A Sample Test~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ The most accurate tests are conducted by university and private soil laboratories. Contact your cooperative extension service to find a lab in your area. These labs have had years of experience testing the soils in your state and giving specific fertilizer recommendations based on the soil types and crops grown.
The basic tests usually cost less than $20 but can be more if you include tests for specific minor nutrients such as zinc or contaminants such as lead. Results often come as a number and a graph for relative levels of each nutrient (see sample test report below).
The graph is more helpful in understanding nutrient levels. This sample describes some of the common results found on soil test forms. I’ve also included information on deficiency symptoms and some suggested fertilizers high in those nutrients.
Symptoms of excessive fertilization tend to manifest themselves as deficiency symptoms of other nutrients. For example, high calcium levels interfere with the uptake of potassium. 1. Type of sample. Laboratories will ask what kind of plants are growing in your test site (vegetables, flowers, lawn, orchard).
Each type of planting needs a separate soil test. 2. Soil pH. This is measured on a scale of 1 (acid) to 14 (alkaline). Most garden crops grow well at a pH of 6 to 7, but specific crops such as blueberries and azaleas may need a lower (more acidic) pH.
Soils tend to be more acidic in high-rainfall areas (the Southeast and Pacific Northwest), while drier climates (Southwest deserts) can have more alkaline soils. In general lime is used to raise pH, while sulfur is recommended to lower it.
If your soil also lacks magnesium, dolomitic limestone (which contains magnesium along with calcium) is recommended. Apply lime and sulfur in summer when the soils are warm and microorganism activity is high. 3. Nitrogen (N).
Though nitrogen is one of the key nutrients needed for plant growth, many labs won’t test for it because of its high mobility. Nitrogen leaches out of the soil easily, and levels can fluctuate through the growing season. Deficiency usually appears as pale yellow leaves (often the older leaves first) and stunted growth.
Since organic matter can hold and then slowly release nitrogen as it breaks down, some labs link the organic matter content to the nitrogen level in the soil. However, organic matter may tie up more nitrogen than it releases (see “Percent organic matter”).
Alfalfa meal, cottonseed meal, urea, and fish meal are some fertilizer sources of nitrogen. 4. Phosphorus (P). Phosphorus levels are often reported as either available or reserve. Available phosphorus can be used now, while reserve is tied up due to pH or nutrient imbalance.
Often, just raising or lowering the pH to the ideal 6.5 will free up phosphorus for plant use. It isn’t used up quickly, and adding too much will build excessive levels that run off, causing pollution. Deficiencies are indicated by purple leaves, brittle roots, skinny stems, and late fruit set and maturity.
In early spring, deficiency symptoms on seedlings may disappear with warmer temperatures and increased microbial activity. Superphosphate, rock phosphate, and bonemeal are good sources of phosphorus. 5. Potassium (K). Potassium is vital for stem strength, root growth, and disease resistance.
Many soils are naturally high in potassium, and it is readily available to plants. However, sandy and highly weathered soils can be deficient. Signs are irregular yellowing of lower leaves and poor root growth.
Muriate of potash, greensand, and wood ash are good sources. 6. Calcium (Ca). Calcium is important for cell-wall integrity and root and leaf growth. If you’re liming your soil regularly to keep the pH above 6, calcium deficiency would be unlikely.
However, on alkaline soils (pH above 7) add gypsum (calcium sulfate) instead of lime. Low levels of calcium show as deformed new leaves and branches, and weak stems and roots.
7. Magnesium (Mg). Magnesium is essential for chlorophyll and green leaf development. Pale leaves with green veins are a sign of deficiency. Adding dolomitic lime to raise the pH often corrects deficiency symptoms; on alkaline soils, add Epsom salts (magnesium sulfate). 8. Cation exchange capacity (CEC). CEC measures the ability of soil particles to hold and release specific nutrients. In general, sandy soils tend to have a lower CEC than most clay soils.
Adding well- rotted compost raises the CEC. High CEC usually means a more fertile soil. If your soil has a low CEC, add small amounts of fertilizer throughout the growing season to prevent runoff and waste. Most labs report CEC levels in milliequivalents per 100 grams of soil (meq/100g). A rating of 5 is considered low, while 25 is high. 9. Percent organic matter.
Organic matter is essential for nitrogen absorption and release, and as a food for microorganisms that help make other nutrients available. A level of 3 to 5 percent organic matter is considered ideal. But it’s the quality, not the amount, that can make the difference. Soils high in undecomposed organic matter, such as wood chips or sawdust, can tie up nitrogen and create a deficiency.
The best-quality organic matter to apply, especially right before planting, is well-rotted compost. 10. Percent base saturation. Some experts consider the relationship between four key elements (calcium, potassium, magnesium, and sodium) an indication of soil health. The ideal ratio is approximately 60 to 80 percent calcium, 10 to 15 percent magnesium, 5 to 7 percent potassium, and less than 3 percent sodium.
Adding these figures gives a number called the base saturation. In general, the higher the number, within the given ratios, the more fertile the soil. Labs that test for base saturation believe that the optimum levels of specific nutrients aren’t as important as the relationship among these nutrients. 11. Recommendations.
Most labs give recommendations for adding specific nutrients to bring them to their optimum levels. Recommendations are often given in pounds of that element per 1,000 square feet of garden.