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Lab Difference in Soil Quality
November 5, 2007
Written By: Craig Dick

As reported in past blogs about the importance of soil quality (A Pictorial of High Quality Soil, Improving Water Infiltration, and Quality Soil Update) I promised that I would run soil tests on the field and the garden (I am waiting on tests form another lab). There were some striking differences. The garden had almost double the organic matter, much better pH, and double the calcium content.

One of the main differences is pH, the field has a pH of 5.0 compared to the garden, which had 6.5 pH. 

Fun Facts: 

At a pH of 5.0 the potential yield of corn is reduced by 27%, soybeans by 21% and alfalfa by 91%.

At a pH of 5.0 1/2 of N, 1/3 of P, and 1/2 of K is unavailable for plant uptake.

At a pH of 5.0 nodulation is reduced up to 40%

Click here to view lab report

With the high costs of fertilizer and fuel, wouldn't it make sense to make those inputs work harder for you? Working to improve you soil quality makes high priced fertilizers more available to your plants, resulting in decreased costs. High quality soils allow irrigation water and rainfall to infiltrate into the pore space, making it available to plants. Ponding is the first sign that water is not entering the soil, eventually causing de-nitrification, and evaporating, wasting fuel, fertilizer, and lowering yield.

Adding SuperCal 98G pelletized lime and SuperCal SO4 pelletized gypsum to your fertility program will ensure your soils maintain the proper pH, superior infiltration rates, reduce future input costs, decrease soil erosion, and increase yields.

Calcium Products, lower input costs, higher yields, better soil


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