with the imposition of waterlogging (simulated with nitrogen bubbling of the solutions), sodium concentrations in the shoots were more than doubled.

For nearly all plants, the changes to ion relations in the shoots impair crop growth and final yield. The consequences of these adverse ion relations can be seen in the photos below in wheat.

With zero salt in the solutions (top photo), plants grown in hypoxic solutions were healthy-looking but had a 60% decrease in dry weight compared with plants grown in aerated solutions. With 20 millimolar sodium chloride (middle photo), the shoots of plants in hypoxic solutions were very chlorotic and also had a 60% decrease in dry weight compared with aerated controls at the same salinity (centre photo). At 120 millimolar sodium chloride (bottom photo), the shoots of plants in hypoxic solutions were dead; however, the plants grown in aerated solutions at this salinity were healthy-looking and had similar shoot weights as plants grown in hypoxic solutions at 20 millimolar sodium chloride. Overall, the photos show that in wheat there is a huge adverse interaction between waterlogging and salinity.

Images of wheat in waterlogged or drained soil at three salinity levels. The photos show the effects on wheat of 33 days of growth in hypoxic (left hand side) nutrient solutions (simulating waterlogged soils) or aerated (right hand side) nutrient solutions (simulating drained soil) at three salinities: 0, 20 and 120 mM sodium chloride. Images from: Barrett-Lennard EG (2003). The interaction between waterlogging and salinity in higher plants: causes, consequences and implications. Plant and Soil 253: 35–54.

References

ebook Soil Quality: 8 Sodic & Alkaline Soil

Barrett-Lennard E, Hall D, Parker W and Munir R (2022).

Barrett-Lennard EG (2003). The interaction between waterlogging and salinity in higher plants: causes, consequences and implications. Plant and Soil 253: 35–54.

Barrett-Lennard EG and Shabala SN (2013). The waterlogging/salinity interaction in higher plants revisited – focusing on the hypoxia-induced disturbance to K+ homeostasis. Functional Plant Biology 40: 872–882.

Barrett-Lennard EG, Leighton PD, McPharlin IR, Setter T and Greenway H (1986). Methods to experimentally control waterlogging and measure soil oxygen in field trials. Australian Journal of Soil Research 24: 477–483.

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