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PLANT PROTECTION 1 – Pests, Diseases and Weeds

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<strong>PLANT</strong> <strong>PROTECTION</strong> 1 – <strong>Pests</strong>, <strong>Diseases</strong> <strong>and</strong> <strong>Weeds</strong><br />

Non-living agents (contd)<br />

CLIMATE CHANGE, SALINITY.<br />

CLIMATE<br />

CHANGE<br />

‘global warming’<br />

‘greenhouse<br />

effect’<br />

Although the term ‘climate change’ can refer to any variation in climate or atmospheric<br />

conditions which has taken place over millions of years, in recent times, the term is taken<br />

to mean changes in climate that are the direct result of human activity.<br />

The most important greenhouse gases are water vapour, carbon dioxide, methane <strong>and</strong><br />

ozone. Increases in these gases over recent decades are considered to be due to human<br />

activity, eg transportation, agriculture, etc. The effect on sea levels, water <strong>and</strong> food<br />

supplies, pests, weeds, social conflict <strong>and</strong> the migration of peoples is being researched.<br />

Dept. of Climate Change www.climatechange.gov.au/<br />

Left: Sun <strong>and</strong> Earth Under Normal Conditions The greenhouse effect is a natural process -<br />

<br />

redistributed around the globe through atmospheric <strong>and</strong> oceanic circulation patterns (winds, ocean<br />

currents, etc). Energy is then radiated back from the earth into the atmosphere as long-wave radiation.<br />

Over time long <strong>and</strong> short wave radiation should balance. Right: Increasing energy radiated back to<br />

earth. Greenhouse gases absorb some of the energy radiated back into the atmosphere as long wave<br />

radiation. Increasing concentrations of these gases mean that more is absorbed <strong>and</strong> less released into<br />

space - radiation is trapped in the atmosphere <strong>and</strong> reflected back to earth causing a heating of the<br />

www.ecn.ac.uk)<br />

SALINITY<br />

Do not confuse<br />

salinity with<br />

acid soils or<br />

sodicity:<br />

Sodicity refers to soil<br />

containing levels of<br />

sodium that affects its<br />

physical properties,<br />

when they become wet,<br />

clay particles lose their<br />

tendency to stick<br />

together, become<br />

unstable, erode <strong>and</strong><br />

impermeable to water<br />

<strong>and</strong> roots<br />

Acid soils are a<br />

condition in which the<br />

surface soil pH has<br />

declined to less than<br />

pH 5.5 as a result of<br />

human activity, such as<br />

agriculture (page 395<br />

Fig. 228)<br />

Saline soils are defined as those in which the concentration of soluble salts in soil<br />

<strong>and</strong> water is sufficient to restrict plant growth, increase soil erosion <strong>and</strong> salt pollution of<br />

rivers, water supplies, irrigation systems, damage roads, fences <strong>and</strong> buildings.<br />

Department of Agriculture, Fisheries & Forestry www.daff.gov.au/<br />

Primary or natural salinity has developed in former marine areas or on rocks which<br />

contained trapped marine salts that break down to form soils.<br />

Secondary or induced salinity occurs when surplus water percolates into the water<br />

table making it rise. Naturally occurring salts found in the soil <strong>and</strong> rock are dissolved<br />

<strong>and</strong> brought to the surface, coming into contact with vegetation.<br />

– Irrigation salinity results from poor irrigation practices. More water is applied than can be<br />

used by the crop, excess water causes water to rise bringing the salts into contact with plants.<br />

– Dryl<strong>and</strong> salinity is typically caused by extensive clearing of vegetation (mainly trees) for<br />

agricultural <strong>and</strong> grazing l<strong>and</strong>.<br />

CSIRO L<strong>and</strong> & Water www.clw.csiro.au/issues/salinity/<br />

Effects on soils <strong>and</strong> plants. Soils crust on the surface, soil clays swell <strong>and</strong> fine soil<br />

particles disperse. Salt in soil reduces the availability of water to plants <strong>and</strong> at high<br />

enough concentrations can kill plants, it may also result in toxicity of certain ions<br />

namely sodium <strong>and</strong> calcium, nutritional imbalances <strong>and</strong> deficiencies, <strong>and</strong> favour some<br />

diseases, eg Phytophthora root rot of some tomato cultivars. Salt-affected sites are<br />

complex <strong>and</strong> are influenced by interaction between soil, water, plant species <strong>and</strong> climate.<br />

Salt may occur in the soil/media, fertilizer or irrigation water. Some forms of fertilizers are<br />

more prone to result in salinity problems, eg potassium as potassium chloride (potassium as<br />

potassium sulphate less likely)<br />

Plants continually remove water from soil via evapo-transpiration. Left: Trees have deeper <strong>and</strong> more<br />

extensive roots systems <strong>and</strong> extract more water from the ground than do grasses <strong>and</strong> shallow-rooted crops.<br />

Right: When trees are removed <strong>and</strong> replaced with shallow-rooted grasses <strong>and</strong> crops, surplus water<br />

percolates into the water table causing it to rise bringing dissolved salts with it (adapted from Wakefield 1994).<br />

394 Non-parasitic pests <strong>and</strong> diseases

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