CFAES Give Today

Ohio State University Extension


Interpreting a Soil Test Report

Agriculture and Natural Resources
Greg LaBarge, Field Specialist, Agronomic Systems
Laura Lindsey, Assistant Professor, Soybean and Small Grain Production

Soil test reports vary from laboratory to laboratory; however, they all report key results of pH, lime test index (LTI) or buffer pH, phosphorous, and potassium. These results are used to develop fertilizer recommendations. Other useful measures on the report, such as cation exchange capacity (CEC), organic matter, and base saturation, further define soil factors related to nutrient availability and holding capacity that should be considered as nutrient plans are developed. Desirable ranges to maximize crop production for each of the tests performed in a standard soil test are listed in Table 1. This table should serve as a general guideline to help determine if your soil is within the desirable range for each of the parameters tested. Thorough guidelines are given in Tri-State Fertilizer Recommendations for Corn, Soybeans, Wheat, and Alfalfa.

Soil pH and Buffer pH

The level of active soil acidity is measured using soil pH. A pH value above 7.0 is alkaline; a value below 7.0 is acidic. A pH value of 7.0 is neutral. LTI or buffer pH is an indicator of the reserve (potential) acidity in the soil and is used to determine the quantity of lime needed to correct the pH of an acidic soil. In Ohio, subsoil pH varies based on soil parent material. Limestone parent materials found in western and northwestern Ohio may have a subsoil pH that is greater than 7.0 and contain as much as 50% calcium carbonate or its equivalent. Eastern and southeastern Ohio soils, developed mainly from sandstones and shale and subsoil, may have pH values as low as 5.0. The Ohio State University Extension fact sheet Soil Acidity and Liming for Agronomic Production, AGF-505-07, provides a detailed explanation of pH, buffer pH, and liming considerations in Ohio.

Phosphorus, Potassium, Calcium, and Magnesium

Soil test values may be reported in parts per million (ppm) or pounds per acre (lb/ac). To convert from ppm to lb/ac, multiply ppm by two. Phosphorus, potassium, calcium, and magnesium soil test values are indicators of the relative available nutrient levels in the soil and not equal to the total amounts of these nutrients available in the soil for plant uptake. Phosphorus and potassium soil test values are correlated with crop yield response and fertilizer needs (i.e., as the soil test value increases, the need for supplemental fertilizer decreases).

Soil organic matter, CEC, and base saturation are other variables that are shown on the soil test report to quantify soil characteristics and help understand other qualitative factors associated with the area represented by the sample. Typical ranges for organic matter, CEC, and base saturation are shown in Table 2. 

Table 1. Common soil test result parameters with desirable ranges for corn and soybean production.
Test Item Desirable Ranges Use of Measure
pH 6.3–7.0 Water pH (Neutral pH = 7.0)
Buffer pH
Lime Test Index
Used to determine lime requirement.
  When reported as pound per acre When reported as part per million  
Phosphorous (P) 30–60 15–30 Used to make phosphorous recommendation.
Potassium (K)     Used to make potassium recommendation. CEC is used in determining desirable range.
CEC= 5 meq/100g 176–236 88–118
CEC=10 meq/100g 200–260 100–130
CEC=20 meq/100g 250–310 125–155
CEC=30 meq/100g 300–360 150–180
Calcium (Ca) 800–16,000 400–8,000 Levels less than 200 ppm are a concern. Ca deficiencies are rare in Ohio.
Magnesium (Mg) 150–2,000 75–1,000 Levels less than 20 ppm are a concern. Dolomitic limestone is a major source of Mg.
Table 2. Additional soil test variables given in a soil test report.
Soil Test Variable Typical Ranges
Organic Matter 1–6%
Cation Exchange Capacity (CEC) meq/100g
Coarse Texture Soil (sand) 1–5
Medium Texture Soil (silt) 6–20
Fine Texture Soil (clay) 21–30 or more
Base Saturation  
% Ca 40–80
% Mg 10–40
% K 1–5

Organic Matter

Tillage, parent material, crop productivity, and other management factors influence soil organic matter. Organic matter is important in nutrient holding capacity.

Cation Exchange Capacity (CEC)

CEC measures the capacity of the soil to hold exchangeable cations (positively charged ions) and is reported as meq/100g of soil (meq = milliequivalents). Reports may also be reported as cmolc/kg of soil (cmolc = centimoles of charge).

One cmolc/kg is equal to one meq/100 g. Exchangeable cations include aluminum, hydrogen, calcium, magnesium, and potassium. The CEC depends largely on the amount and type of clay and the organic matter content. The higher the CEC value, the more cations the soil is able to hold, reducing the likelihood of leaching. It is not practical to attempt to increase the CEC of a soil by adding clay or organic matter. Liming an acid soil will slightly increase the effective CEC.

Base Saturation: % Calcium, % Magnesium, and % Potassium

Base saturation is the extent to which the adsorption complex of a soil is saturated with exchangeable cations other than hydrogen or aluminum. It is expressed as a percentage of the total CEC. The calcium to magnesium ratio is calculated on the basis of percentage saturation of the soil CEC by both elements. This ratio should be considered when lime is added to the soil. If the Ca:Mg ratio is 1:1 or less (less Ca than Mg), a lower percentage magnesium limestone should be used. Agronomic crops grow over a wide range of ratios with the ideal ratio being about 6:1 to 10:1.

The magnesium to potassium ratio should be greater than 2:1. In other words, the percent base saturation of Mg should be at least two times the percent base saturation of K. High K frequently results in reduced uptake of Mg by plants. Therefore, to help prevent plant nutrient imbalance, additional Mg may be required to maintain an Mg:K ratio of at least 2:1. The greatest concern with this ratio is for grass hay production where forage produced on a field with less than 2:1 Mg:K ratio can result in grass tetany conditions.


  • Barker, David, et al. Ohio Agronomy Guide, 14th Edition. 2005. Ohio State University Extension bulletin 472.
  • Mullen, Robert, Edwin Lentz, and Maurice Watson. Soil Acidity and Liming for Agronomic Production, AGF-505-07. 2007. Ohio State University Extension. Available at
  • Vitosh, M.L., J.W. Johson, and D.B. Mengel. 1995. Tri-state Fertilizer Recommendations for Corn, Soybeans, Wheat, and Alfalfa. Ohio State University Extension bulletin E-2567. 
Originally posted Oct 17, 2012.