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Soil Management Handbook - Ministry of Agriculture and Lands

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efer to the following Factsheets: <strong>Soil</strong> Acidity <strong>and</strong><br />

Liming Facts, Liming Acid <strong>Soil</strong>s in Central B.C. <strong>and</strong><br />

<strong>Soil</strong> Liming Recommendations available at the<br />

Resource <strong>Management</strong> Branch, BCMAFF,<br />

Abbotsford).<br />

For best results, lime should be applied in the fall or a<br />

few weeks prior to seeding, <strong>and</strong> thoroughly<br />

incorporated into the plow layer on tilled fields. For<br />

grape <strong>and</strong> tree fruits, lime can be applied at any time,<br />

except within one month <strong>of</strong> fertilizer application.<br />

Where possible, lime should be evenly broadcast <strong>and</strong><br />

incorporated with care between rows. Liming<br />

programs should be considered carefully during the<br />

establishment <strong>of</strong> perennial crops. Lime has a low<br />

level <strong>of</strong> solubility, so lime applied <strong>and</strong> left on the soil<br />

surface will only be slightly effective in raising soil<br />

pH in the rooting zone.<br />

<strong>Soil</strong> pH is a poor indicator <strong>of</strong> lime requirement.<br />

Factors, such as organic matter levels, clay content<br />

<strong>and</strong> age <strong>of</strong> soils, markedly affect the amount <strong>of</strong> lime<br />

needed to adjust the pH level one unit. A lime<br />

requirement test, performed by a reputable soil testing<br />

laboratory, is recommended to ensure the correct rate<br />

<strong>of</strong> lime application.<br />

Surface application <strong>of</strong> lime on low pH areas under<br />

trickle or drip irrigation may not alter the soil pH<br />

below the soil surface. The use <strong>of</strong> lime in these<br />

situations may have some affect on the soil nutrient<br />

solution <strong>and</strong> reduce the negative impact <strong>of</strong> iron,<br />

aluminum <strong>and</strong> manganese toxicity.<br />

4.5.2.3 Acidification Resistance Index (ARI)<br />

ARI is a soil test which measures the amount <strong>of</strong> acid<br />

required to lower a soil to pH 5.0 from its present<br />

level. From the ARI, recommendations on fertilizer<br />

<strong>and</strong> lime use can be made to aid in controlling the pH<br />

level <strong>of</strong> a soil. ARI takes into account both the<br />

buffering capacity <strong>and</strong> pH <strong>of</strong> the soil.<br />

Acidification <strong>of</strong>ten occurs in poorly buffered soils due<br />

to irrigation <strong>and</strong> use <strong>of</strong> acidifying fertilizers such as<br />

ammonium sulfate (21-0-0). Any producer<br />

considering fertigation <strong>of</strong> orchards should have an<br />

ARI test completed. The table below gives general<br />

recommendations for 3 ARI ranges.<br />

ARI Ranges<br />

0 to 5 Very sensitive to acidification, lime to<br />

pH 7 prior to planting tree fruits, use<br />

calcium nitriate<br />

6 to 25 Moderately sensitive to acidification,<br />

lime to pH 7 prior to planting, use<br />

calcium nitrate in combination with<br />

other sources <strong>of</strong> nitrogen.<br />

>26 Not sensitive, do not lime, use any<br />

nitrogen fertilizer source.<br />

4.5.2.4 Sulphur <strong>and</strong> Acidification<br />

Sulphur<br />

Sulphur may be required as an essential plant nutrient,<br />

however, this section will refer to the use <strong>of</strong> sulphur<br />

as a soil acidifier.<br />

In some areas <strong>of</strong> the Okanagan <strong>and</strong> Similkameen<br />

Valleys, soil pH is above 8.0. It may be desirable to<br />

lower the pH to increase the availability <strong>of</strong> some plant<br />

nutrients. Lowering soil pH involves the same<br />

cultural practices <strong>and</strong> considerations as raising the pH<br />

with liming, except that different products are<br />

required. Adjusting a soil pH downward is more<br />

difficult <strong>and</strong> <strong>of</strong>ten more costly than moving a soil pH<br />

up. Care must be taken to ensure that the high pH<br />

>8.0 is not the result <strong>of</strong> an alkali (sodium) or saline<br />

condition which may require other soil management<br />

such as gypsum addition or drainage.<br />

Acidification<br />

The principal agents used to lower soil pH are<br />

elemental sulphur, sulphuric acid, aluminum sulphate<br />

<strong>and</strong> iron sulphate (ferrous sulphate). Ammonium<br />

sulphate, ammonium phosphate <strong>and</strong> other ammonium<br />

containing fertilizers are also quite effective in<br />

reducing soil pH, though they are primarily sources <strong>of</strong><br />

plant nutrients.<br />

For large areas, elemental sulphur (or a mixture <strong>of</strong> it<br />

<strong>and</strong> bentonite to improve its stability <strong>and</strong> safety when<br />

h<strong>and</strong>led in confined spaces) is probably the most<br />

economic product. However, elemental sulphur has<br />

to be oxidized by soil microorganisms. Sulphuric<br />

76 <strong>Soil</strong> <strong>Management</strong> <strong>H<strong>and</strong>book</strong> – Okanagan-Similkameen Valleys

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