YOUR INDUSTRY
World Soil Day – organic carbon key to soil productivity The United Nations Food and Agriculture Organisation (FAO) through its Global Soil Partnership has deemed the 5th of December to be World Soil Day. By Robin Boom : Member of the Institute of Professional Soil Scientists This initiative is to raise awareness of the fragility of our productive soils upon which not just human, but all terrestrial life depends, and the importance of their preservation and enhancement through sustainable management practices for food production. This year’s theme is ‘Halt soil salinisation, boost soil productivity’. Fortunately, in New Zealand our temperate climate with enough natural rainfall means we are not totally dependent on irrigation, and with relatively good soil organic matter levels, soil salinity is not yet a problem here. Increased salinity (build-up of salts) is making what was once a lot of productive land around the globe, unproductive. Large parts of the United States, Argentina, North Africa and the Middle East, former Russian Eastern block countries, the Indo-China region and small pockets of Southern Australia have salt levels so high that crops can no longer be grown in them. Salt layers can build up from the use of irrigation water high in salt, causing sodification, but also high bicarbonate and carbonated water in semi-arid and arid regions can cause salinity problems. White crusting on the soil surface, or white spots and streaks in the soil profile, are indicative of salinity issues. Improving drainage, reducing compaction and adding large amounts of compost and other soil amendments high in organic matter, are vital in the reclamation of saline soils. Last year, the United Nations World Soil Day theme was ‘Keep soil alive, protect soil biodiversity’, to encourage people around the world to engage in proactively improving soil health. Soil health is often measured by the amount of organic matter in the soil, as this provides many ‘soil ecosystem services’ such as regulating the flow and quality of water, providing clean air, filtering pollutants and contaminants and supporting biodiversity. In general, soils with more organic carbon have a more stable structure through better aggregation, are less prone to run-off and erosion, have greater water infiltration and retention and increased biological activity and nutrient supply compared to similar soils with lower organic matter levels.
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The ORCHARDIST : DECEMBER 2021
At last month’s COP26 United Nations Climate Change conference in Glasgow, British soil scientists were able to present information on the importance of preserving and building up soil carbon as a contributing solution to mitigating climate change. Currently there is around 800 gigatonnes of CO2 in the atmosphere, whereas the topsoils (up to one metre depth) currently hold approximately 1,500 gigatonnes of carbon, and the subsoil (one to three metre depth) holds a further 800 gigatonnes of carbon. All living plant matter above and below ground contains 700 gigatonnes of carbon, whereas the oceans contain a whopping 40,000 gigatonnes of inorganic carbon. One cause of concern is the potential uncontrolled escalation of global warming that could occur from the release of carbon held in the permafrost areas of northern Russia and Canada which are estimated to be as high as 1,000 gigatonnes. As the planet warms and these permafrost areas melt, some of this carbon will escape into the atmosphere as carbon dioxide through mineralisation of the organic matter and also as methane gas. Carbon makes up approximately 58% of soil organic matter and this is a combination of dead and living organisms including plant roots, exudates, fungi, microbes, decaying plant materials and animal manure. With the cutting down of forests and development of agriculture worldwide through cultivation practices that have occurred for many decades and in some cases millennia, the soil organic matter levels in many countries are only a fraction of what they had previously been for thousands of years. On New Zealand’s pastoral farms, the loss of soil carbon has been minimal except on peat soils, where carbon losses have been significantly
