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Maximise Neil du Sautoy Agricultural Services your soil potential Dr Neil du Sautoy, Natural Resources Specialist of Senwes Agricultural Services, discusses the challenges and opportunities that modern technology and research bring to soil assessments. Plant growth is driven by trapping energy from the sun and using it to convert carbon dioxide into plant material through the process of photosynthesis. A plant acquires carbon dioxide by opening the stomata in the leaf (Figure 1). When the stomata are open, water is lost from the plant in a process known as transpiration. Loss of water is the natural tax that a plant must pay to get its basic requirements! Based on this principle, Tanner and Sinclair showed in 1983 that daily plant growth is directly proportional to the amount of water a plant transpires 38 Senwester, Julie 2005 per day and inversely proportional to the dryness of the atmosphere (i.e. vapour pressure deficit), thus: Daily plant growth = k*(T/V) Where k is a plant constant known as the dry matter water ratio, T is transpiration in mm and V is the vapour pressure deficit. Put numbers to intuitive observations This principle, coupled with a series of other algorithms describing Figure 1: Diagrammatic representation of transpiration – open stomata in a leaf allow carbon dioxide intake, whilst losing water. crop growth processes is the basis of research done by the University of Pretoria (funded by the Water Research Commission) to establish the Soil Water Balance Model. This research has shown that by following the water balance in the soil-plantatmosphere-continuum, a very good indication of the production potential of a soil-climate unit can be derived. Research done by the University of the Free State has also shown the value of including climate in assessments, i.e. the SWAMP model. The value of these models are that, with the use of modern technology such as desktop computers and automated climate monitoring systems, it is possible to put numbers to intuitive observations. For example we know maize yields in the Bethlehem district are lower than other regions due to lower heat units while the Schweizer-Reneke district has ample heat units, but rainfall is a limitation. New opportunities and challenges for soil cartographers These models have opened new opportunities, as well as challenges, to soil cartographers when assessing lands. The opportunity is that by adopting these techniques soil cartographers can derive more accurate and scientifically based estimates on yield potential of soils. This is essential for effective precision farming and sound management of the natural resources. The challenge is to numerically
ecord the soil features that have a direct effect on the soil-profile-waterholding characteristics and link these features to the crop’s response to climatic factors such as: • rainfall (distribution instead of season total), • energy (temperature and heat units) as well as • atmospheric evaporative demand (evapo-transpiration). By doing this, it is possible to quantify the expected yield response for a soil characteristic, e.g. effective depth for different areas. This is shown in Figure 2. When incorporating weather data in the yield potential calculations, the effect of rainfall distribution is clearly identified. Generally it is possible to identify three types of seasons: • a very good season where rainfall distribution as well as quantity is very favourable for maize growth, • a good season where there is sufficient rain, but distribution is poor, and then • a poor season where rainfall is either just low or there is a severe midsummer drought. This effect is shown in Figure 3 for simulated yield responses done for soil and climate data from the Bethal district. Although this technique was initiated in South Africa and the first work done only in 2003, excellent agreement between predicted and actual results have been obtained where it has been possible to do comparisons with field trials or yield monitor data. Where differences have been identified, this has been as a result of either nutrient deficiencies or another overriding yield limiting factor. Enquiries If you require any further information about soil assessments please contact Dr Neil du Sautoy at Senwes Agricultural Services on 082 419 0949 or (018) 464-7391 or send an e-mail to neil.dusautoy@senwes.co.za. At present Senwes Agricultural Services is implementing this approach to soil potential assessments and building up its database. We would therefore appreciate the cooperation of anybody who has yield monitor data that could be used. landbou in praktyk Figure 2: Simulated yield potential increases with increase in root depth for two districts. Figure 3: Simulated yield potential increases with increase in root depth for three season types in the Bethal district. Percentage values are the frequency of occurrence for a specific type of season. The effect of rainfall distribution has a great effect on yield potential calculations. 39
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