Soil Management Handbook - Ministry of Agriculture and Lands
Soil Management Handbook - Ministry of Agriculture and Lands
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